EMBRYOPSIDA Pirani & Prado

Gametophyte dominant, independent, multicellular, thalloid, with single-celled apical meristem, showing gravitropism; rhizoids +, unicellular; acquisition of phenylalanine lysase [PAL], flavonoids [absorbtion of UV radiation], phenylpropanoid metabolism [lignans], xyloglucans +; plant poikilohydrous [protoplasm dessication tolerant], ectohydrous; cuticle +; cell wall also with (1->3),(1->4)-ß-D-MLGs [Mixed-Linkage Glucans], lignin +; chloroplasts per cell, lacking pyrenoids; glycolate metabolism in leaf peroxisomes [glyoxysomes]; centrioles in vegetative cells 0, metaphase spindle anastral, predictive preprophase band of microtubules, phragmoplast + [cell wall deposition spreading from around the spindle fibres], plasmodesmata +; antheridia and archegonia jacketed, stalked; spermatogenous cells monoplastidic; blepharoplast, bicentriole pair develops de novo in spermatogenous cell, associated with basal bodies of cilia [= flagellum], multilayered structure [4 layers: L1, L4, tubules; L2, L3, short vertical lamellae] + 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; oogamy; sporophyte dependent on gametophyte, embryo initially surrounded by haploid gametophytic tissue, plane of first division horizontal [with respect to long axis of archegonium/embryo sac], suspensor/foot +, cell walls with nacreous thickenings; sporophyte multicellular, with at least transient apical cell [?level], sporangium +, single, dehiscence longitudinal; meiosis sporic, monoplastidic, microtubule organizing centre associated with plastid, cytokinesis simultaneous, preceding nuclear division, sporocytes 4-lobed, with a quadripolar microtubule system; spores in tetrads, sporopollenin in the spore wall, wall with several trilamellar layers [white-line centred layers, i.e. walls multilamellate]; nuclear genome size <1.4 pg, LEAFY gene present, ethylene involved in cell elongation; chloroplast genome with close association between trnLUAA and trnFGAA genes.

Many of the bolded characters in the characterization above are apomorphies of subsets 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.


Abscisic acid, ?D-methionine +; sporangium with seta, seta developing from basal meristem [between epibasal and hypobasal cells], sporangial columella + [developing from endothecial cells]; stomata +, anomocytic, cell lineage that produces them with symmetric divisions [perigenous]; underlying similarities in the development of conducting tissue and in rhizoids/root hairs; spores trilete; polar transport of auxins and class 1 KNOX genes expressed in the sporangium alone; shoot meristem patterning gene families expressed; MIKC, MI*K*C* and class 1 and 2 KNOX genes, post-transcriptional editing of chloroplast genes; gain of three group II mitochondrial introns.

[Anthocerophyta + Polysporangiophyta]: archegonia embedded/sunken in the gametophyte; sporophyte long-lived, chlorophyllous; sporophyte-gametophyte junction interdigitate, sporophyte cells showing rhizoid-like behaviour.


Sporophyte branched, branching apical, dichotomous; sporangia several, each opening independently; spore walls not multilamellate [?here].


Photosynthetic red light response; plant homoiohydrous [water content of protoplasm relatively stable]; control of leaf hydration passive; (condensed or nonhydrolyzable tannins/proanthocyanidins +); sporophyte soon independent, dominant, with basipetal polar auxin transport; vascular tissue +, sieve cells + [nucleus degenerating], tracheids +, in both protoxylem and metaxylem, plant endohydrous; endodermis +; root xylem exarch [development centripetal]; stem with an apical cell; branching dichotomous; leaves spirally arranged, blades with mean venation density 1.8 mm/mm2 [to 5 mm/mm2]; sporangia adaxial on the sporophyll, derived from periclinal divisions of several epidermal cells, wall multilayered [eusporangium]; columella 0; tapetum glandular; gametophytes exosporic, green, photosynthetic; basal body 350-550 nm long, stellate array in transition region initially joining microtubule triplets; placenta with single layer of transfer cells in both sporophytic and gametophytic generations, embryonic axis not straight [root lateral with respect to the longitudinal axis; plant homorhizic].


Sporophyte branching ± indeterminate; lateral roots +, endogenous, root apex multicellular, root cap +; (endomycorrhizal associations + [with Glomeromycota]); tracheids with scalariform-bordered pits; leaves with apical/marginal growth, venation development basipetal, growth determinate; sporangia borne in pairs and grouped in terminal trusses, dehiscence longitudinal, a single slit; cells polyplastidic, microtubule organizing centres not associated with plastids, diffuse, perinuclear; blepharoplasts +, paired, with electron-dense material, centrioles on periphery, male gametes multiciliate; chloroplast long single copy ca 30kb inversion [from psbM to ycf2]; LITTLE ZIPPER proteins.


Sporophyte woody; lateral root origin from the pericycle; branching lateral, meristems axillary; cork cambium + [producing cork abaxially], vascular cambium bifacial [producing phloem abaxially and xylem adaxially].


Plant evergreen; nicotinic acid metabolised to trigonelline, (cyanogenesis via tyrosine pathway); primary cell walls rich in xyloglucans and/or glucomannans, 25-30% pectin [Type I walls]; lignins derived from (some) sinapyl and particularly coniferyl alcohols [hence with p-hydroxyphenyl and guaiacyl lignin units, so no Maüle reaction]; root stele with xylem and phloem originating on alternate radii, not medullated [no pith], cork cambium deep seated; shoot apical meristem interface specific plasmodesmatal network; stem with vascular cylinder around central pith [eustele], phloem abaxial [ectophloic], endodermis 0, xylem endarch [development centrifugal]; 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; leaves with single trace from vascular sympodium [nodes 1:1]; stomatal pore with active opening in response to leaf hydration, control by abscisic acid, metabolic regulation of water use efficiency, etc.; buds axillary (not associated with all leaves), exogenous; prophylls two, lateral; leaves with petiole and lamina, development basipetal, blade simple; plant heterosporous, sporangia borne on sporophylls, sporophylls spiral; microsporophylls aggregated in indeterminate cones/strobili; grains monosulcate, aperture in ana- position [distal], exine and intine homogeneous; ovules unitegmic, parietal tissue 2+ cells across, megaspore tetrad linear, functional megaspore single, chalazal, lacking sporopollenin, megasporangium indehiscent; pollen grains land on ovule; gametophytes dependent on sporophyte; apical cell 0, male gametophyte development initially endosporic, tube developing from distal end of grain, gametes two, developing after pollination, with cell walls; female gametophyte endosporic, initially syncytial, walls then surrounding individual nuclei; embryo cellular ab initio, endoscopic, plane of first cleavage of zygote transverse, suspensor +, short-minute, embryonic axis straight [shoot and root at opposite ends; plant allorhizic], cotyledons 2; plastid transmission maternal; ycf2 gene in inverted repeat, whole nuclear genome duplication [zeta duplication], two copies of LEAFY gene, PHY gene duplications [three - [BP [A/N + C/O]] - copies], nrDNA with 5.8S and 5S rDNA in separate clusters; mitochondrial nad1 intron 2 and coxIIi3 intron and trans-spliced introns present.


