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Until recently, the last common ancestor of African apes and humans was presumed to resemble living chimpanzees and bonobos. This was frequently extended to their locomotor pattern leading to the presumption that knuckle-walking was a likely ancestral pattern, requiring bipedality to have emerged as a modification of their bent-hip-bent-knee gait used during erect walking. Research on the development and anatomy of the vertebral column, coupled with new revelations from the fossil record (in particular, Ardipithecus ramidus), now demonstrate that these presumptions have been in error. Reassessment of the potential pathway to early hominid bipedality now reveals an entirely novel sequence of likely morphological events leading to the emergence of upright walking.
For several decades, largely subsequent to the recovery of A.L.288-1 (‘Lucy’) (Johanson et al. 1982), upright walking in early hominids was argued to have relied on a bent-hip–bent-knee (BHBK) gait (see, e.g. Stern & Susman 1983; Susman et al. 1984; Stern 2000). This argument rested on observations of locomotion in chimpanzees and gorillas, coupled with the presumption that the post-cranium of our last common ancestor (LCA) of Pan and Homo was fundamentally similar to those of extant African apes (but see Filler 1981). Despite the fact that early hominids such as A.L.288-1 (and other members of Australopithecus afarensis and Australopithecus anamensis) exhibit pelves, knees and feet with highly advanced adaptations to a striding, bipedal gait (Latimer & Lovejoy 1989; Lovejoy 2005a,b, 2007), the BHBK hypothesis has remained largely unchallenged save arguments based on energy consumption (e.g. Crompton et al. 1998; Carey & Crompton 2005; Sellers et al. 2005).
The BHBK gait of Pan and Gorilla, however, is not a function of limitations imposed by hip or knee anatomy, but is instead a direct consequence of an absence of lumbar spine mobility. African apes are unable to lordose their lumbar spines, and therefore must flex both the hip and knee joints in order to position their centre of mass over the point of ground contact (Lovejoy 2005a). Lumbar immobility in Pan and Gorilla is a consequence of their possession of only three to four lumbar vertebrae and the ‘entrapment’ of the most caudal lumbar vertebra(e) between cranially extended ilia (Stevens 2004; Stevens & Lovejoy 2004; Lovejoy 2005a; McCollum et al. 2009). Although all three African ape species share these features, there is now considerable evidence indicating that they have not been retained from the common ancestor shared with the human clade. Instead, a more detailed study of the vertebral formulae and the lumbar column of African apes and early hominids indicates that the LCA of Pan and Homo most probably possessed a long (six to seven segments) mobile lumbar spine similar in number to those of Old World monkeys (OWMs), Proconsul and Nacholapithecus (McCollum et al. 2009). Because such columns would have been capable of near-full lordosis, these new findings in and of themselves contraindicate pronounced African ape-like BHBK bipedality in early hominids. New revelations about LCA structure provided by Ardipithecus ramidus (especially ARA-VP-6/500; Lovejoy et al. 2009a–d; White et al. 2009) further establish that hominids never displayed any of the numerous African ape-like specializations that have reduced lumbar mobility and thus required an unusually restricted BHBK gait. Here we review this new evidence.
As is discussed more fully in McCollum et al. (2009), it is reasonable to assume that the modal vertebral formula of basal hominoids and the LCA of Pan and Homo to have been 7-13-6/7-4–one that differs from those of OWMs merely by the addition of a fourth sacral vertebra, and replacement of the external tail by a short coccyx. Two lines of evidence support this view.
First is evidence provided by the vertebral formulae of Australopithecus and early Homo (Sanders 1995). Although complete axial data are unavailable for any single early hominid specimen, a number of partial specimens, including A.L. 288-1 (complete sacrum) and KNM-WT 15000 (interpretable lumbar column), indicate a pre-coccygeal vertebral formula of 7-12/13-6-4 (Pilbeam 2004; McCollum et al. 2009).
