EXTANT SEED PLANTS
Plant woody, evergreen; nicotinic acid metabolised to trigonelline; primary cell walls rich in xyloglucans and/or glucomannans, 25-30% pectin [Type I walls]; lignins rich in guaiacyl units; true roots present, apex multicellular, xylem exarch, branching endogenous; arbuscular mycorrhizae +; shoot apical meristem multicellular; stem with ectophloic eustele, endodermis 0, xylem endarch, branching exogenous; vascular tissue in t.s. discontinuous by interfascicular regions; vascular cambium + [xylem ("wood") differentiating internally, phloem externally]; wood homoxylous, tracheids +; tracheid/tracheid pits circular, bordered; sieve tube/cell plastids with starch grains; phloem fibers +; stem cork cambium superficial, root cork cambium deep seated; nodes ?; stomata ?; leaf vascular bundles collateral; leaves spiral, simple, axillary buds?, prophylls [including bracteoles] two, lateral, veins -5 mm/mm2 [mean for all non-angiosperms 1.8]; plant heterosporous, sporangia eusporangiate, on sporophylls, sporophylls aggregated in indeterminate cones/strobili; true pollen [microspores, i.e. no distal pore for release of gametes] +, grains mono[ana]sulcate, exine and intine homogeneous, ovules unitegmic, crassinucellate, 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, with cell walls, with many flagellae; female gametophyte endosporic, initially syncytial, walls then surrounding individual nuclei; seeds "large", first cell wall of zygote transverse, embryo straight, endoscopic [suspensor +], short-minute, with morphological dormancy, white, cotyledons 2; plastid transmission maternal; two copies of LEAFY gene, PHY gene duplication [N/O//A/C and P//BE lines], mitochondrial nad1 intron 2 and coxIIi3 intron present.
MAGNOLIOPHYTA
Plant woody, evergreen; lignans, O-methyl flavonols, dihydroflavonols, triterpenoid oleanane, non-hydrolysable tannins, quercetin and/or kaempferol +, apigenin and/or luteolin scattered, cyanogenesis via tyrosine pathway [ANITA grade?], lignins derived from both coniferyl and sinapyl alcohols, containing syringaldehyde [in positive Maüle reaction, syringyl:guaiacyl ratio less 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; stem with 2-layered tunica-corpus construction; wood fibers and wood parenchyma +; reaction wood ?, with gelatinous fibres; starch grains simple; primary cell wall mostly with pectic polysaccharides; tracheids +; sieve tubes eunucleate, with a sieve plate and cytoplasm with P-proteins, companion cells from same mother cell that gave rise to the sieve tube; nodes unilacunar [1:?]; stomata with ends of guard cells level with pore, paracytic, outer stomatal ledges producing vestibule; leaves with petiole and lamina [the latter formed from the primordial leaf apex], development of venation acropetal, 2ndary veins pinnate, fine venation reticulate, veins (1.7-)4.1(-5.7) mm/mm2, endings free; flowers perfect, polysymmetric, parts spiral [esp. the A], free, development in general centripetal, numbers unstable, P not differentiated, outer members not enclosing the rest of the bud, smaller than inner members, A many, with a single trace, introrse, filaments stout, anther ± embedded in the filament, tetrasporangiate, dithecal, with at least outer secondary parietal cells dividing, each theca dehiscing longitudinally by action of hypodermal endothecium, endothecial cells elongated at right angles to long axis of anther, tapetum glandular, binucleate, microspore mother cells in a block, microsporogenesis successive, walls developing by centripetal furrowing, pollen subspherical, binucleate at dispersal, trinucleate eventually, tectum continuous or microperforate, ektexine columellar, endexine thin, compact, lamellate only in the apertural regions, pollen germinating in less than 3 hours, tube elongated, growing at 80-600 µm/hour, with callose plugs and callose-based walls, penetrating between cells, siphonogamy, penetration of ovules within ca 18 hours, distance to first ovule 1.1.-2.1 mm, nectary 0, G free, several, ascidiate, with postgenital occlusion by secretion, few [?1] ovules/carpel, ovules marginal, anatropous, bitegmic, [outer integument often largely subdermal in origin, inner integument dermal], micropyle endostomal, integuments 2-3 cells thick, megasporocyte single, megaspore lacking sporopollenin and cuticle, chalazal, female gametophyte four-celled [one-modular, nucleus of egg cell sister to one of the polar nuclei], stylulus short, hollow, stigma ± decurrent, dry [not secretory]; P deciduous in fruit; seed exotestal; double fertilisation +, endosperm diploid, cellular [first division oblique, micropylar end initially with a single large cell, chalazal end more actively dividing], copious, oily and/or proteinaceous, embryo cellular ab initio, minute; germination hypogeal, seedlings/young plants sympodial; Arabidopsis-type telomeres [(TTTAGGG)n]; whole genome duplication, 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 PHYA + C/PHYB + E gene pairs.