Lignans, O-methyl flavonols, dihydroflavonols, triterpenoid oleanane, apigenin and/or luteolin scattered, [cyanogenesis in ANITA grade?], S [syringyl] lignin units common [positive Maüle reaction - syringyl:guaiacyl ratio more than 2-2.5:1], and hemicelluloses as xyloglucans; root apical meristem intermediate-open; root vascular tissue oligarch [di- to pentarch], lateral roots arise opposite or immediately to the side of [when diarch] xylem poles; origin of epidermis with no clear pattern [probably from inner layer of root cap], trichoblasts [differentiated root hair-forming cells] 0, exodermis +; shoot apex with tunica-corpus construction, tunica 2-layered; reaction wood ?, associated gelatinous fibres [g-fibres] with innermost layer of secondary cell wall rich in cellulose and poor in lignin; starch grains simple; primary cell wall mostly with pectic polysaccharides, poor in mannans; tracheid:tracheid [end wall] plates with scalariform pitting, wood parenchyma +; sieve tubes enucleate, sieve plate with pores (0.1-)0.5-10< µm across, cytoplasm with P-proteins, cytoplasm not occluding pores of sieve plate, companion cell and sieve tube from same mother cell; sugar transport in phloem passive; nodes 1:?; stomata brachyparacytic [ends of subsidiary cells level with ends of pore], outer stomatal ledges producing vestibule, reduction in stomatal conductance to increasing CO2 concentration; lamina formed from the primordial leaf apex, margins toothed, development of venation acropetal, overall growth ± diffuse, venation hierarchical-reticulate, secondary veins pinnate, veins (1.7-)4.1(-5.7) mm/mm2, endings free; most/all leaves with axillary buds; flowers perfect, pedicellate, ± haplomorphic; protogynous; parts spiral [esp. the A], free, numbers unstable, development in general centripetal; P +, members each with a single trace, outer members not sharply differentiated from the others, not enclosing the floral bud; A many, filament not sharply distinguished from anther, stout, broad, with a single trace, anther introrse, tetrasporangiate, sporangia in two groups of two [dithecal], sporangium pairs dehiscing longitudinally by a common slit, ± embedded in the filament, walls with at least outer secondary parietal cells dividing, endothecium +, endothecial cells elongated at right angles to long axis of anther; (tapetum glandular), cells binucleate; microspore mother cells in a block, microsporogenesis successive, walls developing by centripetal furrowing; pollen subspherical, tectum continuous or microperforate, ektexine columellate, endexine lamellate only in the apertural regions, thin, compact; nectary 0; carpels present, superior, free, several, ascidiate, with postgenital occlusion by secretion, stylulus at most short [shorter than ovary], hollow, cavity not lined by distinct epidermal layer, stigma ± decurrent, carinal, dry [not secretory]; ovules few [?1]/carpel, marginal, anatropous, bitegmic, micropyle endostomal, outer integument 2-3 cells across, often largely subdermal in origin, inner integument 2-3 cells across, often dermal in origin, parietal tissue 1-3 cells across [crassinucellate], nucellar cap?; megasporocyte single, hypodermal, functional megaspore, chalazal, lacking cuticle; female gametophyte four-celled [one module, nucleus of egg cell sister to one of the polar nuclei]; supra-stylar extra-gynoecial compitum +; ovule not increasing in size between pollination and fertilization; pollen grains land on stigma, bicellular at dispersal, mature male gametophyte tricellular, germinating in less than 3 hours, pollen tube elongated, unbranched, growing between cells, growth rate (20-)80-20,000 µm/hour, apex of pectins, wall with callose, lumen with callose plugs, penetration of ovules via micropyle [porogamous], whole process takes ca 18 hours, distance to first ovule 1.1-2.1 mm; male gametes lacking cell walls, cilia 0, siphonogamy; double fertilization +, ovules aborting unless fertilized; P deciduous in fruit; mature seed much larger than ovule when fertilized, small [], dry [no sarcotesta], exotestal; endosperm diploid, cellular, heteropolar [micropylar and chalazal domains develop differently, first division oblique, micropylar end initially with a single large cell, divisions uniseriate, chalazal cell smaller, divisions in several planes], copious, oily and/or proteinaceous; dark reversal Pfr → Pr; Arabidopsis-type telomeres [(TTTAGGG)n]; nuclear genome size <1.4 pg [1 pg = 109 base pairs], whole nuclear genome duplication [epsilon duplication]; protoplasm dessication tolerant [plant poikilohydric]; ndhB gene 21 codons enlarged at the 5' end, single copy of LEAFY and RPB2 gene, knox genes extensively duplicated [A1-A4], AP1/FUL gene, paleo AP3 and PI genes [paralogous B-class genes] +, with "DEAER" motif, SEP3/LOFSEP and three copies of the PHY gene, [PHYB [PHYA + PHYC]].

[NYMPHAEALES [AUSTROBAILEYALES [[CHLORANTHALES + MAGNOLIIDS] [MONOCOTS [CERATOPHYLLALES + EUDICOTS]]]]]: wood fibres +; axial parenchyma diffuse or diffuse-in-aggregates; pollen monosulcate [anasulcate], tectum reticulate-perforate [here?]; ?genome duplication; "DEAER" motif in AP3 and PI genes lost, gaps in these genes.

[AUSTROBAILEYALES [[CHLORANTHALES + MAGNOLIIDS] [MONOCOTS [CERATOPHYLLALES + EUDICOTS]]]]: vessel elements with scalariform perforation plates in primary xylem; essential oils in specialized cells [lamina and P ± pellucid-punctate]; tension wood +; tectum reticulate; anther wall with outer secondary parietal cell layer dividing; carpels plicate; nucellar cap + [character lost where in eudicots?]; 12BP [4 amino acids] deletion in P1 gene.

[[CHLORANTHALES + MAGNOLIIDS] [MONOCOTS [CERATOPHYLLALES + EUDICOTS]]] / MESANGIOSPERMAE: benzylisoquinoline alkaloids +; sesquiterpene synthase subfamily a [TPS-a] [?level], polyacetate derived anthraquinones + [?level]; outer epidermal walls of root elongation zone with cellulose fibrils oriented transverse to root axis; P more or less whorled, 3-merous [possible position]; pollen tube growth intra-gynoecial; embryo sac bipolar, 8 nucleate, antipodal cells persisting; endosperm triploid.

[MONOCOTS [CERATOPHYLLALES + EUDICOTS]]: (extra-floral nectaries +); (veins in lamina often 7-17 mm/mm2 or more [mean for eudicots 8.0]); (stamens opposite [two whorls of] P); (pollen tube growth fast).

[CERATOPHYLLALES + EUDICOTS]: ethereal oils 0.

EUDICOTS: (Myricetin, delphinidin +), asarone 0 [unknown in some groups, + in some asterids]; root epidermis derived from root cap [?Buxaceae, etc.]; (vessel elements with simple perforation plates in primary xylem); nodes 3:3; stomata anomocytic; flowers (dimerous), cyclic; protandry common; K/outer P members with three traces, ("C" +, with a single trace); A few, (polyandry widespread, initial primordia 5, 10, or ring, ± centrifugal), filaments fairly slender, anthers basifixed; microsporogenesis simultaneous, pollen tricolpate, apertures in pairs at six points of the young tetrad [Fischer's rule], cleavage centripetal, wall with endexine; G with complete postgenital fusion, stylulus/style solid [?here]; seed coat?

[PROTEALES [TROCHODENDRALES [BUXALES + CORE EUDICOTS]]]: (axial/receptacular nectary +).

Age. The approximate age for this node is 191 m.y. (Wu et al. 2014) or only 130.3 m.y.o. (Magallón et al. 2015). In many phylogenies Sabiaceae are adjacent to other members of the order along the eudicot spine, but whatever the topology, ages are rather younger. Estimates for a topology [Proteales [Sabiales [Buxales...]]] range from (143-)129, 126(-116) m.y. (Bell et al. 2010 for details), while Xue et al. (2012) estimate (126.4-)121.4(-110.2) m.y., Naumann et al. (2013) around 124.8 m.y., and Magallón et al. (2013) about 121.5 m.y.. Wikström et al. (2001) estimated (150-)144-130(-124) m.y. for the stem Nelumbo, etc., clade and (145-)140, 128(-123) m.y. for stem-group Sabiaceae; Anderson et al. (2005) dated stem group Sabiaceae to 122-118 m.y.a., and it would be slightly older than the stem Nelumbo, etc., clade.

