Plant a shrub or tree; true roots +, origin endogeneous, root cap +, apex multicellular; endodermis +; shoot apical meristem multicellular; lateral meristems +, cork cambium producing cork abaxially, vascular cambium producing phloem abaxially and xylem adaxially; lamina with mean venation density 1.8 mm/mm2 (to 5 mm/mm2).
EXTANT SEED PLANTS/SPERMATOPHYTA
Plant woody, 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, thus containing p-hydroxyphenyl and guaiacyl lignin units, so no Maüle reaction; root xylem exarch, cork cambium deep seated; arbuscular mycorrhizae +; shoot apical meristem interface specific plasmodesmatal network; stem with vascular tissue around central pith [eustele], vascular bundles with interfascicular tissue, ectophloic, endodermis 0, xylem endarch; 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 +; stem cork cambium superficial; branches exogenous; leaves with single trace from vascular sympodium ["nodes 1:1"]; vascular bundles collateral [stem: phloem external; leaf: phloem abaxial]; stomata morphology?, pore opening controlled by abscisic acid; leaves with petiole and lamina, spiral, development basipetal, blade simple; axillary buds +, not associated with all leaves; prophylls two, lateral; plant heterosporous, sporangia borne on sporophylls; microsporophylls aggregated in indeterminate cones/strobili; true pollen +, grains mono[ana]sulcate, exine and intine homogeneous; ovules unitegmic, parietal tissue 2+ cells across, megaspore tetrad tetrahedral, only one megaspore develops, megasporangium indehiscent; male gametophyte development first endo- then exosporic, tube developing from distal end of grain, to ca 2 mm from receptive surface to egg, gametes two, developing after pollination, with cell walls, flagellae numerous; ovules increasing considerably in size between pollination and fertilization, female gametophyte endosporic, initially syncytial, walls then surrounding individual nuclei; seeds "large" [ca 8 mm3], but not much bigger than ovule, with morphological dormancy; embryo cellular ab initio, endoscopic, plane of first cleavage of zygote transverse, suspensor +, short-minute, embryo straight, shoot and root at opposite ends [allorrhizic], white, cotyledons 2; plastid transmission maternal; ycf2 gene in inverted repeat, 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, non-hydrolysable tannins, quercetin and/or kaempferol +, 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 unilacunar [1:?]; stomata brachyparacytic [ends of subsidiary cells level with ends of pore], outer stomatal ledges producing vestibule; lamina formed from the primordial leaf apex, margins toothed, development of venation acropetal, secondary veins pinnate, overall growth ± diffuse, venation hierarchical, fine venation reticulate, veins (1.7-)4.1(-5.7) mm/mm2, endings free; most/all leaves with axillary buds; flowers perfect, pedicellate, ± haplomorphic, parts spiral [esp. the A], free, numbers unstable, development in general centripetal; P not sharply differentiated, with a single trace, outer members not enclosing the rest of the bud, often smaller than inner members; A many, filament not sharply distinguished from anther, stout, broad, with a single trace, anther introrse, tetrasporangiate, sporangia in two groups of two [dithecal], ± embedded in the filament, with at least outer secondary parietal cells dividing, each theca dehiscing longitudinally, 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 columellar, endexine thin, compact, lamellate only in the apertural regions; nectary 0; G superior, free, several, ascidiate, with postgenital occlusion by secretion, stylulus short, 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, megaspore tetrad linear, functional megaspore chalazal, lacking sporopollenin and cuticle; female gametophyte four-celled [one module, nucleus of egg cell sister to one of the polar nuclei]; ovule not increasing in size between pollination and fertilization; pollen binucleate at dispersal, male gametophyte trinucleate, germinating in less than 3 hours, pollination siphonogamous, tube elongated, growing between cells, growth rate 20-20,000 µm/hour, outer wall pectic, inner wall callose, 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, flagellae 0, double fertilization +, ovules aborting unless fertilized; P deciduous in fruit; seed exotestal, becoming much larger than ovule at time of fertilization; endosperm diploid, cellular [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; embryogenesis cellular; germination hypogeal, seedlings/young plants sympodial; Arabidopsis-type telomeres [(TTTAGGG)n]; 2C genome size 1-8.2 pg [1 pg = 109 base pairs], whole genome duplication, 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]]]]]: vessels +, elements with elongated scalariform perforation plates; 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]]]]: essential oils in specialized cells [lamina and P ± pellucid-punctate]; tension wood 0; 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 +; 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 positiion]; embryo sac bipolar, 8 nucleate, antipodal cells persisting; endosperm triploid; ?germination.
[MONOCOTS [CERATOPHYLLALES + EUDICOTS]]: (veins in lamina often 7-17mm/mm2 or more [mean for eudicots 8.0]); (stamens opposite [two whorls of] P); (pollen tube growth fast).
MONOCOTYLEDONS / MONOCOTYLEDONEAE / LILIANAE Takhtajan
Plant herbaceous, perennial, rhizomatous, growth sympodial; non-hydrolyzable tannins [(ent-)epicatechin-4] +, neolignans, benzylisoquinoline alkaloids 0, hemicelluloses as xylans; root apical meristem?; root epidermis developed from outer layer of cortex; trichoblast in atrichoblast [larger cell]/trichoblast cell pair further from apical meristem, in vertical files, or hypodermal cells dimorphic; endodermal cells with U-shaped thickenings; cork cambium in root [uncommon] superficial; root vascular tissue oligo- to polyarch, medullated, lateral roots arise opposite phloem poles; primary thickening meristem +; vascular bundles in stem scattered, (amphivasal), closed, vascular cambium 0; vessel elements in root with scalariform and/or simple perforations; tracheids only in stems and leaves; sieve tube plastids with cuneate protein crystals alone; stomata parallel to the long axis of the leaf, in lines, brachyparacytic; leaves with broad sheath plus blade [not petiole plus lamina], blade linear, main venation parallel, veins joining successively from the outside at the apex, endings not free, margins entire, (teeth spiny), Vorläuferspitze +, leaf base sheathing, sheath open, colleters [intravaginal squamules] +; prophyll single, adaxial; inflorescence terminal, racemose; flowers 3-merous [6-merous to the pollinator?], polysymmetric, pentacyclic; P = T, each member with three traces, median member of outer whorl abaxial, aestivation open, members of whorls alternating, similar, [pseudomonocyclic, each providing a sector for the T tube when present]; stamens = and opposite each T member [primordia often associated, and/or A vascularized from tepal trace], anther and filament more or less sharply distinguished, anthers subbasifixed, endothecium from outer secondary parietal cell layer, inner secondary parietal cell layer dividing; G , with congenital intercarpellary fusion, opposite outer tepals [thus median member abaxial], placentation axile; ovule with outer integument often largely dermal in origin, parietal tissue 1 cell across; antipodal cells persistent, proliferating; fruit a loculicidal capsule; seed testal; endosperm with distinct nuclear and chalazal chambers, embryo long, cylindrical, cotyledon 1, apparently terminal, plumule apparently lateral; primary root unbranched, not very well developed, "adventitious" roots numerous, hypocotyl short, (collar rhizoids +), cotyledon with a closed sheath, unifacial [hyperphyllar], both assimilating and haustorial; duplication producing monocot LOFSEP and FUL3 genes, [latter duplication of AP1/FUL gene], PHYE gene lost.
