EMBRYOPSIDA Pirani & Prado
Gametophyte dominant, independent, multicellular, initially ±globular, not motile, branched; showing gravitropism; glycolate oxidase +, glycolate metabolism in leaf peroxisomes [glyoxysomes], acquisition of phenylalanine lysase* [PAL], flavonoid synthesis*, microbial terpene synthase-like genes +, triterpenoids produced by CYP716 enzymes, CYP73 and phenylpropanoid metabolism [development of phenolic network], xyloglucans in primary cell wall, side chains charged; plant poikilohydrous [protoplasm dessication tolerant], ectohydrous [free water outside plant physiologically important]; thalloid, leafy, with single-celled apical meristem, tissues little differentiated, rhizoids +, unicellular; chloroplasts several per cell, pyrenoids 0; centrioles/centrosomes in vegetative cells 0, microtubules with γ-tubulin along their lengths [?here], interphase microtubules form hoop-like system; metaphase spindle anastral, predictive preprophase band + [with microtubules and F-actin; where new cell wall will form], phragmoplast + [cell wall deposition centrifugal, from around the anaphase spindle], plasmodesmata +; antheridia and archegonia +, jacketed*, surficial; blepharoplast +, centrioles develop de novo, bicentriole pair coaxial, separate at midpoint, centrioles rotate, associated with basal bodies of cilia, multilayered structure + [4 layers: L1, L4, tubules; L2, L3, short vertical lamellae] (0), spline + [tubules from L1 encircling spermatid], basal body 200-250 nm long, associated with amorphous electron-dense material, microtubules in basal end lacking symmetry, stellate array of filaments in transition zone extended, axonemal cap 0 [microtubules disorganized at apex of cilium]; male gametes [spermatozoids] with a left-handed coil, cilia 2, lateral, asymmetrical; oogamy; sporophyte +*, multicellular, growth 3-dimensional*, cuticle +*, plane of first cell division transverse [with respect to long axis of archegonium/embryo sac], sporangium and upper part of seta developing from epibasal cell [towards the archegonial neck, exoscopic], with at least transient apical cell [?level], initially surrounded by and dependent on gametophyte, placental transfer cells +, in both sporophyte and gametophyte, wall ingrowths develop early; suspensor/foot +, cells at foot tip somewhat haustorial; sporangium +, single, terminal, dehiscence longitudinal; meiosis sporic, monoplastidic, MTOC [= MicroTubule Organizing Centre] associated with plastid, sporocytes 4-lobed, cytokinesis simultaneous, preceding nuclear division, quadripolar microtubule system +; wall development both centripetal and centrifugal, 1000 spores/sporangium, sporopollenin in the spore wall* laid down in association with trilamellar layers [white-line centred lamellae; tripartite lamellae]; plastid transmission maternal; nuclear genome [1C] <1.4 pg, main telomere sequence motif TTTAGGG, KNOX1 and KNOX2 [duplication] and LEAFY genes present, ethylene involved in cell elongation; chloroplast genome with close association between trnLUAA and trnFGAA genes [precursors for starch synthesis], tufA, minD, minE genes moved to nucleus; mitochondrial trnS(gcu) and trnN(guu) genes +.
Many of the bolded characters in the characterization above are apomorphies of more or less inclusive clades of streptophytes along the lineage leading to the embryophytes, not apomorphies of crown-group embryophytes per se.
All groups below are crown groups, nearly all are extant. Characters mentioned are those of the immediate common ancestor of the group,  contains explanatory material, () features common in clade, exact status unclear.
Sporophyte well developed, branched, branching dichotomous, potentially indeterminate; hydroids +; stomata on stem; sporangia several, terminal; spore walls not multilamellate [?here].
II. TRACHEOPHYTA / VASCULAR PLANTS
Sporophyte long lived, cells polyplastidic, photosynthetic red light response, stomata open in response to blue light; plant homoiohydrous [water content of protoplasm relatively stable]; control of leaf hydration passive; plant endohydrous [physiologically important free water inside plant]; PIN[auxin efflux facilitators]-mediated polar auxin transport; (condensed or nonhydrolyzable tannins/proanthocyanidins +); borate cross-linked rhamnogalactan II, xyloglucans with side chains uncharged [?level], in secondary walls of vascular and mechanical tissue; lignins +; roots +, often ≤1 mm across, root hairs and root cap +; stem apex multicellular [several apical initials, no tunica], with cytohistochemical zonation, plasmodesmata formation based on cell lineage; vascular development acropetal, tracheids +, in both protoxylem and metaxylem, G- and S-types; sieve cells + [nucleus degenerating]; endodermis +; stomata numerous, involved in gas exchange; leaves +, vascularized, spirally arranged, blades with mean venation density ca 1.8 mm/mm2 [to 5 mm/mm2], all epidermal cells with chloroplasts; sporangia in strobili, sporangia adaxial, columella 0; tapetum glandular; sporophyte-gametophyte junction lacking dead gametophytic cells, mucilage, ?position of transfer cells; MTOCs not associated with plastids, basal body 350-550 nm long, stellate array in transition region initially joining microtubule triplets; archegonia embedded/sunken [only neck protruding]; embryo suspensor +, shoot apex developing away from micropyle/archegonial neck [from hypobasal cell, endoscopic], root lateral with respect to the longitudinal axis of the embryo [plant homorhizic].[MONILOPHYTA + LIGNOPHYTA]
Sporophyte growth ± monopodial, branching spiral; roots endomycorrhizal [with Glomeromycota], lateral roots +, endogenous; G-type tracheids +, with scalariform-bordered pits; leaves with apical/marginal growth, venation development basipetal, growth determinate; sporangium dehiscence by a single longitudinal slit; cells polyplastidic, MTOCs diffuse, perinuclear, migratory; blepharoplasts +, paired, with electron-dense material, centrioles on periphery, male gametes multiciliate; nuclear genome [1C] 7.6-10 pg [mode]; chloroplast long single copy ca 30kb inversion [from psbM to ycf2]; mitochondrion with loss of 4 genes, absence of numerous group II introns; LITTLE ZIPPER proteins.
Sporophyte woody; stem branching axillary, buds exogenous; lateral root origin from the pericycle; cork cambium + [producing cork abaxially], vascular cambium bifacial [producing phloem abaxially and xylem adaxially].
SEED PLANTS† / SPERMATOPHYTA†
Growth of plant bipolar [plumule/stem and radicle/root independent, roots positively geotropic]; plants heterosporous; megasporangium surrounded by cupule [i.e. = unitegmic ovule, cupule = integument]; pollen lands on ovule; megaspore germination endosporic, female gametophyte initially retained on the plant, free-nuclear/syncytial to start with, walls then coming to surround the individual nuclei, process proceeding centripetally.
EXTANT SEED PLANTS
Plant evergreen; nicotinic acid metabolised to trigonelline, (cyanogenesis via tyrosine pathway); microbial terpene synthase-like genes 0; primary cell walls rich in xyloglucans and/or glucomannans, 25-30% pectin [Type I walls]; lignin chains started by monolignol dimerization [resinols common], particularly with guaiacyl and p-hydroxyphenyl [G + H] units [sinapyl units uncommon, no Maüle reaction]; roots often ≥1 mm across, stele diarch to pentarch, xylem and phloem originating on alternating radii, cork cambium deep seated, gravitropism response fast; stem apical meristem complex [with quiescent centre, etc.], plasmodesma density in SAM 1.6-6.2[mean]/μm2 [interface-specific plasmodesmatal network]; eustele +, protoxylem endarch, endodermis 0; wood homoxylous, tracheids and rays alone, tracheid/tracheid pits circular, bordered; mature sieve tube/cell lacking functioning nucleus, sieve tube plastids with starch grains; phloem fibres +; cork cambium superficial; leaf nodes 1:1, a single trace leaving the vascular sympodium; leaf vascular bundles amphicribral; guard cells the only epidermal cells with chloroplasts, stomatal pore with active opening in response to leaf hydration, control by abscisic acid, metabolic regulation of water use efficiency, etc.; branching by axillary buds, exogenous; prophylls two, lateral; leaves with petiole and lamina, development basipetal, lamina simple; sporangia borne on sporophylls; spores not dormant; microsporophylls aggregated in indeterminate cones/strobili; grains monosulcate, aperture in ana- position [distal], primexine + [involved in exine pattern formation with deposition of sporopollenin from tapetum there], exine and intine homogeneous, exine alveolar/honeycomb; ovules with parietal tissue [= crassinucellate], megaspore tetrad linear, functional megaspore single, chalazal, sporopollenin 0; gametophyte ± wholly dependent on sporophyte, development initially endosporic [apical cell 0, rhizoids 0, etc.]; male gametophyte with tube developing from distal end of grain, male gametes two, developing after pollination, with cell walls; embryo cellular ab initio, suspensor short-minute, embryonic axis straight [shoot and root at opposite ends], primary root/radicle produces taproot [= allorhizic], cotyledons 2; embryo ± dormant; chloroplast ycf2 gene in inverted repeat, trans splicing of five mitochondrial group II introns, rpl6 gene absent; ??whole nuclear genome duplication [ζ/zeta duplication event], 2C genome size (0.71-)1.99(-5.49) pg, two copies of LEAFY gene, PHY gene duplications [three - [BP [A/N + C/O]] - copies], 5.8S and 5S rDNA in separate clusters.
EXTANT GYMNOSPERMS / PINOPHYTA / ACROGYMNOSPERMAE
Biflavonoids +; ferulic acid ester-linked to primary unlignified cell walls, silica usu. low; root apical meristem organization?, protophloem not producing sieve tubes, with secretory cells, sieve area of sieve tube with small pores generally less than 0.8 µm across that have cytoplasm and E.R., joining to form a median cavity in the region of the middle lamella, Strasburger/albuminous cells associated with sieve tubes [the two not derived from the same immediate mother cell], phloem fibres +; sclereids +, ± tracheidal transfusion tissue +, rays uniseriate [?here]; stomatal poles raised above pore, no outer stomatal ledges or vestibule, epidermis lignified; cuticle waxes as tubules, nonacosan-10-ol predominates, n-alkyl lipids scanty; buds perulate/with cataphylls; leaves simple, lamina 1-veined, development marginal; plants dioecious; parts of strobili spirally arranged; microsporangia abaxial, dehiscing by the action of the epidermis [= exothecium]; pollen saccate, tectate, endexine lamellate at maturity all around grain, esp. intine with callose; ovules aggregated into compound strobili, erect, pollen chamber formed by breakdown of nucellar cells, nucellus massive; ovules increasing considerably in size between pollination and fertilization, but aborting unless pollination occurs; ovule with pollination droplet, catches pollen; male gametophyte: two prothallial cells + tube cell + antheridial cell, the latter → sterile cell + 2 gametes; pollen germinates on ovule, usu. takes two or more days, tube with wall of pectose + cellulose microfibrils, branched, growing at up to 10(-20) µm/h-1, haustorial, breaks down sporophytic cells; male gametes released by breakdown of pollen grain wall, with >1000 cilia, basal body 800-900 nm long, spline hundreds of tubules wide, chromatin not condensed; fertilization 7 days to 12 months or more after pollination, to ca 2 mm from ovule surface to egg; seeds "large" [ca 8 mm3], but not much bigger than ovule, with morphological dormancy; testa mainly of coloured sarcoexotesta, scleromesotesta, and ± degenerating endotesta; first zygotic nuclear division with chromosomes of male and female gametes lining up on separate but parallel spindles, embryogenesis initially nuclear, embryo ± chlorophyllous; gametophyte persists in seed; plastid and mitochondrial transmission paternal; genome size [1C] 10< pg [1 pg = 109 base pairs]/(2201-)17947(-35208) Mb; two copies of LEAFY gene [LEAFY, NEEDLY] and three of the PHY gene, [PHYP [PHYN + PHYO]]; plastome IR expanded, with duplicated ribosomal RNA operons; chondrome with second intron in the rps3 gene [group II, rps3i2].
[CUPRESSALES [GNETALES + PINALES]]: tree, branched; βaryl ether concentration in lignin lower, biphenyls higher; wood pycnoxylic, torus:margo pits + [tracheid side walls]; phloem with polyphenol-containing parenchyma (PP) cells, resin ducts/cells in phloem and or xylem +/0; lignins with guaiacyl units (G-lignin) [lacking syringaldehyde, Mäule reaction negative]; cork cambium ± deep seated; bordered pits on tracheids round, opposite; nodes 1:1; axillary buds + (0); leaves with single vein, fasciculate, needle-like or flattened; plants monoecious; microsporangiophore/filament simple, hyposporangiate; dehiscing by the action of the hypodermis [endothecium]; pollen saccate, exine thick [³2 µm thick], granular; ovulate strobilus compound, erect, ovuliferous scales flattened, ± united with bract scales; ovules lacking pollen chamber, inverted [micropyle facing axis]; pollen buoyant, not wettable, pollen tube unbranched, growing towards ovule, wall with arabinogalactan proteins; gametes non-motile, lacking walls, siphonogamy [released from distal end of tube]; female gametophyte lacking chlorophyll, seed coat dry, not vascularized; embryo initially with 2 to 4 free-nuclear divisions, with upper tier or tiers of cells from which pro- or secondary suspensor develops, elongated primary suspensor cells and basal embryonal cells [or some variant]; one duplication in the PHYP gene line; germination phanerocotylar, epigeal, (seedlings green in the dark).
Note: In all node characterizations, boldface denotes a possible apomorphy, (....) denotes a feature the exact status of which in the clade is uncertain, [....] includes explanatory material; other text lists features found pretty much throughout the clade. Note that the precise node to which many characters, particularly the more cryptic ones, should be assigned is unclear. This is partly because homoplasy is very common, in addition, basic information for all too many characters is very incomplete, frequently coming from taxa well embedded in the clade of interest and so making the position of any putative apomorphy uncertain. Then there are the not-so-trivial issues of how character states are delimited and ancestral states are reconstructed (see above).
Age. Clarke et al. (2011: also other ages) suggested a crown age for this clade of (286-)252(-212) Ma, Magallón et al. (2013) an age of ca 278 Ma, Won and Renner (2006) an age of (324-)298(-270) Ma, while ca 290 Ma is the estimate in Ran et al. (2018a). The estimates by Crisp and Cook (2011) of around 270 Ma and of around 260.9Ma by Tank et al. (2015: Table S2) are broadly comparable. Leslie et al. (2012) suggested an age of around 350-275 Ma (in Leslie et al. 2016 the suggestion was (329.3-)313.5(-287.9)) and Ran et al. (2018b) an age of (312.6-)276.2(-206.7) Ma, but Zhou et al. (2014) and Magallón et al. (2015) offered appreciably younger ages of (187.3-)161.4(-147) and ca 127 Ma respectively; see also P. Soltis et al. (2002).
N.B.. In many of these estimates Gnetales were not included; "conifers" in the discussion below refers to Pinales and Cupressales together, but excluding Gnetales, and this group has also been called Pinophyta, Coniferophyta, Coniferae, Pinopsida... For Pinales, see below.
What follows is rather incomplete, most notably, the rich fossil record of stem [Cupressales [Gnetales + Pinales]], and of the three orders themselves, along with most of that of the gymnosperms as a whole, is currently largely ignored below.
Evolution. Divergence & Distribution. Leslie et al. (2012, see also 2018) offer ages for many conifer clades (see below) and evaluate the fossil data critically; their four- and three-gene trees (respectively) are based on a very good sampling of the group, in the latter study 578 species being included, although 18S sequences were obtained for less than a quarter of them.