Possible apomorphies are in bold. Note that the actual level to which many of these features, particularly the more cryptic ones, should be assigned is unclear, because some taxa basal to the [magnoliid + monocot + eudicot] group have been surprisingly little studied, there is considerable variation between families in particular for several of these characters, and also because details of relationships among gymnosperms will affect the level at which some of these characters are pegged.
NYMPHAEALES [AUSTROBAILEYALES [[CHLORANTHALES + MAGNOLIIDS] [MONOCOTS [CERATOPHYLLALES + EUDICOTS]]]]: vessels +, elements with scalariform perforation plates; ?genome duplication; "DEAER" motif in AP3 and PI genes lost, gaps in these genes.
AUSTROBAILEYALES [[CHLORANTHALES + MAGNOLIIDS] [MONOCOTS [CERATOPHYLLALES + EUDICOTS]]]: ethereal oils in spherical idioblasts [lamina and P ± pellucid-punctate]; tension wood 0; tectum reticulate-perforate, nucellar cap + [character lost where in eudicots?]; 12BP [4 amino acids] deletion in P1 gene.
[CHLORANTHALES + MAGNOLIIDS] [MONOCOTS [CERATOPHYLLALES + EUDICOTS]] : benzylisoquinoline alkaloids +; P more or less whorled, 3-merous [possible position], carpels plicate; embryo sac bipolar, 8 nucleate, antipodal cells persisting; endosperm triploid; ?germination.
MONOCOTS [CERATOPHYLLALES + EUDICOTS]: (A opposite [2 whorls of] P).
[CERATOPHYLLALES + EUDICOTS]: ethereal oils 0.
EUDICOTS: myricetin, delphinidin scattered, asarone 0 [unknown in some groups, + in some asterids]; root epidermis derived from root cap [?Buxaceae, etc.]; nodes 3:3; stomata anomocytic; flowers (dimerous), cyclic, K/outer P members with three traces, "C" with a single trace, A few, (polyandry widespread, from few initial [5, 10, ring] primordia), filaments fairly slender, anthers basifixed, microsporogenesis simultaneous, walls developing by centripetal furrowing, pollen with endexine, tricolpate, G with complete postgenital fusion, style solid [?here]; seed coat?
[[SABIACEAE + PROTEALES] [TROCHODENDRALES [BUXALES + CORE EUDICOTS]]]: (axial/receptacular nectary +).
PROTEALES Dumortier Main Tree, Synapomorphies.
Epidermal waxes with tubules [2/3], nonacosan-10-ol the main wax; nodes?; leaf teeth?; stipules surrounding stem [2/3]; 1-2 pendulous ovules/carpel [?really an apomorphy], stigma dry; seed coat?; endosperm development?, slight or 0, embryo long. - 3 families, 82 genera, 1610 species.
Evolution. Both Nelumbonaceae and Platanaceae are known as fossils from the Albian (the dates are ca 106 and ca 110 million years before present, respectively; for the former records, see Upchurch & Wolfe 2005), and Anderson et al. (2005, using both molecular and fossil data) date stem group Platanales from 121-119 million years before present, divergence beginning 121-115 million years before present. From the molecular point of view, at least, both Platanus and Nelumbo can perhaps be thought of as living fossils (Sanderson & Doyle 2001).
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).
Phylogeny. Chase et al. (1993) and Drinnan et al. (1995) found Platanaceae and Nelumbonaceae to be sister taxa. Indeed, although the order is small, it seems uncomfortably heterogeneous; it has moderate support in molecular analyses. For discussion on the phylogenetic position of Proteales, see the Ranuculales page.