The second source of evidence is the axial morphology of bonobos (Pan paniscus). Unlike chimpanzees (Pan troglodytes) and modern humans, whose modal number of pre-coccygeal vertebrae is 29/30, bonobos possess an axial column typically composed of 30/31 vertebrae, identical to that inferred for the basal hominoid. Although it is certainly possible that the long axial column of bonobos re-evolved from an ancestor with an abbreviated column similar to that of chimpanzees and modern humans, such modification has no obvious selective advantage and runs counter to the trend towards axial length reduction observed in all suspensory anthropoids (Benton 1967; McCollum et al. 2009). Rather, the long axial column of bonobos, along with the significantly different combinations of sacral, lumbar and thoracic vertebrae that are characteristic of common chimpanzees (seven cervical, 13 thoracic, three to four lumbar, five to six sacral) and bonobos (seven cervical, 13–14 thoracic, four lumbar, six to seven sacral), suggest instead that the two species of Pan evolved their short lumbar spines from an ancestor with a long axial column (n = 30/31 pre-coccygeal vertebrae) and a long lumbar spine after division from their own LCA. This receives support from data which suggest that lumbar spine reduction in chimpanzees apparently occurred through sacralization of the caudal-most lumbar vertebrae plus reduction in the number of somites (figure 1). Bonobos, conversely, appear to have reduced their lumbar column purely through transformations of segment identity, i.e. by transforming lumbar vertebrae into sacral and thoracic vertebrae (McCollum et al. 2009).
The Ar. ramidus limb skeleton indicates that much of extant African ape locomotor anatomy has been independently derived for vertical climbing, suspension and a feeding habitus that probably included high canopy access in relatively large-bodied hominoids (Lovejoy et al. 2009a). While OWMs also frequently climb vertically, they nevertheless retain adaptations that are primarily for more active, above-branch pronograde running and leaping. Such acrobatics appear to have become much more limited in hominoids, presumably inter alia, because of their significantly larger body mass (Cartmill 1985).
The locomotor skeleton of Ar. ramidus establishes that the LCA, unlike modern apes, retained many OWM-like features sufficiently primitive to assure a primary gait pattern of above-branch pronograde palmigrady (Lovejoy et al. 2009a–c). To be sure, numerous modifications of OWM-like anatomy had become more like that of extant hominoids in the LCA (Lovejoy et al. 2009c)—alterations known to have been initiated in likely exemplars of its remote ancestors, especially various species of Proconsul (Ward 1991, 1993; Ward et al. 1991, 1993; Nakatsukasa et al. 2003). However, the Ar. ramidus foot still retained a relatively elongated mid-tarsus, a robust os peroneum complex and presumably numerous soft tissue features associable with an inherently stiff plantar structure more typical of the above-branch propulsion seen in OWMs. These latter features can be reliably extended to the LCA by parsimony, since they are still present in the feet of modern humans (quadratus plantae, plantaris, os peroneum, elongated cuboid, etc.), but have been largely eclipsed by specializations in the feet and ankles of more highly specialized, extant African apes (Desilva 2009; Lovejoy et al. 2009a).
Similar observations of the Ar. ramidus forelimb suggest that it also shares a number of primitive features with humans. These include a very primitive and unreinforced central joint complex (CJC) (capitate, trapezoid, metacarpals 2 and 3), a relatively substantial pollex, a short metacarpus, a lack of significant Mc4/Mc5–hamulus contact, a narrow trapezoid, a palmarly displaced capitate head and an unmodified, markedly rugose, deltopectoral crest. Each of these has since been modified in extant large-bodied African apes in favour of ones associable with knuckle-walking, suspension and/or vertical climbing (Lovejoy et al. 2009c).