The current distributions of many extant conifer groups is much smaller than and/or very different from their past distributions, thus McIver (2001) reported fossils of the African Widdringtonia (Cupressaceae) from rocks of Cretaceous age in Alabama (for distribution maps of all conifers, see Farjon & Filer 2013). Many conifers have fossil records going back to the Cretaceous; see Manchester (1999) for north temperate distributions). For the early Caenozoic fossil history of what are now East Asian endemics, see Ferguson et al. (1997) and Manchester et al. (2009) - genera in Taxaceae, Pinaceae, Sciadopityaceae and Cupressaceae are included. However, Biffin et al. (2010b) note that some calibration scenarios have crown-group divergence of Araucariaceae and Podocarpaceae largely a (mid-Cretaceous to) Caenozoic phenomenon, which would question the attribution of early fossils to crown groups of/in those families.
Sundaman et al. (2019) looked at biodiversity hotspots in conifers in general, noting that 80% or more of the species in them are not restricted to these hotspots, which are in stable mountainous areas; they are areas where species accumulate, as much refugia as anything else (see also Harrison & Noss 2017 in part). These hotspots include West Mexico (slightly different from the others, active diversification of Pinus in particular), Cascades-Sierra Nevada, China, Japan, Taiwan (some Pinaceae in all), and Sabah, New Guinea Highlands, and New Caledonia (Cupressales dominant).
There are no known synapomorphies for a clade containing living and fossil conifers (e.g. Rothwell & Serbet 1994). However, the morphology of extinct conifers and coniferophytes is being re-evaluated as entire organisms are being reconstructed from what are turning out to be separate form genera; the result is that many of the conventional taxonomic groupings are being radically overhauled (e.g. Rothwell et al. 2005; Hernandez-Castillo et al. 2009; see also below). As this is done, the extent of the diversity of these fossil plants is becoming clear. Not only are forked leaves common, but stomatal distribution, etc., may differ dramatically on leaves from the one plant, compound microsporangiate strobili are known (c.f. Gnetales!), as are megasporagiate strobili which do not terminate the vegetative growth of the axis on which they occur (e.g. Hernandez-Castillo et al. 2001; Rothwell & Mapes 2001) - but see Cycas...
The rate of molecular evolution of conifers is substantially slower than that in woody angiosperms, let alone that of herbaceous angiosperms, although the rate of non-synonymous substitutions is higher, perhaps connected with their large populations, outcrossing, and overall low population structure (Buschiazzo et al. 2012; see Jaramillo-Correa et al. 2016; Ran et al. 2018a, also elsewhere under Pinaceae and Araucariaceae).
Conifers are unusual compared to other vascular plants in that they show a gradual increase in disparity, that is, the amount/extent of morphological variation in their taxa, since their initial appearance in the Carboniferous (Oyston et al. 2016). More commonly it is during the initial radiation of a group that most of the morphospace that its clades now occupy is filled very quickly.
Diversification in most conifer genera occurred in the Caenozoic, as emphasized by Klaus et al. (2017), indeeed, the median node age of Pinus is a mere 4.4 Ma. Leslie et al. (2012) observed that most southern hemisphere clades are older than northern clades, and this is particularly true of the southern Cupressaceae-Callitroideae - its mean node age is four times that of the northern Cupressaceae-Cupressoideae. Leslie et al. (2012) associated this with the more equable climate in at least parts of the southern hemisphere compared with the major climate swings in the northern hemisphere beginning in the Oligocene. Earlier, during the Palaeocene-Eocene thermal maximum, conifers, perhaps especially Cupressaceae and Podocarpaceae, had been replaced by angiosperm-dominated vegetation (Wing & Currano 2013), although now, of course, Pinaceae dominate boreal forests in particular, and southern conifers, too, can be locally very abundant.
Extinction rates in conifers in general may have increased during the period 110-100 Ma, i.e. near the beginning of the Cretaceous Terrestrial Revolution, and this is perhaps the result of competition between conifers and angiosperms. These extinction rates have remained high while speciation rates may always have been rather low; the former may be due to more rapid growth, animal pollination, etc., in angiosperms and the latter in part to long generation time, large genome size, etc. (Condamine et al. 2020 and references). This conifer decline is indeed of long standing, furthermore, the rate of conifer decline may have increased as temperatures decreased in the Oligocene (Condamine et al. 2020). Note, however, that competition can be considered from other points of view, and then conifers may seem to come out not so badly - see Ecology & Physiology below.
Doyle (2009) discussed the evolution of exine morphology; granular exine may be an apomophy and then lost twice, or alveolar/honeycomb exine may be plesiomorphous, with granular exine gained three times, or the may be some other combination of gains and losses, but always adding up to three steps. Hence, the optimization here is an arbitrary choice! Franceschi et al. (2008) note possible anatomical apomorphies that are associated with defence against herbivorous insects.
Ecology & Physiology. There are four major clades of conifers: Pinaceae, mostly northern (= Pinales), [Araucariaceae + Podocarpaceae], now mostly southern, and two major clades in Cupressaceae (the last three = Cupressales) that have largely inhabited the northern and southern hemispheres respectively since the Jurassic (Brodribb et al. 2012). There may not be that many species of conifers, but they are ecologically a remarkably successful group. They dominate boreal forests in particular, but they are common in many other places outside the humid lowland tropics. Overall, they are more or less dominant in 39% of the world's forests, yet they include a mere 615 species or so, compared with the ca 352,000 species of angiosperms, so they are less than 0.27% of all seed plants (see also Krokene et al. 2008; Ran et al. 2018a, etc.). Bond (1989), Keeley and Zedler (1998), Brodribb et al. (2012), Augusto et al. (2014) and others have emphasized that after the seedling stage conifers in general can out-compete angiosperms in a number of environments that are low in nutrients, being able to tolerate poor soils, and they also can handle extreme conditions such as drought and cold (the [Podocarpaceae + Araucariaceae] clade tolerates extreme cold less well), they also grow well in high-light environments, and despite lacking vessels their wood shows moderate hydraulic conductance and is resistant to cavitation, etc. (Brodribb et al. 2012; Augusto et al. 2014). Indeed, their wood has larger hydraulic safety margins than that of angiosperms, so they can handle extreme drought conditions better, although Pinus may be an exception here (Breshears et al. 2005; Stovall et al. 2019).
Sperry (2003), Pitterman et al. (2005, 2011), Hacke et al. (2005, 2015) and Sperry et al. (2006) compare water transport in tracheids that have the torus:margo pits found in many conifers (including Ginkgo), with that in other kinds of tracheids and in vessels. Pore size in the margo is relatively large facilitating water transport, while the torus provides a valuable safety feature guarding against embolism as it will plug the pit if pushed against one side by pressure from the embolism. Indeed, hydraulic conductance in tracheids with torus:margo pits is somewhat greater than in vessels of similar diameter when expressed on a sapwood area basis, while studies of cavitation in this system suggest that it is not connected with the size of the pores in the margo, but rather with the torus:pit aperture ratio, since if the torus is relatively too narrow, air will seep in around the sides (Pittermann et al. 2010). Vascular tissue with tracheids only may be less hydraulically efficient than vascular tissue with vessels that have simple perforations, but they are tolerant of hydraulic stress and are resistant to cavitation, despite gymnosperms investing only about half as much as angiosperms in wall material - but at the same time they can make up the trunk of very large trees (Sperry 2003; Hacke et al. 2015). Lipid surfactants in the xylem of angiosperms, at least, i.a. coat nanobubbles as they form and so prevent the formation of embolisms, and they should be looked for here, too (Schenk et al. 2017). As Pitterman et al. (2005: p. 1924) note, "the evolution of the torus-margo membrane within the gymnosperm lineage from homogeneous pits was equivalent to the evolution of vessels within the angiosperms" (see also Wilson 2015; Hacke et al. 2015), but water transport can be surprisingly efficient in ferns, too (Pittermann et al. 2011, 2015).
Another element in the control of water flow in conifers is transfusion tissue, groups of tracheid cells just outside the vascular bundles. These cells collapse as the leaf loses water and water deficits are not too great (-<3 MPa), but readily regain their size when the leaf becomes rehydrated. When collapsed, they reduce the flow of water from the xylem (Y.-J. Zhang et al. 2014). The plesiomorphic condition for controlling water flow in the leaf during drought is for rising foliar abscisic acid concentrations to cause the stomata to close; the tracheids are prone to cavitation (Brodribb et al. 2014), however, abscisic acid is not involved in stomatal closure in some other conifers, a change that can perhaps be placed at the [Taxaceae + Cupressaceae] node.
The diameter of first order roots is linked to mycorrhizal type and how the plant forages for nutrients, and it varies considerably (W. Chen et al. 2013, 2016), but no comprehensive survey seems to have been carried out.
Litter and wood decay of gymnosperms in general is slower than that of angiosperms (e.g. Wardle et al. 2008; Cornwell et al. 2008b; Weedon et al. 2009), and root decay of conifers in particular is slower (Silver & Miya 2001), however, litter of the arbuscular mycorrhizal juniper has a lower C:N ratio than that of Pinus edulis and decomposes faster (Gehring et al. 2017b and references). Brown rot fungi like boletes are common on conifers, and they can access much of the cellulose in the cell wall but they cannot destroy lignin; they have often evolved from white-rot fungi (e.g. Floudas et al. 2012; Kohler et al. 2015), although the basal dacrymycete Calcera cornea may have evolved from a soft-rot ancestor (Nagy et al. 2015).
Many Pinaceae, ECM plants, grow successfully in low N conditions, while podocarps, AM plants, can grow in low P conditions (Brodribb et al. 2012).
Conifers frequently dominate the communities in which they grow and are often long-lived plants; the high-light conditions they prefer are often associated with infrequent catastrophic disturbances that allow seedling establishment. Some emergent and apparently dominant conifers (often other than Pinaceae) may have have remarkably little effect on the forests in which they grow, the basal area of angiosperm trees in forests with and without these emergents, but which are otherwise comparable, being similar (Enright & Ogden 1995; Aiba et al. 2007).
Pollination Biology & Seed Dispersal. For pollinators of fossil coniferales, see Peris et al. (2017). Fossils suggest Cheirolepidaceae were visited by Neuroptera ca 155 Ma and by Diptera 130-105 Ma (Peris et al. 2017).
Overall, there are three main kinds of reproductive cycles in Pinales, and these are based on how long reproduction takes, 2 or 3 years. In the two-year cycle, pollination, fertilization, etc. all occur in the second year. In the three-year cycle, there is variation in details of development, in particular, whether fertilization occurs in the second or third year (Turgeon et al. 1994).
For male cone variation and evolution, see Schulz et al. (2014). Much has been learned about pollination and pollen germination in conifers in the last few years, and this is summarized by Leslie et al. (2015a), although important work had been carried out about 80 years ago. Details of the fascinating story in Leslie et al. (2015a) depend on the topology of the tree used, which in Podocarpaceae, for instance, differs from that below (in such cases, data checked against Leslie et al. 2015b). Wind pollination is ubiquitous. The pollen grains directly impact the ovulate cones rather than being swept around them by a turbine-like action (Cresswell et al. 2007). There are correlations between the presence of pollen sacci or wings, exine thickness and structure, whether (no wings) or not (wings) the pollen is wettable/pollen buoyancy, ovule and cone orientation, and presence of a pollination drop (Tomlinson 1994; Little et al. 2014; Leslie et al. 2015a). For the composition of the pollination droplet, see Ziegler (1959) and Nepi et al. (2009, esp. 2017); like other wind-pollinated gymnosperms, it is relatively lower in sugars but higher in amino acids than gymnosperms in which insect pollination is sometimes involved. It had been thought that the sacci on conifer pollen facilitated its dispersal by wind, however, they function more like water wings. The sacci help orient the pollen grains in the pollination droplet (Doyle & O'Leary 1935; Salter et al. 2002 and references), or, more particularly, when the ovules are inverted, a common condition, the pollen grains are wetted and float up to the micropyle where the saccus orients the grain on the nucellus, separating and exposing the sulcus through which the pollen tube germinates (Salter et al. 2002; Leslie 2010b). Sacci also help in the selection of appropriate pollen grains during pollination. Thus the proportion of saccate to non-saccate pollen grains inside the ovules is higher than that outside (Leslie 2009). Changes in pollination mechanisms seem not to be accompanied by changes in diversification rates, and although sacci have been lost several times, in no case have sacci re-evolved within esaccate clades, loss being something of a one-way street (Leslie et al. 2015a). The pollination droplet in Phyllocladus and many taxa with erect ovules is resorbed through the micropyle, and again the pollen grains are brought close to the nucellus; in Juniperus communis and other taxa this resorbtion may be an active process happening quite soon after the pollen grain lands (Mugnaini et al. 2007). There are further variants of these pollination mechanisms in Pinales (e.g. Owens et al. 1998; Salter et al. 2002; Fernando et al. 2005; Nepi et al. 2017) and in other ancient gymnosperms (Leslie 2008).
Recent work suggests that the pollen story may be more complex. Sacci may indeed increase the distance the pollen grain can travel before it falls to the ground, so facilitating wind dispersal (Schwendemann et al. 2007). However, this depends on the nature of the sacci; if they have extensive air sacs, as in Pinus, pollen is likely to travel further, but if the sacci are composed of denser material, as in Falcatifolium, the pollen will fall faster - as it may also if the surface of the pollen grain is not smooth (Grega et al. 2013). Furthermore, the pollination droplet may also be involved in insect pollination, as in a number of Gnetales. For additional information on pollination, see Doyle (1945), Tomlinson (1994, 2000, 2012), Tomlinson et al. (1997), and Tomlinson and Takaso (2002); see also Williams (2009).
There is considerable variation in the development of the male gametophyte (Fernando et al. 2010: summary, terms used). The actual process of pollen germination varies, and the feature "pollen exine shed during microgametophyte germination", is likely to have evolved more than once (?three times) in Pinaceae alone (see also Rydin & Friis 2005); for cell death induced by the growing pollen tube, see Fernando et al. (2005 and references). Proteins have been found in the pollination droplet, and these may be involved in defence against pathogens and in promoting male gametophyte development (Wagner et al. 2007).
For details of seed morphology, dispersal type, etc., and their evolution, see Contreras et al. (2016). Fleshy (the fleshiness is of several kinds) animal-dispersed seeds have evolved several times from winged seeds, and there have been no reversals, however, the dry animal-dispersed seed type in Pinus has reversed to the winged type (Contreras et al. 2016). Bateman et al. (2011; see also Givnish 1980) note a correlation between dioecy and fleshy, animal-dispersed seeds and monoecy and dry, wind-dispersed seeds in gymnosperms, a correlation that is evident within Pinales. Leslie et al. (2013) suggest that this is largely due to the persistence of groups which are dioecious and have fleshy disseminules and monoecious and have dry disseminules; they note common transitions from the monoecy/fleshy to dioecy/fleshy combinations, although overall such features had little effect on diversification. Pollen and dry seed cone size in particular correlates with branch thickness, etc., in conifers; fleshy seed cones are notably smaller than dry cones (Leslie et al. 2014). Variation in seed size links with dispersal mechanisms - abiotic dispersal < seed subtended by attractant tissues < attractant issues part of the seed - and there are also correlations with clades (Leslie & Beaulieu 2015; see also Leslie et al. 2017 for detailed discussion). Furthermore, cone scales may reflex to allow the seeds to disperse, or they may fall from the cone, seeds dispersing at the same time; the latter condition is commoner when the seeds are larger and are packed more densely in the cone (Losada et al. 2019). There is substantial variation in the fatty acid composition of seed oils (Wolff et al. 1997) that may be linkable with phylogeny.
Plant-Animal Interactions. Herbivory in gymnosperms as a whole is relatively low (Turcotte et al. 2014: see caveats). In an earlier survey (Turgeon et al. 1994), almost 400 species of insects were recorded as eating the cones, and of these almost half (184 spp.) were Lepidoptera. Larger genera involved include Megastigmus (torimyid Hymenoptera), Dioryctria (pyralid moths) and Cydia (tortricid moths). Caterpillars of Yponomeutoidea-Argyresthidae, ditrysian moths and some leaf miners, are quite common here (Sohn et al. 2013).