Previous Relationships. Thorne (2007) includes the order, variously broken up, along with Sabiales and Buxales, in his hetereogeneous Ranunculidae, however, most authors (e.g. Cronquist 1981; Takhtajan 1997) have not seen any connections at all between the three families here.
Includes Nelumbonaceae, Platanaceae, Proteaceae.
Synonymy: Nelumbonales Willkommen & Lange, Platanales J. H. Schaffner - Proteanae Takhtajan, Nelumbonanae Reveal - Nelumbonidae Takhtajan - Nelumbonopsida Endlicher, Proteopsida Bartling
NELUMBONACEAE Berchtold & J. Presl, nom. cons. Back to Proteales
Aquatic herbs; aporphine alkaloids +; radicle aborts; 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 in groups of three along the stem, vertically two-ranked, sheathing cataphyll on one side then cataphyll and expanded leaf on the other side; leaf peltate, involute, main veins dichotomous, proceeding to margin, stipule sheathing, open; flowers ?axillary, large, with cortical vascular system; K 2, C 10-30, spiral, A many, from a ring meristem, at least outer extrorse, connective with a terminal appendage, receptacle massive, with emergent druses, G (2-)10-30, carpels ascidiate, immersed in receptacle, occluded by secretion, pollen canal long-papillate, one pendulous ovule/carpel, outer integument ca 30 cells and inner integument 8-10 cells thick, nucellar cap and funicular obturator +, antipodals multiplying, multinucleate, stylulus 0, stigma expanded, wet; fruit a nutlet, with an apical pore; seed ?pachychalazal, testa undistinguished; embryo green, large, with a tubular but basically double cotyledon, several leaf primordia, radicle aborting, roots adventitious; n = 8.

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.]
Evolution. Stem group Nelumbonaceae have been dated from 121-115 million years before the present (Anderson et al. 2005), while fossils of 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 early Cretaceous from the mid to late Albian (Upchurch & Wolfe 2005).
Vogel (2004a) provides 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 flowers are thermogenic, with breakdown of starch in the expanded receptacle (Vogel & Hadacek 2004; Watling et al. 2006; Li & Huang 2009). The sharp-pointed and often six-rayed epidermal druses on the surface of the receptacle may protect it against herbivores (Vogel 2004b).
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.
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, there is an endodermis present. The two sepals are inserted in the vertical plane. Stamens develop from an androecial ring, and they and the carpels may be irregularly whorled (Hayes et al. 2000). The pollen tectum is reticulate.
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; pollen morphology (Kreunen & Osborne 1999); and growth pattern (cf. Eichler 1878; Wignand & Dennert 1888; Miki 1926; Esau & Kosakai 1975).
Some general information is taken from Williamson and Schneider (1993) and Hayes et al. (2000), for chemistry, see Hegnauer (1969, 1990 - under Nymphaeaceae), for the receptacular druses, see Vogel (2004b).
Previous Relationships. Nelumbonaceae used to be associated with Nymphaeaceae (e.g. Cronquist 1981), the two having superficially similar flowers and vegetative body (both are aquatics). Takhtajan (1997) removed Nelumbonaceae from the vicinity of Nymphaeales, but considered it to be a very isolated group and placed it 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, the difference not emphasised by Barthlott et al. 2003).
Platanaceae + Proteaceae: woody; non-hydrolysable tannins, myricetin +, benzylisoquinoline alkaloids 0; (pits vestured); wood with broad rays [8+-seriate]; stomata laterocytic; flowers 4-merous [see fossil Platanaceae], stamens equal and opposite perianth members, carpels with 5 vascular bundles, hairy, postgenital fusion complete, ovules straight, style long; endosperm nuclear.
Evolution. 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, although the former have concave vessel-parenchyma festoons and the latter concave growth ring boundaries in common, in addition to their broad rays. These differences may be connected with the different climatic conditions under which the two groups grow (Baas et al. 2003). 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.