At the same time, it is equally clear that the LCA differed fundamentally from its likely ancestors (including Proconsul) in several major ways, none more important than the structure of its vertebral column and its position within the thorax (Lovejoy et al. 2009c). In comparison with Proconsul and OWMs, in which the pectoral girdle is positioned more anteriorly on the thoracic cage, the hominoid pectoral girdle is located more dorsolaterally, in a manner that causes its glenoid fossa to face more laterally than is typical of more primitive taxa (Waterman 1929; Schultz 1961; Erikson 1963; Ward 2007). Such ‘posterolateralization’ places the girdle into a more favourable position for circumduction, which in turn permits relatively large-bodied primates to successfully negotiate the canopy via clambering, bridging and suspension. What has gone almost entirely unrecognized until the recovery of Ar. ramidus, however, is that repositioning of the scapula (so as to make the glenoid face more laterally and less anteriorly) in hominoids was achieved by thoracic reorganization which relied on invagination of the post-cervical spine ventrally into the thorax. This resulted in dorsal repositioning of the lumbar transverse processes (LTPs), a change in bauplan that apparently occurred independently and repeatedly even in some early Miocene hominoid taxa (e.g. in Morotopithecus by 17 Ma; MacLatchy et al. 2000; Filler 2007a,b), and was significantly progressing in a number of forms by the Mid-Miocene (e.g. in Pierolapithecus by at least 10 Ma; Moya-Sola et al. 2004; Almecija et al. 2009). This shift appears to have accompanied other forelimb modifications, especially ulnar withdrawal and olecranon abbreviation. These modifications increased potential wrist adduction, enhanced stability during complete elbow extension and greatly increased the forelimb's range of motion at the shoulder girdle (Rose 1988; Lewis 1989). However, as this change in bauplan also resulted in the sacrifice of substantial erector spinae mass (Benton 1967; Lovejoy 2005a), increasing the range of motion of the shoulder came at the expense of dynamic stabilization of the lower back. Consequently, African ape suspension and vertical climbing required compensatory lumbar column reduction—virtually to the point of inherent (i.e. osteological) rather than dynamic (i.e. muscular) rigidity. Thus, LTP position, rather than being the primary target of selection during lumbar column shortening, as has long been argued (e.g. Benton 1967), was instead a product of the fundamental change in the hominoid bauplan that centred about a general restructuring of the thorax.
Features assignable to the LCA, therefore, now point to a pattern of cautious climbing that combined above-branch palmigrady with occasional below-branch suspension, enhanced by a highly mobile, lateralized shoulder girdle in combination with marked wrist adduction (Cartmill & Milton 1977; Lewis 1989) and elbow extension (Rose 1988). Below-branch suspension, however, must not have been so frequently employed (and/or so vigorously performed) as to require emergence of the considerably more advanced metacarpal, carpal, elbow and shoulder modifications seen only extant African apes. This suggests that much of the LCA's activities may have been largely low-canopy, and might have been combined, possibly extensively, with terrestrial travel between food patches (White et al. 2009). The latter supposition receives support from the fact that the adaptations to terrestrial travel present in extant African apes (knuckle-walking) and fossil hominids (bipedality) are extensive, fundamentally divergent, and therefore likely to be of substantial antiquity. It is also likely that reliance on terrestrial travel between food patches was driven by increasing competition with radiating OWMs in the Mid-Miocene (Andrews 1981). That the post-crania of Pongo and the lesser apes (Hylobates, Symphalangus) differ substantially from those of the African apes is probably largely due to the absence of a significant terrestrial component in their respective adaptive strategies, and their entirely independent evolution from much more primitive ancestors.
If the above hypothesis is correct, what was the LCA's terrestrial locomotor habitus prior to the emergence of either knuckle-walking in apes or bipedality in hominids? One possible pattern ‘of choice’ might have been a simple extension of its primary arboreal pattern to ground travel, i.e. palmigrade quadrupedality. In fact, some of the more unusual characters present in Ar. ramidus are strongly suggestive that hominids once exhibited such an ancestral gait pattern. These include its primitive intermembral index, relatively short metacarpus, allowance of substantial metacarpal–phalangeal dorsiflexion and especially the strongly palmar positioning of the head of its capitate (Lovejoy et al. 2009b). Indeed, the latter can be viewed as being particularly advantageous to palmigrade terrestrial quadrupedality, and this would now seem to be a possible explanation for this unusual peculiarity in Ar. ramidus, i.e. it inherited it from a habitually terrestrial palmigrade LCA.