Conifers have a variety of defences against insects, both constitutive and induced (e.g. Krokene et al. 2008). All conifers have layers of polyphenol-containing parenchyma (PP) cells in the phloem, possibly offering some protection against insects (Li et al. 2012), and methyl jasmonate is part of the inductive pathway (e.g. Hudgins et al. 2003; Hudgins & Franceschi 2004); these PP cells contain unidentified polyphenols, and they may also produce more PP cells, wound periderm, new cork cambium (Krokene et al. 2008). Resins are either constitutive or inducible, in the latter case developing in response to stimuli like insect attack, wounding, and the like; perhaps ironically, bark beetles use these resins to produce pheromones that result in the aggregation of the beetles and the overwhelming of the plant's defences (Krokene et al. 2008). In conifers in general, constitutive resin-based defences are found only in some Pinaceae, which, paradoxically, are susceptible to attacks by scolytid beetles, while Cupressales largely have inducible resiniferous structures, or they may lack both constitutive and inducible rein defences, but are not susceptible to attack by these beetles. The pattern of evolution of these resin defences seems rather miscellaneous, but this may be because I have not looked at the pertinent primary literature (but c.f. Franceschi et al. 2005; Krokene et al. 2008; Krokene 2015). There are other defences, too, the PP cells mentioned (most studied in Pinaceae) in the phloem, and arranged in various ways, calcium oxalate crystals of different sizes, lignified tissues of various kinds (Krokene et al. 2008); for further details, see the characterizations of individual groups. Different herbivores elicit different responses by the plant (Moreira et al. 2013), and even within Pinus there is variation in how much particular defences are expressed constitutively, the very distinction between constitutive and inducible sometimes being unclear (Krokene et al. 2008; Carrillo-Gavilán et al. 2014; Krokene 2015). See below for some details about the interactions between bark beetles, their associated fungi, and the conifer host.
Favret and Voegtlin (2004), Meseguer et al. (2015) and R. Chen et al. 2016) discuss speciation of Cinara aphids, found on Cupressaceae and especially Pinaceae (see also below). Many of the wood-eating basal termites (protozoans in their guts can break down lignin) seem to like the wood of Pinales; the crown-group age of termites is Jurassic, ca (170-)149(-136) Ma (Bourguignon et al. 2014).
Bacterial/Fungal Associations. A number of rusts, including those on ferns, Rosaceae, Grossulariaceae, etc., have part of their life cycles on Pinales, especially Pinaceae (Savile 1979b). For foliar endophytes and their bacterial associates, see Hoffman and Arnold (2010). Basidiomycete brown rot fungi are common in coniferous forests and are also found in broad-leaved, more temperate forests, but they are at most uncommon in tropical forests (Gilbertson 1981); for the relationships of (and uncertain distinction between) brown and white rot fungi, see Riley et al. (2014), Nagy et al. (2015). For the blue-staining ascomycete fungi associated with ambrosia beetles, see below.
Vegetative Variation. Secondary growth (only phloem is produced) has been reported from the leaves of a number of conifers, including those of Pinus longaeva the needles of which can live for 30 years or more (Ewers 1982; Hacke et al. 2015). There are short shoots in a number of taxa (see Dörken 2012 for a summary), and the shedding of branchlets, cladoptosis, which also occurs in taxa other than those with short shoots, is widespread (Burrows et al. 2007 and references; Dörken 2012). Below a distinction is made between evergreen and deciduous trees, the latter having no photosynthetic leaves during the winter, and cladoptosis, the shedding or abscission of branchlets. The latter may be the normal way in which leaves fall from the plant in both evergreen (e.g. Araucaria) and deciduous (e.g. Metasequoia) taxa and in those with (e.g. Pinus - evergreen) and without (e.g. Taxodium - deciduous) short shoots. (Note that the distinction between short and long shoots here is whether (long shoots) or not (short shoots) internodes are elongated.) Organised bud meristems usually occur in the axils of only some leaves, although more cryptic meristems are quite widespread (Namboodiri & Beck 1968a; Fink 1984; Burrows 1999, 2009); in taxa like Pinus and Sciadopitys axillary buds on the main axes are much more common, although most produce short shoots. Serial axillary buds occur in some taxa, particularly in those with cladoptosis since in their absence the supply of reserve meristems along a branch is reduced with the abscission of the branchlets; the oldest buds are furthest away from the axil.
Genes & Genomes. Chromosome number shows little variation in Pinales, and overall there is little polyploidy (Murray 2013; Scott et al. 2016). Based on their study of the coast redwood, Sequoia sempervirens, the only hexaploid in the whole group, Scott et al. (2016) emphasized the rarity of polyploidy in extant conifers, perhaps connected with their slow rate of diploidization. However, there appear to have been three genome duplications in the Pinales area, one in stem Pinaceae, another in stem [Taxaceae + Cupressaceae] (Sciadopitys was not examined), and a third in Welwitschia (Z. Li et al. 2015, but c.f. Zwaenepoel & Van de Peer 2019).
Conifers are noted for their very large nuclear genomes with 2C values of up to 72 pg (Zonneveld 2012); for 1C values, see the Plant DNA C-values Database (consulted vi.2013). These massive genomes are in part the result of the activity of a number of transposable elements that is not counteracted by mechanisms for slimming genomes, as in angiosperms (Ahuja & Neale 1005; Nystedt et al. 2013; see also Guan et al. 2016: Stevens et al. 2016). Note, however, that genome size in Pinales is quite similar to that in other gymnosperms. Reductions in genome size have probably occurred in Podocarpaceae and in particular in Gnetum (but not Ephedra, see H. Wu et al. 2020), so the increase in size in gymnosperms is not totally a one-way ticket (c.f. Bennetzen & Kellogg 1997). Leaf mass per unit area seems to be associated with with genome size, but this may be because of phylogenetic correlations (Beaulieu et al. 2007b).
C.-S. Wu et al. (2011b) suggested that a different copy of the chloroplast inverted repeat (IR) had been lost in Pinales (the IRb copy) and in Cupressales (the IRa copy). Raubesen and Jansen (1992a), Lackey and Raubeson (2008), Hirao et al. (2008) and Yi et al. (2013: can the copies be distinguished?) also discuss the loss of a copy of the inverted repeat; Guo et al. (2014) and J. Li et al (2016) note that in both cases short and novel IRs have developed. Overall, plastid genome size is small, although c.f. Ginkgo (Y. Yu et al. 2019b).
For chloroplast and mitochondrial inheritance of conifers, sometimes leaky, see Adams (2019) and references.
Chemistry, Morphology, etc.. For fatty acids in the seeds, see Wolff et al. (2002 and references), and for resin composition and gum production, see Tappert et al. (2011). Conifer lignin, primarily made up of guaiacyl units, is denser, more highly condensed, has a larger polymer size, etc., than the S-rich lignins of angiosperms; the two also differ in how common a numebr of minor lignin components are (A. Wagner et al. 2012, 2015). Andersson et al. (1973) briefly mention lignin composition of the bark of some conifers.
The interpretation of the stem apex in terms of tunica-corpus construction is not easy (see Napp-Zinn 1966). I have not integrated much of the considerable variation in wood anatomy with the clades recognised here (see e.g. Zhou & Jiang 1992 for information). Cork cambium is often more or less deep seated, although in Sequoia and Phyllocladus (e.g.) is is superficial (Möller 1882). Bark anatomy is very complex, but fortunately it has been studied in detail (e.g. Franceschi et al. 2008). Calcium oxalate microcrystals are commonly found in some cell walls throughout the group (Fink 1991; Hudgins et al. 2003: ?Cephalotaxaceae, Sciadopityaceae), but their distribution in other gymnosperms is unclear; they may be absent. Their position within tissues is linked with the development of fibres, the amount of resin secreted, etc. (Hudgins et al. 2003). For details of resin structures, see Krokene et al. (2008), they note i.a. that induced resin canals will tend to be vertical, while constitutive canals can be radial . There is generally a single trace per leaf, but if the leaves are opposite, there may be two traces, but then they fuse before they enter the petiole (Namboodiri & Beck 1968a, b), and leaf traces can also make connections with xylem produced during the second and subsequent years (Maton & Gartner 2005). Which taxa (few? most?) have a foliar endodermis is unclear (c.f. Lersten 1997; Dörken 2014). Dörken (2012) discussed the long/short-shoot distinction, suggesting (ibid.: p. 81) that shoot differentiation in genera like Pinus and Sciadopitys was a "reminiscence of a deciduous ancestor".
Bisexual strobili have ovuliferous scales above the microsporangia, i.e., the same basic arrangement as in angiosperm flowers, and they are scattered through the clade (Flores-Rentería et al. 2011). Basic cone morphology is very variable. Conifer seed cones have become more massive and strongly constructed since the Triassic, and particularly the Jurassic, presumably in reponse to animal predation pressure (Leslie 2011b), and although Taxus, for instance, is distinctive among extant taxa in having tiny female cones each with a single, erect ovule, cones are often quite massive structures. The ovuliferous scale is often well-developed and the bract scale inconspicuous, or the bract and ovuliferous scales may be largely separate, as in Pseudotsuga, while in Cupressaceae there is frequently little evidence of an ovuliferous scale in the mature cone, which consists largely of bract scales (e.g. Schulz & Stützel 2007; Rothwell et al. 2011 for references). Understanding details of the morphological evolution of cones will depend on advances in our understanding of the fossil record, and it is likely that heterochrony has been involved; Cupressaceae can be linked with the fossil Voltziaceae (e.g. Rothwell et al. 2011). Developmental studies may also be of value. Thus Englund et al. (2011) found that gene expression patterns linked the epimatium of Podocarpus with the ovuliferous scale of Pinus (see also e.g. Tomlinson & Takaso 2002), but not with the aril of Taxus. However, when comparing the expression of these genes in Cupressaceae, no particular similarities were observable (Groth et al. 2011).
For differences in the growth of the pollen tube in Pinaceae and angiosperms see Rounds and Bezanilla (2013); branched pollen tubes occur sporadically in Pinales (Friedman 1987 for references). Male gametes need more study. Some taxa have binucleate sperm cells, i.e., a cell plate does not form in the spermatogeneous cell, or, if it does, it is incomplete. The male gametes here may be unequal in size, as in Dacrydium, and one may even be extruded from the cytoplasm, as in Podocarpus spp. and Taxus. In at least some Gnetum, Podocarpus andinus, and Torreya taxifolia two unequally-sized male cells are produced (Singh 1978 for literature: I am grateful to Ned Friedman for help in understanding this complicated pattern of variation). Double fertlization sometimes occurs in Pinales (Friedman 1992). The free-nuclear stage in the proembryo of Pinales is shorter than that of other gymnosperms, being only 5 or 6 rounds of nuclear division in Podocarpaceae and Araucariaceae and even fewer in other members of the order (Owens et al. 2003c). Embryo size is rather variable, although it is often rather larger than that of the common ancestor of extant seed plants; in Pinus it may be close to the length of the seed.
Detailed studies on both fossil and extant conifers by Florin (e.g. 1951) laid the foundation for subsequent work on the group; see also Page (1990) and especially Gifford and Foster (1988), Farjon (2005b) for a bibliography and Farjon (2008) for an excellent general account; see also Debreczy and Rácz (2006), Eckenwalder (2009), Garnandt et al. (2011) and Plomion et al. (2011) for general information, Trapp and Croteau (2001a: resin biosynthesis), Geyler (1867), Barthelmess 1935, and Kumari (1963: nodal anatomy), Möller (1882: cork cambium), Napp-Zinn (1966) and Yao and Hu (1982), both leaf anatomy, Den Outer (1967) and Schulz (1990), both phloem anatomy, much detail unincorporated, Zhou and Jiang (1992: wood anatomy), Khan et al. (2019: epidermis); see also Sivak (1975: detailed study of saccate pollen), Owens et al. (1995b: cytoplasmic inheritance, nuclei sometimes incorporate cytoplasm), Williams (2009: reproductive biology), Mundry (2000: cone/strobilus development, emphasis on Taxaceae and friends), Sklonnaya and Ruguzova (2003: spermatogenesis), Bobrov and Melikian (2006: seed anatomy, both testa and tegmen present?), Buchholz (1929: embryogeny), Butts and Buchholz (1940: cotyledon number), Hill and de Fraine (1908, 1909: seedlings), Mathews and Tremonte (2012: greening of seedlings in the dark), and Herrmann (1951: intergeneric grafting). A valuable resource is the Gymnosperm Database (Earle 1997 onwards).
For further information on the major seed plant groups, see angiosperms, Cupressales (below), Cycadales, Ginkgoales, Gnetales and Pinales, and for discussion about their relationships, see also Angiosperm History I, above for conifers in general, and elsewhere for extant seed plants in general.
Within conifers, relationships are being clarified. Pinaceae (Pinus, Cedrus, etc.) are sister to the rest, as a morphological cladistic analysis by Hart (1987) suggested some time ago (but c.f. Nixon et al. 1994; Doyle 1996b). Molecular data and additional morphological work largely confirm the relationships in the tree here, which is based on the work of Quinn et al. (2002: successive approximations weighting), see also Price et al. (1993), Tsumura et al. (1995: RFLP analysis, tree [unrooted] with the same topology as the tree above), Kelch and Cranfill (2000), Gugerli et al. (2001: e.g. the mitochondrial nadI gene), Rai et al. (2002, especially 2008a), Burleigh et al. (2012), the four-gene analysis of Leslie et al. (2012) with its excellent sampling (but not Gnetum, etc.) and Ruhfel et al. (2014). However, the topologies in the scenarios of Biffin et al. (2010b) are either [Pinaceae [Podocarpaceae + Araucariaceae]] or [Pinaceae + Sciadopityaceae, etc.]... Sciadopityaceae are also somewhat migratory in the nuclear gene analyses of Y. Lu et al (2014), being either sister to [Taxaceae + Cephalotaxaceae] or to [Podocarpaceae + Araucariaceae] depending on whether the 1st and 2nd codon positions alone were included, or all three.
In the previous paragraph, Gnetales are not mentioned - they were not included in the studies mentioned. Indeed, the position of Gnetales has long been problematical. Morphological analyses in the 1980s often recovered an [angiosperm + Gnetales] clade, other extant gymnosperms being quite separate - this is the so-called anthophyte hypothesis (see the Cycadales page; Coiro et al. 2018 for a useful summary). However, the molecular work that soon started appearing either removed Gnetales from both angiosperms and gymnosperms or, more often, linked Gnetales with gymnosperms.
There are currently four main hypotheses as to the relationships of Gnetales in play.
1, Gnetales are sister to a clade including all other seed plants (e.g. Sanderson et al. 2000: two genes, third positions only; Seider et al. 2002: rbcL gene only; Rydin et al. 2002: nuclear genes only; Rai et al. 2003: large chloroplast data set; Quandt et al. 2004: trnL intron; C.-S. Wu et al. 2012b: LBA, 2013: some analyses). Extant gymnosperms would then be paraphyletic (see also Burleigh & Mathews 2004; Rai & Graham 2010: [Pinales [Ginkgoales [Cycadales + Angiosperms]]]; C.-S. Wu et al. 2011b: only in maximum parsimony, high substitution rate; Z.-D. Chen et al. 2016).