Evolution. Divergence & Distribution. Endress (2011a) suggested that syncarpy might be a key innovation somewhere around here; optimization on the tree is not easy. Positioning of other apomorphies is also difficult. Although the androecial feature "stamens numerous, but then usually fasciculate and/or centrifugal" is placed at the [Rosids et al. + Asterids et al.] / Pentapetalae node, there is no particular reason why it should not be placed here. If CRABSCLAW expression is found in the nectaries of Sabiaceae and Proteaceae, this, to could be placed at this node (and it would also be interesting to look at what is going on in Buxaceae, too); along the same lines, sucrose synthesis and secretion is similar in the floral nectaries of the Brassicaceae and Solanaceae examined, which are extrastaminal and gynoecial nectaries respectively (Lin et al. 2014). See also the Pentapetalae page.

Chemistry, Morphology, etc. For the distinction between gynoecial (supposedly asterids only) and receptacular nectaries, see Smets (1988) and Smets et al. (2003); for a general survey of nectaries, see Bernadello (2007). Nectary vascularization can vary between quite closely related taxa (e.g. Saxena 1973; de Paula et al. 2011).

PROTEALES Berchtold & J. Presl  Main Tree.

Lamina margin serrate, ?tooth morphology; stigma dry; ovules 1-2/carpel, apical, pendulous, apotropous; seed coat?; endosperm development?, slight or 0, embryo long. - 4 families, 85 genera, 1710 species.

Age. Magallón and Castillo (2009) suggest dates of ca 122.8 and 123.6 m.y. for the crown-group age of this clade while the age in Magallón et al. (2015) is about 127.5 m.y., but the estimate in Z. Wu et al. (2014), at ca 189 m.y.a., is considerably older.

Note: Possible apomorphies are in bold. However, the actual level at which many of these features, particularly the more cryptic ones, should be assigned is unclear. This is partly because many characters show considerable homoplasy, in addition, basic information for all too many 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 is the not-so-trivial issue of how ancestral states are reconstructed (see above).

Phylogeny. For discussion of the monophyly and relationships of this very unexpected clade, see the eudicot node.

Previous Relationships. Thorne (2007) includes the order, variously broken up, along with Buxales, in his hetereogeneous Ranunculidae, however, most authors (e.g. Cronquist 1981; Takhtajan 1997) have not seen any connections at all between the four families here.

Classification. The inclusion of Sabiaceae in Proteales seems the sensible thing to do, assuming its relationships hold up. Ovule number and embryo are similar in the combined group.

Includes Nelumbonaceae, Platanaceae, Proteaceae, Sabiaceae.

Synonymy: Proteinae Reveal - Meliosmales C. Y. Wu et al., Nelumbonales Martius, Platanales Martius, Sabiales Takhtajan - Nelumbonineae Shipunov - Proteanae Takhtajan, Nelumbonanae Reveal, Sabianae Doweld - Nelumbonidae Takhtajan - Nelumbonopsida Endlicher, Proteopsida Bartling

SABIACEAE Blume, nom. cons.   Back to Main Tree


Evergreen (deciduous) trees or lianes; pentacyclic triterpenoids +, tanniniferous, benzylisoquinoline alkaloids?; vessel elements with simple to scalariform perforation plates, bars few (-30); wood with broad rays (0 - Sabia), (true tracheids +); (pits vestured - Meliosma); secondary phloem with broad or flaring rays; nodes complex unilacunar [Meliosma]; (sieve tube plastids also with protein crystalloids); cuticle wax crystalloids 0; stomata also paracytic; buds perulate or not; leaves spiral or two-ranked, simple to odd-pinnately compound, lamina vernation conduplicate [Meliosma], teeth ± spiny, or 0; flowers poly- or obliquely monosymmetric, (3-)5-merous; P = calyx + corolla, K C A opposite each other, C quincuncial [Sabia]; A basally adnate to C [Meliosma, Ophiocaryon], or 2 A fertile, with 2 basal processes and opposing C small, 2-3 A staminodial [Sabia)], or A 5, bisporangiate, dithecal [?Ophiocaryon], dehiscence transverse or valvate; pollen colporate; nectary a thin ± lobed disc; G connate, [2-3], completely closed (also secretory canal), when 2, oblique or median, styluli +, (marginal, ovary roof + - Ophiocaryon) short or not, stigmas punctate, wet; ovules 1 or 2/carpel, campylotropous, uni(bi-)tegmic, integument ca 6 cells across [Sabia], nucellus apex exposed; ?antipodals; fruit a (bilobed) ± drupelet to ± dry, loculicidally dehiscent, (stylulus excentric), seed with condyle [placental intrusion]; seed coat ?; endosperm helobial[?], chalazal endosperm haustorium +, embryo curved, (± spiral or coiled), cotyledons usually folded, suspensor ± 0; n = 12, 16.

3[list]/100: Meliosma (70). South East Asia to Malesia, tropical America (map: from van Beusekom 1973; Sinimbu, pers. comm. Rafael Sühs). [Photo - Flower, Fruit.]

Age. Anderson et al. (2005) date crown group Sabiaceae at 119-91 m.y.a.; (135-)129, 114(-108) m.y. is the figure in Wikström et al. (2001).

Fossils identified as Sabiaceae are known from the Cretaceous-Cenomanian ca 98 m.y.a. (Insitiocarpus, c.f. Meliosma) and -Turonian (Sabia) of Europe (Knobloch & Mai 1986; Friis et al. 2011).

Evolution. Pollination Biology & Seed Dispersal. Meliosma has explosively dehiscent anthers that are held under tension by the complex staminodes, but there is also a kind of secondary pollination presentation in which pollen collects on the broad connective between the anthers sacs (Ronse De Craene & Wanntorp 2008 for discussion).

Chemistry, Morphology, etc. Sabiaceae are distinctive among members of the eudicot grade in that the perianth is differentiated into a calyx and corolla (Drinnan et al. 1994; Hoot et al. 1999) and there is a nectary that appears to be axial/receptacular. However, the interpretation of the flower of Meliosma, especially of the nature of the perianth members, is difficult. Two sepals are smaller than the others and have been called bracteoles, as by Endress (2010c), who would then interpret the flower as being basically monosymmetric and trimerous, and the calyx whorl and the two whorls of both corolla and androecium as all alternating (one member of each is reduced). According to Baillon (1874), the two carpels of Sabia are median; Warburg (1896) drew the two carpels of Meliosma as being oblique to the vertical axis of the flowers, but median to the plane between the two bracteoles; van Beusekom and van der Water (1989) show the carpels as being oblique both to the vertical axis and to the plane between the bracteoles, and the flower could be called obliquely monosymmetric. Wanntorp and Ronse de Craene (2007) illustrate the carpels as being more or less collateral, and Ronse de Craene (2010) as slightly oblique, bracteoles are not shown, but their position is described as being variable. Ronse De Craene et al. (2015) note substantial differences in the floral development of the two species of Sabia they examined that they suggest is connected to the incorporation of a bracteole into the flower in S. japonica as a "sepal".

Ophiocaryon paradoxum has a coiled embryo; it is known as the snake nut.

For wood anatomy, which is very variable, see Carlquist et al. (1993), for chemistry, see Hegnauer (1973, 1990), and for a general account, see Kubitzki (2006b).

Classification. For a revision of Sabia, see van de Water (1980).