Unlike OWMs, quadrupedal terrestrial gait in large-bodied hominoids (including the LCA) may have required a much more compliant wrist, i.e. palmigrady that included more extreme dorsiflexion. Absence of such extreme adaptations in OWMs is likely explicable by their retention of primary above-branch adaptations at the radiocarpal, elbow and shoulder joints. Palmar disposition of the capitate head as seen in Ar. ramidus (Lovejoy et al. 2009b) may even now serve, given further fossil evidence, as an indicator of palmigrade/plantigrade terrestrial quadrupedality in yet undiscovered, large-bodied, Miocene forms. In combination with the retention of a long mid-tarsus, a robust os peroneal complex and other primitive aspects of its foot (retained M. quadratus plantae, retained M. plantaris and associated dense palmar fascial aponeurosis (see earlier)), palmigrade/plantigrade quadrupedality seems to have been, at the least, a likely terrestrial locomotor habitus in the African ape/hominid LCA (Lovejoy et al. 2009c).
If so, from whence came the relatively highly specialized gait patterns of the LCA's descendants: bipedality in hominids and knuckle-walking in the African apes? The latter is reasonably explicable in these taxa as a relatively facile means of modifying palmigrade/plantigrade terrestrial travel into a form that could be successfully combined with their highly specialized modifications of the pelvis, thorax and limb skeletons for suspension and vertical climbing. Such changes included (independently in each taxon) elongation of the forelimb, abbreviation of the hindlimb, elongation of the metacarpus, stabilization of several major carpal joints either by ligamentous reinforcement or joint enlargement or both (especially in the CJC), major revisions of overall scapular morphology (predominantly in Pan as opposed to Gorilla), cranial retroflexion of the ulnar trochlear notch, modification of the deltopectoral enthesis and especially, virtual fusion of the thorax and pelvis via abbreviation and iliac fixation of the lumbar column (see earlier) (Lovejoy et al. 2009c,d). All of the modifications to the forelimb would have reduced its inherent stability and increasingly restricted its energy-dissipating capacity during prolonged terrestrial travel. These difficulties appear to have been resolved by adoption of knuckle-walking, which permits reliance on substrate-forced dorsiflexion of the wrist that can be eccentrically resisted by powerful wrist flexors as well as both the connective tissue envelopes and contractile components of the long digital flexors. The uniqueness of these long flexors is evidenced by development of a distinctive flexor tubercle on the proximal ulna in both Pan and Gorilla (Lovejoy et al. 2009b).
The most salient question remaining, of course, is the issue of the eventual adoption of bipedality in hominids. Why did hominids exchange palmigrade/plantigrade quadrupedality for upright walking? While there have been many theories advanced for this locomotor shift, most have been made untenable by evidence now provided by Ar. ramidus (White et al. 2009). The recent suggestion that bipedality is a sequel to an arboreal upright stance stabilized by overhead forelimb grasping (Thorpe et al. 2007a,b, 2009) is untenable because the practice has emerged in Pongo as a consequence of that taxon's extreme adaptations to suspension, none of which were ever present in hominids or their ancestors (Lovejoy et al. 2009c). The most likely explanation for the adoption of terrestrial bipedality, in our view, continues to involve novel adaptations in hominid social structure that required upright locomotion for carrying. These have been discussed extensively elsewhere (Lovejoy 1981, 1993, 2009).
As noted above, still equipped with a mobile lumbar spine, the LCA was probably capable of at least facultative lordosis, sufficient to place its hip and knee either directly below its centre of mass or sufficiently close to that centre so as not to generate excessive ground-reactive torques so large as to require debilitating muscle recruitment during terrestrial travel. While the earliest hominid gait pattern probably required some degree of hip and knee flexion, research on bipedality in OWMs now suggests that it would not have been nearly as excessive as it is in extant apes, so long as the lumbar column remained long and mobile (as it is in OWMs). Studies of OWMs have now greatly illuminated our understanding of its origins in hominids (Nakatsukasa et al. 1995, 2004, 2006; Hirasaki et al. 2004). Macaques trained to walk bipedally expend less energy than do those in which the behaviour is novel, so much so that the animal's long flexible spine is permissive for convergence with ‘human-style’ walking in the former. While those using bipedality ‘in the wild’ exhibit upright gaits that differ kinesiologically from human walking, those exposed to long-term training for bipedality walk ‘with longer, less-frequent strides, more extended hindlimb joints, double-phase joint motion at the knee joint, and most importantly, efficient energy transformation by using inverted pendulum mechanics’ (Hirasaki et al. 2004: 748).
