Body size and body shape in early hominins – implications of the Gona Pelvis
Introduction
The recently reported early Pleistocene (0.9–1.4 Ma) hominin pelvis from Gona, Ethiopia, BSN49/P27, attributed to Homo erectus (Simpson et al., 2008), is significant for a number of reasons. It is the only largely complete and undistorted hominin pelvis temporally intermediate between two australopithecine specimens, A.L. 288-1 (Tague and Lovejoy, 1986) at 3.2 Ma (Walter, 1994), and Sts 14 (Robinson, 1972) at about 2.5 Ma (Schwarcz et al., 1994), and the Homo Pelvis 1 from Atapuerca (Arsuaga et al., 1999) at 0.6 Ma (Bischoff et al., 2007). This was a time period during which major changes in body form were occurring within the hominin lineage (McHenry and Coffing, 2000). Because pelvic morphology is critical for interpreting obstetric and locomotor adaptations, as well as reconstructing overall body size and shape, the Gona pelvis provides important new information for readdressing these issues within a time period where little direct evidence of this kind has been available.
Previously known early Pleistocene hominin pelvic specimens include the Paranthropus robustus adult partial os coxae SK 50 and subadult partial os coxae SK 3155 (Robinson, 1972, McHenry, 1975a), the adult early Homo partial os coxae KNM-ER 3228 (Rose, 1984), the juvenile Homo erectus (or ergaster) partial pelvis of KNM-WT 15000, and the adult H. erectus partial os coxae OH 28 (Day, 1971). Other pelvic specimens from this time period are more fragmentary and consequently less informative. Of the above specimens, a full pelvic reconstruction was attempted only for KNM-WT 15000 (Walker and Ruff, 1993). However, this specimen did not preserve the pubic portion of the os coxae and preserved only portions of the sacrum; thus, the full reconstruction was only approximate (e.g., see Ruff, 1995). Also, adult morphology of the specimen can only be estimated through extrapolation. Therefore, estimated adult dimensions for this specimen are subject to relatively wide error ranges. Although incomplete, the above specimens have nevertheless proven useful in assessing hip biomechanical function as well as some general obstetric and body shape parameters in australopithecines and early Homo (Day, 1971, McHenry, 1975b, Rose, 1984, Ruff, 1995, Ruff et al., 1999).
The present study focuses primarily on temporal and geographic variation in body size and body shape among early hominins, incorporating the new evidence from the Gona pelvis as well as a reassessment of previously described specimens (e.g., Ruff, 1994, Ruff et al., 1997, Rosenberg et al., 2006). A number of other recent studies have also provided new data and the possibility of new interpretations relevant to a reconsideration of these issues (Lordkipanidze et al., 2007, Spoor et al., 2007, Trinkaus, 2009, Weaver and Hublin, 2009).
The BSN49/P27 pelvis was reconstructed from several fragments using high resolution plaster casts, which also allowed correction of distortions in the original specimens (Simpson et al., 2008). Substantial portions of the iliac blades are missing; however, enough is preserved from each side that, with mirror imaging, a realistic reconstruction of this region is possible (Simpson et al., 2008, and Simpson, pers. comm.). The pubic and ischial portions are largely intact, and the right acetabulum is complete and undistorted. Simpson and colleagues used several morphological similarities to modern human females (e.g., sciatic notch and subpubic shape) to argue that the fossil was female.
In the present context, a major feature of interest of the Gona pelvis is its great total mediolateral (bi-iliac) breadth, measured as 288 mm (Simpson et al., 2008). This is considerably larger than the 266 mm originally estimated for the adult bi-iliac breadth of KNM-WT 15000 (Ruff and Walker, 1993). The relatively narrow body of KNM-WT 15000 was interpreted as an adaptation in early Homo to tropical environments, i.e., maximizing of surface area to body mass (Ruff, 1991, Ruff and Walker, 1993). In this respect, KNM-WT 15000 conformed to both modern human geographic variation in body form as well as patterns of variation among later Pleistocene Homo (Ruff, 1994, Ruff, 2002b, Trinkaus et al., 1999, Rosenberg et al., 2006; although also see Trinkaus, 2009). In contrast, the much wider pelvis of the Gona specimen suggested that “early Homo … did not exhibit the same ecogeographic patterns of body form as seen in modern humans” (Simpson et al., 2008: 1091).