[ALISMATALES [PETROSAVIALES [[DIOSCOREALES + PANDANALES] [LILIALES [ASPARAGALES + COMMELINIDS]]]]]: ethereal oils 0; raphides + (druses 0); leaf blade vernation variants of supervolute-curved; endothecium develops directly from undivided outer secondary parietal cells; tectum reticulate with finer sculpture at the ends of the grain, endexine 0; (septal nectaries + [intercarpellary fusion postgenital]).
[PETROSAVIALES [[DIOSCOREALES + PANDANALES] [LILIALES [ASPARAGALES + COMMELINIDS]]]]: cyanogenic glycosides uncommon; starch grains simple, amylophobic; leaf blade developing basipetally from hyperphyll/hypophyll junction; epidermis with bulliform cellls [?level]; stomata anomocytic, (cuticular waxes as parallel platelets); colleters 0.
[[DIOSCOREALES + PANDANALES] [LILIALES [ASPARAGALES + COMMELINIDS]]]: nucellar cap 0; endosperm nuclear [but variation in most orders].
[LILIALES [ASPARAGALES + COMMELINIDS]]: (inflorescence branches cymose).
ASPARAGALES + COMMELINIDS: style long.
COMMELINIDS Back to Main Tree
Unlignified cells walls with UV-fluorescent ferulic and coumaric acids; (vessels in stem and leaves); SiO2 bodies +, in leaf bundle sheaths; stomata para- or tetracytic, (cuticular waxes as aggregated rodlets [looking like a scallop of butter]); inflorescence branches determinate, peduncle bracteate; T = calyx + corolla [stamens adnate to corolla/inner whorl]; pollen starchy; embryo short, broad.
Note: Possible apomorphies are now being added throughout the site; they 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 because there is very considerable homoplasy for many characters, with with variation within and between clades. Furthermore, basic information for all too many characters is very incomplete, often 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...
Evolution. Divergence & Distribution. Estimates of the time when divergence began within commelinids are ca 120 m.y.a. (Janssen & Bremer 2004), 94-86 m.y. (Wikström et al. 2001), or ca 116 m.y. (Bremer 2000b). Wikström et al. (2004) suggest an age of 99-91 m.y., Magallón and Castillo (2009: relaxed and constrained penalized likelihood datings) estimate ages of ca 128 and 115 m.y., and Magallón et al. (2013) an age of around 83.4 m.y.
Ecology & Physiology. Silica, an apomorphy for the commelinids, is an important plant defence, causing mechanical damage to mouthparts of would-be grazers and also having a number of physiological effects. For discussion on the effects of silica and silica bodies on herbivores, see Poaceae; most of the experimental work on this subject has been carried out on grasses.
The element silicon is important ecologically in other ways. There is a negative correlation between leaf longevity and silicon concentration in plant tissues (Cooke & Leishman 2011b), and hardly surprisingly the latter tends to be high in commelinids as a whole (Hudson et al. 2005).
Plant-Animal Interactions. Larval food plants of Satyrinae (Nymphalidae) butterflies, "browns", are widely distributed in the commelinids (Ehrlich & Raven 1964; Peña & Wahlberg 2008). Basal clades in Satyrinae feed on BLAs, while larvae of other clades eat monocots, especially commelinids (and within commelinids, especially Poaceae); Amathusiini seem to be the only satyrines that use a variety of non-commelinid monocot hosts (Peña & Wahlberg 2008; see also Peña et al. 2011). Unfortunately, the sister group of Satyrinae is unclear (Heikkilä et al. 2011).
Beetles of the Chrysomelidae-Hispinae+Cassidinae group are also common on commelinids (Jolivet 1988; Schmitt 1988; Vencl & Morton 1999; Chaboo 2007). 14/39 tribes of Hispinae+Cassidinae for which there is at least some larval host plant data are found on commelinids, 26/39 on some monocot or other (Chaboo 2007); the beetle larvae eat between the veins. Among the core eudicots larvae are mostly found on Boraginaceae, Solanaceae, Convolvulaceae and Asteraceae - asterids are particularly favoured. However, it is unclear if Criocerinae are in a clade immediately related to Donaciinae/Hispinae and related monocot-eating beetles, or not; the latter situation seems more likely (check Chaboo 2007; c.f. Wilf et al. 2000; Gómez-Zurita et al. 2007); Gómez-Zurita et al. (2007) found that hispines, including cassidines, were widely separated from Donaciinae, the latter being part of the [Criocerinae [Bruchinae + Donaciinae]] clade. Furthermore, feeding patterns evident in fossil material cannot simply be ascribed to the activities of hispine beetles, as García-Robledo and Staines (2008) noted.
Genes & Genomes. The rate of molecular evolution in commelinids is generally high, ca 0.003 substitutions/site/m.y. (Smith & Donoghue 2008). However, in genes like ndhF, at least, the rate is similar to that in Asparagales, etc. (Givnish et al. 2006). Although genes in all three genomic compartments apparently evolve slowly in Arecaceae (Wilson et al. 1990; Baker et al. 2000a, 2000b), the rate seems similar to that in a number of other monocots other than commelinids (S. W. Graham et al. 2006). Was there an increase in the rate of molecular evolution within commelinids, some Poales being spectacular examples?
Chemistry, Morphology, etc. Silicon concentrations in tissues of commelinids are generally high, although less so in groups that do not have SiO2 bodies (Ma & Takahashi 2002; Hudson et al. 2005). Lignins from Poaceae and Arecaceae (and elsewhere?) have p-coumaryl alcohol as well as coniferyl and sinapyl monomers (Seigler 1998). For the chemistry of the distinctive epicuticular waxes scattered in this area of the monocots (Barthlott & Fröhlich 1983), see Meusel et al. (1994), and for cell wall ferulates, almost entirely restricted to this clade, see Harris and Hartley (1980) and Rudall and Caddick (1994).