While lordosis was certainly facilitated by the presence of six to seven lumbar vertebrae in the LCA (most probably six; figure 1), even in most OWMs lordosis is not as complete as it is in five-lumbared humans (Nakatsukasa et al. 1995; Hirasaki et al. 2004). One probable and very important reason is that complementary motion in the most caudal lumbar vertebra in OWMs is usually restricted by its proximity to the posterosuperior portion of each iliac blade. Such iliac–lumbar propinquity is usually sufficient to probably assure at least some degree of ligamentous restriction of potential motion.
Two characters that are uniquely associated with hominid pelvic adaptations to bipedality are therefore of particular interest: (i) an exceptionally short superoinferior iliac height (coupled with both anterior extension of the anterior inferior iliac spine (AIIS) and development of the greater sciatic notch) and (ii) an extremely wide sacrum generated largely by exceptionally broad sacral alae (figures 2 and and3).3). Both of these characters eliminate contact between the posteromost iliac crest and the most caudal lumbar vertebra, and are therefore likely to have appeared early in hominids as a means of increasing the lordotic capacity of the lumbar spine during terrestrial bipedality. Indeed, these changes are likely to have been the earliest in the evolution of bipedality in hominids, and largely exaptive for increased abductor capacity during the single-support phase of upright walking (Lovejoy et al. 2009c).
Moreover, three features of ape sacra appear to have directly opposite polarity compared with those of hominids (figures 22–4): (i) their strongly abbreviated sacral alae, (ii) their reduced lumbar number, and (iii) their greater number of fused sacral elements, the latter almost certainly achieved by progressive sacralization of the most caudal lumbar element(s) (McCollum et al. 2009). Alar reduction reduces the space between the two ilia so as to promote contact with the most caudal lumbar vertebra(e). In combination with the additional extension of the ilia superiorly (especially by elongation of the iliac isthmus at least in Pan; Lovejoy et al. 2009c), the African apes achieved stabilization of the entire lower spine by its fixation to the thorax—creating a rigid pelvothoracic ‘block’ in which the pelvis and thorax are separated by a distance of only a single intercostal space (Schultz 1961). Both mechanisms compensate for the loss of erector spinae mass (see earlier). Thus, both sacral structure and superoinferior iliac length directly reflect hominoid post-cranial natural history. Panids and gorillids independently elongated their ilia, narrowed their bi-iliac spaces and reduced the number of lumbar vertebrae (often by sequestration as additional sacral segments), all mechanisms that stiffened the lower back and eliminated any possibility of lordosis. Hominids, per contra, remained almost entirely plesiomorphic, retaining both the primitive number of lumbar (mode = six) and sacral vertebrae (mode = four), and in addition, expanded the sacral alae so as to assure the full independence of the most caudal lumbar, assuring its freedom to participate in lordosis as well.
Delineation of the vertebral evolutionary pattern of African apes and hominids throws considerable new light on the troublesome issue of both the locomotor pattern and phylogeny of perhaps the most enigmatic hominoid of the later Miocene, Oreopithecus. Arguments as to its potential phylogenetic relationships and locomotor patterns have been many (reviewed in Harrison 1986, 1991; Kohler & Moya-Sola 1997; Rook et al. 1999). However, all have been hampered by its extremely poor condition, largely the consequence of its extreme compression during fossilization. This has frequently led to excessively liberal interpretations of its badly compromised structure.
A case in point is the attribution of a lordotic spine to this taxon based on a sagittal section of specimen BA72, a crushed and compressed amalgam of three lumbar vertebrae (Kohler & Moya-Sola 1997). It seems inconceivable to us that such sectioning can reliably indicate the presence/absence of wedging in centra after they have been compressed to less than one half of their dorsoventral diameter. A far more conservative approach is to rely on more straightforward morphological characters of greater inherent reliability, and which are more resistant to misinterpretation from crushing defects. Not all of these appear to have been considered.