Another notable feature of the Gona pelvis is its very small articular surfaces. Specifically, small dimensions include acetabular breadth, sacral auricular surface, and S1 body surface areas (Simpson et al., 2008). No body mass estimate was attempted by the original authors, but stature estimates of 120-146 cm were derived from a variety of regressions based on joint size and estimated femoral length. This is considerably shorter than statures estimated previously for any specimens attributed to H. erectus, which range between about 150 and 185 cm (Feldesman and Lundy, 1988, McHenry, 1991, Ruff and Walker, 1993). Even considering smaller, very early Pleistocene Homo specimens probably closely related to H. erectus, including KNM-ER 1472 and 1481, and the Dmanisi adult specimens, estimated stature ranges extend only down to the largest estimated stature for the Gona specimen, i.e., about 145 cm (Ruff and Walker, 1993, Lordkipanidze et al., 2007). The very small body size of the Gona specimen implies both a greater than previously recognized range of body size in H. erectus, as well as very marked sexual dimorphism in body size (Simpson et al., 2008). This issue is further considered in the present study in the context of body mass estimations for the Gona and other early hominin specimens.
Section snippets
Femoral head breadth
Femoral head breadth is used as an index of body mass in this study, both as a morphological variable itself and as an estimator of body mass. This approach has several advantages. First, the hip is a major weight-bearing joint and so theoretically should be correlated with body mass; this has been demonstrated empirically within and between species (e.g., Jungers, 1988, Ruff, 1988, Ruff, 2002a, Jungers, 1990; also see below). Second, several equations for estimating body mass in hominins from
Results
Acetabular breadths are plotted in Figure 2, by date and assigned taxonomic group. Here and elsewhere, all non-Homo specimens (Orrorin, Australopithecus, Paranthropus) are grouped together (for individual specimen values, see Table 1). Except for the Gona specimen, distributions for non-Homo and Homo do not overlap, with non-Homo falling between 37 and 45 mm, and Homo between 50 and 61.5 mm. The Gona specimen (41 mm) falls within the range of the non-Homo group and well below the range of other
Body size
As noted by its original describers (Simpson et al., 2008), the articulations of the Gona BSN49/P27 pelvis, in particular the acetabulum, are small relative to other Early Pleistocene Homo specimens. They estimated a femoral head breadth for this specimen of 35.1 mm using a multiple regression based on acetabular breadth, S1 sacral body area, and auricular surface area derived from a sample of modern humans from the Hamann-Todd Osteology collection. Correlations of 0.804-0.845 between these
Conclusions
Early Homo and australopithecines show distinct differences in acetabular and femoral head size, and estimated body mass, with a 70-80% increase in body mass among Early Pleistocene Homo compared to australopithecines, and a even greater increase in Middle Pleistocene Homo. In terms of acetabular breadth, estimated femoral head breadth, and estimated body mass, the Gona BSN49/P27 specimen falls in the middle of the australopithecine size distribution, and well below any previously discovered
Acknowledgements
I would like to thank Henry McHenry, Erik Trinkaus, and Laura Shackelford for providing acetabular and femoral head breadth data for modern humans and fossil specimens, Juan-Luis Arsuaga and Martin Haeusler for providing unpublished data on the Atapuerca 1 and Sts 14 pelves, respectively, Bob Tague for providing individual data for modern pelvic samples, and Scott Simpson for several useful communications regarding the Gona pelvis. I would also like to thank the reviewers and Editor for several
References (81)
- et al.
High-resolution U-series dates from the Sima de los Huesos hominids yields 600(-66)(+infinity) kyrs: implications for the 66 evolution of the early Neanderthal lineage
J. Archaeol. Sci.
(2007) - et al.
Stature estimates for some African Plio-Pleistocene fossil hominids
J. Hum. Evol.
(1988) - et al.
Comparison of the pelves of Sts 14 and AL 288-1: implications for birth and sexual dimorphism in australopithecines
J. Hum. Evol.
(1995) - et al.
Dental remains from Dmanisi (Republic of Georgia): morphological analysis and comparative study
J. Hum. Evol.
(2008) Biomechanical interpretation of the early hominid hip
J. Hum. Evol.
(1975)Behavioral ecological implications of early hominid body size
J. Hum. Evol.
(1994)- et al.
Sexual dimorphism in Australopithecus afarensis revisited: how strong is the case for a human-like pattern of dimorphism?
J. Hum. Evol.
(2005) Hindlimb articular surface allometry in Hominoidea and Macaca, with comparisons to diaphyseal scaling
J. Hum. Evol.
(1988)Climate, body size and body shape in hominid evolution
J. Hum. Evol.
(1991)- et al.
Body mass prediction from stature and bi-iliac breadth in two high latitude populations, with application to earlier higher latitude humans
J. Hum. Evol.
(2005)