A contribution to the question of early Homo in southern Africa : researches into dating, taxonomy and phylogeny reconstruction
Abstract
The origin of genus Homo is a core problem in contemporary
palaeoanthropology. Most research in early hominid studies has hitherto
focussed on the bearing of East African hominids on this problem. This
dissertation examines the importance of southern African early Homo to this
question, and provides a comprehensive assessment of the age, morphology,
taxonomic status and evolutionary relationships of these fossils.
This study establishes the reliability of electron spin resonance
(ESR) dating of tooth enamel for samples from South African early hominid
cave sites. These sites are characterised by a number of geological and
geochemical factors, including low sample uranium concentrations, which allow
for the dating of Upper Pliocene and Lower Pleistocene samples with this
method. Given sufficient understanding o f the depositional history and
provenance of fossil teeth, age estimates can be derived which are consistent
with established views of the antiquity of early hominids from these deposits.
This study marks the first comprehensive numerical dating of the
sites of Sterkfontein and Swartkrans, and experimental dating of Kromdraai and
Gladysvale. It also combines the first direct dating of australopithecine remains
to provide the first chronological framework for early hominid evolution in
southern Africa based on numerical dating. Remains from Sterkfontein
previously attributed to A. africanus, but H. africanus in this study, are dated
from around 3.0 to 2.0 Ma. Homo habilis from Sterkfontein, or Homo sp. nov.
in this study, is dated around 1.6-1.7 Ma. Paranthropus robustus (SKW 11)
from the “Hanging Remnant” of Member 1 of the Swartkrans Formation has
been directly dated in this study to around 2.0-2.1 Ma. The estimated age of
SKW 11, and faunal samples from this unit, provide an inferential age for early
Homo from the “Hanging Remnant” of around 2.0 Ma.
ESR dating of the hominid bearing unit of the Kromdraai B cave site
suggests P. robustus survived well into the Middle Pleistocene. If the single
tooth dated in this study is representative of the stratigraphic unit as a whole,
then Paranthropus may have gone extinct after 1.0 Ma, and possibly as late as
800 ka. ESR dates for Kromdraai A suggest an age of around 1.6 to 2.0 Ma,
which is consistent with faunal estimates for this site (Vrba, 1985a; Delson,
1984, 1988). A ‘blind’ ESR dating study of the Gladysvale cave site provides
an internally consistent chronology, suggesting an age range of around 320 ka to
2.2 Ma.
Considerable support has been found in this study for the inclusion
of fossils previously assigned to the taxon A. africanus to Homo. This has a
number of important implications for contemporary views of hominid evolution, including a Southern African origin for genus Homo, an origin of
Homo greater than 3.0 Ma, and invalidity of genus Australopithecus.
Early Homo from southern Africa appears to be very distinct from
taxa sampled in East Africa during the same time period. The southern African
sample appears to be taxonomically heterogenous, containing separate Homo
taxa at Sterkfontein and Swartkrans. It also appears to contain the ancestor of
H. habilis, Homo aff. H. habilis, a taxon which includes SK 847 and SK 15
from Swartkrans. The Sterkfontein Homo remains Stw 53 are herein assigned
to Homo sp. nov., and possess a morphology consistent with ancestral status
to Homo aff. H. habilis.
The bearing of southern Africa on questions of fundamental
importance to contemporary palaeoanthropology is immense. The results of
this study suggest Homo first appeared in this region; that it provided the
ancestor of H habilis from Olduvai Gorge, a species which appears to be the
ancestor of H. ergaster and H. erectus\ and it documents the survival of
australopithecines well into the Middle Pleistocene. Many important questions
about the origins and subsequent diversification of Homo, the human genus,
and our australopithecine cousins, may ultimately be resolved in southern
Africa.
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