Although vessels in the stem and leaves are common (Wagner 1977), this does not appear to be a synapomorphy. For floral development, see Endress (1995b) in part. In those few commelinids where floral developmental genes have been studied in detail, expression of the B-class gene orthogue of PISTILLATA seems to be restricted to the stamens/staminode and petals (Adam et al. 2007); this may be connected with the more fully bicyclic nature of the perianth in most commelinids. The perianth may quite sharply differentiated into a calyc and corolla, or both whorls may be petal-like, but in either case the inner whorly surrounds the ape and the stamens are borne inside it. In some of the few other monocots studied, development may be somewhat different. Starch-containing pollen is common, but has not been found in Hanguanaceae or Dasypogonaceae (only one species of the latter examined) and in some species of Haemodoraceae, Bromeliaceae, etc. Broad embryos may be a synapomorphy at about this level.
Some morphological information about the commelinids is summarized by Givnish et al. (1999).
Phylogeny. Commelinids are well supported in molecular studies (e.g. S. W. Graham et al. 2006, and references), and they have morphological support as well, but support for relationships between the main groups has quite often been weak (Chase et al. 2000a; Soltis et al. 2007a). The clade [Commelinales + Zingiberales] is more or less well supported (Chase et al. 2006; Givnish et al. 2006, 2010b; Soltis et al. 2007a), and with Poales sister to this clade, also by Qiu et al. (2010: mitochondrial genes; Davis et al. 2013). Hilu et al. (2003: matK) suggested that Poales might be sister to other commelinids, as did Soltis et al. (2011: Kingia, etc. not included), but in both cases support was weak, as was that for the position of Arecales as sister to remaining commelinids in the latter study. Arecales were weakly supported as sister to Poales in some analyses (e.g. S. W. Graham et al. 2006; Givnish et al. 2010b, maximum parsimony).
The position of Dasypogonaceae remained unclear. Neyland (2002b: 26s rDNA) found Dasypogonaceae to be strongly associated with Restionaceae and other families (Poales), but this particular relationship has not been recovered in other molecular or morphological analyses. Multi-gene analyses did not link Dasypogonaceae with Arecales, even if where they ended up had no strong support (see Givnish et al. 2006 and Chase et al. 2006: near Poales; S. W. Graham et al. 2006: near [Commelinales + Zingiberales]). More recently, Givnish et al. (2011b) and Davis et al. (2011: structural mutations; see also Barrett & Davis 2011; Barrett et al. 2012a, esp. b) have found some support in maximum likelihood analyses of plastomes for a position sister to Arecaceae, consistent with what morphological data there is, although in a maximum parsimony analysis they were placed sister to [Commelinales + Zingiberales], if with little support. This position was also found by Barrett et al. (2013). In a tree based on the work of Givnish et al., Carlquist (2012a) showed the relationships [[Arecales [Commelinales + Zingiberales]] [Dasyopogonales + Poales]], while Rudall and Conran (2012) were inclined to think Dasypogonaceae might be included in Poales, partly because both have epidermal silica bodies, and might be close to Rapateaceae in particular - indeed, alternative topologies remained possible in some analyses in Barrett et al. (2013), and these included completely novel relationships.
However, analysis of plastid genomes suggests the relationships [[Dasypogonaceae + Arecacles] [Poales [Commelinales + Zingiberales]]] (Barrett et al. 2012a, esp. b), those long followed here... See also Commelinales, Zingiberales, and Poales for further discussion of relationships.
Classification. Givnish et al. (1999) erected a classification of four superorders and 10 orders for the commelinids based on a rbcL phylogeny. A.P.G. (2009) recognises four orders; these are generally well supported clades with stable contents.
Unplaced: Back to Main Tree
Plant non-mycorrhizal; (extensive primary thickening +); vessels only in roots; 2 peripheral phloem strands in foliar bundles; raphides 0 [in vegetative plant]; SiO2 bodies epidermal, stomata anomocytic; leaves spiral, isobifacial, (margin serrulate), sheath well developed, bases persisting; P = T, T dry; A ± adnate to base of T; septal nectaries +; ovule 1/carpel, ascending, epitropous[?], micropyle bistomal (zig-zag), outer integument 6-8 cells across, parietal tissue ca 2 cells across, nucellar cap ca 2 cells across; fruit indehiscent, T persistent; seeds rounded, testa pale yellow; endosperm type?
4[list]/16 - two groups below. West Australia, Victoria. [Photo - Habit, Flowers].
1. Dasypogoneae Engler
Stem erect, woody, or plant rhizomatous, or with stilt roots; (chelidonic acid + - Dasypogon); SiO2 bodies sand-like; hairs branched; raphides only in flowers; SiO2 epidermal; stomatal accessory cell ontogeny odd; bundle girders 0, enclosing three vascular bundles; (leaves bifacial); inflorescence axillary, capitate and scapose, or flower single; T, or outer whorl only, connate, tube short; (anthers centrifixed, dehiscing by pores - Calectasia); (G unilocular, septal nectaries 0 - Calectasia); storage nucellus massive, starchy; tegmen collapsing; n = 7, 9; cotyledon not photosynthetic, mesocotyl and coleoptile +.
2/14. S.W. Australia; South Australia/Victoria (map: from Barrett & Dixon 2001; FloraBase 2004).
Synonymy: Calectasiaceae Endlicher
2. Kingieae Horaninow
Stem erect, growth monopodial, with epicortical roots (Kingia), or subrhizomatous; SiO2 bodies druse-like; substomatal cells distinctive; leaf bundle girders + [originating in mesophyll]; inflorescence axillary, with inflorescence bracts, capitate, surrounded by bracts [Kingia, or flower single, terminal; flower large [Baxteria, ca 8 cm long]; T free; pollen extended sulcate [unipantocolpate]; stylar canals 3 - Kingia); storage nucellus well developed; (fruit explosively loculicidal + septifragal, vales separating periclinally and acropetally - Baxteria); n = 7; seedling?
2/2. S.W. Australia (map: from FloraBase 2004).
Synonymy: Baxteriaceae Takhtajan, Kingiaceae Schnizlein
Evolution. Divergence & Distribution. Stem group Dasypogonaceae are dated to ca 119 m.y., divergence within crown group Dasypogonaceae to ca 100 m.y. (Janssen & Bremer 2004: they place Dasypogonaceae rather near the base of the commelinids). Magallón and Castillo (2009) estimate ages of ca 128 and 115 m.y. for relaxed and constrained penalized likelihood datings for stem group Dasypogonaceae. Dasypogon and Calectasia may have diverged 49-41 m.y.a. (Wikström et al. 2001).
Chemistry, Morphology, etc. Some species of Calectasia have stilt roots. Both Calectasia and Baxteria have single flowers surrounded by numerous bracts. Calectasia has a 1-locular ovary (Barrett & Dixon 2001: monograph). In Kingia the apical meristem is depressed, as in Arecaceae, and the plant is also monopodial; adventitious roots grow down to the ground in persistent sheathing leaf bases.