2. There is a [Gnetales [Pinales and Cupressales]] clade - the Gnetifer hypothesis - has frequently been recovered (e.g. Samigullin et al. 1999: not all analyses; Antonov et al. 2000; Sanderson et al. 2000; Chaw et al. 2000; Gugerli et al. 2001: rather strong support; de la Torre et al. 2006: much hidden support, but not from the chloroplast partition, 2017; Wu et al. 2007; Rydin & Korall 2009: Bayesian analysis; Ran et al. 2010: the mitochondrial rps3 gene; Rai & Graham 2010: support not very strong; Burleigh et al. 2012; C.-S. Wu et al. 2013: some analyses; Magallón et al. 2013; Rothfels et al. 2015b; Ickert-Bond & Renner 2016; Puttick et al. 2018: a variety of analyses; O.T.P.T.I. 2019: ASTRAL analyses), and it is the preferred topology in Englund et al. (2011) and Groth et al. (2011).
3. Gnetales are sister to Cupressaceae/Cupressales/conifer II group, the GneCup hypothesis, as in an analysis of an amino acid matrix derived from chloroplast genomes (Zhong et al. 2010; see also Ruhfel et al. 2014); both quickly-evolving proteins and also proteins in which there appeared to be much parallel evolution in Cryptomeria and the branch leading to all Gnetales were removed. If they were not removed, a clade [Cryptomeria + Gnetales] was obtained (Zhong et al. 2010; see also Moore et al. 2011; C.-S. Wu et al. 2013; Y. Lu et al. 2014: some analyses). Similarly, an analysis of variation in 83 plastid genes strongly suggested a grouping [Pinaceae [Gnetales + Cupressales]], although other relationships could not be entirely rejected (Chumley et al. 2008; see also Ruhfel et al. 2014; Evkaikina et al. 2017; Gitzendanner et al. 2018a: chloroplast data; O.T.P.T.I. 2019: plastid data). (Raubeson et al. (2006) found that Welwitschia grouped with Podocarpus, but this may be due to rate heterogeneity.)
4. Gnetales are sister to the Pinaceae/Pinales/conifer I group, the GnePine hypothesis (e. g. Chaw et al. 2000; Bowe et al. 2000; Gugerli et al. 2001; Hajibabaei 2003; Burleigh & Mathews 2004, 2007c: supermatrix analyses; Hajibabaei et al. 2006: genes from all three compartments, sampling?; Qiu et al. 2007; Graham & Iles 2009; Finet et al. 2010: quite strong support; Soltis et al. 2011; Y. Lu (2014: some analyses), Shen et al. 2017; evaluation of support; O.T.P.T.I. 2019: nuclear genes, supermatrix analysis). This topology was also found by Zhong et al. (2011, see also 2010; also C.-S. Wu et al. 2011b, 2014) when the most variable sites in concatenated alignments were removed, so reducing the LBA/heterotachy problem (clpP and matK genes in particular showed considerable heterotachy - Wu et al. 2011b), and by the concatenation-based transcriptome analyses of Wickett et al (2014). As Wu et al. (2011b: p. 1293) noted, "ndh genes (Braukmann et al. 2009) and the rps16 gene (Wu et al. 2007), and expansion of IRs to 3# psbA gene (Wu et al. 2007, 2009)" all supported this position. Although the possibility of any paraphyly of conifers has been strongly questioned (Rydin et al. 2002), a recent phylotranscriptomic study that included members of all gymnosperm families provides strong support for the GnePine hypothesis (Ran et al. 2018a).
The discussion below is structured around relationships suggested by the GnePine hypothesis, with Gnetales being sister to Pinales. There are some specific points of genomic similarity between Gnetum, etc., and some or all Pinales, and there are also some morphological similarities between the two groups, perhaps particularly with Pinaceae. The binucleate sperm cells, basic proembryo structure, development of polyembryony, etc., of Ephedra agree with conifers in general and perhaps Pinaceae in particular (Ran et al. 2018a). Some Pinus species have mesogenous stomata in which the subsidiary cells are produced from the same initial that gives rise to the guard cells (Gifford & Foster 1989; see also Mundry & Stützel 2004), as in Gnetales. Strobili with both micro- and megasporangia are common as abnormalities in conifers (Chamberlain 1935; Rudall et al. 2011a) and of course occur normally in Gnetum. Of course, wherever Gnetales are placed, they will have numerous apomorphies. Thus although nearly all Pinales have megasporangiate strobili with spirally-arranged ovuliferous scales or modifications of them, Gnetales have decussating bracts (Magallón & Sanderson 2002); loss of the ovuliferous scale, etc., might be additional apomorphies (Finet et al. 2010).
Note that some of the analyses mentioned individually above, including those by O.T.P.T.I. (2019), suggest that nuclear and chloroplast genomes may be telling different stories. Thus Xi et al. (2013b), using much nuclear and plastid data, although they included only ten gymnosperms, found a poorly to moderately supported [Gnetum + Pinaceae] clade in analyses of nuclear genes only. In analyses of chloroplast data a relationship with Cupressaceae was preferred (see also Davis et al. 2014a for the influence of different genomes); in both cases the alternative topology was rejected with a p-value of 0.001. This suggested to Xi et al. (2013b) that the two genomes of Gnetum had different histories. See also X.-Q. Wang and Ran (2014) for discussion; they noted that analyses of different classes of genes resulted in different topologies.
A final and rather different complication comes from the fossil record, and it is a challenge to incorporate the fossil data into the GnePine topology. In particular, seeds of Ephedraceae are perhaps similar to those of Erdmanithecales (Rydin et al. 2006); see also angiosperm stem and gymnosperm relationships. Detailed studies of small Early Cretaceous seeds suggests that both Erdmanithecales and Bennettitales have seeds very similar to those of Gnetum and Welwitschia in particular, the latter order agreeing in details of micropylar closure, and all have paracytic stomata (Friis et al. 2007, 2009, 2011, 2019c; Mendes et al. 2008; Cullen & Rudall 2016; Pott 2016 and references; c.f. Rothwell et al. 2009). Members of this BEG group (Bennettitales, Erdtmanithecales, Gnetales) have chlamydospermous seeds (the group has been called Chlamydospermae) in which a thin testa is surrounded by a thicker layer probably derived from (a) bract(s); there is a long micropylar tube (Friis et al. 2014 and references). The ovules are radiospermic and lack a cupule, the nucellus but not the integument is vascularized, and the seeds have an outer sarcotesta, a sclerotesta, and a layer inside that (Rothwell & Stockey 2002). A further link with Ephedra is in the granular infratectum of the pollen that all share (Friis et al. 2007), although the pollen of Jurassic-Cretaceous Eucommiidites (Erdmanithecales) is psilate and has two equatorial colpi as well (Pedersen et al. 1989); this latter pollen had been considered to be eudicot (Coiro et al. 2019 and literature). Finally, both Gnetales and Bennettitales commonly have stomata that are mesogenous and paracytic (Rudall & Bateman 2019). Members of the BEG group were very diverse in the northern hemisphere in the Lower Cretaceous and they co-occur with early angiosperms (Friis et al. 2014); Gnetales in particular have a very rich fossil record (most of the fossils are somewhat like Ephedra: Y. Yang et al. 2017 and references), are abundant in the Brazilian Crato formation of around 115-112 Ma (e.g. Löwe et al. 2013), but have not been found in Africa (Y. Yang et al. 2017). Recent work on the composition of the cuticle waxes of fossils suggests a connection between Bennettitales and Nilssoniales (Vajda et al. 2017).
With the addition of Gnetales, relationships can be depicted as follows.
Classification. Producing evolutionary classifications, or classifications that emphasise one or two favored morphological characters, remained popular for quite some time with those working on conifers (e.g. Keng 1975; Melikian & Bobrov 2000; Fu et al. 2004: Nageiaceae and Podocarpaceae well separated; Bobrov & Melikian 2006: Araucariaceae and other conifers quite separate from Pinaceae and Sciadopityaceae). However, see Farjon (1990, 2005a, c, 2017) in particular for detailed treatments of the conifers, Farjon (2001) for a checklist, and Christenhusz et al. (2011b) for a linear classification.
CUPRESSALES Link / Conifers II / Cupressophyta - Main Tree
Highly oxygenated diterpenes with phenolic rings [phenolic abietanes]; reaction wood on lower side of stem, xylem/phloem resiniferous structures 0; phloem with ring of PP cells one cell across, alternating with ring of phloem, ring of fibre cells, ring of phloem, then ring of PP cells again, etc., calcium oxalate crystals small, extracellular, resiniferous structures 0; (leaves opposite, sometimes then with two vascular traces); pollen grains atectate; euAP3 + TM6 genes [duplication of paleoAP3 gene: B class], chloroplast IRa copy lost, but ycf2 and psbA regions retained, plastid accD protein elongated because of tandem repeats; mitochondrial nadI gene intron 2 lost, also both rps3 introns, duplication in the PHYN clade. - 5 families, 57 genera, 383 species.
Includes Araucariaceae, Cupressaceae, Podocarpaceae, Sciadopityaceae, Taxaceae.
Note: In all node characterizations, boldface denotes a possible apomorphy, (....) denotes a feature the exact status of which in the clade is uncertain, [....] includes explanatory material; other text lists features found pretty much throughout the clade. Note that the precise node to which many characters, particularly the more cryptic ones, should be assigned is unclear. This is partly because homoplasy is very common, in addition, basic information for all too many characters is very incomplete, frequently coming from taxa well embedded in the clade of interest and so making the position of any putative apomorphy uncertain. Then there are the not-so-trivial issues of how character states are delimited and ancestral states are reconstructed (see above).
Age. Leslie et al. (2018) suggested an age of (301.7-)279.1(-250.3) Ma for this node, Magallón et al. (2013) an age of around (276.6-)259-256.9(-244.4) Ma and Won and Renner (2006) an age of (303-)273(-243) Ma, while around 249 Ma is the estimate in Ran et al. (2018a) and (282.6-)177.5(-89.1) Ma in Ran et al. (2018b: sampling), 230.9 Ma in Tank et al. (2015: Table S2) and as little as 184 Ma in Evkaikina et al. (2017).
Evolution: Divergence & Distribution. Leslie et al. (2018) evaluate the fossil record of the group, an although there is fairly good congruence between the fossil record and the dates they suggest in Cupressaceae, this is not true for Araucariaceae and the fossil record of Podocarpaceae is poor.
Sundaman et al. (2019) listed eight biodiversity hotspots for conifers in general, and these include West Mexico, Cascades-Sierra Nevada, China, Japan, Taiwan, Sabah, New Guinea Highlands and New Caledonia. In the last six hotspots in particular, Cupressales are notable components, while in the last three they make up (almost) all the conifers in the hotspots.
For other possible synapomorphies of this group, see Hart (1987). Isoflavonoids are known from Cupressaceae, Podocarpaceae and Araucariaceae (Reynaud et al. 2005).
Ecology & Physiology. This node is distinctive in having low leaf nitrogen, extant gymnosperms as a whole having a relatively high ratio of leaf mass per area (Cornwell et al. 2014).
Pollination Biology & Seed Dispersal. The combination of dry disseminules and dioecy has evolved several times in members of this clade growing in the southern hemisphere (Leslie et al. 2013).
Genes & Genomes. Yi et al. (2013) note that the chloroplast accD gene is notably large here (see also Hirao et al. 2008), usually over 600 amino acids long, having become about double the size of that of most other gymnosperms because of tandem repeats that may be unique to particular groups of Cupressales (Sudianto & Chaw 2019). The small repeats may be long enough to allow homologous recombination (for plastome recombination - plastomic sublimons - see Sudianto et al. 2018, ?not in Taxaceae); overall, variation in the chloroplast genome is considerable (e.g. C.-S. Wu et al. 2011b; Wu & Chaw 2014, 2016; Sudianto et al. 2018). J. Li et al. (2016; see also W. Guo et al. 2014) discuss the evolution of the small trnQ inverted repeat in this clade; they suggest as a sequence: single copy (Podocarpaceae, Araucariaceae) → tandem repeat (Sciadopitys) → inverted repeat (the rest).
For mitochondrial genes, especially the rps3 gene, see Ran et al. (2010). For the inheritance of chloroplasts and mitochondria, see Adams (2019 and references).
Chemistry, Morphology, etc.. For southern conifers, making up part of this clade, see Hill and Brodribb (1998: general) and Cox et al. (2007: oxygenated di- and tricyclic terpenoids). Krokene et al. (2008) discusss resiniferous tissue in xylem and phloem and Yao and Hu (1982) and Dörken and Stützel (2012a) discuss leaf anatomy; see Khan et al. (2019) for epidermal features.
Phylogeny. For relationships, see especialy Cycadales and Pinales, also angiosperms, Gnetales and Ginkgoales.
Synonymy: Actinostrobales Doweld, Araucariales Gorozhankin, Athrotaxidales Doweld, Cephalotaxales Reveal, Cunninghamiales Doweld, Cupressales Bromhead, Falcatifoliales Melikian & Bobrov, Metaxyales Doweld, Microstrobales Doweld & Reveal, Parasitaxales Melikian & Bobrov, Podocarpales Reveal, Saxegothaeales Doweld & Reveal, Sciadopityales Reveal, Taxales Knobloch, Taxodiales Heintze - Araucariidae Doweld, Cupressidae Doweld, Podocarpidae Doweld & Reveal, Taxidae Reveal - Araucariopsida A. V. C. F. Bobrov & Melikian, Podocarpopsida Doweld & Reveal, Taxopsida Lotsy
[Araucariaceae + Podocarpaceae]: gums +; roots with endomycorrhizal nodules; lamina vascular bundles not surrounded by sheath; three-year reproductive cycle, fertilization in 3rd year - ?), discrete pollination droplet 0; male gametophyte: prothallial cells divide; ovule one/bract scale; proembryo with 5 or 6 free-nuclear divisions; mitochondrial genome paternally inherited; 2nd intron in nad1 gene lost.
Age. The age of this node has been estimated at (287-)257(-228) Ma (Won & Renner 2006), (274-)245(-197.9) Ma (Leslie et al. 2018), (318-)263(-223) and (255-)198, 177(-157) Ma (Biffin et al. 2010b: latter age preferred), (237-)205(-177) Ma (Biffin et al. 2011b: text, c.f. fig. 2), 230-176 Ma (Leslie et al. 2012), around 243 Ma (Magallón et al. 2013), (284-)250, 225(-202) Ma (Kranitz et al. 2014), ca 186.3 Ma (Y. Lu et al. 2014), and ca 195 Ma (Ran et al. 2018a).
Note that "Podocarpaceae" (paratetracytic stomata, leaves forming a spray by twisting of the pedicels) have recently been found in deposits from Jordan dated as late Permian ca 253 Ma (Blomenkemper et al. 2018).
Chemistry, Morphology, etc.. Chamberlain (1935) notes that there is no stalk cell per se in the male gametophyte, but when the generative cell divides, one of the cells dies, the remaining cell divides and produces the gametes.
ARAUCARIACEAE Henkel & W. Hochstetter - Back to Cupressales
Phloem (with clusters of stone cells/inducible resiniferous structures - Araucaria), fibre rows 0; branches whorled, plagiotropic, branchlets ultimately abscise [cladoptosis]; secretory cells in the centre of the root; stem apex with tunica/corpus construction; phloem fibres scattered; only resin plugs present in vascular tissue; pits on radial walls of tracheids touching, hexagonal in outline; single leaf trace branching profusely in the cortex; stomata tetracytic, usu. traversely oriented; axillary meristems present on the trunk, undifferentiated, submerged by cork, persistent; leaves multiveined, lamina (veins branching dichotomously at base), petiole 0; (plants dioecious); to 20 microsporangia/microsporophyll; pollen not saccate; tapetum amoeboid [Araucaria]; bract and ovuliferous scales fused (not in Araucaria); ovule erect, nucellus protrudes from micropyle [?Araucaria]; pollination droplet 0, pollen not buoyant, germinates on ovuliferous scale and tubes grow over the scales [extra-ovular caputure and germination], prothallial cells numerous; seeds developing in association with the bract scale, wings entire or (asymmetrically) bilobed (0)/wings derived from integument, entire, scales falling from cone at maturity; free nuclear stage in proembryo with many nuclei, central, embryonal cells surrounded by cap cells that degenerate; cotyledons (4 - some Araucaria), with (3-)4-8 vascular bundles [?Agathis]; n = 13, nuclear genome [1C] 13.5-22.5 pg; (germination cryptocotylar).