One of the most important is the vertebral formula of Oreopithecus. There is general agreement, based on the ‘1958 specimen’ (IGF 11 778), that Oreopithecus had five lumbar vertebrae (Harrison 1986, 1991; Kohler & Moya-Sola 1997; Rook et al. 1999). A largely overlooked vital statistic, however, is that it also had six sacral vertebrae (Straus 1963; method of Schultz 1961; for details, see McCollum et al. 2009). This can be safely concluded from specimen BA-50, which preserves five sacral foramina on the left side, and at least four on the right. Moreover, the masses of the right and left halves of the sixth sacral vertebra appear to be fully symmetrical (therefore the right side presumably had five full foramina as well). We have demonstrated elsewhere that the basal hominoid column almost certainly exhibited 13 thoracics (among living taxa, only Homo and Pongo have any significant incidences of fewer). Thus, the minimum pre-coccygeal vertebral number in Oreopithecus was 31, which, as noted above, is the likely pre-coccygeal vertebral number for basal hominoids and was probably modal for Early and Mid-Miocene apes as well. Except for P. paniscus, a modal vertebral number as high as 31 is extremely rare in extant species, occurring in only 2.8 per cent of P. troglodytes and 0.06 per cent of Homo (McCollum et al. 2009).
Much has been made of the putative ‘short, broad, ilium’ of Oreopithecus and of its relatively broad retroauricular segment (Hürzeler 1958). However, a substantial reduction in the size of the post-auricular region of the pelvis appears to have accompanied the spinal invagination underlying scapular relocation in all hominoids (see earlier). That reduction was in turn accompanied by a broadening of the pre-auricular portion of the pelvis and is therefore expected in any clade in which shoulder reorganization occurred (Lovejoy et al. 2009c). This same developmental process is likely to have re-occurred a number of times in hominoid evolution, and is almost certainly universally responsible for the dorsal migration of the LTPs. Broadening of the ilium well beyond comparable dimensions in Proconsul is therefore fully expected in virtually any large-bodied Miocene hominoid that exhibits posterolateralization of the shoulder.
The fifth lumbar vertebra of the ‘1958 specimen’ lies (in situ) directly within its bi-iliac space, sharing the same functional position as the trapped (immobilized) L7 of a typical Presbytis and the L3 or L4 of Pan (see Straus 1963; figure 5). Therefore, Oreopithecus exhibits a maximum of only four potentially mobile lumbar vertebrae. This is fully consistent with its ‘classic’ adaptive regimen for suspension as also seen in Gorilla, Pan and Pongo, and with directly opposite polarity compared with their homologues in bipedal hominids in a host of major adaptive characters (table 1). These included transformation of lumbars via their sacralization, direct reduction in lumbar number from the primitive condition and entrapment (immobilization) of at least one lumbar by contact with a posterodorsally extended iliac crest. Given its primitive vertebral number, and a series of others, such as its retention of an anterior keel on its lumbar vertebrae (Straus 1963), Oreopithecus appears to have acquired extensive adaptations to suspension entirely independently of other Miocene clades (as did Nacholapithecus; Nakatsukasa et al. 2007). It is thereby unrelated to hominids, its similarities (which are few; table 1) being largely minor convergences. Any bipedality would have been largely driven by the same context that does so in hylobatids—excessively long forelimbs combined with highly abbreviated hindlimbs (table 1).
One additional supposedly hominid character in Oreopithecus is worthy of brief note. The degree of protuberance of its AIIS is not unusual for a non-hominid. What distinguishes the AIIS in hominids from those in apes is not its protuberance (those of Gorilla are often very prominent), but rather its emergence from a novel, separate physis, a hominid adaptation that is almost certainly associated with dramatic expansion of iliac isthmus breadth (Lovejoy et al. 2009b). There is no evidence of a similar degree of broadening in Oreopithecus (note its relative pelvic breadth in table 1) and certainly none suggesting its origin by means of a separate physis.