Additional information is taken from Chanda and Ghosh (1976: pollen), Rudall (1994: embryology), Clifford et al. (1998b: general), and Rudall and Conran (2012: floral morphology).
Phylogeny. See Rudall and Chase (1996) for the dismemberment of the old Xanthorrhoeaceae and the relationships of the genera of Dasypogonaceae.
Previous Relationships. Dasypogonaceae have often been linked with other similar-appearing xeromorphic monocots from Australia such as Xanthorrhoeaceae and Lomandraceae, as in Takhtajan (1997); for the two, see Asparagales as Xanthorhoeaceae-Xanthorhoeoideae and Asparagaceae-Lomandroideae.
Classification. The name Dasypogonales Doweld is available for this clade if needed, but if Dasypogonaceae are sister to Arecaceae, Arecales can be expanded to include both families.
ARECALES Bromhead Main Tree.
Growth monopodial, plant unbranched, stem well-developed, woody; vessels also in stem and leaf; cuticular waxes as aggregated rodlets, stomata tetracytic; leaves spiral, massive, vernation reduplicate-plicate, pinnately pseudocompound, petiolate, with closed sheath; flowers ± sessile; septal nectaries +; ovule 1/carpel, apotropous, sessile, attachment broad; seeds large [>1 cm long].
1 family, 183 genera, 2361 species.
Evolution. See below, after the family.
Synonymy: Cocosales Nakai
ARECACEAE Berchtold & J. Presl, nom. cons.//Palmae Jussieu, nom. cons. et nom. alt. Back to Arecales
Flavonoid sulphates abundant; roots lacking real elongation zone, with radially elongated air spaces; sieve tubes with simple sieve plates; endodermal cells with O-shaped thickenings; cellulose fibrils in the outer epidermal walls randomly oriented; SiO2 bodies spherical, often spiny-verrucate, esp. associated with fibre bundles or vascular bundles; leaf epidermal cells rectangular, hypodermal cells rectangular, longitudinally elongate; stomatal subsidiary cells with oblique cell divisions; fibre strands +, both free in mesophyll and attached to epidermes, sheaths of transverse veins fibrous, centrifugal differentiation of fibrous phloem cap of fibrovascular bundle; plant monoecious; inflorescence axillary, with basal bicarinate prophyll, inflorescence units cymose, prophylls lateral [units are cincinni]; staminate flowers: A basifixed, (many, but basically trimerous); pistillode ± +; pistillate flowers: staminode +; G 1-4 [2-10]; outer integument 8+ cells across, inner integument 2-3 cells across, parietal tissue (0)1-5(-6) cells across; (postament +), suprachalazal area ± massive; micropylar embryo sac haustorium +; fruit with outer layer with vascular bundles; seeds 1(-3)/fruit, rounded; testa usually with two outer layers thickened, (basal portion vascularized); micropylar endosperm haustorium +, endosperm with hemicellulose [mannans], thick-walled; cotyledon not photosynthetic, collar short (with roots), primary root strong, branched.
183[list]/2361 - five groups below. Humid tropics and subtropics (warm temperate), Africa is relatively depauperate. [Photo - Flowers, Fruits.]
1. Calamoideae Beilschmied
Plant spiny; sustained primary growth slight-0; root periderm 0; 1 (2) vessels/fibrovascular bundle; epidermal cells rectangular, anticlinal walls sinuous; adaxial subepidermal fibre bundles +; parenchyma cells near protoxylem inflated (not), longitudinal veins bridging to adaxial epidermis via vertically-elongated sclereids, lateral veins adaxial to longitudinal veins, adaxial non-vascular fibres subepidermal; internodes usu. well-developed; flowers in dyads; C valvate, basally connate; ovule basal, epitropous[?], [funicle twisted]; fruit covered by reflexed scales.
21/615. Tropical, but esp. Sri Lanka to West Samoa and Fiji.
1a. Eugeissoneae W. J. Barker & J. Dransfield
Growth sympodial [hapaxanthic]; endodermal cell walls barely thickened; SiO2 bodies minute, disciform; inflorescence terminal, inflorescence units surrounded by cupule of 7-11 overlapping bracts; diad with staminate and perfect flowers; flowers large [to 7 cm long]; K connate, C woody; stamens numerous; scales small; mesocarp forming stony layer, with carpel plus additional bundles, lignified, ridged, endocarp massive, becoming crushed; seeds longitudinally ruminate; n = ?
1/6. S. Thailand to Borneo (Map: from Dransfield et al. 2008).
1b. The Rest.
Plant often lianes, climbing by ± recurved spiny structures; (leaves palmate); (inflorescence axes adnate to the internode above, or to sheath of the leaf of the next node); breeding system various; (C free); A <12; (pollen equatorially disulcate - Calameae); (style branched); fruit dry, pericarp not woody, (berry), scales large, endocarp thin; seeds 1-3, sarcotesta +, usually thick, (testa thin, dry); n = 13, 14.
20/600: Calamus (375), Daemonorops (100). Tropical, but esp. Sri Lanka to West Samoa and Fiji (map: from Uhl & Dransfield 1987).
Synonymy: Calamaceae Perleb, Lepidocaryaceae Martius, Sagaceae Schultz-Schultzenstein
[Nypoideae [Coryphoideae, Ceroxyloideae, Arecoideae]]: sustained primary growth +; root periderm +; 2 (1, 3, 4) vessels/fibrovascular bundle; anticlinal epidermal walls ± straight, adaxial subepidermal fibre bundles 0.
2. Nypoideae Griffith
Growth sympodial, stem dichotomously branched; endodermal cell walls barely thickened; no centrifugal differentiation of fibrous phloem cap of fibrovascular bundle; epidermis with hydathodes, epidermal cells hexagonal to spindle-shaped, guard cells with several ledges [in t.s.], SiO2 bodies small, hat-shaped; hypodermal cells several layered, lignified, hexagonal, transversely elongate, veins bridging to epidermis via vertically-elongated sclereids, sheaths of transverse veins sclereidal, veins sinuous, irregular; inflorescence terminal, inflorescence axis adnate to the internode above, racemose, staminate inflorescence a spike, carpellate inflorescence a head; C free; staminate flowers: P undifferentiated; A 3, opposite outer P, connate, extrorse; pollen with encircling sulcus; pistillode 0; carpellate flowers: staminodes 0; G 3 (4), margins conduplicate, placentation laminar to submarginal; ovule [position?], outer integument ca 10 cells across; n = ?17.
1/1: Nypa fruticans. Bengal to Queensland (map: current distribution in red, from Uhl & Dransfield 1987; Spalding et al. 2010; fossil records from places outside this area in blue, from Plaziat et al. 2001).