Synonymy: Meliosmaceae Meiser, Wellingtoniaceae Meisner

>[Nelumbonales [Platanales + Proteales]]: epidermal waxes with tubules [2/3], nonacosan-10-ol the main wax; nodes?; stipules sheathing [2/3]; connective extended beyond anther loculi.

Age. Wikström et al. (2001) estimate this node to be (143-)137, 125(-119) m.y.o., Bell et al. (2010) suggested ages (131-)116, 110(-101) m.y., Xue et al. (2012) ages of (122.8-)109.3(-75.2[- 16.3 m.y.!]) m.y., almost the age of fossils reliably assigned to Nelumbonaceae, and Anderson et al. (2005) date this node to around 121-115 m.y.a.. Magallón and Castillo (2009) and Magallón et al. (2015) suggest an age of around 117 m.y., Magallón et al. (2013) an age of around 105 m.y. and Xue et al. (2012) ages of (123.8-)ca 109(-16.3) m.y.; a low ca 82.6 m.y. is the age in Naumann et al. (2013) and a high ca 177 m.y.a. in Z. Wu et al. (2014).

The oldest fossils of this clade (Nelumbonaceae, Nelumbites are around 107-99.6 m.y.a. (Upchurch & Wolfe 2005; see also Doyle & Endress 2010; Friis et al. 2011).

Chemistry, Morphology, etc. Barthlott et al. (1996) noted that the cuticle waxes of Platanaceae and Nelumbonaceae were very different. Hayes et al. (2000) emphasise that there are only two sepals in Nelumbo, and possibly the whole order can be characterised as having dimerous flowers (see Doyle & Endress 2000 for Proteaceae). However, fossils assignable to Platanaceae are very variable in their floral morphologies, and some seem to have much more conventional, almost core eudicot-like flowers (von Balthazar & Schönenberger 2009). For variation in microsporogenesis and pollen morphology, see Furness and Rudall (2004) and Denk and Tekleva (2006); successive microsporogenesis has been reported from both Nelumbonaceae and Platanaceae.

Phylogeny. Chase et al. (1993) and Drinnan et al. (1995) found Platanaceae and Nelumbonaceae to be sister taxa; a close relationship was confirmed in the chloroplast genome analysis of Xue et al. (2012). Indeed, although the order is small, it is morphologically heterogeneous; for further discussion on the phylogenetic position of Proteales, see the eudicot node.

NELUMBONACEAE A. Richard, nom. cons.   Back to Proteales


Aquatic herbs, rhizomatous; aporphine alkaloids +; radicle aborts; roots polyarch; cork?; plant with air canals; vascular bundles scattered, lacking fibrous sheath; tubular P-protein and rod-shaped bodies +; nodes ?; articulated laticifers +; cuticle waxes as clustered tubules; prophyll adaxial; leaves vertically two-ranked, in groups of three along the stem, sheathing cataphyll on one side then cataphyll and expanded leaf on the other side; leaf peltate, lamina with a central disc, vernation involute, venation actinodromous, midrib unbranched, with many primary veins, venation dichotomising, proceeding to margin, stipule sheathing, open; flowers ?axillary, protogynous, large [>4 cm across], with complex cortical vascular system; K[?] 2, 4, C 10-30, spiral; A many, from a ring meristem, development chaotic, at least outer extrorse, connective with a terminal appendage, filament often with more than one bundle; tapetal cells multinucleate; microsporogenesis also successive; receptacle massive, with emergent druses; G (2-)10-30, carpels ascidiate, immersed in receptacle, occluded by secretion, pollen canal long-papillate, stylulus 0, stigma expanded, wet; ovule one/carpel, outer integument ca 30 cells across, inner integument 8-10 cells across, parietal tissue 3-5 cells across, nucellar cap ca 4 cells across, chalaza massive, postament +, hypostase +, funicular obturator +; antipodal cells multiplying, multinucleate, persistent; fruit a nutlet, with an apical pore; seed ?pachychalazal, testa undistinguished; embryo green, large, differentiated, cotyledon tubular but basically double, several leaf primordia; n = 8; radicle aborting, roots adventitious.

1[list]/1-2. Temperate, E. North America and E. Asia (map: from Fl. N. Am. III 1997; Fu & Hong 2000; Sculthorpe 1987; Wu 1983 [the last two include all Malesia and N. Australia, but not there in NW Australia, at least, in FloraBase 2006, the former also includes the Antilles and NW South America...]). [Photo - Nelumbo Flower © J. Manhart, Collection.]

Age. Crown-group Nelumbonaceae may be (6.5-)1.6(-0.1) m.y.o. (Xue et al. 2012).

Fossil Nelumbonaceae, as Nelumbites, the leaves with rather different venation but the flowers with the distinctive expanded floral receptacle of extant Nelumbo, are reported from the mid to late Albian (late Lower Cretaceous) ca 107-99.6 m.y.a. (Upchurch & Wolfe 2005; see also Doyle & Endress 2010; Friis et al. 2011; Doyle & Upchurch 2014).

Evolution. Divergence & Distribution. Fossils of Nelumbonaceae - leaves and fruits, although not connected - are known from southern Argentina in late Upper Cretaceous rocks of Campanian-Maastrichtian age (Gandolfo & Cuneo 2005). Other fossils are discussed by Estrada-Ruiz et al. (2011) and Friis et al. (2011).

Given the great age of the clade, 100 m.y. or substantially more, Nelumbo has been called a living fossil, at least from the molecular point of view, and it also shows considerable morphological stasis (Sanderson & Doyle 2001; Xue et al. 2012).

Ecology & Physiology. Vogel (2004a) provided a fascinating account of air circulation in Nelumbo, i.a. suggesting the air flows in different halves of the leaf in different directions, similarly in the petiole. The central disc has many stomata and is the site of air exchange for the petiolar canals (see also Estrada-Ruiz et al. 2011); if covered by water, air from the petiolar canals bubbles up through it.

Pollination Biology & Seed Dispersal. The flowers are thermogenic, starch breaking down in the expanded receptacle, halictid bees and especially chrysomelid bettles being the likely pollinators (Vogel & Hadacek 2004; Watling et al. 2006; Li & Huang 2009; Dieringer et al. 2014). The progamic phase, the time between pollination and fertilization, is notably short, as in at least some other aquatic angiosperms (including Nymphaea: see Williams et al. 2010). The sharply pointed and often six-rayed epidermal druses on the surface of the receptacle may protect it against herbivores (Vogel 2004b).

Lotus fruits are noted for their longevity, and fruits 1350 ± 220 yrs old have been germinated (Shen-Miller et al. 1995). This may be connected with the chemical composition of the fruit wall which is distinctive in its high polysaccharide (galactose, mannose) and tannin content, compared to the lignin + cellulose composition of (e.g.) the seed coat of Nymphaeaceae (ven Bergen et al. 1997).

Genes & Genomes. For the chloroplast genome of Nelumbo, see Z. Wu et al. (2014).

Chemistry, Morphology, etc. Understanding how Nelumbo grows is difficult. The cataphylls more or less surround the stem and presumably represent the stipular portion of the leaf. Axillary branches show the same arrangement of leaves as described above, but with the addition of the prophyll which is on the same side of the branch as the first cataphyll. Flower buds develop in the axis of the second cataphyll, axillary branches in the axil of the expanded leaf, however, other interpretations are also possible. The sheathing stipule associated with the foliage leaf is open on the side of the stem opposite to the leaf insertion. For some literature on the growth pattern of Nelumbo, see Eichler (1878), Wignand and Dennert (1888), Miki (1926), Esau and Kosakai (1975), etc.