3 [list]/33. Southern South America, Malesia to E. Australia and New Zealand (map: from Florin 1963; de Laubenfels 1988; Cretaceous and Jurassic fossils, green, from Sequiera & Farrell 2001). [Photos - Collection.]
Age. Crown-group Araucariaceae may be 185-165 Ma - or perhaps around 167.2 Ma (Laenen et al. 2014) or 205 Ma (see also Stöckler et al. 2002; Wallis & Trewick 2009). Biffin et al. (2010b) suggest ages of (215-)191(-169) or (94-)65(-47) Ma, the latter being their preferred age; 225-185 Ma is the estimate in Knapp et al. (2007), (179.7-)168.9(-165.2) Ma in Leslie et al. (2018), 172-162 Ma in Wilf and Escapa (2014, q.v. for other dates), (134-)94, 81(-60) Ma in Kranitz et al. 2014) and ca 51.2 Ma (Y. Lu et al. 2014). Dating here is in more than its normal mess.
Araucariaceae are well known as fossils from the Mid Jurassic (ca 175 Ma) onwards. Araucaria in particular is found in even older Triassic deposits in many parts of the world in both hemispheres; the remarkably preserved A. mirabilis in Patagonian middle Jurassic deposits ca 160 Ma has been associated with the monotypic section Bunya (Florin 1963; Stockey 1982, 1994; Hill & Brodribb 1989; Kunzmann 2007; see also Escapa et al. 2018; Hill et al. 2019). However, identification of Araucarioxylon wood can be difficult (Ash & Creber 2000). For Agathis fossils, see Hill ( 2008); the crown-group position of the ca 52.2 Ma South American Ag. zamunerae (Wilf et al. 2014, see Escapa et al. 2018) is in conflict with some of the ages above.
Evolution: Divergence & Distribution. See also Kranitz et al. (2014) for more ages. Biffin et al. (2010b, esp. 2011b) noted that stem-group calibration scenarios make crown-group divergence of Araucariaceae largely a (mid-Cretaceous to) Caenozoic phenomenon (see also Crisp & Cook 2011). This would question the placement of the early fossils just mentioned in extant sections of Araucaria; indeed, they form a basal polytomy along with A. hunsteinii and A. bidwillii (Escapa et al. 2018: support low; see also Kranitz et al. 2014).
Araucarioid wood was by far the commonest conifer wood in the Barremian-Hauterivian 145.5-125 Ma, but declined steadily through the Cretaceous, there being few records of any conifer group from the Campanian-Maastrichtian 84-65.5 Ma (Peralta-Medina & Falcon-Lang 2012: Gnetales not mentioned). The current southern distribution of Araucaria is best interpreted as the remnants of a much more widespread range (Stockey 1982; Hill & Brodribb 1989; Kunzmann 2007; Givnish & Renner 2004; Kooymnan et al. 2014; Kranitz et al. 2014; Escapa et al. 2018 for discussion), fossils being known from Europe as recently as the very Late Cretaceous ca 66 Ma just before the KP boundary (van der Ham et al. 2010). Eocene fossils are well known from Patagonia (Markhofer et al. 2015). Although Araucaria is diverse on New Caledonia, there is little genetic divergence between the species, suggesting that the genus has not been there long (Gaudeul et al. 2012; Cruaud et al. 2012c; Kranitz et al. 2014). In gymnosperms in general, rates of genome change are low, as are speciation rates, the two being correlated; however, Araucariaceae have very low rates of genome change when compared with all other land plants (Puttick et al. 2015).
Knapp et al. (2007; see also Kranitz et al. 2014) discuss the possibility of the long-term persistence of Agathis in New Zealand since the Eocene or before. Many floristic elements in the island that are known fossil there in the Oligocene-Miocene subsequently seem to have become extinct, their contemporary representatives being relatively recent immigrants (e.g. Jordan et al. 2010; Puente-Lelièvre et al. 2012), however, the distinctive frog Leiopelma may be an ancient lineage that has persisted on the islands (Carr et al. 2015). Agathis was until recently thought to be Australian, but well-preserved and abundant fossils have turned up in Patagonian Eocene deposits about 52.2 My; they were previously identified as Zamia (Wilf et al. 2014); see Fagaceae for other examples. Dilwynites pollen is similar to that of Wollemia and some species of Agathis (so it could be the stem group of these genera); it is widely disributed in austral areas, its first records being from the Late Cretaceous up to 93.9 Ma (Mcphail et al. 2013).
The quite recent discovery very close to Sydney of a few trees of the remarkable Wollemia, very similar to some fossil Araucariaceae (Jones et al. 1995; see e.g. Pastoriza-Piñol 2007 for a general account), occasioned some excitement. However, suggested divergence ages of Wollemia vary considerably, a mere (37-)18(-younger) Ma (Crisp & Cook 2011), (68.6-)55.8(-52.3) Ma (Leslie et al. 2018), to at least 110 Ma (Kunzmann 2007), so some of these ages suggest that comparison of Wollemia with Cretaceous fossils may be inappropriate (c.f. Chambers et al. 1998).
For possible apomorphies, perhaps including "dehiscent" seeds, i.e. seeds separating from the cone-scale, see Cantrill and Raine (2006), Escapa and Catalano (2013: most quantitative). Apomorphies for the family may be affected by the position of Wollemia within it.
Ecology & Physiology. Associations between both Araucaria and Agathis and a variety of insects and fungi may be of very long standing - 50 million years or more. See Plant-Animal Interactions below.
Leaves of Araucaria may remain on the plant for 25 years or so (references in Chabot & Hicks 1982).
Araucaria, and to a lesser extent Agathis (this in Burmese amber), have been major sources of fossilized resins, a.k.a. amber, since the late Triassic (Seyfullah et al. 2018).
Pollination Biology. The time from pollination to fertilization in Agathis australis is about twelve months, although this includes three months after pollination before the pollen grain germinates, and then another three months over winter when nothing much happens (Owens et al. 1995b). The pollen grains do not rupture when placed in water (Tomlinson 1994).
Plant-Animal Interactions. Sequeira and Farrell (2001) suggested that the association between Araucaria and the scolytine Hylurgini (used to be Tomicini) bark beetles was Cretaceous in age; the beetles seem to have moved on to Araucaria from angiosperms, and from thence moved on to Pinaceae. These weevils are in a clade separate from the Hylurgini found on pines (Jordal & Cognato 2012). García Massini et al. (2011) found evidence of wood-boring beetles, fungi and mites in fossilized araucarian wood of Middle Jurassic age from Argentinian Patagonia.
Caterpillars of the two species of Agathiphagus (Agathiphagidae), a small group of near-basal jawed lepidoptera, eat the seeds of Agathis, and they are known from Australia to the Pacific (Shields 1988; Powell et al. 1998); the moths can diapause for up to twelve years. It has been suggested that Agathiphagidae diverged from the Nothofagus-eating Heterobathmidae as much as 158.5 Ma (Wahlberg et al. 2013), but some favour a position sister to Micropterigoidea, together forming the basalmost branch of the lepidopteran clade (Regier et al. 2015; Kristiansen et al. 2015; see also Mitter et al. 2016) or sister to all Lepidoptera apart from Micropterigoidea and (297-)280.6(-257.4) Ma (Kawahara et al. 2019). It would be interesting to learn more about the history of this association.
There are other suggestions of very long-term associations. Donovan et al. (2020) looked at the patterns of damage caused by insects - leaf miners, gallers, armoured scale insects and the like - and fungi evident on the fossil Agathis from Patagonian Argentina (see Age above) and found that they were remarkably similar to those on extant Agathis. They suggested that these associations had persisted since the Palaeocene-Eocene even although Agathis is now found thousands of kilometres away from the fossil localities; they acknowledge the possibility that this assembly of organisms may have arisen independently where it now grows (Donovan et al. 2020).
Genes & Genomes. Araucariaceae have the largest plastid genomes (ca 145 kb) in Pinales but with the greatest percentage (>41.5%) of non-coding content, in the latter feature they are in line with seed plants in general, except other Pinales and Gnetales (C.-S. Wu & Chaw 2016).
Chemistry, Morphology, etc.. For the essential oils of Wollemia, see Staniek et al. (2010 and references), and for a possible taxol-producing endophyte, see Strobel et al. (1997).
Tomlinson (2008) noted that the axillary branches of Wollemia are evident in the resting terminal bud, but do not grow out until extension growth of the latter starts; there are undifferentiated resting meristems in the axils of the leaves of the main axis which develop if the apical meristem is destroyed (Tomlinson & Huggett (2011). The single leaf trace divides into three or more as it proceeds into the leaf (Tomlinson 2008; Tomlinson & Murch 2009), and this may be connected with branch shedding or cladoptosis, which is particularly striking here (Looy 2013 and references). Araucariaceae also have platelet structures in their cuticular waxes (Wilhelmi & Barthlott 1997); the stomata of Araucaria have a wax plug which may block penetration of fungal hyphae (Mohammadian et al. 2009 - see also Winteraceae).
The adaxial part of the cone scale is made up of bract scale tissues, the adaxial part of ovuliferous scale tissues (Dörken & Rudall 2018). Cones of Araucaria have a "ligule" that is more or less adnate to the ovule. The seeds of Wollemia have integumentary wings, unlike the seeds of other members of the family (Contreras et al. 2016).
For general information, see Stockey (1982), Bieleski and Wilcox (2009), Gee and Tidwell (2010: literature from late Triasssic to end Cretaceous), and especially the Gymnosperm Database, for comparative anatomy, see Thomson (1913), for axillary buds, see Burrows (1999 and references, 2009), for details of reproductive biology compared with those of other Pinales, see Owens et al. (1995a, b, c), for pollen morphology, see Dettmann and Jarzen (2000), and for phylogeny, see Setoguchi et al. (1998).
Phylogeny. For a comprehensive phylogeny of Araucariaceae, see Escapa and Catalano (2013). Wollemia has been placed variously sister to Agathis or sister to the rest of the family (Jones et al. 1995; Gilmore & Hill 1997; Setoguchi et al. 1998; S. S. Renner in Kunzmann 2007), the particular position being sensitive to the choice of outgroups (Knapp et al. 2007), but the former position seems more likely. A [Wollemia + Agathis] clade was retrieved in the comprehensive four-gene tree in Leslie et al. (2012) and by Escapa and Catalano (2013). Within Agathis, the New Zealand endemic Agathis australis is sister to the rest of the genus (e.g. Escapa et al. 2018 and references).
Botanical Trivia. Araucaria columnaris, the New Caledonian endemic Cook pine, leans towards the south in the northern hemisphere and to the north in the southern hemisphere, and the higher the latitude, the more pronounced the lean (Johns et al. 2017).
PODOCARPACEAE Endlicher - Back to Cupressales
Podocarpic acid + [particular diterpene with phenolic ring], (syringyl lignin + - positive Mäule reaction); (nodes 1:2); sclereids numerous, with large lumen; lamina with transfusion tissue in patches lateral to vascular bundles, laterally-elongated sclereids in middle of lamina; microsporophylls with two sporangia; pollen exine thin, except distally; male gametophytes with 3-6(-8) prothallial cells, sperm nuclei unequal in size (one extruded); proembryo [E tier] cells binucleate; propagules fleshy; polyembryony common; cotyledon with two vascular bundles [?all]; nuclear genome [1C] 4-11(-13.8 pg - Manaoa colensoi).
17 [list]/186. Largely southern Hemisphere, scattered, N. to Japan, Central America and the Caribbean (map: from Florin 1963; Dalling et al. 2011; Adie et al. 2011).
Age. Crown-group Podocarpaceae are estimated to be ca 102 Ma (Magallón et al. 2013), although many other estimates are substantially older, ca 132.7 Ma (Y. Lu et al. 2014), (194-)145(-99) Ma in Biffin et al. (2011b: c.f. Fig. 2), (223.6-)188.9(-159.5) Ma (Leslie et al. 2018) and (259.2-)230.3, 226.9(-196.7) Ma (Quiroga et al. 2016) - note the topologies. Leslie et al. (2018) estimated crown group diversification to begin (223.6-)188.9(-159.5) Ma while the comparable age in Sudianto et al. (2018) is 142-134 My.
Fossil Podocarpaceae (as Rissikia) are known from the Middle Triassic of Antarctica ca 225 Ma, although the material has since been lost (apparently the fossils had 2 ovules/scale, see also Saxegothaea: Townrow 1967; Eckert & Hall 2006; Axsmith et al. 1998; Biffin et al. 2011b: Suppl. 4; Rothwell et al. 2012). Distinctive podocarp root nodules are known from very well-preserved fossils from ca 240 Ma in the Early Triassic (Schwendemann et al. 2008, esp. 2011).
1. Podocarpoideae Beilschmied
Age. Saxegothaea diverged from other Podocarpoideae (197.2-)163.9(-131.9) Ma (Leslie et al. (2018).
1a. Saxegothaeeae Gordon
Plants monoecious; leaves petiolate, held vertically, ?isobifacial; pollination droplet 0; ovuliferous cone facing sideways [= lateral], two ovules/scale, nucellus protrudes from micropyle; pollen germinates on ovuliferous scale and tubes grow over the scales [extra-ovular caputure and germination]; whole cone ± fleshy; n = 12.
1/1: Saxegothaea conspicua. South Chile and Argentina.
Synonymy: Saxegothaeaceae Doweld & Reveal
The Rest Gordon
Leaves (opposite - Microcachrys), lamina (multiveined, branching dichotomous - Nageia); ovuliferous scales (aggregated into cones - Microcachrys); n = (18) 19.
Podocarpus (107), Dacrydium (20). Photos Collection.
Synonymy: Acmopylaceae Melikian & A. V. Bobrov, Bracteocarpaceae Melikian & A. V. Bobrov, Dacrycarpaceae Melikian & A. V. Bobrov, Falcatifoliaceae Melikian & A. V. Bobrov, Microcachrydaceae Doweld & Reveal, Nageiaceae D. Z. Fu, Pherosphaeraceae Nakai
2. Phyllocladoideae W. Hochstetter
(pollen not saccate - Phyllocladus).
Photos Collection, Phyllocladus trichomanoides, Phyllocladus megasporangia, microsporangia].
Age. Huncocladus, in deposits ca 52 Ma from Patagonia, Argentina, is close to Phyllocladus, but the latter now grows only from the Antipodean-Malesian region (Andruchow-Colombo et al. 2019).
Synonymy: Halocarpaceae Melikian & A. V. Bobrov, Lepidothamnaceae Melikian & A. V. Bobrov, Parasitaxaceae Melikian & A. V. Bobrov, Phyllocladaceae Bessey, Prumnopityaceae Melikian & A. V. Bobrov
The Rest - in the process of being dismembered... Microstrobaceae Doweld & Reveal ??
Leaves petiolate or not; plants dioecious (monoecious); exine alveolate/honeycomb; ovuliferous scales not aggregated into cones, ± reduced, fused with ovule and ± enveloping it [looking like an integument]; (ovule erect); pollination droplet spreads along surface of scale, scavenges pollen; ovuliferous scale fleshy [= epimatium], fleshy (not); n = (9-)10(-15, 17-19).
Evolution: Divergence & Distribution. For dates in the family, see Leslie et al. (2018).