Synonymy: Nypaceae Le Maout & Decaisne
[Coryphoideae [Ceroxyloideae + Arecoideae]]: sieve tube with compound sieve plates; endodermal cell walls with U-shaped thickenings (thickened all around); (leaf veins bridging to epidermis by fibres); microsporogenesis simultaneous; (postament +).
3. Coryphoideae Burnett
(Stem branched - e.g. Caryota); septate fibres +; no centrifugal differentiation of fibrous phloem cap of fibrovascular bundle; no fibre bundles free in mesophyll, longitudinal veins with ad/abaxially elongated bridging sclereids, transverse veins with broad sheath of fibres, adaxial vein rib with 5 or more independent vascular bundles; leaves palmate or costapalmate (pinnate), induplicate; inflorescence various, (terminal; adnate to the internode above; plant monoecious - Caryotinae), flowers solitary or in cincinni (triads); C often valvate, connate (free); microsporocyte with callose ring [not Caryota, Bismarckia]; G free, (1), or postgenitally connate by style, or style present, with 3 [Coryphinae] or 1 [Sabalinae] stylar canals, or style 0 [Caryoteae].
45/ca 500: Coccothrinax (50). Pantropical (to warm temperate), fewer in South America, quite frequently outside tropical rain forest (map: from Uhl & Dransfield 1987).
Synonymy: Borassaceae Schultz-Schultzenstein, Coryphaceae Schultz-Schultzenstein, Phoenicaceae Burnett, Sabalaceae Schultz-Schultzenstein
[Ceroxyloideae + Arecoideae]: petiole bundles arranged in one or more Vs (scattered); sheaths of transverse veins sclereidal, veins sinuous, irregular, epidermal cells hexagonal to spindle-shaped.
4. Ceroxyloideae Drude
Plant dioecious, or flowers perfect; inflorescence racemose, spicate; (K and C elongate); (A numerous, not trimerous, centrifugal - Phytelepheae); (seeds more than 3).
8/42. Mostly Central and W. South America, also N.E. Australia, Madagascar, Florida and the Antilles (map: from Uhl & Dransfield 1987).
Synonymy: Phytelephantaceae Perleb
5. Arecoideae Beilschmied
(Stem with crownshaft [formed by elongated leaf sheaths]); (SiO2 bodies hat-shaped); hypodermal cells hexagonal, transversely elongate; (plant dioecious); flowers in triads [central (upper) flower carpellate, lateral flowers staminate] or in two vertical rows [acervuli], (inflorescences spicate); (1 G fertile), style branches separate (style single, short or long); (inner integument ca 7 cells across - Cocos); n = 16.
112/1100: Bactris (240), Dypsis (140), Pinanga (120), Chamaedorea (110), Geonoma (75), Desmoncus (65<), Areca (60), Astrocaryum (50). Pantropical, the most diverse subfamily in South America (map: from Uhl & Dransfield 1987).
Synonymy: Acristaceae O. F. Cook, Ceroxylaceae Vines, Chamaedoraceae O. F. Cook, Cocosaceae Schultz-Schultzenstein, Geonomataceae O. F. Cook, Iriarteaceae O. F. Cook & Doyle, Malortieaceae O. F. Cook, Manicariaceae O. F. Cook, Moreniaceae O. F. Cook, Pseudophoenicaceae O. F. Cook, Synechanthaceae O. F. Cook
Evolution. Divergence & Distribution. Stem Arecaceae are dated to ca 120 m.y., divergence within the crown group to ca 110 m.y. (Janssen & Bremer 2004), or comparable dates are 99-91 and 73-63 m.y. (Wikström et al. 2001). Magallón and Castillo (2009) estimate ages of ca 128 and 115 m.y. for relaxed and constrained penalized likelihood datings for stem Arecales.
Fossil Arecaceae date to ca 93 m.y. (Pan et al. 2006; Harley 2006), and palm pollen was abundant in tropical Gondwanan areas during the later Cretaceous (Nichols & Johnson 2008). Palm leaves, pollen and/or wood are quite common and widely distributed in the later Cretaceous when global temperatures were warmer (Burnham & Johnson 2004), even in Africa and India where palms are not very diverse today. Palm pollen is even known from palaeo 85o N sediments dated to 53.5 m.y. in the Eocene on the Lomonosov Ridge (Sluijs et al. 2009) and from palaeo 70o S sediments dated to ca 51.9 m.y. in the Eocene off Wilkes Land in the Antarctic (Pross et al. 2012).
Palm fossils are used as climatic markers by palaeontologists (e.g. Greenwood & Wing 1995; Sluijs et al. 2009) based on the climatic restrictions of present-day palms. Palms are very susceptible to frost, most having only a single vegetative meristem and being unable to produce replacement meristems if the first is killed. They are usually found in places where the mean annual temperature is more than 10°, mean temperatures in the coldest month are more than 5°, and the coldest temperature does not dip below -10° (Larcher & Winter 1981; Greenwood & Wing 1995; Tomlinson 2006; Couvreur et al. 2011c; Kissling et al. 2012b). By the Oligocene extra-tropical climates in general were becoming more seasonal, and so less favourable for palms.
It is suggested that Arecaceae have diversified at a constant rate since their origination in the Cretaceous ca 100 m.y. or more ago (perhaps in Laurasia) until ca 24 m.y.a., the K/T boundary passing unmarked (Couvreur et al. 2011b, esp. c). Palms then serve as markers for tropical rainforest - or perhaps a tropical rain forest-like biome (Couvreur et al. 2011b). This being said, the early evolution of the rain forest biome is still not well understood. Coiffard and Gomez (2009) even suggest that early palms may have been swamp dwellers like living basal Arecales (they list Calamus, Nypa, and Mauritia). Fossils (leaf, stem, fruit) from rocks in Texas of Cretaceous-Campanian age some 77 m.y. old have been identified as the modern genus Sabal; young dinosaurs might have eaten their fruits (Manchester et al. 2010a).
The past and present distributions of palms are sometimes difficult to reconcile. Lodoicea is currently restricted to the Seychelles, although its fruits are widely distributed by the sea; ocean crust separating India and the Seychelles dates to ca 63.4 m.y. (Collier et al. 2008), so either Lodoicea is that old, or it has somehow moved onto these islands. Distinctive Nypa seems to have had a more or less world-wide distribution in the early Tertiary, fossils being known from Tasmania, England (the London Clay flora), both Americas, etc. (Plaziat et al. 2001: see map above). Pollen of some species of the West Malesian Eugeissona is distinctive, being thick-walled and extended monosulcate; such pollen has been found throughout the tropics (Dransfield et al. 2008: records need checking). Wood of Coryphoideae-Crysophileae, a New World group, has been found in Lower Oligocene to Upper Miocene deposits in France (Thomas & de Franceschi 2012). Finally, calamoid palm leaves and fruits are found in Late Eocene rocks on the very southern part of New Zealand (Hartwich et al. 2010); the closest Calamoideae grow in eastern Australia, a rather less dramatic range difference than for Nypa, but still noteworthy.