Vessels arise first in the roots, but are also found in the rhizome, and the trend of their specialisation is similar; this is the monocot pattern. Details of the root cortex of Nelumbonaceae differ considerably from those in Nymphaeales (Seago 2002). Although the vascular bundles are scattered in the stem, they are inside an endodermis.

Hayes et al. (2000) noted that the two sepals are inserted in the vertical plane; Moseley and Uhl (1985) found that there may be four, decussating sepals. Although the floral vasculature is complex because of the presence of rings of cortical bundles, the vascularization of individual parts of the flower is undistinguished; the sepals may, however, have but a single trace that quickly divides (Moseley & Uhl 1985). The stamens develop from an androecial ring, and they and the carpels may be irregularly whorled (Hayes et al. 2000). Cronquist (1981) described the stamens as being introrse-latrose; Endress (1995) as extrorse, Takhtajan (1997) as extrorse (the outer members) and introrse (the others). There is also disagreement over endosperm development which has been variously described as nuclear, cellular, or helobial, and over pollen morphology (Kreunen & Osborne 1999).

Some general information is taken from Williamson and Schneider (1993) and Hayes et al. (2000), for chemistry, see Hegnauer (1969, 1990: as Nymphaeaceae), for stamens, see Moseley (1958), and for embryology, etc., see Cook (1909), Khanna (1965) and Batygina et al. (1982).

Previous Relationships. In the past, Nelumbonaceae were usually associated with Nymphaeaceae (e.g. Cronquist 1981), the two having superficially similar flowers and vegetative body (both are "water lilies") - and it turns out that floral gene expression patterns in Nymphaea and Nelumbo are remarkably similar (Yoo et al. 2010). Takhtajan (1997) removed Nelumbonaceae from Nymphaeales, but placed them alone in his subclass Nelumbonidae. Both the morphology of the cuticle waxes and plant chemistry suggest a relationship with Ranunculales, but there the waxes are nonacosan-10-ol rather than 4-10- or 5-10-diol (Barthlott et al. 1996, 2003: the difference not emphasised).

[Platanaceae + Proteaceae]: woody; non-hydrolysable tannins, myricetin +, benzylisoquinoline alkaloids 0; (pits vestured); wood with broad rays [8+-seriate]; stomata laterocytic; flowers 4-merous [but see fossil Platanaceae]; P +; stamens = perianth, opposite them; carpels with 5 vascular bundles, hairy, postgenital fusion complete, stylulus long; ovules straight, inner integument 3-5 cells across; endosperm nuclear.

Age. Wikström et al. (2001) estimate this node to be (124-)117, 108(-101) m.y. old, ages in Bell et al. (2010), at (102-)99, 88(-97) m.y, are a little younger. Anderson et al. (2005) date the node to 119-110 m.y., Barker et al. (2007b) to (126.7-)118.5(-110.3) m.y. ago, while ca 106.2 m.y. is the age in Magallón et al. (2015).

Age. Platanocarpus (most = Friisicarpus) is known fossil from the Lower Cretaceous 113-98 m.y.a. (Crane et al. 1993), and other fossils are associated with Platanaceae in the constrained morphological analysis of Doyle and Endress (2010).

Evolution. Divergence & Distribution. That Platanaceae and Proteaceae are sister taxa may explain why there are so many leaf fossils from the southern hemisphere that are "platanoid" in their general aspect (K. Johnason, in Drinnan et al. 1994; Hoot et al. 1999).

Chemistry, Morphology, etc. The wood anatomy of Proteaceae and Platanaceae is very different, perhaps because of the different climatic conditions under which the two grow (Baas et al. 2003); however, they both have broad rays, and the former have concave vessel-parenchyma festoons and the latter concave growth ring boundaries. For stomatal morphology, see Carpenter et al. (2005). Although flowers of Platanaceae and Proteaceae look very different, von Balthazar and Schönenberger (2009) suggest similarities; both consist of perianth, stamens, and fleshy structures. In Platanaceae the latter may represent an outer staminal whorl, in Proteaceae an inner whorl. This hypothesis needs further study, but because of the difference in their positions they are unlikely to be an apomorphy here.

PLATANACEAE T. Lestibudois, nom. cons.   Back to Proteales


Growth sympodial; (plant deciduous); cork in outer cortex; nodes multilacunar; petiole bundle annular, wing bundles +; hairs candelabriform, basal cell conoid, over the junction of epidermal cells; leaves two-ranked (spiral), lamina vernation plicate-revolute, teeth glandular, with a terminal cavity, higher order veins approach but do not enter it, (margin entire), 2 strong secondary veins near base (venation pinnate; also in seedlings), petiole enclosing the axillary bud (not), stipule tubular, closed (adaxial-sheathing, open); plant monoecious; inflorescences capitate; flowers 3-4(-7) merous; P small, uniseriate, connate or not, often lacking vasculature; staminate flowers: outer whorl staminodial, ca 3, tiny; anthers valvate, connective with subpeltate apex; pollen semitectate-reticulate, 16-22 µm long; (pistillodes +); carpellate flowers: staminodes +; G (3-)5-8(-9), two-whorled, stylulus long, stigma decurrent in two crests, ± dry; ovules 1(-2)/carpel, outer integument 3-4 cells across; fruit an achene, with basal tuft of hairs; mesotesta thick-walled, sclereidal; seed reserves hemicellulosic, endosperm moderate; n = 16-21, chromosomes 1.4µm long [mean].

1[list]/10. North Temperate (map: from Fl. N. Am. III 1997; Jalas et al. 1999 [Europe]; Feng et al. 2005). [Photo - Leaves & Stipules, Collection.]

Age. Fossils with the distinctive petiole bases of subgenus Platanus are abundant in the Palaeocene some 60 m.y.a. (Feng et al. 2005); this puts a lower limit on the crown-group age of the family. However, leaves with such petioles may have small, fugaceous triangular stipules unlike those of extant taxa (Wang et al. 2011).

Maslova (2010) placed Platanaceae in Hamamelidales, along with a number of fossil genera, some placed in the extinct Platanaceae-Gymnoplatananthoideae and also in Bogutchantaceae (sic) N. Maslova (= Bogutchanthaceae) - see also Hamamelidaceae).

Evolution. Divergence & Distribution. The morphology of fossil Platanaceae sometimes differs from that of their extant relatives (see also Kvacek 2008: whole plant reconstruction; Friis et al. 2011). Thus the leaves may be trifoliolate (Kvacek et al. 2001a) or imparipinnnate (= Sapindopsis), and inflorescences may have sessile or pedunculate heads. In Upper Cretaceous plants there is extensive floral variation: staminate flowers P 4, basally connate, stamens equal and opposite perianth members and arising from a short ring of tissue, alternating with ?staminodes, perhaps of an outer whorl, or two 4- or 5-membered whorls of perianth present, A 5, pistillode consistently present, or P in 2 whorls, connate, outer more or less completely so, or free; G 8, 2 opposite each member of inner perianth, ovules perhaps anatropous, stylulus 0. Mindell et al. (2014) described the Late Cretaceous Ambiplatanus with very small heads and some perfect flowers; the 5-merous perianth was in two whorls with the stamens opposite members of the inner whorl. Some fossils have rather smaller pollen that that of extant taxa - are they wind-pollinated? - and tricolporate pollen has even been found in situ in fossils assigned to Platanaceae (e.g. Manchester 1986; Crane et al. 1993; Pedersen et al. 1994; Friis et al. 1988, 2011; Magallón-Puebla et al. 1997: Mindell et al. 2006: Crepet et al. 2004; von Balthazar & Schönenberger 2009; Taylor et al. 2009; Doyle & Upchurch 2014 for other references). Cretaceous Platanaceae do not have hairy fruits (von Balthazar & Schönenberger 2009; Friis et al. 2011).