Until the end of the Eocene Podocarpaceae were very common in southern Patagonia and dominated Antarctic forests, and they were then replaced with Nothofagaceae (for their biogeography, etc., see Mill 2003; Kooyman et al. 2014; Pujana & Ruiz 2017; etc.). Retrophyllum, which still grows in south South America, is known fossil from early end-Cretaceous Argentina 67-66 Ma (Wilf et al. 2017b; see also Wilf 2020). There are other Podocarpaceae that are, however, currently not growing in the New World in Palaeocene/Eocene deposits in Argentinia (Kooyman et al. 2014; Merkhofer et al. 2015 for references, also Fagaceae for discussion about such distributions), and there are also well-substantiated reports of members of the family from the northern hemisphere in the Cretaceous and Early Caenozoic, e.g. Prumnopitys anglica from Eocene southeast England (Greenwood et al. 2013 and references). However, Pujana and Ruiz (2017) note that Podocarpoxylon fossils, quite common in the northen hemisphere, are unaccompanied by other remains that might be placed in Podocarpaceae and so are themselves unlikely to be Podocarpaceae, while this was not the case with fossils of that genus from the southern hemisphere.
Podocarpaceae are still quite common and may dominate the vegetation, largely in the southern hemisphere, however, as Australia has dried out during the Caenozoic, podocarps have become less common there (e.g. Brodribb & Hill 1997, 2004; Biffin et al. 2011b). Diversification in clades whose members have imbricate leaves began in the Late Jurassic ca 150 Ma (Biffin et al. 2011b) or earlier (Quiroga et al. 2016). Diversification in clades whose members have flattened foliage is notably greater, but younger, and is dated to (94-)64(-38) Ma (Brodribb & Hill 2004; Biffin & Lowe 2011; Biffin et al. 2011b; Brodribb & Feild 2010), and crown-group Podocarpus, with 107 species representing well over half the family, is (81.8-)65.2, 60(-52.2) Ma, i.e. late Cretaceous or early Palaeogene, although it could be up to 37 Ma older (Quiroga et al. 2016). Leslie et al. (2012) and Quiroga et al. (2016) offer more dates for splits within Podocarpaceae. Dacrydium may have moved into South East Asia via the Ninety East Ridge and India (Morley 2011). For possible roles of New Caledonia and New Zealand in the persistence of Podocarpaceae, see Condamine et al. (2016: metapopulations on ephemeral islands?).
Ecology & Physiology. Podocarps are slow-growing, long-lived, light-demanding specialists that often grow in nutrient-poor soils, but are mostly poorly adapted to dessication stress; they can be dominants or emergents in southern forests (Brodribb 2011; Coomes & Bellingham 2011). Extant Podocarpaceae with broad leaves are shade tolerant and prefer warmer and higher rainfall conditions, and they also have fleshy diaspores, the often brightly-coloured seed being associated with a fleshy epimatium (Farjon 2018). Foliage variation in Podocarpaceae is considerable. Biffin and Lowe (2011, see also Biffin et al. 2011b) suggest that podocarps with broad leaves or functionally equivalent structures like the phylloclades of Phyllocladus evolved about four to six times, probably slightly after the venation density of angiosperm leaves increased - (94-)64(-38) versus 109-60 Ma. In taxa like the spiral-leaved Afrocarpus the leaves orient themselves to form a spray of foliage, all leaves having their upper surfaces uppermost in the spray, but in the amphistomatous Retrophyllum all leaves twist in the same direction so the upper surface may face the lower side of the spray (Wilf et al. 2017b). Broad-leaved podocarps are now largely meso-megathermal shade-tolerant plants (high rates of transitions from microthermal) while the imbricate-leaved taxa are mostly microthermal (high rates of transitions from meso-megathermal: Biffin & Lowe 2011; Biffin et al. 2011b; Brodribb & Feild 2010). Fossils with apparent affinities to podocarps and with broad leaves are known from the Triassic and Jurassic (Biffin et al. 2011b).
Podocarp leaves decompose only slowly (although there are few studies on this), with a high concentration of condensed tannins (Ushio et al. 2017), carbon/lignin build up in the soil, nutrients are sequestered, and soil fertility is further reduced (Wardle et al. 2008); they have been described as ecosystem engineers because of this combination of features (Coomes & Bellingham 2011). Soils beneath the tree may be low in both N and P, but Dacrydium gracilis, at least, effectively removes the little inorganic N that is there, while saprophytic microbes may contribute to the high acid phosphatase activity in the soil which relieves the P limitation (Ushio et al. 2017).
There are often root nodules in Podocarpaceae. The roots involved tend to be superficial, and the nodules may be in longitudinal rows and represent modified lateral roots (Becking 1965; Duhoux et al. 2001). The fungus Glomus is involved, and nitrogen does not seem to be fixed (Russell et al. 2002), however, what these nodules might do is poorly understood (Dickie & Holdaway 2011).
The New Caledonian Parasitaxus usta (Parasitaxoideae) is hemiparasitic on the roots of Falcatifolium taxoides (Podocarpoideae), where it taps the xylem and from which it obtains water and nutrients (the stomata of Parasitaxus are insensitive to light), and the plant is a mycoheterotroph, obtaining carbon from an ?ectomycorrhizal fungus that is also associated with its host and whose hyphae grow through the vascular systems of both host and parasite (Woltz et al. 1994; Feild & Brodribb 2005; Merckx et al. 2013a; Imhof et al. 2013a).
Pollination Biology & Seed Dispersal. There is a correlation between the absence of pollen wings and the shedding of the pollen exine when the microgametophyte germinates. In Phyllocladus, which has erect ovules, the pollination droplet is actively resorbed (see Tomlinson et al. 1991, esp. 1997: useful comparisons; Rydin & Friis 2005). For pollen tube growth in Saxegothaea, see Doyle and O'Leary (1935a); if that genus is sister to the rest of the family, one may have to rethink aspects of the evolution of pollination mechanisms in Podocarpaceae (c.f. Leslie et al. 2015). See also Little et al. (2014) for pollination.
For details of seed morphology, dispersal, etc., and their evolution, see Contreras et al. (2016); the diaspores are usually fleshy and animal-dispersed, the epimatium/ovuliferous scale being variously developed and more or less surrounding the seed.
Vegetative Variation. Phyllocladus has phylloclades, flattened, photosynthetic stems; these bear highly reduced, scale-like leaves which may lack leaf gaps, and it is in the axils of these leaves that the reproductive structures are found. However, the seedling has more conventional needle-like leaves. The foliar units of podocarps with flattened foliage units, whether leaves or phylloclades, have transfusion tissue or there are several veins, unlike the single vein and absence of transfusion tissue in the leaves of other podocarps (Biffin et al. 2011b).
Genes & Genomes. Quinn et al. (2002) noted that dysploid chromosome evolution was quite common in the group.
Sudianto et al. (2018) discuss the plastid genome of Podocarpaceae, which varies in size from 121.1-151.5 kb, that of Lagarostrobus being the largest, and that genus has notably high intergenic spacer content and abundant repeats. Although Parasitaxus has chlorophyll a and b, it has lost its genes for photosynthesis, furthermore, its light-independent chorophyll biosynthesis genes chlB, chlL and chlN have become pseudogenized (X.-J. Qu et al. 2019). The plastome has regained an IR of 9,256 bp long (Qu et al. 2019).
Chemistry, Morphology, etc.. For secondary metabolites in Podocarpus s.l., see Abdillahi et al. (2010); taxol has been found in Afrocarpus gracilior (fungi involved here, too?). Syringyl lignins have been reported quite widely from Podocarpaceae, although mostly from subepideraml fibres and sclereids (e.g. Gibbs 1958). For cuticular features and how they may be affected by the environment, see Clugston et al. (2017). Accessory transfusion tissue extends to the lamina margin in Podocarpus macrophyllus and a number of other species of the genus (Gifford & Foster 1989); Knopf et al. (2012) provide many details of foliar anatomy for the whole group.
The morphological nature of the epimatium has occasioned some controversy. Chamberlain (1935) interpreted it as possibly being equivalent to the ovuliferous scale (see also Tomlinson & Takaso 2002; Englund et al. 2011: similarity confirmed by gene expression data), and functionally, perhaps, it can be considered equivalent to the second integument of an angiosperm ovule - hence the "anatropy" of the ovules here (Endress 2011b). The epimatium may be free from or adnate to the integument (see also Contreras et al. 2016 for seed morphology). Phyllocladus is sometimes described as having an aril, although this is more probably a somewhat reduced and retarded epimatium (de Laubenfels 1988); Tomlinson and Takaso (1989) found evidence that the structure was paired, c.f. modified leaves, also Taxaceae?
The pollen of Phyllocladus has often been described as having a wing (e.g. Singh 1978), but a wing seems to be absent. Although the single ovules of most Podocarpaceae do seem very different from the multiovulate cones of most other Pinales, Lower Cretaceous podocarps with more conventional bract-scale complexes, as in the extant Saxegothaea, have been described (X. Wang et al. 2008). For details of embryogeny, see Buchholz (1941), and for nucleus number in the E-tier cells, see also Quinn (1986). Cleavage and true polyembryony are common in Podocarpaceae, indeed, embryos seem able to develop from almost any cell of the early embryo (Buchholz 1941; for polyembryony, see also Doyle and Brennan (1972: integrate this character better).
For Podocarpus, see Mill (2014: summary of literature) and for Phyllocladus, see Quinn (1986: embryogeny) and Tomlinson et al. (1989: cone, etc.). For general information, see Turner and Cernusak (2011: Smithsonian Contrib. Bot. 95. 2011), and the Gymnosperm Database, and for cuticle morphology, see Mills and Schilling (2009) and for wood anatomy, see Woltz et al. (2009 and references).
Phylogeny. For phylogeny, see also Kelch (1998), a comparison of morphology and molecules. RbcL analyses (Conran et al. 2000; Wagstaff 2004b) tended to place Phyllocladus within Podocarpaceae, other analyses, whether (Quinn et al. 2002) or not (Sinclair et al. 2002) including rbcL sequences, placed the two as sister groups. Indeed, in the latter, relationships were [Phyllocladus [Lepidothamnus [[Prumnopitys [Lagarostrobus, Parasitaxus, etc.]] [Saxegothea [Falcatifolium, etc.]]]]] (Sinclair et al. 2002). Inclusion of Phyllocladus within rather than sister to all other Podocarpaceae is likely, as in Peery et al. (2008: nuclear XDH gene), and it was in the small prumnopityoid clade in the combined analysis of Knopf et al. (2012: support in/for this clade not strong in single gene analyses; see also Biffin et al. 2011a, b; Quiroga et al. 2016). Other groupings of genera are becoming evident (Kelch et al. 2010), including the dacrydioid and podocarpoid clades (Knopf et al. 2012). The closest relatives of Parasitaxus are Lagarostrobus and Manoao, both monotypic and from Tasmania and New Zealand respectively - [Parasitaxus [Lagarostrobus + Manoao]] (Sinclair et al. 2002; Rai et al. 2009; Lam et al. 2009; Sudianto et al. 2018; summary, c.f. Quiroga et al. 2016: Lagarostrobus in a different part of the family). Saxegothaea has some support as being sister to all the rest of the family (Knopf et al. 2012, but c.f. Biffin et al. 2011a, b; Y. Lu et al. 2014; Quiroga et al. 2016: sister to [Microcachrys [Pherosphaera [Acmopyle + ...]]]; Leslie et al. 2012, 2018: sister to the Tropical Clade). This has considerable implications for character evolution in the clade; as Mabberley (2007) noted, the plant has some features reminiscent of Araucariaceae. Sudianto et al. (2018) in their study of chloroplast genomes of Podocarpaceae used variation in 81 genes to disentangle relationships, finding i.a. that Saxegothaea was sister to Podocarpoideae, not to the whole family. For other general relationships, see Lu et al. (2014: Parasitaxus and Phyllocladus sister taxa), Leslie et al. (2018), and for relationships within Podocarpus in particular, see Biffin et al. (2011, 2012) and Quiroga et al. (2016) and Leslie et al. (2018).
Classification. For generic limits in Podocarpaceae, see Page (2019).
Previous Relationships. Phyllocladus was long considered to be very distinctive, so distinctive that it was sometimes separated from all other conifers (e.g. Keng 1974, 1979).
[Sciadopityaceae [Taxaceae + Cupressaceae]]: roots with endomycorrhizae; secretory cells in the centre of the root [?or next node up]; two-year reproductive cycle/three-year, fertilization in 2nd/3rd year; pollen without sacci, not buoyant, exine shed on microgametophyte germination [microgametophyte naked]; ovuliferous cone horizontal to pendant, with <10 basal sterile scales; bract scale becoming narrowed at the base; ovuliferous scale adnate at base of bract scale, ovules erect, becoming inverted; prothallial cells 0; seed winged, wing developing from the integument, narrow; scales reflex at maturity.
Age. Leslie et al. (2012) estimate an age for this node of over 250 Ma, some time in the late Permian, and Leslie et al. (2018) put the age at (276.6-)247.6(-222.1) My; ca 230 Ma is the estimate in Ran et al. (2018a).
Evolution: Genes & Genomes. The occurence of chloroplast genome isomers is scattered in this clade, but they are particularly common in Cupressoideae (Hsu et al. 2016; Qu et al. 2017), and are also common in angiosperms and at least some ferns (W. Wang & Lanfear 2019).
Chemistry, Morphology, etc.. The pollen grains expand and rupture when placed in water (Tomlinson 1994), and the intine-clad pollen, although sometimes much larger than the pollen grain itself, may deform more easily and so be tranferred along the narrow micropylar canal (Takaso & Owens 2008). Whether or not all taxa have male gametes each surrounded by cell walls needs to be confirmed (see Singh 1978).
SCIADOPITYACEAE Luersson - Back to Cupressales
Wood parenchyma 0, walls of tranverse and tangential ray cells not pitted; short shoots ultimately abscise [= cladoptosis]; 8-12 subsidiary cells/stoma; leaves on long shoots reduced to scales; short shoots +, subtended by a scale leaf, with a pair of connate needles, apically bifid (not), vascular bundles surrounded by sheaths, petiole 0; pollen cones in clusters/pseudowhorls, microsporophyll with flattened apical expansion, (1-)2 microsporangia/microsporophyll; pollen inaperturate, surface microtuberculate (microechinate), exine granules confluent by sporopollenin deposition; sterile cell?; ovules (1-)7-9(-12)/bract scale, margin of ovuliferous scales fringed, ± connate; pollen chamber?; seeds (1-)7-9(-12)/scale; n = 10, nuclear genome [1C] ca 20 pg, chloroplast accD gene to nucleus.
1 [list]/1: Sciadopitys verticillata. C. and S. Japan (map: from Florin 1963). [Sciadopitys Photos - Collection]
Evolution: Divergence & Distribution. Fossils of Sciadopitys are known from the Upper Cretaceous and afterwards, but apart from material from Japan and the Upper Pliocene of Germany, the identities of many are questionable (Stockey et al. 2005).
Ecology & Physiology. Resin from Sciadopitys may have contributed to Baltic amber 47-34 Ma (Sadowski et al. 2016a), indeed, Sciadopitys may be the main source of resin for the ca 105 tons of this amber (Wolfe et al. 2009), but Pinaceae, Araucariaceae and perhaps Cupresssaceae may also have contributed (Seyfullah et al. 2018).
Genes & Genomes. For the distinctive chloroplast genome of Sciadopitys with two inverted repeats and the formation of four chimaeric gene clusters, see J. Li et al. (2016) and Hsu et al. (2016). The chloroplast accD gene has moved to the nucleus (Sudianto & Chaw 2019), perhaps soon after Sciadopitys split from the other Cupressales (J. Li et al. 2016).Chemistry, Morphology, etc.. There are apparently no resin canals in the wood (Pierce 1935); resin exudes from the pith and cortex in the cones and appears to be exuding from the cortex of twigs/small branches (Wolfe et al. 2009: Fig. 4j, k).