Despite the size of the palm plant and the size of the fruit, dispersal rather than vicariance is increasingly frequently being invoked to explain many apects of the present distribution of the family (Baker & Couvreur 2012a, b). The scattered and apparently ancient Gondwanan distribution of Ceroxyloideae is probably best explained by several mid-Tertiary trans-oceanic dispersal events (Trénel et al. 2007). Species of Hyophorbe (Arecoideae-Chamaedoreeae) are disjunct on the Mascarenes, and the genus may have radiated in that area on islands that are now submerged, hopping from island to island (Cuenca et al. 2007); some Myrtaceae, Begoniaceae, and Sapotaceae may also be island-hoppers.
In Africa palms became less common at the beginning of the Tertiary and again at the end of the Eocene ca 34 m.y.a. (Pan et al. 2006; Harley 2006: summary of the fossil record; Kissling et al 2012a); overall, the paucity of palms on the continent can perhaps be explained by the increase in diversifications rates elsehwhere (Baker & Couvreur 2012b). The diversity and diversification of palms in the New World and the Indo-Malayan areas has been linked to the persistence of the relatively warm and wet areas that they favour, and also the environmental heterogeneity of those areas (Svenning et al. 2008; Kissling et al. 2012b; Baker & Couvreur 2012b). Arecoideae-Bactridineae diverged in America at the end of the Eocene (Eiserhardt et al. 2011a); for details of diversification of palms worldwide, see Kissling et al. (2012a, b) and Baker and Couvreur (2012a, b). Roncal et al. (2008) explored the biogeography of Antillean palms and Roncal et al. (2010) examined the biogeography of the mostly understorey Geonomateae. Here crown group divergence began in the Oligocene and species are older than Quaternary refugium theory would predict; again, there seems to have been considerable dispersal. In the Old World, Couvreur et al. (2011b) suggest that the stem age of Calamus, currently with some 400 or more species, is only 24 m.y.a. Although palms are poorly represented in Africa, they are richer in Madagascar (Snow 1981); the radiation of Dypsis there - some 140 species - is particularly spectacular.
Ecology & Physiology. Eiserhardt et al. (2011b) think about the distribution of palms world-wide in the context of ecological determinants both of geography and diversity. The suspects are very much as one might expect, with climatic limitations (see above) having a major effect on broad-scale patterns while dispersal affects patterns at all scales. Interestingly, over two thirds of the palm genera that grow outside tropical rainforest are members of Coryphoideae (Thomas & de Franceschi 2012).
Arecaceae include many examples of the eco-morphological combination of shaded conditions, net-veined leaves and fleshy fruits that has evolved several times in monocots (Givnish et al. 2005, 2006b) and may be very conspicuous elements of the vegetation. Nypa dominates some mangrove habitats, preferring less saline conditions than many other mangrove plants; it is found along rivers up to the limit of tidal influences (for the evolution of the mangrove habitat, see Rhizophoraceae; see also Clade Asymmetries). Calamoid palms are a very important liane group in the South East Asian forests (Gentry 1991).
Arecaceae are the largest clade of woody monocots (bamboos are the other large woody clade). They have the oldest functioning xylem elements and sieve tubes in vascular plants, but how the conducting system remains functional is unknown. Since the oldest palm is hundreds of years old and there is no secondary thickening, the vascular tissue at the base of the stem must remain active for the whole life of the plant. However, old palm stem are not inert. Thus Renninger and Phillips (2012, 2013; c.f. Tomlinson & Quinn 2013) found that the stems of Iriartea, at least, can lengthen appreciably, and this was accompanied by a straightening of the spiral course of the vascular bundles; lengthening has also been noticed in other palms (Waterhouse & Quinn 1978). The walls of vascular fibres continue to thicken, so increasing stem stiffness as the tree grows bigger (Tomlinson et al. 2011). Ground tissues in both stem and root may remain undifferentiated for some time, with limited mitosis and/or cell expansion and/or formation of schizogenous lacunae occurring and the trunk markedly thickening and lengthening (diffuse secondary thickening - Tomlinson 1961c; sustained primary growth Waterhouse & Quinn 1978; see also Tomlinson et al. 2009, 2011). This ability of cells to remain metabolically active may help explain the functional longevity of palm vascular tissue. (At least some palms are reported to have monocot-type secondary thickening [Angyalossy et al. 2008], perhaps the same as this sustained primary growth.) Waterhouse and Quinn (1978) suggested that in some palms there was initially sustained primary growth and then there was a change to growth in which the palm trunk did not increase in width and was strictly columnar. Tomlinson and Huggett (2012) concluded that metabolically functioning cells in palms were extremely old. However, the longevity of cells in seed plant vascular tissue in general would repay investigation - some xylem parenchyma cells even in broad-leaved angiosperms may remain metabolically active for 200 years or so (Spicer & Holbrook 2007), xylem in lianas perhaps being particularly long-lived (refs in Angyalossy et al. 2012).
Vessels in Rhapis excelsa are quite resistant to embolism, but what goes on in the very long vessels of some calamoid palms - some over 0.5 mm wide and to almost 4 m long, and spanning (8-)13(-18) internodes - is unclear (Sperry 1986; Fisher et al. 2002; Tomlinson 2006b); Tomlinson (2006b) thought of xylem function in the context of stem length. However, Davis (1961) noted that root pressures in several palms he studied in India were very high, sometimes exceeding the height of the plant, and this could help remove cavitations (see also Cao et al. 2012).
Plant-Animal Interactions. Satyrinae-Morphini butterfly larvae may be found on Arecaceae, along with larvae of Hispinae-Cassidinae beetles; these latter can be serious pests of oil palms and other commercial or ornamental palms (Chaboo 2007). Stem Bruchinae - the highly speciose seed beetles, now found mostly on Fabaceae - are about 85-82.6 m.y. old (age spread far greater); that is, they evolved long before Fabaceae, and their original diet may have been seeds of Arecaceae (Kergoat et al. 2011). A male of the (now) palm-eating Pachymerini was found in Canadian amber dated at ca 79 m.y. (Poinar 2005)
Pollination Biology & Seed Dispersal. Pollination is predominantly by insects, whether beetles (mainly Nitidulae and Cuculionidae-Derelomini [weevils]), bees, especially Halictidae (sweat bees) and Meliponini (stingless bees), and flies, which may visit especially understorey palms (Henderson 1986, 2002; Barfod et al. 2011). However, there is no clear correlation of pollen morphology with pollinator (Sannier et al. 2009). There may be mimicry of male by female flowers in Geonoma (Stauffer et al. 2002 and references), but presentation of the nectar of both flower types in a similar fashion (c.f. Meliaceae) may be another explanation. Volatiles produced by the leaves of Chamaerops humilis attract its weevil pollinator (Dufaÿ et al. 2003), while thermogenesis has been detected in the flowers of some Arecaceae (Seymour 2001). The speciose New World Chamaedoreeae (Arecoideae) all have raphides in the flowers and in Chamaedorea these are particularly common in the perianth and gynoecium; there are other potentially protective structures in the flowers (Askgaard et al. 2008).