From the molecular point of view, at least, Platanus can be considered a living fossil (Sanderson & Doyle 2001).

Pollination Biology. There is about five weeks between pollination and fertilization in Platanus racemosa, at least (Floyd et al. 1999).

Genes & Genomes. There is some evidence from the stomatal size of fossils that polyploidization occurred within this clade (Masterson 2004).

Chemistry, Morphology, etc. Hennig et al. (1994) described the cuticle wax as lacking crystalloids, Fehrenbach and Barthlott (1988) as having rodlets and platelets. There is some variation in stomatal morphology (Carpenter et al. 2005). Subgenus Castaneophyllum (P. kerrii) differs in lamina morphology and venation, petiole base and stipule morphology from subgenus Platanus.

Von Balthazar and Schönenberger (2009) described the parts of the flower as alternating regularly; the androecium was biseriate, the outer, very much reduced whorl appearing late in development. Developmental studies suggest that flowers of Platanus are basically 4-merous (A. Douglas in Hoot et al. 1999).

Some information is taken from Kubitzki (1993b); see Floyd et al. (1999) and Floyd and Friedman (2000) for embryology and endosperm development and Denk and Tekleva (2006) for pollen of extant and fossil taxa. See Smets (1986) for nectaries, Melikian (1973) and Takhtajan (1991) for testa anatomy, and Floyd et al. (1999) for embryology; for chemistry, see Hegnauer (1969, 1990), and for vegetative characters, see Doyle and Upchurch (2014).

Phylogeny. For a phylogeny of Platanus, see Grimm and Denk (2008).

Previous Relationships. Platanaceae were included in Hamamelidales by both Cronquist (1981) and Takhtajan (1997).

PROTEACEAE Jussieu, nom. cons.   Back to Proteales


Trees or (acaulescent) shrubs; lateral roots of limited growth, forming clusters [proteoid roots], plant rarely mycorrhizal; vessel elements with simple perforation plates (scalariform, bars few); true tracheids and libriform fibres +; phloem stratified or not; nodes (1:1), 3:3, 5:5; petiole bundles numerous, pattern complex; sclereids common; hairs with 2 short cells, one in epidermis, apical cell elongated, bifid or not; leaves spiral (opposite), (odd-pinnately, rarely palmately, compound or lobed), lamina often coriaceous, vernation usu. conduplicate, margins spiny toothed to entire, base of petiole often swollen, stipules 0; inflorescence various; flowers 4-merous; P petal-like, valvate, decussate-diagonal; (connective appendage 0); tapetal cells binucleate (uninucleate - Macadamia); microsporogenesis also successive, cleavage centrifugal; pollen triangular in polar view, oblate, triporate, pores broadly operculate, apertures in three's at four points of the young tetrad [Garside's Rule], (colpate), exine with ektexine only; nectary receptacular, vascularized; G 1, orientation adaxial, stigma terminal or lateral, often slit-like, secretory; ovules long, vascular bundles forming a ring in the chalazal region, outer integument 2(-9) cells across, inner integument 3-4(-6) cells across, parietal tissue (?0-)2-16 cells across, nucellar cap 2-7 cells across, ± endothelial, hypostase +; (antipodals not persistent); endotesta palisade, crystalliferous, (exotegmen fibrous); cotyledons large, embryonic suspensor 0.

80[list]/1600 - five subfamilies below. Largely southern hemisphere, esp. Australia and S. Africa (map: from Johnson & Briggs 1975; Trop. Afr. Fl. Pl. Ecol. Distr. 1. 2003; Weston 2006; Prance et al. 2007).

Age. Anderson et al. (2005) date crown-group Proteaceae at 96-85 m.y., and Barker et al. (2007b) at around (126-)118(-110) m. years.

Hill et al. (1995) and Weston (2006) summarize the fossil record of the family, Carpenter (2012) that of leaf fossils. Leng et al. (2005) discuss small but mature capsular fruits from late Cretaceous (late Santonian/early Campanian) Sweden which have several attributes of Proteaceae, e.g. the flowers are paired, the stigma is somewhat abaxial on the fruit. However, there are also differences, e.g. there are only three vascular bundles per carpel and there seems to be little in the way of a perianth; one species has the most remarkable papillate seeds. Proteaceae fossils are known from sediments ca 94 m.y. old in Australia, i.e., shortly after the separation of Australia from Antarctica some 97 m.y.a. (Hill & Brodribb 2006).

1. Bellendenoideae P. H. Weston

Plants Al-accumulators; inflorescence terminal, bracts 0; ovules 2/carpel; fruit dry, indehiscent, 2-winged; n = 5, chromosomes ca 6.7 µm long, ca 1 pg DNA (means).

1/1: Bellendena montana. Australia (Tasmania).

[Persoonioideae [Grevilleoideae + Symphionematoideae + Proteoideae]]: stomata brachyparacytic; P connate; A adnate to P, more or less sessile; usu. 4 nectary lobes; stylulus long; endosperm +; (cotyledonary blade cordate).

Age. Wikström et al. (2001: see sampling!) estimated that this node was (67-)60, 47(-40) m.y. old.

2. Persoonioideae L. A. S. Johnson & B. Briggs

(Plants Al-accumulators - Placospermum); proteoid roots 0; tepals with Vorlaüferspitze, 1-2(+) ovules carpel; fruit a drupe (follicle - Placospermum); cotyledons obreniform; n = 7, chromosomes 9.1-14.4 µm long, 2.5-4.3 pg DNA (means).

5/110: Persoonia (100). Mostly Australia, also New Caledonia and New Zealand.

Age. This clade may be (84.1-)72.3(-60.5) m.y. old (Barker et al. 2007b).

[Grevilleoideae [Symphionematoideae + Proteoideae]]: (tyrosine-derived cyanogenic glycosides +); T orthogonal [?level]; flowers vertically or obliquely monosymmetric [P split to base on one side (4:0), or 3 P connate, 1 free (3:1)]; (secondary pollen presentation, the apex of the style bearing the pollen); (ovules anatropous); x = 14, chromosomes 0.5-5 µm long, 0.05-0.27 pg DNA (means).

3. Grevilleoideae Engler

Plants Al accumulators; sieve tubes with rosette-like non-dispersive protein bodies; paired flowers subtended by a common bract (not); (A not adnate to P), pollen biporate, also with abundant endexine, also in the apertural region; (carpel orientation other than adaxial); ovules (1-)2+/carpel; fruit a drupe or follicle, the latter with winged seeds [wing from outer integument]; (seeds pachychalazal); endosperm with chalazal and nuclear haustorium; cotyledons basally auriculate; n = (10-)14(-15), chromosomes 1-2.6µm long [mean].

45/855: Grevillea (515), Helicia (100), Banksia (175). Australia and the S.E. Pacific to Southeast Asia, S. India and Sri Lanka, South America, South Africa (Brabejum) and Madagascar (Madagascaria). [Photos - Grevillea Flower, Embothrium Flower, Fruit, Habit.]

Synonymy: Banksiaceae Berchtold & J. Presl

[Symphionematoideae + Proteoideae]: fruit indehiscent.


Symphionematoideae P. H. Weston & N. P. Barker

Proteoid roots 0; T orientation?; nectaries 0; ovules 1-2/carpel; fruit dry; n = 10.

2/3. S.E. Australia, inc. Tasmania.

Age. The crown-group age of this clade is slightly less than 80 m.y. (Barker et al. 2007b).