PLATANACEAE T. Lestibudois, nom. cons. Back to Proteales
Cork in outer cortex; nodes multilacunar; petiole bundle annular, wing bundles +; hairs candelabriform; growth sympodial; leaves two-ranked (spiral), plicate, teeth glandular, with a cavity, higher order veins approach but do not enter (margin entire), 2 strong 2ndary veins near base (pinnate; also seedlings), petiole enclosing the axillary bud (not), stipule tubular, closed (adaxial-sheathing, open); plant monoecious; inflorescences capitate; flowers with odd member of outer whorl abaxial, P connate or not, often lacking vasculature; staminate flowers: P ca 3, tiny, free, "ridged staminodes" +, anthers valvate, connective with subpeltate continuation above the anther, pollen semitectate-reticulate, 16-22 µm long, (pistillodes +); carpellate flowers: P 3-4, "ridged staminodes" +, staminodes +, G (3-)5-8(-9), two-whorled, 1(-2) pendulous ovules/carpel, inner integument ca 5 cells thick, stigma long, decurrent in two crests, ± dry; fruit an achene, with tuft of basal hairs; testa with hypodermal layer of thickened cells; seed reserves hemicellulosic; n = 16-21.

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.]
Evolution. Platanaceae are known fossil from the Lower Cretaceous, 98-113 million years before present (Platanocarpus - Crane et al. 1993). Anderson et al. (2005) date stem group Platanaceae to 119-110 million years before present. Fossils with the distinctive petiole bases of subgenus Platanus are abundant in the Palaeocene some 60 million years before present (Feng et al. 2005: note that subgenus Castaneophyllum [P. kerrii] lacks them).
The morphology of these fossil plants differs in several respects from that of their extant relatives. Thus inflorescences in Upper Cretaceous plants may have sessile or pedunculate heads, in 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 inner whorl, or two 4- or 5-membered whorls of perianth present, pistillode consistently present; in carpellate flowers often 4-5-merous, 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, no achenial hairs, etc. Fossils assigned to Platanus may have trifoliolate leaves (Kvacek et al. 2001), while other fossils have somewhat 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; Magallón-Puebla et al. 1997: Mindell et al. 2006: Crepet et al. 2004; von Balthazar & Schönenberger 2009 for other references). Fossil Platanaceae do not have hairy fruits (von Balthazar & Schönenberger 2009). Finally, there is some evidence from stomatal size of fossils that polyploidization occured within this clade (Masterson 2004).
Chemistry, Morphology, etc. Hennig et al. (1994) describe 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). Smets (1986) mentions the presence of nectaries; Melikian (1973) and Takhtajan (1991) describe testa anatomy; Floyd et al. (1999) describe the embryology; for chemistry, see Hegnauer (1969, 1990). Endress (1971) describes the flower as having the odd perianth member abaxial; he also describes the 6 carpels as being opposite sepals and corolla. However, there is clearly plenty of room for differences in the interpretation of floral morphology; von Balthazar and Schönenberger (2009) suggest that the parts of the flower alternate regularly and that the androecium is biseriate (see also above). 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).
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; cyanogenic glycosides +; vessel elements with simple perforation plates (scalariform, bars few); true tracheids and libriform fibers +; phloem stratified or not, rays broad; (nodes 1:1); sclereids common; hairs with 2 short cells, one in epidermis, apical cell elongated, bifid or not; leaves spiral (opposite; odd-pinnately (palmately) compound or lobed), usu. conduplicate, often thick, margins spiny toothed to entire, base of petiole often swollen, stipules 0; inflorescence various; flowers 4-merous, P valvate, pollen triangular in polar view, oblate, porate, pores broadly operculate, arranged according to Garside's Rule [three pores at four points in the tetrad], (colpate), nectary receptacular, G 1, vascular bundles forming a ring in the chalazal region, stigma terminal or lateral, often slit-like, secretory; endotesta palisade, crystalliferous, (exotegmen fibrous); cotyledons large, suspensor 0.

80[list]/1600 - five subfamilies below. Largely southern hemisphere, esp. Australia and S. Africa (Map: from Johnson & Briggs 1975; Weston 2006; Prance et al. 2007).
1. Bellendenoideae P. H. Weston
Al accumulation +; inflorescence terminal, bracts 0; 2 ovules/carpel; fruit dry, indehiscent, 2-winged; endosperm at most slight; n = 5, chromosomes ca 6.7 µm long (mean).
1/1: Bellendena montana. Australia (Tasmania).