Seed size increased considerably in stem Arecaceae (Moles et al. 2005a; Linkies et al. 2010: Sims 2012). This may be associated with their woody habit, but seeds of Arecaceae are absolutely large when compared with those of all other angiosperms. Their dispersal is primarily by animals, although Cocos nucifera, dispersed by sea currents, is a notable exception (Zona & Henderson 1989; Henderson 2002).
Vegetative Variation. Seedling morphology is very variable within Arecaceae (Henderson 2002, 2006; Tillich 2007). In palms with aerial stems there is usually a period of establishment growth of the seedlings that may last up to 50 years (Henderson 2002 and references). During this time the apical meristem becomes gradually larger, as does the width of the axis it produces, and only when it has reached adult size does elongation growth of the trunk occur (but see above). With some exceptions, the size of the apical meristem and hence the width of the trunk remains constant for rest of the life of the palm. Iriarteeae (Arecoideae) are one of those exceptions. Here there is no underground establishment growth, and the trunk becomes gradually wider as it grows, being narrowly obconical overall. A plant with such a stem is obviously highly unstable, but massive prop roots develop from the lower part of the trunk and stabilise it. The base of the stem rots away, the older plant then depending entirely on its prop roots.
Despite appearances, the leaves of all palms are simple. The deep lobes in simple palm leaves and the leaflets in apparently compound leaves, are commonly thought of as being the result of cell death. However, a detailed study of species of Chamaedorea showed that the process is more like abscission (Nowak et al. 2007, 2008), although nothing (apart, sometimes, from the lamina margin, see below) falls off. The parts that will separate first become thin, then split; tissue at the zone of separation becomes lignified, suberised, or covered by a cuticle, so protecting the rest of the blade. Details of this process differ even between closely-related species, and depend on the timing of events (Nowak et al. 2007, 2008). In a number of palms thin "reins" hang down from the sides of the leaves; these are the lamina margins of the originally simple blade. Fibrous filaments occuring between the leaflets is other evidence for the originally simple nature of the leaf. Given the distinctive nature of compound palm leaves, it is not surprising to find that KNOX genes are not involved in their development, although they are in the compound leaves of broad-leaved angiosperms (Nowak et al. 2011).
Fibers at the bases of the leaves are produced by the decay of the sheaths, while the spines found on so many palms are produced in various ways. They may be modified leaflets (Phoenix), adventitious roots (Crysophila, but relatively uncommon), partly detaching outer parts of the stem that become erect, etc. (Tomlinson 1962b; Tomlinson et al. 2011).
Many Calamoideae (the rattans) and some Arecoideae (Desmoncos), are climbers, either by the aid of a long, hook-bearing apical portion of the leaf, the cirrus, and also, in Calamus, etc., a very much modified long and very thin inflorescence axis with recurved spines, the flagellum, that is adnate to the sheath of the leaf at the node above. Although these climbing aids are remarkably effective (Calamus is sometimes called the lawyer vine, because once you are caught by the the flagellum, it can be very difficult to get free), they eventually fall off with the leaves, and the stems, which can reach lengths of up to some 200 m, then tend to sag (Isnard & Rowe 2008 for details).
Dichotomous branching is scattered in the family, having first been recorded from Hyphaene thebaica by Schoute in 1909 (Fisher 1974 and references).
Genes & Genomes. The rate of molecular evolution in Arecaceae is rather low, as might be expected from a woody plant with a relatively long generation time, and is ca 0.0014 substitutions/site/m.y.; this is interpreted as a reduction in the rate of molecular evolution (Smith & Donoghue 2008; also Gaut et al. 1996: comparison between Poaceae and Arecaceae).
Economic Importance. Domestication and cultivation of the coconut, Cocos nucifera Arecoideae-Cocoseae), seems to have occurred independently in southern India and the Malesian archipelago (Gunn et al. 2011). There is much debate as to where Cocos originated. Gunn (2004) suggested that it it might be sister to the New World Parajubaea and be at least 22 m.y. old, while Meerow et al. (2009a, esp. b) found a sister relationship with the New World Syagrus from which it diverged (39.5-)34.9(-20.7) m.y.a., crown group divergence beginning ca 11 m.y.a. (Meerow et al. 2009b: 95% HPD limits). On the other hand, Kapgate (2009) found fruits in the Deccan Intertrappean Beds that are of Late Cretaceous to Early Tertiary age (ca 65.5 m.y.: Gómez-Navarro et al. 2009 for additional references) and Gómez-Navarro et al. (2009) found fruits that they compared with Cocos from northern Colombia that are perhaps a little younger - about 58 m.y. old... Something is wrong.
Elaeis guineensis (also Cocoseae), the oil palm, is a major tropical plantation crop; its cultivation has been responsible for particularly massive deforestation.
Chemistry, Morphology, etc. Horn et al. (2008, 2009b, 2010a, esp. 2009b) and especially Tomlinson et al. (2011) look at various aspects of lamina anatomy in the context of the phylogeny of the family; this has in part been integrated above, but there is widespread homoplasy in the characters. Parthasarathy (1974) described phloem development. According to Arber (1925), the vascular bundles are not amphivasal. "Leaflets" of induplicate leaves are V-shaped in cross section, those of reduplicate leaves are inverted V-shaped (see also Kaplan 1997, vol. 2: chap. 17 for leaf morphology).
For variation in details of the inflorescence units in Arecoideae-Chamaedoreae, which have acervuli, modified largely ebracteate cincinni, see Uhl and Moore (1978), Cuenca et al. (2009), and Ortega-Chávez & Stauffer 2011). The flower in general (e.g. Rudall et al. 2003b; Uhl & Moore 1971) and pollen in particular (see Harley 1999b; Harley & Baker 2001) is remarkably variable. The stamens are never adnate to the corolla/inner tepals in staminate flowers, although in carpellate flowers of Roystonea the corolla has a broad staminal cup at the base, and in carpellate flowers of Geonomeae (Arecoideae), both the calyx and corolla are connate and the stamens are adnate to the latter (Stauffer & Endress 2003); the style there is more or less gynobasic. Nadot et al. (2011) map androecial evolution on a phylogenetic tree; developmental details of polyandrous flowers vary considerably, but apart from Phytelepheae, the androecium is basically trimerous. Microsporogenesis is simultaneous in some Coryphoideae and Arecoideae (Harley 1999a; Sannier et al. 2006). Variaton in gynoecial development is especially pronounced in Coryphoideae, where there are all intermediates between syncarpous and apocarpous gynoecia, and sometimes only a single carpel; all told, apocarpy has probably evolved some four times within Arecaceae (Rudall et al. 2011b). Cocos may have a bisporic 8-nucleate embryo sac and ovules that lack parietal tissue (Robertson 1976). For details on the development of the pericarp, see Bobrov et al. (2012a, b); Dransfield et al. (2008) note that the stony layer of Eugeissona differs from that of other Arecaceae. In Voaniola n = 298 or more.