In considering the anatomy of the lumbosacral spine, it is of some interest that whereas in humans both the overall size of the centrum and the distances separating the articular facets (zygapophyses) increase in each successively more caudal lumbar vertebrae, centrum size and interfacet distances in extant African apes instead decrease caudally (Latimer & Ward 1993; figure 6). Lumbar centrum dimensions do not appear to differ substantially in the only column that permits their observation in Australopithecus (Sts-14; Robinson 1972). There is, however, an increase in the interfacet distance between the putative L3 and sacrum of A.L. 288-1 (Lovejoy 2005a). The latter findings suggest that the progressive caudal expansion of both the interfacet distances and centrum dimensions evident in Homo, but only partially adumbrated in Australopithecus (i.e. no increase in lumbar centrum dimensions, a retention of six lumbar vertebrae, but a partial increase in interfacet distance), may be an adaptation that permits a more intense lordosis in humans, ultimately enhancing lumbar column stability by allowing a reduction in total lumbar number. If so, emergence of this gradient must have postdated Homo erectus at 1.6 ma, since the lumbar column in KNM-WT-15000 still numbers six with four sacral vertebrae (Latimer & Ward 1993; Pilbeam 2004; McCollum et al. 2009).
New evidence from the fossil record and from observations of extant hominoid skeletal anatomy leads to several conclusions. Among the most important is that hominids never acquired the numerous specializations seen in extant apes for vertical climbing, suspension or knuckle-walking. This demonstrable divergence between the natural histories of hominids and those of all living apes renders most observations of locomotor behaviour in the latter, whether conducted in the laboratory or observed in the wild, no longer directly relevant to the reconstruction of the earliest locomotion of hominids. Bipedality in hominids can instead now be seen to have emerged from a predominantly primitive locomotor skeleton with a long lumbar spine capable of at least partial lordosis, and one never restrictively modified for suspension, vertical climbing or knuckle-walking.
Suspension (e.g. Pongo, Hylobates) and vertical climbing (e.g. extant African apes) have repeatedly induced a rigid lower spine, especially as body mass increased. This has been accomplished in a variety of taxa in several ways, but always by a combination of reduction in lumbar number (by reduction in somite vertebral number and/or transformation of lumbar identity) via modification of hox regulation and further entrapment of a portion of the remaining lumbar vertebrae by narrowing of the bi-iliac space. The latter has been accomplished either by sacral narrowing or dorsal extension of the iliac crest (e.g. Pan and Gorilla), or both. The failure of hylobatids (but not symphalangids (i.e. modal lumbar number = 4) to achieve the extreme lumbar column reductions seen in African apes is probably a product of their modest body size and the unique nature of suspension in these lesser apes.
The earliest hominids were able to functionally achieve bipedality because they had never rigidified their lumbar spines. Instead, they evolved an opposite morphology—a reduction in iliac height and a broadening of the sacrum, both of which assured sufficient lordosis to reduce and eventually eliminate what were probably only moderate vertical moments about the knee and hip. Were hominids to have first engaged in African ape-like behaviours, the ‘Rubicon’ to bipedality may have become too great to cross. Our decades-long assumption that the abducent capacity of the early hominid pelvis was its primary selective agent (e.g. Lovejoy et al. 1973) was, in retrospect, entirely misdirected. The favourable position of the anterior gluteal muscles in hominids that allows them to control pelvic tilt during single support can now be seen to have been largely a refinement that followed the initial primary adoption of a lordotic spine with an emancipated caudal-most lumbar vertebra. The generalized structure of earliest hominids that permitted this sequence of events is almost certainly extendable to the LCA. At least initially in pre-divergence hominoids, it now suggests a combination of cautious, palmigrade, plantigrade climbing with a long flexible back during arboreal travel, and possibly, palmigrade quadrupedality during terrestrial travel as well.
We thank Alan Walker and Chris Stringer for organizing the discussion meeting and the staff of the Royal Society for ensuring its success. We thank David Pilbeam for extensive help in constructing the bonobo sample used in this paper. We thank Wim Wendelen and the staff and administration of the Royal Museum for Central Africa, Tervuren, Belgium for access to the primate collections in their care and for the valuable assistance during our examination of their specimens, and Yohannes Haile-Selassie and Lyman Jellema for aid with examination of specimens housed at the Cleveland Museum of Natural History.
One contribution of 14 to a Discussion Meeting Issue ‘The first four million years of human evolution’.