Persoonioideae [Grevilleoideae + Symphionematoideae + Proteoideae]: stomata brachyparacytic; P connate, A adnate to P, more or less sessile, (connective appendage +), usu. 4 nectary lobes +, stylulus long; endosperm +.
2. Persoonioideae L. A. S. Johnson & B. Briggs
Al accumulation infrequent [e.g. 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 (mean).
5/110: Persoonia (100). Mostly Australia, also New Caledonia and New Zealand.
Grevilleoideae + Symphionematoideae + Proteoideae: flowers vertically or obliquely monosymmetric [P split to base on one side, or 3 P connate, 1 free], (secondary pollen presentation, the apex of the style bearing the pollen), (ovules anatropous); x = 14, chromosomes 0.5-5 µm long (mean).
3. Grevilleoideae Engler
Plants Al accumulators; sieve elements with rosette-like non-dispersive protein bodies; paired flowers subtended by a common bract very common; pollen with abundant endexine in the apertural region, (1-)2+ ovules/carpel; fruit a drupe or follicle, the latter with winged seeds; (seeds pachychalazal); endosperm with chalazal ± nuclear haustorium; cotyledons basally auriculate; n = (10-)14(-15).
45/855: Grevillea (515, inc. Hakea, Finschia), Helicia (100), Banksia (175: inc. Dryandra, see Mast et al. 2005). 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.]
Symphionematoideae + Proteoideae: fruit indehiscent.
4. Symphionematoideae P. H. Weston & N. P. Barker
Proteoid roots 0; nectaries 0, 1-2 ovules/carpel; fruit dry; n = also 10.
2/3. S.E. Australia, inc. Tasmania.
5. Proteoideae Eaton
Al accumulation infrequent; sieve elements with non-dispersive protein bodies; flowers sessile, (hypanthium +), (A monothecal; 1-3); 1(2) ovules/carpel; fruit often single-seeded, drupe or nut; n = (10-)11-13(-14).
25/640: Protea (115), Leucadendron (80), Conospermum (55), Petrophile (55), Synaphea (55), Serruria (50). Africa S. of the Sahara, esp. the Cape region, Australia.
Evolution. Hill et al. (1995) and Weston (2006) summarise the fossil record of the family. Anderson et al. (2005, see also Barker et al. 2007b) date stem group Proteaceae at 119-110 million years before present, crown group members at 96-85 million years before present. 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, including the fact that 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. There is a great diversity of proteaceous pollen from the late Cretaceous (Campanian-Maastrichtian) in S.E. Australia (Dettmann & Jarzen 1991).
Although some transoceanic disjunctions in the family such as that of the sister taxa Cardwellia in Australia and Gevuina in South America, are possibly caused by vicariance/drift events, others, like Brabejum in Africa which is sister to Panopsis in South America, involve genera whose divergence is later than the geological events that possibly caused them (Barker et al. 2007b). Several lines of molecular evidence suggest that there may have been a rapid diversification within Grevilleoideae (Hoot & Douglas 1998). The diversification of Protea, notably speciose in southern Africa, has been studied by Barraclough and Reeves (2005), although they find it difficult to pin down the timing of this; however, Sauquet et al. (2009) suggest that it may have diversified within the last 18 million years, while Leucadendrinae started diversifying there as much as 39 million years ago, even though they have been in the Cape region for a shorter time than Protea.Given the size of the family, caterpillars of Lycaenidae butterflies seem to eat its members quite frequently (see Fiedler 1991).
Pollination in the family has been studied in some detail, and 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, and the pollen may even cover the stigmatic area (Ladd et al. 1996), but selfing is uncommon; Proteaceae show very great variation in these pollen presenting areas (Ladd 1994). Monosymmetric flowers are common the family, but the Cape species Mimetes cucullatus has monosymmetric groups of flowers, the flowers being borne under a more or less brightly coloured inflorescence bract. The inflorescences of some species of the Australian Conospermum (Proteoideae) in particular look rather like those of Anigozanthus... Serotiny is scattered in the family, the follicles sometimes opening only after a fire.