Students of palms are fortunate in having a series of major works devoted to the family; these include von Martius's (and collaborators) magnificent Historia naturalis palmarum (1823-1850 - see also Martius 2010), surely one of the greatest of all botanical publications, Corner (1966), Uhl and Dransfield (1987), Tomlinson (1990), Henderson (2002), Dransfield et al. (2005, 2008) and Tomlinson et al. (2011).
Additional information may be found in Moore (1973), Zona (1997: esp. south east U.S.A.), Dransfield and Uhl (1998), and Tomlinson (2006a), all general, Uhl (1972: Nypa), Tomlinson (1970: vascular organization in the stem), Tomlinson (1974: stomatal development), Uhl and Moore (1971: gynoecium), Seubert (1998 and references: root anatomy), Thomas and di Franceschi (2013: stem anatomy), Harley and Dransfield (2003: triporate pollen), Zona (2004: embryo raphides), Prychid et al. (2004) and Piperno (2006), both SiO2 bodies/phytoliths, Bjorholm et al. (2006: patterns of diversity in neotropical subfamilies, the Antilles excluded), Henderson (2006: detailed descriptions of germination, not integrated with phylogeny), Gunawardena and Dengler (2006: leaf development), Sannier et al. (2007: microsporogenesis evolution, Ceroxyloideae not included), Essig (2008 and references: pericarp anatomy), Stauffer et al. (2009: labyrinthine nectaries), and Romanov et al. (2011 and references: fruit anatomy).
Phylogeny. [[Nypoideae + Calamoideae] (strong support for that clade) + the rest of the family (moderate support)] formed a trichotomy in a three-gene study by Asmussen et al. (2000); other characters supported these general relationships. Soltis et al. (2007a) also recovered a well-supported clade [Nypoideae + Calamoideae]. However, Calamoideae were probably sister to all other Arecaceae in other studies, if some morphological groupings were not supported by molecular data (Hahn 2002a, b; see also Baker et al. 1999a; Asmussen & Chase 2001; Lewis & Doyle 2001). Henderson and Stevenson (2006), after a analysis of morphological and anatomical features for selected genera, discussed groupings, relationships and character evolution. They found that Phoenix and Thrinax appeared as successively sister to the rest of the family, which seemed even then rather unlikely. However, Asmussen et al. (2006: very good generic-level sampling, four genes) clarified this confusion and presented the rather well supported set of relationships summarized in the tree here; those parts less well supported (the monophyly of Ceroxyloideae and Arecoideae) were strongly supported by low copy number nuclear DNA data (W. J. Baker, unpubl. data, in Asmussen et al. 2006). These relationships were confirmed in the comprehensive analysis of Baker et al. (2009), although the position of Nypoideae was less well supported than that of the other subfamilies.
For morphology, phylogeny and classification in Calamoideae, see Baker et al. (1999b, 2000a, b, c); there are three main clades, and Eugeissona is probably sister to the rest. Coryphoideae include Arecoideae-Caryoteae, previously placed in Arecoideae (Uhl and Dransfield 1987; see also Dransfield et al. 2008a for a phylogeny). Ceroxyloideae include Phytelephantoideae (Dransfield et al. 2005). Phytelephas and its relatives have 4-merous flowers with up to 1000 centrifugal stamens (Palandra) and 10 carpels; Palandra also has monopodial flower clusters, unique in the family.
Baker et al. (2011, 2012) examined phylogenetic relationships within Arecoideae; tribes were monophyletic, but relationships within the large Areceae were unclear (see also Lewis & Doyle 2002; Baker et al. 2006). Norup et al. (2006) discuss generic limits in Areceae; a distinctive crown shaft is a tribal apomorphy. Gunn (2004) provided a phylogeny of Cocoseae and and Eiserhardt et al. (2011a) that of the spiny Neotropical Bactridinae, which includes the climbing Desmoncus. Cuenca and Asmussen-Lange (2007) and Cuenca et al. (2007, 2008) discuss the phylogeny and biogeography of the largely New World understorey Chamaedoreeae; for the phylogeny of Chamaedorea itself, see Thomas et al. (2006).
Classification. Dransfield et al. (2008, see also Dransfield et al. 2005) present the classification followed above. Arecoideae above are the Arecoideae of Uhl and Dransfield (1987), but minus Caryoteae, and they also include Ceroxyloideae-Hyophorbeae (Hahn 2002b; also Baker et al. 1999a), basically, the arecoid line of Moore (1973: see Dransfield et al. 2005). Govaerts and Dransfield (2005) provide a checklist for the family, for which, see also the World Checklist of Monocots, but the best - and ever improving - resource for the family is PALMweb.
Previous relationships. The old Spadiciflorae included those taxa with a spadix and often also a spathe. Families included, Pandanaceae, Cyclanthaceae, Araceae and Arecaceae, are now placed in three immediately unrelated orders, Pandanales, Alismatales and Arecales. Engler (1892) linked Pandanaceae, Arecaceae and Cyclanthaceae.
Botanical Trivia. Arecaceae have the largest leaf - Raphia sp., ca 25 x 3 m; the largest inflorescence - Corypha umbraculifera, ca 7.5 m long with some 10,000,000 flowers and 5280 m of flower-bearing axes (Tomlinson & Soderholm 1975); the largest seed - Lodoicea maldavica, to 50 cm long and 15-30 kg, which in turn produces the longest cotyledon (strictly speaking, an apocole or elongated, unifacial, non-photosynthetic part of the cotyledonary hyperphyll) which may be "several yards" or "twelve feet or more" long (Thiselton-Dyer 1910); the longest stems, perhaps up to 200 m long in Calamus manan; the oldest functioning xylem elements and sieve tubes - palms can be hundreds of years old, and there is no secondary thickening; and perhaps the longest vessels, to 3.96 m long in some calamoid palms. They also have close to the oldest viable seeds; a seed of Phoenix dactylifera perhaps 2,000 years old has recently been germinated (Sallon et al. 2008; see also Kew Magazine, Winter 2008: 28-31).