There has been much debate over whether the photosynthesising structures of Sciadopitys are some kind of phylloclade - perhaps formed by the connation of two leaves - or cladode, a modified stem structures. The two vascular bundles, each with its own endodermis, tend to have have abaxial xylem and adaxial phloem, perhaps a rather odd arrangement for a leaf-derived structure. Sporne (1965) noted that on occasion branches develop from these leafy structures, so perhaps favoring the cladode hypothesis (see also Farjon 2005c). However, Dörken and Stützel (2011) examined probably only the second known case of intermediate structures and considered the "needles" to be two congenitally connate needle leaves, the orientation of the vascular tissue reflecting the relation of the leaves to the axis that bore them (see also Dörken & Stützel 2012a). The "needle" is thus comparable with the fascicles of separate needles in Pinaceae.
For a monograph, see Farjon (2005c), and for general information, see also Gymnosperm Database, for pollen, see Page (1990) and Uehara and Saichi (2011), and for ovule and cone, see Takaso and Tomlinson (1991).
[Taxaceae + Cupressaceae]: subsidiary cells 4-7/stoma; lamina vascular bundles ?surrounded by sheath; microsporangia hypodermal in origin; chloroplast trnQ IR +.
Age. Leslie et al. (2012) estimate that these two families diverged 217-197 Ma, Y. Lu et al. (2014) estimated an age of ca 211.5 Ma, Leslie et al. (2018) put this age at (220.7-)202.8(-197.1), Mao et al. (2012) offer an age of (293-)245, 242(-194) Ma, while estimates in Yang et al. (2012) are 217-197 Ma (or perhaps 237 My), in Won and Renner (2006) they are (265-)227(-189) Ma, while in Magallón et al. (2013) they are ca 175.4 Ma; ca 208 Ma is the figure in Ran et al. (2018a).
Evolution: Ecology & Physiology. The evolution of cavitation-resistant xylem and stomata that stay open during periods of drought (Brodribb et al. 2014) can perhaps be placed at this node, although not all species show this combination of characters - Cunninghamia, Sequoiadendron and Glyptostrobus are examples.
Chemistry, Morphology, etc.. Cunninghamia and Taxus had by far the thickest roots (roots developing after root pruning) of the fourteen species of seed plants examined (B. Liu et al. 2015). Burrows (2009) noted that axillary buds occur in several members of this clade, but they were superficial and so did not form shoots in older branches - c.f. Araucariaceae.
Gene expression studies suggest little in common between the scaly structures of the Cupressaceae cones studied or the arils of Taxus with the ovuliferous scales of Pinaceae... (Englund et al. 2011; Groth et al. 2011).
TAXACEAE Berchtold & J. Presl - Back to Cupressales
Bands of fibres in phloem crystalliferous; leaves shortly petiolate; plant dioecious (monoecious); pollen cones compound (simple), sporangiophores peri-(also hypo-)sporangiate, [pendulous from peltate scutellum to abaxial and with a phyllome-like adaxial process], pollen shed at 1-cell stage, inaperturate; ovuliferous cone pendulous, scales opposite; (ovules erect), pollen chamber +; male gametes unequal in size; disseminule fleshy ["arillate"], coat vascularized, with sarco- and sclerotesta; n = 12, nuclear genome [1C] 11.5-30 pg.
6 [list]/30. Northern Hemisphere, scattered, also New Caledonia.
Age. Estimates of the age of this node vary - e.g. (247.4-)210.5(-173.6) Ma (J. Liu et al. 2013), (231-)187(-144) Ma (Won & Renner 2006), (201.8-)172.3(-131.1) Ma (Leslie et al. 2018), ca 144.4 Ma (Y. Lu et al. 2014), or ca 134 Ma (Ran et al. 2018a).
1. Cephalotaxeae Wettstein
2-3 microsporangia/microsporophyll; ovuliferous scale much reduced, ovules 2/bract scale; female gametophyte with 1024-4096 free nuclei; ?embryo.
1/6. E. Himalayas to Japan (map: from Florin 1963). [Cephalotaxus koreana Photos - Collection, C. fortunei, Collection.]
leaves (bijugate), with resin canals below vascular bundle, hypodermis fibrous, discontinuous; microsporangia abaxial; "aril adnate to seed" [Ceph.?]"; n = (7 [Amentotaxus]).
Synonymy: Cephalotaxaceae F. W. Neger
2. Taxeae Duby
Sclereids + [Taxus]; leaves lacking resin canals; 2-10 microsporangia/microsporophyll (partly connate - Austrotaxus); bract and ovuliferous scale 0, ovule solitary, on shoot in axil of vegetative leaf; female gametophyte with ca 256 free nuclei; (seed "arillate" - Taxus); embryo short/minute (cotyledons 3); n = (11).
5/32: Taxus (16). Scattered in the Northern Hemisphere, esp. South East Asia, also New Caledonia (map: from Florin 1963; de Laubenfels 1988). [Photos - Collection.]
Age. The age of the [Torreya + Taxus] clade is some 138 Ma (Magallón et al. 2013).
Synonymy: Amentotaxaceae Kudô & Yamamoto, Austrotaxaceae Nakai, Torreyaceae Nakai
Evolution: Divergence & Distribution. Möller et al. (2020 and refs) give ages for various clades here.
Taxus and its immediate relative have female cones with a single ovule and the seed is surrounded by an aril. The sarcotesta of Cephalotaxus has been tentatively equated with the aril of Taxus (Mundry 2000), although the two would not seem to be homologous. A reinterpretation of the female reproductive structures (Stützel & Röwekamp 1999a) suggest that Taxus in particular can be linked with Torreya and then to other conifers; its aril is the equivalent of the sarcotesta of other taxa. On the other hand, Dörken et al. (2018), emphasizing terata in Pseudotaxus chienii, suggested that the aril there might represent a pair of modified fused leaves, although there is no vascularization (c.f. Phyllocladus); they start developing only when the ovule is already large. In other Taxaceae this structure is adnate to the ovule. See also Leslie et al. (2018) for ovule evolution.
Pollination Biology & Seed Dispersal. Fleshy disseminules occur throughout Taxaceae (see Leslie et al. 2017).
Bacterial/Fungal Associations. Taxol and related compounds are synthesized by Taxus and also by several fungi that either grow in the soil around the plant or are endophytes (Cassady et al. 2004 and references); the fungi may have acquired the ability to synthesize taxol from the plant (Strobel et al. 1996). Pestalotiopsis guepinii, which can synthesize taxol, is also endophytic in Wollemia (Araucariaceae), etc. (Strobel et al. 1997).
Chemistry, Morphology, etc.. (S)norcolaurine synthase activity is high in both Cephalotaxus and other Taxaceae; this might suggest that benzyisoquinoline alkaoids may be found here (Liscombe et al. 2005). Cephalotaxus contains some very distinctive alkaloids (Parry et al. 1980). Cuticle/epidermis micromorphology is quite extensive (Elpe et al. 201), as is leaf anatomy (Ghimire et al. 2014a), but they do not suggest broad relationships.
For male cones and their similarities, see Mundry and Mundry (2001). Taxaceae lack sacci on their pollen (Anderson & Owens 2006). The scales subtending the ovules of Austrotaxus are spiral.
For the morphology of Taxus and relatives, see Hart and Price (1990), for male reproductive structures, see Wang et al. (2008) and Dörken and Nimsch (2016), for male gametes, see Chamberlain (1935) and Singh (1978), for the megasporangiate cone, see André (1956) and Liang and Wang (1989), for embryology in general, see Chen and Wang (1990: sperm somewhat to very unequal in size), and for a general account, see Cope (1998).
Phylogeny. Page (1990) included Amentotaxus in Cephalotaxaceae, although he noted that affinities between the two were "somewhat enigmatic"; a family so delimited appears para- or polyphyletic to Taxaceae s. str., c.f. e.g. Price (2003), Hao et al. (2010), Leslie et al. (2018). Quinn et al. (2002) in a broad survey of Pinales found that Cephalotaxus, Torreya and relatives, and Taxus and relatives formed a tritomy in their unweighted rbcL and matK analyses; only when weighted were Cephalotaxaceae and Taxaceae separate. Price (2006) looked at variation in the same two genes and found weak support for Cephalotaxus as sister to [Amentotaxus + Torreya]; sampling overall was poor, but good for Taxaceae s.l., and support for the monophyly of Taxaceae s.l. was strong. These relationships were found by Wang et al. (2003) in analyses of trnL/F singly and when combined with rbcL data, but not in an analysis of rbcL alone, when Cephalotaxus alone was sister to all other Taxaceae; for the latter relationship, see also Rai et al. (2009) and Leslie et al. (2018), who found [Torreya + Amentotaxus] to be sister to other Taxeae. Analyzing RNAseq data, Majeed et al. (2018) found that a clade [A [T + C]] was srongly supported as being sister to the rest of the family; see also Y. Lu et al. (2014: [C [T + A]]; very different topologies were recovered in some analyses). For phylogenies, see also Cheng et al. (2000) and Ghimire and Heo (2014a: morphology only).
Möller et al. (2020) discuss relationships in Taxus; migration and hybridization have played major roles in shaping the evolution and distribution of the genus.
Classification. Cephalotaxaceae and Taxaceae have sometimes been separated (e.g. Hao et al. 2008) and this idea has also been supported recently by Majeed et al. (2018). Tribal rank seems adequate; the work of Rai et al. (2008a) also supports a broad circumscription of Taxaceae, as does that of Leslie et al. (2012).
Previous Relationships. Taxus has sometimes been considered quite distinct from all other conifers, and, as Taxopsida, supposedly being separate from Coniferopsida since pernaps the late Palaeozoic (Florin 1958, also Florin 1949, 1954; Miller 1999).
CUPRESSACEAE Bartling - Back to Cupressales
(Root stele pentarch); wood rays <10 cells tall; (stem apex with tunica/corpus construction); xylem or phloem resin ducts inducible [in separate clades]); branchlets deciduous, leaves shed along with them [?level]; foliar resin canal single, abaxial to vascular bundle [check Contreras]; leaves ± amphistomatous, stomata arranged (±) longitudinally; pollen cones in clusters/pseudowhorls; (1-)2-10(-14) microsporangia/microsporophyll; pollen shed at 2-cell stage; male gametophyte without sterile cell, gametes with separate cell walls; bract and seed scale ± evident, ovules develop on the base of the subtending scale [= subaxillary]; seed with lateral wing; n = 11; chloroplast large inverted repeat 0, smaller IR duplicating the trnQ gene, mitochondrial transmission paternal.
30 [list - as subfamilies]/133. Esp. Northern Hemisphere, more scattered in south temperate regions. [Photos - Collection.]
Age. Mao et al. (2012) offer an age of (259-)219, 211(-168) Ma for crown Cupressaceae, while estimates in Yang et al. (2012) are (231-)229, 197(-186) My and in Y. Lu et al. (2014) ca 197.1 Ma; ca 171 Ma is suggested by Ran et al. (2018a) and (192.2-)171(-146.4) my by Leslie et al. (2018).
Jurassic fossils placed in crown-group Cupressaceae in morphological analyses, specifically in a clade along with Cunninghamia and Taiwania, in turn part of a pentatomy that made up the family as a whole (Escapa et al. 2008), are known from both Yorkshire, England - Elatides, Bajocian, ca 169 Ma (Harris 1943), and Chubut, Argentina - Austrohamia, also early Jurassic 187-183 Ma (and also known from Inner Mongolia!!) (Escapa et al. 2008; Bodnar & Escapa 2016; Contreras et al. 2019).
1. Cunninghamioideae Silba
Leaves linear, twisted at the base, (margin denticulate), (hypostomatous), narrowed at base, petiole 0; pollen cones 16-many, growth of shoot continuing later [= proliferating]; 3(-6) microsporangia/microsporophyll; ovuliferous cone initially pendulous, bract scales lacking adaxial stomata; ovuliferous scale soon degenerating [small, <1/3 length of cone scale, free, margin initially 3-lobed], ovules 2-3(-6)/scale; seeds ca 2/bract scale; nuclear genome [1C] ca 12.5 pg.
1/2. Laos, Vietnam, Southern China, Taiwan (map: from Farjon & Filer 2013).
Synonymy: Cunninghamiaceae Siebold & Zuccarini
[Taiwanioideae [Athrotaxidoideae [Sequoioideae [Taxodioideae [Callitroideae + Cupressoideae]]]]]: extensions of torus in tracheidal pit; ovuliferous shoot not proliferating.
Age. The age of this clade is estimated to be (179.9-)157.1(-132.5) Ma (Leslie et al. 2018).
2. Taiwanioideae L. C. Li
Leaves shortly linear, amphistomatous, not narrowed at base, petiole 0; pollen cones 2-7, axillary; bract scales with adaxial stomata, not narrowed at the base; ovuliferous cone initially erect, ovuliferous scale invisible; ovules (1-)2/bract scale, subaxillary; seeds ca 2/bract scale; nuclear genome [1C] ca 11.5 pg.
1/2. Northern Myanmar and Vietnam, S.W. China, Taiwan.
Synonymy: Taiwaniaceae Hayata
[Athrotaxidoideae [Sequoioideae [Taxodioideae [Callitroideae + Cupressoideae]]]]: pollen surface microverrucate/papillate.
Age. This clade is some (167.7-)145.8(-121.9) Ma (Leslie et al. 2018).
3. Athrotaxidoideae L. C. Li
Leaves scale-like to linear, not narrowed at base, petiole 0; pollen cone 1, terminal; ovuliferous cone initially ?, ovuliferous scale soon degenerating, ovules 1-9/bract scale, adaxial thickening developing on adaxial side of bract scale above ovules after pollination [?= ovuliferous scale]; nuclear genome [1C] ca 10 pg.
Synonymy: Athrotaxidaceae Doweld
[Sequoioideae [Taxodioideae [Callitroideae + Cupressoideae]]]: ?wood anatomy.
Age. This clade may be a mere 66.4 Ma (Magallón et al. 2013) or (159-)135(-114) Ma (Leslie et al. 2018).
4. Sequoioideae Quinn
(Plant deciduous); xylem with inducible axial resin canals; phloem with constitutive ?radial resin canals; shoots abscise [= cladoptosis]; (leaves opposite - M); ovuliferous cone initially erect; bract scales (opposite - Metasequoia), ovuliferous scale invisible; ovules 1-10/bract scale, in two (three - Sequoiadendron) series, adaxial thickening developing above ovules after pollination; pollination droplets coalescing; ovuliferous scales apparent after pollination; (early embryo lacking free-nuclear stage - Sequoia); nuclear genome [1C] 9.5-10.5(-29 - Sequoia) pg. M = Metasequoia.
3/3: China, Pacific North America.
Synonymy: Metasequoiaceae Hu & W. C. Cheng, Sequoiaceae Luersson
[Taxodioideae [Callitroideae + Cupressoideae]]: ovules axillary to cone [= bract] scale, straight at maturity.
Age. This clade is around 104 Ma (Crisp et al. 2011b) or (143-)120(-101) Ma (Leslie et al. 2018).
5. Taxodioideae K. Koch
(Plant deciduous); iso/chamaecydin + [terpenoids]; (phloem with inducible axial resin canals); shoots ultimately abscise [cladoptosis]; ovuliferous cone initially pendulous (horizontal), ovuliferous scale late-developing, conspicuous after pollination, ovules 1-2(-5)/cone scale; (seed not winged - Taxodium); nuclear genome [1C] 9-10.5 pg.
3/4: East Asia, E. North America, Mexico.
Age. Crown-group Taxodioideae are (101.7-)82.2(-69) Ma (Leslie et al. 2018).
It has been suggested that the resin that formed the ce 98.8 Ma amber deposits in Myanmar that are so rich in fossils was produced by Taxodiaceae (Cognato & Grimaldi 2009).