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 at any one time (Shane & Lambers 2008). They exude organic acids, especially as tricarboxylates, into the soil and mobilize phosphate, and perhaps other nutrients like manganese that are at a premium in the phosphorous-poor soils on which members of the family are often found (Weston 2006). Many but not all members of the family develop phosphorous toxicity when growing on relatively phosphorous-rich soils; phosphorous uptake cannot be down-regulated and it eventually starts accumulating in palisade mesophyll cells in particular eventually causing their death (Shane et al. 2004; Shane & Lambers 2008). For the evolution of scleromorphic leaf anatomy, see Jordan et al. (2005, 2008); some of the structures involved are implicated in photoprotection and also are associated with some combination of open, oligotrophic, cold and dry conditions. In general, Proteaceae are most diverse in rather dry climates in Australia and southern Africa; lignotubers have evolved several times.
In Australia, the fungal pathogen Phytophthora cinnamomi is proving especially destructive to members of this family in the Mediterranean climates of the southwest. For myrmecochory (Grevillea, Leucadendron, etc.), see Lengyel et al. (2009).
Chemistry, Morphology, etc. Sieve tubes have sieve areas for most of their length. The roots have 4-7 protoxylem poles. Nodes in Panopsis appear to be pentalacunar. Cotyledonary nodes commonly have split laterals (Naubauer 1991), however, the distribution of this character is unclear. The lenticels are often horizontally elongated (Keller 1996). Foliar anatomy is notably variable within Grevilleoideae.
For flower pairs, which represent reduced inflorescence branches, see Douglas and Tucker (1996a), for the variable floral orientation, see Douglas and Tucker (1996b); the flowers may be mirror images, as in Orites (image at: www.anbg.gov.au/proteaceae/illustrations.html). There is no evidence that the uniseriate perianth is derived from a biseriate structure, and the individual 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, but it also occurs elsewhere in the family. The nectary has very variable vasculature and is best considered an enation rather than a modified stamen, etc. (Douglas & Tucker 1996c). The position of the embryo sac in the ovule varies considerably (Venkata Rao 1971). 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. Testa and tegmen variation is considerable, parly because the fruits are sometimes indehiscent, and both may sometimes be multiplicative (Venkata Rao 1971; Corner 1976); however, the ovary wall and integuments may be adnate (so the fruit is a caryopsis??!!) and there has been much misinterpretation of fruit/seed anatomy (Manning & Brits 1993: their interpretation is followed here). Testa anatomy is similar to that in Papaveraceae, Chloranthaceae, and Aristolochiaceae... Cotyledons of Bellendena are not cordate are they often are elsewhere in the family. That 'palaeo-polyploidy' has been involved in the evolution of chromosome number in the family is questionable (Stace et al. 1998).
For Al-accumulation, see Webb (1954), for proteoid roots, see Purnell (1960) and Dinkelaker et al. (1995), for general chemistry, see Hegnauer (1969, 1990), for polyol distribution, see Bieleski and Briggs (2005), for pollen development, see Blackmore and Barnes (1995: Garside's Rule), for general information, see Johnson & Briggs (1963, 1975: including chromosome lengths) and Venkata Rao (1971), for nodes, Catling and Gates (1998), for a survey of seed coat anatomy, Takhtajan (2000), for pollen, see Sauquet et al. (2006) and Sauquet and Cantrill (2007), and for general information see especially Weston (2006).
Phylogeny. For phylogeny, see Hoot and Douglas (1998) and Weston and Barker (2006). 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) suggests that Bellendenoideae and Persoonioideae are sister taxa. Carnarvonia and Sphalmium, sometimes segregated as subfamilies, may be immediately related, and although definitely in Grevilleoideae, relationships within that clade are unclear.
For relationships in Proteoideae, see 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 and is segregated as Eidotheoideae in The Flora of Australia, was not included. However, the biogeography of the subfamily is clearly interesting.
Classification. For a new classification, the outlines of which are followed here, and a generic checklist, see Weston and Barker (2006) and Weston (2006). Carnarvonia and Sphalmium are both morphologically very distinctive, the first having fully compound leaves and the latter only a short stylulus, and are segregated as Carnarvonioideae L. A. S. Johnson & B. Briggs and Sphalmioideae L. A. S. Johnson & B. Briggs in The Flora of Australia), but they are included in Grevilleoideae here.
Synonymy: Lepidocarpaceae Schultz Schultestein