5. Proteoideae Eaton

(Herbaceous), (plants Al-accumulators); sieve tubes with non-dispersive protein bodies; flowers sessile; (hypanthium +); (A monothecal; 1-3); ovules 1(2)/carpel; fruit often single-seeded, drupe or nut; n = (10-)11-13(-14), chromosomes 1.2-3.4µm long [mean].

25/640: Protea (115), Leucadendron (80), Conospermum (55), Petrophile (55), Synaphea (55), Serruria (50). Africa S. of the Sahara, esp. the Cape region, Australia.

Synonymy: Lepidocarpaceae Schultz Schultestein

Evolution. Divergence & Distribution. There is a great diversity of proteaceous pollen from the late Cretaceous (Campanian-Maastrichtian) in southeast Australia (Dettmann & Jarzen 1991, 1998; see also Friis et al. 2011), and from fossil evidence, Proteaceae seem to have been very diverse and ecologically important in at least parts of Australia by the end of the Eocene (Itzstein-Davey 2004).

Although some transoceanic disjunctions in the family, for example, that of the sister taxa Cardwellia in Australia and Gevuina in South America, could reflect vicariance/continental drift events, others, like Brabejum in Africa which is sister to Panopsis in South America, involve genera whose estimated time of divergence is later than the geological events that from their distribution patterns might seem to have caused them (Barker et al. 2007b). There has been extensive extinction of Proteaceae in New Zealand (Lee et al. 2001).

Several lines of molecular evidence suggest that there may have been rapid diversification within Grevilleoideae (Hoot & Douglas 1998). The stem age of the very largely Australian Banksieae is estimated at (94.9-)87.9(-80.9) m.y. (Barker et al. 2007b, q.v. for other ages). Banksia itself may be ca 60.8 m.y. old, the crown group (56.9-)44.5(-36.6) m.y. (He et al. 2011: HPD). More recent diversification within Banksia may have been instigated by vicariance events such as the aridification of the Nullarbor Plain some 14-13 m.y.a. which led to the separation of what became eastern and western clades (Crisp & Cook 2007). However, although it is diverse in areas with a Mediterranean climate, it does not seem to have undergone particularly rapid speciation, rather, unexceptionable rates over a long period of time may be the cause (Cardillo & Pratt 2013). Crown group Hakea s. str. may be as young as (14.0-)9.6(-6.4) m.y. (Mast et al. 2012, see also 2009; c.f. Hanley et al. 2008). Fires may also have spurred diversification, as in Banksia, where flower retention on inflorescences and leaf retention on plants may increase the intensity of fires, even if exactly how this might benefit a species is not entirely clear (He et al. 2011; see also Bond & Midgley 1995). Fire-dominated eucalypt vegetation had begun to develop in Australia in the earliest Caenozoic a little before Banksia diversified (Crisp et al. 2011).

Protea, notably speciose in southern Africa with some 70 out of its 115 species being restricted to the Cape, has been studied by Barraclough and Reeves (2005), although they found it difficult to pin down dates for diversification. However, Sauquet et al. (2009a, b) suggest that this may have occurred within the last 18 m.y., yet Leucadendrinae had started diversifying there as much as 39 m.y.a., even though they had been in the Cape region for a shorter time than Protea. On the other hand, Schnitzler et al. (2011) suggested that diversification in Protea began ca 28 m.y.a. in the middle of the Oligocene and was connected with edaphic (soil mediated) speciation; rates of diversification throughout its range were similar (Valente et al. 2010b; see also Silvestro et al. 2011).

Tonnabel et al. (2014a) examined the evolution of various life history traits in Leucadendron (see also Barker 2004). They found frequent trade offs between traits, so if, for example, the seeds of a particular species commonly dispersed squite a distance, its pollen was not so likely to be well dispersed.

Ecology & Physiology. Proteaceae are most diverse in rather dry climates on nutrient-, especially phosphorus-, poor soils in Australia (see also Orians & Milewski 2007) and also southern Africa. They are distinctive in having a relatively large seed mass and both very low leaf nitrogen and high leaf mass per area (i.e. they show a decrease in SLA), the latter features tending to be linked (Cornwell et al. 2014). From examination of fossil leaves, scleromorphy may have evolved in the late Palaeocene, xeromorphy in the late Eocene/Oligocene (Hill 1998; Hill & Brodribb 2001). Jordan et al. (2005, 2008) outline the evolution of scleromorphic leaf anatomy, in particular, aspects of stomatal morphology. Sclerophylly itself is implicated in photoprotection and occur in association with some combination of open, oligotrophic, cold and dry conditions, while sunken stomata help reduce water loss (Weston 2014). The family as a whole shows great variation in aspects of leaf anatomy and morphology like cell size, stomatal and fine vein density, leaf size and thickness, etc., that affect productivity, transpiration, etc. (Brodribb et al. 2013), interestingly, there is no simple correlation between productivity and success. Bellendena, perhaps sister to the rest of the family (see below), has medium-sized stomata, while Persoonioideae (perhaps sister to Bellendena) and Protea in particular have large stomata and other anatomical features that are common in taxa of more open habitats (Brodribb et al. 2013). Aspects of leaf anatomy that enable the plant to move water through the leaves are correlated with annual precipitation (Jordan et al. 2013). Lignotubers have evolved several times in Proteaceae.

Proteoid roots are short lived clusters of roots of determinate growth that have densely set root hairs; they may account for over 50% of the mass of all roots of a plant at any one time (Shane & Lambers 2008; see also Purnell 1960; Dinkelaker et al. 1995). They exude organic acids, especially as tricarboxylates, into the soil, and this enables them to mobilize phosphate, and perhaps other nutrients like manganese, that are at a premium in the phosphorus (P)-poor soils on which Proteaceae often grow (Weston 2006); they are phosphorus miners (Lambers et al. 2008). Furthermore, some species can remove the P component of cell membranes (as phospholipids) and divert it to maintaining their photosynthetic rates (Lambers et al. 2012a, b). Interestingly, many members of the family develop P toxicity when growing on relatively P-rich soils; they cannot down-regulate P uptake, and it accumulates in palisade mesophyll cells in particular, eventually causing the death of the plant (Shane et al. 2004; Shane & Lambers 2008; Lambers et al. 2011 for a general summary). Particularly in Australia, and there perhaps particularly in serotinous species, P is preferentially moved into the seeds (Groom & Lamont 2009). It is interesting that proteoid roots also develop in Lupinus, Arabidopsis and a number of Fagaales, etc., under conditions of low P and as soils age (López-Bucio et al. 2003; Lambers et al. 2008; Kang et al. 2014: development of prote\oid roots in Arabidopsis).

In South America soils may be richer in P, but it is not readily available (Lambers et al. 2012b). However, it mas been suggested that in the Patagonian Embothrium coccineum cluster root formation could induced by low nitrogen rather than low P, even if P uptake was also subsequently enhanced (Piper et al. 2013).

Lomatia tasmanica appears to be represented by a single clone about 1.2 km across; only recently what may be the same clone may have been ca 6 km across, and fossil records suggest that it might be up to 43,600 years old (Lynch et al. 1998).

Pollination Biology & Seed Dispersal. Pollination in Proteaceae is not very well known, particularly in Australia. In both Australia and southern Africa non-flying mammals (rodents, marsupials) are among the pollinators (Collins & Rebelo 1987). Secondary pollen presentation by regions at the apex of the style is common. There is great variation in these pollen presenting areas (Ladd 1994) and the pollen may even cover the stigmatic area (Ladd et al. 1996), the stigma itself often being slit- or groove-like; however, selfing is uncommon. Pollination in the speciose Persoonia, which lacks secondary pollen presentation, was found to be by bees (Bernhardt & Weston 1996). Monosymmetric flowers are common the family, but the Cape species Mimetes cucullatus has monosymmetric groups of flowers, the pendulous polysymmetric flowers being borne under a more or less brightly coloured inflorescence bract. The inflorescences of some species of the Australian Conospermum (Proteoideae) look rather like those of Anigozanthus (Haemodoraceae).