Synonymy: Cryptomeriaceae Gorozhankin, Taxodiaceae Saporta
[Callitroideae + Cupressoideae]: fertile cone scales whorled, ovuliferous scale 0. (map: from Florin 1963, 1966; Farjon 2005c). [Photos - Collection.]
Age. This clade is perhaps 101 Ma (Crisp et al. 2011b), (163-)148.4, 127(-105) Ma (Crisp et al. 2018), or (183-)153(-124) or (193.2-)178.2-143.0(-134.3) Ma (Mao et al. 2012); see Z.-Y. Yang et al. (2012) for more dates.
6. Callitroideae Saxton
(Leaves opposite); ovuliferous cone erect to pendulous, fertile cone scales 2 whorls, (central columella +); ovules 1-2(-3)/scale, (in two rows).
10/32: Callitris (15). Southern Hemisphere.
Age. The crown-group age of Callitroideae may be a little over 115 Ma (Crisp et al. 2018), around 98 Ma (Crisp et al. 2011b), (102.1-)81.7(-62.5) Ma (Leslie et al. 2018) or 71.9-51.9 Ma (Leslie et al. 2012: other estimates older).
Synonymy: Actinostrobaceae Lotsy, Callitridaceae Seward, Diselmaceae A. V. Bobrov & Melikian, Fitzroyaceae A. V. Bobrov & Melikian, Libocedraceae Doweld, Neocallitropsidaceae Doweld, Pilgerodendraceae A. V. Bobrov & Melikian, Widdringtoniaceae Doweld
7. Cupressoideae Sweet
((Iso)chamaecydin +), (syringyl lignin + - Tetraclinis); phloem with inducible axial resin canals; nodes 1:2; leaves opposite [not in some seedlings], scale-like to linear; pollen cones often on elongated axes; (1-)2-10(-14) microsporangia/microsporophyll; fertile cone scales 2-6 whorls, (fleshy - Juniperus), (central columella 0); ovules 1-9(-many)/scale, in 1-6 rows (ovules 12< scale), (ovule 1/cone, terminal or not - Microbiota); (cone fleshy, not opening); seeds (not winged); cotyledons (-9(-15)), nuclear genome [1C] 9-14(-38 - Juniperus) pg.
29/131: Juniperus (67), Cupressus (12). Esp. Northern Hemisphere, also N.E. Africa.
Synonymy: Arceuthidaceae A. V. Bobrov & Melikian, Juniperaceae Berchtold & J. Presl, Limnopityaceae Hayata, Microbiotaceae Nakai, Platycladaceae A. V. Bobrov & Melikian, Tetraclinaceae Hayata, Thujaceae Burnett, Thujopsidaceae Bessey
Evolution: Divergence & Distribution. For the Middle Jurassic ca 173 Ma fossil Scitistrobus duncaanensis, see Spencer et al. (2015); it has some similarities with Voltziales, e.g. the ovules are attached to to the free tips of the ovuliferous scale, but in the compact cone, etc., it is assignable to Cupressaceae, and that is where Spencer et al. place it. There is a rich Cretaceous fossil record of cupressoid plants like Elatides and Hughmillerites that have ovuliferous scales and spiral cone scales, plesiomorphic features, and several of these fossils may form a clade with extant Cunninghamia (sister to all other Cupressaceae), even if, as might be expected with fossil material, support is not overwhelming (Shi et al. 2014). The fossil record of such plants from the northern hemisphere and stretching back to the Late Jurassic ca Ma (Rothwell et al. 2011), suggests that they formed an important early radiation in Cupressaceae (e.g. Shi et al. 2014; Atkinson et al. 2014). Cunninghamia itself is known from the Late Cretaceous (Buczkowski et al. 2015 and references). Herrera et al. (2016) review fossils that can be linked to Cunninghamia and Taiwania (basal in Cupressaceae).
The distribution of extant Cupressoideae is predominantly northern and that of Callitroideae are predominantly southern, a vicariance pattern that may reflect the break-up of Pangaea (Mao et al. 2012; X.-Q. Wang & Ran 2014 for a summary). The split between the two is dated to (183-)153(-124) Ma or (193.2-)178.2-143.0(-134.3) Ma (Mao et al. 2012; see Z.-Y. Yang et al. 2012 for more dates). However, there has been much E.-W. and some N.-S. movement even of extant genera, thus the northern Sequoioideae are known from rocks from the Upper Cretaceous of Queensland (Peters & Christophel 1978: its leaves are like those of the southern Arthrotaxis). The southern Callitroideae seem to have been particularly peripatetic. Thus Widdringtonia is found in 97 Ma rocks from North America (McIver 2001) - an estimate of the stem-group age of Widdringtonia is ca 94 Ma (Crisp et al. 2011b). The largely New Guinean Papuacedrus is known from Eocene deposits in Argentinia ca 52 Ma, and also from Antarctica, New Zealand, and southern Australia (Wilf et al. 2009); see also Kooyman et al. (2014) and Crisp et al. (2018: this and other genera), also Fagaceae for discussion about such distributions. The stem-group age of Libocedrus, now known only from New Zealand and New Caledonia, and with fossils only from the Antipodes, has been estimated to be (97-)70(-63) Ma, suggesting that it could have been on Zealandia as it broke off from Pangaea, and that both New Zealand and New Caledonia have been long-emergent (Wallis & Jorge 2018: the reference there is to Crisp et al. 2011b, but it would seem to be apocryphal, and the stem-group age of Libocedrus (inc. Pilgerodendron) is ca 95 Ma in Crisp et al. 2011b). Wilf and Escapa (2014) suggest some fossil-based dates within this clade. Although Ma et al. (2012) emphasized the importance of vicariance in explaining many distribution patterns in Cupressaceae, expecially in Callitroideae, but increased sampling, etc., suggests that some of these are better explained by dispersal events (Crisp et al. 2018).
In Callitroideae in particular there was much Caenozoic extinction, probably around the Oligocene-Miocene boundary ca 23 Ma, and diversification in extant genera can be dated to after this period (Crisp & Cook 2011; Mao et al. 2012; Pittermann et al. 2012); four of the five genera growing in Australia at the beginning of the Oligocene went extince (Crisp et al. 2018). Arid-adapted members of Callitroideae diversified some 52.6-34 Ma (Pittermann et al. 2012); Leslie et al. (2012) suggest that diversification began a little before the K/T boundary ca 65.5 Ma and continued throughout the Caenozoic. Pittermann et al. (2012; see also Edwards & Donoghue 2013) suggested that Juniperus and Cupressus s.l., most of whose species have become adapted to dry conditions and have developed cavitation-resistant xylem, diverged 38.7-32 Ma, while figures in Leslie et al. (2012) are 53-33 Ma (and some much older). Mao et al. (2010; see also Adams & Schwarzbach 2013) throught that there was E->W migration across the North Atlantic Land Bridge in Juniperus, initially Eurasian in distribution, around 47-30.3 Ma (Mao et al. 2010 for more dates).
If the basal topology of the family, [Cunninghamioideae [Taiwanioideae [Athrotaxidoideae [....]]], is confirmed (see below), then features common to these genera (e.g. Atkinson et al. 2014) will be features for the family as a whole, while loss of ovuliferous scales and other characters are best placed within the family and are not apomorphies for it (see above). For apomorphies for basal members of Cupressaceae, somewhat adjusted above, see Schulz and Stützel (2007: unfortunately Juniperus etc. not included); for wood anatomy and phylogeny, see Román-Jordán et al. (2016).
Ecology & Physiology. Biomass estimates for forests with Sequoia sempervirens are 2.3 x 106 kg ha-1 (Franklin & Dryness 1973).
For details of xylem function in relation to the environment in Cupressaceae, see Pittermann et al. (2010). The initial preferences for the family were for mesic conditions, but Pittermann et al. (2012) noted that a number of species of both Cupressoideae and Callitroideae had evolved drought resistance, their xylem-specific conductivity and stomatal conductances being lower, and also their CO2 assimilation rates were much reduced. The cost of these adaptations was slow growth.
Resin from various Cupressaceae has formed amber in various parts of the world since the Late Cretaceous (Seyfullah et al. 2018).
Pollination Biology & Seed Dispersal. For the active and irreversible withdrawal of pollination drops within half an hour of deposition of pollen, see Dörken and Jagel (2014); this happens also when there is pollen from other Cupressaceae in the pollination drops, but not when there is pollen from angiosperms or Pinus. In Cupressus the pollination droplets of adjacent ovules may become confluent (Jagel & Stützel 2001), a sort of gymnospermous extragynoecial compitum.
For monoecy, dioecy, etc., see Jagel and Dörken (2015a). There is paternal apomixis in Cupressus dupreziana, unknown in any other seed plant. Here the embryo develops from unreduced male gametes (Pichot et al. 2000, 2001), but there are other forms of androgenesis, asexual reproduction of the male nuclear genome, as in Solanaceae, etc. (Hedtke & Hillis 2011).
For details of seed morphology, dispersal, etc., and their evolution, see Contreras et al. (2016); dry and winged (the wings develop from the ovules) seeds are common, but Juniperus is noted for its fleshy disseminules. Serotiny has evolved five times here, and it is associated with the evolution of larger seed cones (Swarup et al. 2020).
Bacterial/Fungal Associations. The telial stage of Gymnosporangium rust is common on some Cupressaceae, especially Juniperus, while the aecial stage characterises Rosaceae-Maloideae (Savile 1979b).
Genes & Genomes. See Zonneveld (2014) for discussion of genome size in taxa like Juniperus; there are connections with polyploidy, as elsewhere in Pinales. The ycf1/2 area discussed below is evidence of a very ancient introgression event some 60-40 Ma (Zhu et al. 2018).
Cryptomeria japonica has a much reduced chloroplast inverted repeat containing only a few genes (Hirao et al. 2008), and the loss of this repeat in Cupressaceae is connected with the fact that the plastome size is often small in Cupressaceae, as in Callitris where it is only about 121 kb (Wu & Chaw 2016). For the organization of the chloroplast genome in the whole family, see C.-S. Wu and Chaw (2016) and Qu et al. (2017) and references. Wu and Chaw (2016) noted the frequency of inversions within this clade - there are some 28 - compared to other conifers (Araucariaceae, for example have none, Taxaceae and Podocarpaceae only one).
Chemistry, Morphology, etc.. Characters of wood anatomy may yield phylogenetically interesting variation (Schulz & Stützel 2007), but state delimitation is difficult; for epidermal morphology, see Ma et al. (2009).
Proliferation of the ovuliferous cones is common, and the distribution of this feature may be of phylogenetic interest (Schulz & Stützel 2007). Scales on the ovuliferous cones are wedge-shaped to peltate. Most Cupressaceae lack ovuliferous scales, having only bract (= cone) scales (Zhang et al. 2004; see also Farjon 2005c; Jagel & Dörken 2015a), but Cryptomeria has several "teeth" on the ovuliferous scale and some other subfamilies have structures that appear to be much reduced ovuliferous scales (see also Schulz & Stützel 2007). However, the ovuliferous scales and ovules may be interpreted as the products of serial buds in the axils of the bract scales, the oldest buds being furthest away from the bract scale, rather as are sometimes found in the vegetative part of the plant (Dörken & Rudall 2018: note interpretation of epidermal layer surrounding the ovule in terata). In some Cupressoideae the ovules are not axillary, indeed, the variation in ovule number and position within the cone is considerable (Schulz et al. 2003; Jagel & Dörken 2015a). There is substantial variation in how the cone develops, the seeds being enclosed in various ways (e.g. Jagel & Dörken 2014; Dörken & Rudall 2018) and varying considerably in both their numbers and positional relationships to the bract scales (e.g. Jagel & Dörken 2015a).
For a monograph (and far more) see Farjon (2005c); general information can be found in the Gymnosperm Database and see Contreras et al. (2019) for information about basal taxa, both living and dead. For some terpenoids, see Otto et al. (2002), and for cone and ovule morphology, see e.g. Lemoine-Sébastien (1968a, b), Takaso and Tomlinson (1989, 1990, 1992), Jagel and Stützel (2001), Farjon and Garcia (2003 and references) and Jagel and Dörken (2014, 2015a, b).
Phylogeny. Page (1990) suggested that there were "fundamental" differences between Cupressaceae and Taxodiaceae in the morphology of their reproductive parts, but in the tree of Quinn et al. (2002) Cupressaceae s. str. were embedded in a paraphyletic Taxodiaceae which formed a basal grade. Phenetic analyses had earlier suggested the combination of the two (Eckenwalder 1976), and they are combined in Farjon (2005c). For relationships within Cupressaceae, see Brunsfeld et al. (1994), Gadek et al. (2000), Kusumi et al. (2000), Farjon et al. (2002), Brunsfeld et al. (2003), and Little et al. (2004). The basic phylogenetic structure of the family is probably [Cunninghamioideae [Taiwanioideae [Athrotaxidoideae [Sequoioideae [Taxodioideae [Cupressoideae + Callitroideae]]]]]] (Mao et al. 2012: much support strong; Sen et al. 2016; Z.-D. Chen et al. 2016: no Athrotaxis), but Z.-Y. Yang et al. (2012) found the subfamilial order in the middle of the tree to be [... [Sequoioideae [Athrotaxidoideae [...]]]] while Y. Lu et al. (2014) recovered a clade [Athrotaxidoideae + Sequoioideae], however, other major groupings were similar. Thus the phylogeny is usually strongly pectinate basally, although in some morphological analyses two or more members of the first three branches may unite to form a single clade (e.g. Rothwell et al. 2011).
Within Callitroideae, Callitris is paraphyletic, although morphological (Piggin & Bruhl 2010) and molecular (Pye et al. 2003) studies do not agree over the extent of the paraphyly (see also e.g. Crisp et al. 2018). Papuacedrus is probably sister to the rest of the subfamily; the position of Austrocedrus is uncertain (Crisp et al. 2018; see also Y. Lu et al. 2014).
Within Cupressoideae, for relationships in Juniperus, see Mao et al. (2010) and Adams and Schwarzbach (2013). Cupressus has turned out to be polyphyletic and is now restricted to the Old World (Xiang & Li 2005; especially Little 2006). Terry and Adams (2015: sampling slight) suggest relationships in this area are [Cupressus [Juniperus [Hesperocyparis, Callitropsis, Xanthocyparis]]] (see also Y. Lu et al. 2014; Mao et al. 2018), although chloroplast data were a bit wayward. Indeed, Zhu et al. (2018) found that a ca 15 kb part of the plastome, the ycf1/2 area, helped to produce the conflicting relationships that have been obtained in this area (e.g. Farjon et al. 2002; Little et al. 2004; Mao et al. 2010; Terry & Adams 2015 and references), inclusion of that segment in plastome analyses giving a [Juniperus + Cupressus] clade, while in other analyses the clade [Cupressus [Xanthocyparis [Callitropsis + Hesperocyparis]]] was recovered. Lu et al. (2014) found that the clade [Thuja + Thujopsis] was sister to the rest of the subfamily.
Classification. Having 24 family names for ca 30 genera says a lot about the past. For generic limits around Cupressus, which has turned out to be polyphyletic, see Price and Adams (2009), Little (2006) and Zhu et al. (2018) and for those around Callitris, see Pye et al. 2003) and Piggin and Bruhl (2010). For an account of Cupressus, see Adams (2010).
Botanical Trivia. Juniperus grows at some 4,900 m altitude on the Tibetan Plateau and forms the highest known forest (Opganoorth et al. 2010), but c.f. the Andean Polylepis (Rosaceae)).
The tallest living tree in the world is a coast redwood Sequoia sempervirens, at about 115.5 metres (379 feet), although the giant redwood (Sequoiadendron giganteum is larger and Eucalyptus regnans was almost certainly taller. Sequoia also has the longest fusiform initials known, ca 9 mm long, over five times he length of fusiform initials in angiosperms (Philipson et al. 1961).