It has been suggested that ca 300 species of Proteaceae in Australia may be bird-pollinated (Ford et al. 1979), but this is likely to be an underestimate. There are about 1,100 Australian species of Proteaceae, and many species, including members of the large genera Grevillea and Banksia, are likely to be pollinated by birds (Maynard 1995). Two recent studies have examined bird pollination in Hakea (to be included in Grevillea), its evolution and possible relationship with cyanogenesis in the flowers. From the phylogeny provided by Mast et al. (2012), insect pollination would seem to be derived from bird pollination, while Hanley et al. (2008) suggested the opposite, however, the phylogeny of the latter was based on an earlier morphological study that could not be confirmed by Mast et al. (2012). Dates, as well as a possible association between pollinators and the presence of cyanogenic glycosides suggested by Hanley et al. (2008) also need confirmation. In southern Africa perhaps 87 species of Proteaceae in the Cape Fynbos are pollinated by a few species of nectariniids, and particularly by the sugarbird, Promerops cafer (Promeropidae) (Rebelo et al. 1984: Rebelo 1987); there are two species of Promerops, one of which is more broadly distributed in Africa, as are Proteaceae themselves. In both Australia and the Cape, the prominence of ornithophily in the family may be connected with the nutrient-poor soils on which they grow; nectar costs the plant little (Rebelo 1987; Orians & Milewski 2007).

Serotiny is scattered in the family, the follicles opening only after a fire. Banksia is a major serotinous clade, although with some reversals (He et al. 2011: Dryandra not included, other features associated with serotiny examined). A number of the species involved have massive fruits, but there are only two seeds inside. For myrmecochory in Grevillea, Leucadendron, etc. (Grevilleoideae and Proteoideae), see Lengyel et al. (2009, 2010).

Plant-Animal Interactions. Given the size of the family, caterpillars of Lycaenidae butterflies seem to eat its members quite frequently (see Fiedler 1991).

Bacterial/Fungal Associations. In Australia, the fungal pathogen Phytophthora cinnamomi is proving especially destructive to members of this family in the Mediterranean climates of the southwest. The SAfrican Faurea saligna is reported to be ectomycorrhizal (Högberg & Piearce 1986).

Genes & Genomes. That palaeo-polyploidy has been involved in the evolution of chromosome number in the family is questionable (Stace et al. 1998). There is very considerable variation in chromosome and genome size that correlates with phylogeny/habitat, but much less with chromosome number; there have been changes in stomatal size subsequent to and independent of changes in genome size (Stace et al. 1998; Jordan et al. 2014).

Chemistry, Morphology, etc. For distinctive fatty acids in the seeds, see Badami and Patil (1981); fof cyanogenic glycosides, see Swenson et al. (1989). Sieve tubes have sieve areas for most of their length. The roots have 4-7 protoxylem poles. Nodes in Panopsis appear to be pentalacunar, while those of Finschia are trilacunar, although with some variation in the number of traces departing from each gap (Catling 2010). Cotyledonary nodes commonly have split laterals (Naubauer 1991), however, the distribution of this character is unclear. Stem lenticels are often horizontally elongated (Keller 1996).

The flower pairs common in the family represent reduced inflorescence branches (Douglas & Tucker 1996a). For variation in floral orientation, see Douglas and Tucker (1996a, b); the flowers may be mirror images, as in Orites (image at: www.anbg.gov.au/proteaceae/illustrations.html). In Grevilleoideae, the basical floral orientation is orthogonal to the bract immediately subtending the flower, but the position of this bract relative to the axis that bears it varies (Douglas & Tucker 1996a). Flowers of Proteoideae-Conospermeae show considerable developmental variation (Douglas & Tucker 1997). There is no evidence that the perianth is derived from a biseriate structure, and the individual perianth members - of Macadamia, at least - have three traces; for the family, 1-5 bundles supplying each tepal are reported (Weston 2006). A small, almost spine-like process that is described as a Vorlaüferspitze (Douglas & Tucker 1996c) occurs just abaxial to the apex of the perianth members (see Kaplan 1973) in Persoonioideae, and it is also found elsewhere in the family. Stirlingia, Franklandia, Conosperma, and Synaphea have an exothecium, but no endothecium (Venkata Rao 1971). The nectary has very variable vasculature; it is best considered to be an enation rather than a modified stamen (Douglas & Tucker 1996c). The stigma may be papillate, or it is more or less enclosed, with exudate (Matthews et al. 1999); due to the early growth of the carpel, it may be in a more or less abaxial position on the carpel/style.

The position of the embryo sac in the ovule varies considerably (Venkata Rao 1971). Manning and Brits (1993) suggested that there had been much misinterpretation of fruit/seed anatomy; their interpretation is followed here. Testa and tegmen variation is extensive, partly because the fruits are sometimes indehiscent (Venkata Rao 1971; Corner 1976). The ovary wall may also be adnate to the integuments (so the fruit is a sort of caryopsis?!). Testa anatomy is similar to that in Papaveraceae, Chloranthaceae, and Aristolochiaceae, for what that is worth. The testa and/or the tegmen may be multiplicative. Endosperm and endosperm haustorium development is variable. Cotyledons of Bellendena are not cordate are they often are elsewhere in the family.

For general information, see Johnson & Briggs (1963, 1975: including chromosome lengths!) and especially Weston (2006), for general chemistry, see Hegnauer (1969, 1990), for polyol distribution, see Bieleski and Briggs (2005), for nodes, see Catling and Gates (1998), for Al accumulation, see Webb (1954), for the life history of Grevillea, see Brough (1933), for pollen, see Dettmann (1998), Sauquet et al. (2006), Sauquet and Cantrill (2007), and Blackmore and Barnes (1995: development, Garside's Rule), for some embryology, see Venkata Rao (1959), and for a survey of seed coat anatomy, see Takhtajan (2000).

Phylogeny. For a summary of phylogenetic studies in the family, see Weston (2014). Although the subfamilies recognised here seem to be fairly solidly supported, relationships between them are less clear. Thus the summary tree in Weston and Barker (2006) and Weston (2006) suggest that Persoonioideae and the monotypic Bellendenoideae are sister taxa; the distinctive Carnarvonia (fully compound leaves) and Sphalmium (stylulus short), sometimes segregated as subfamilies (as in The Flora of Australia), may be immediately related, and although definitely to be included in Grevilleoideae, further relationships within that clade are unclear. Although understanding relationships between the major clades was not the focus of the study by Mast et al. (2012), they recovered the relationships [[Persoonoideae + Bellendenoideae] [Grevillioideae [Proteoideae + Symphionematoideae]]].

Relationships in Proteoideae are explored by Barker et al. (2002); the Australian Isopogon and Adenanthos are sister to a clade that represents most of the subfamily, but not including Protea and Faurea (support strong for this set of relationships); unfortunately Eidothea, a distinctive genus segregated as Eidotheoideae in The Flora of Australia, was not included. For the phylogeny of Leucadendron, see Tonnabel et al. (2014a, b), and for relationships in Hakea, to be included in Grevillea, see Mast et al. (2012).

Classification. For a new subfamilial/tribal classification, the outlines of which are followed here, and a generic checklist, see Weston and Barker (2006) and Weston (2006).

Banksia is to include Dryandra (Mast et al. 2005) while Grevillea is also to be expanded to include Hakea and Finschia.