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Australia: The Land Where Time Began |
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Australian Prehistoric Settlement as Revealed by Y chromosome and mtDNA
Analysis
Published, as well as new samples of Australian Aboriginals and
Melanesians were analysed for variations of their Y DNA (n=522) and mt
DNA (n=172), and the profiles
that resulted were compared with the branches known so far with the
global mtDNA and Y chromosome tree.
i)
It was confirmed that all Australian lineages fall within the
mitochondrial founder branches M and N and the Y chromosomal founders C
and F, which are associated with the migration of anatomically modern
humans from Afric ≈50 ka to 70 ka. No evidence of any archaic maternal
or paternal lineages in Australia was revealed by the analysis, in spite
of some suggestively robust features in the Australian fossil record,
therefore weakening the argument for continuity with any earlier
Homo erectus populations
in Southeast Asia.
ii)
The complete mtDNA sequence tree shows that Australian Aboriginals are
most closely related to the autochthonous populations of New
Guinea/Melanesia, which indicates prehistoric Australia and New Guinea
were initially occupied by one and the same colonisation event in the
Palaeolithic ≈50 ka, which agrees with the current archaeological
evidence.
iii)
A considerable isolation following the initial arrival is indicated by
the deep mtDNA and Y chromosomal branching patterns between Australia
and most other populations around the
Indian Ocean.
iv)
Hudjashov et al. detected
only a minor secondary gene flow into Australia, and suggest this could
have occurred before rising sea levels submerged the land connection
between Australia and New Guinea ≈8 ka, and therefore calls into
question that certain significant developments in later Australian
prehistory, the emergence of a backed blade lithic industry, and the
linguistic dichotomy, were motivated externally.
Human evolution – population genetics
Human are believe to have occupied the Australian
continent at least 50,000 ka
(Stringer, 2002) At a time when there was a land bridge between the
Australian mainland and what is now New Guinea and when only narrow
straits separated the region from the Eurasian landmass, such as the
barrier known as Wallacea, a gap of ocean and islands requiring a number
of comparatively narrow ocean crossings that prevented the wildlife of
Eurasia and Australia from mixing, even at times of low sea level, with
the exception of a few such as bats and birds. The Australian fossil
record has remained not well known. The fossil record of Australia
contains anatomically human humans (AMH) that are among the oldest known
outside Africa that has been dated to ≈46,000 ka (Bowler et
al., 2003; O’Connell & Allen,
2004), in spite of the large geographic distance from Africa, the
homeland of AMH (Vigilant et al.,
1991). Also, in Australia the oldest known skeletal material at Lake
Mungo is of a gracile type, whereas at archaeological sites such as Kow
Swamp younger skeletal finds are of a robust morphology (Brӓuer, 1989).
Among some modern Australian Aboriginal people elements of this robust
morphology have been retained, such as in the form of pronounced brow
ridges (supraorbital tori) (Larnach & Macintosh, 1970). A number of
explanations have been proposed for the inconsistent morphological
record, such as that the AMH interbred with Southeast Asian
Homo erectus so that some
of their genomic material has been added to the gene pool of the modern
humans to some degree (Brӓuer, 1989; Thorne & Wolpoff, 1992), or that it
is the result of multiple migrations to Australia which gave rise to
differing morphologies at different times, such as hypothetical new
migrants from India (Huxley, 1870), or that the genetic isolation of
Australia has been long enough for marked continent-/Australian-specific
features to arise on the Australian continent (Pardoe, 1991; Brown,
1992; Lahr, 1996; Sengupta et al.,
2006; Richards et al., 2006).
The intensification of density and complexity of different stone tools
in Australia during the Holocene and the emergence of backed blade stone
tool technology is indicated by archaeological data (Mulvaney &
Kamminga, 1999). Also at about the same time, 3,500-4,000 years ago, the
first dingoes (Canis
lupus dingo) appear in the fossil record of Australia, and have
been suggested to have arrived with new arrivals of humans from India
(Gollan, 1985), as well as new stone tool types (Glover & Presland,
1985). This is a debate that is ongoing (Mulvaney & Kamminga, 1999;
Corbett, 1985; Savolainen et al.,
1985).
A diversity of interpretations have resulted from recent molecular
studies, which range from a deep though undated split that distinguishes
Australia Aboriginal people even from their immediate neighbours to the
north in New Guinea (20), to a very recent migration event that occurred
in the Holocene sometime in the past 10,000 years (21,22).
According to Hudjashov et al.
an attempt can now be made to clarify some of the salient features of
the record of the Australian population history and confirm its
considerable isolation, by using new samples from Australia and New
Guinea which have been screened for variations in the Y chromosome and
the mt DNA, and benefiting from the increasing genetic coverage
available in Australia (Vigilant et al., 1985; Brӓuer, 1989; Forster et
al., 1998; Redd & Stoneking, 1999; Redd et al., 2002; van Holst
Pellekaan et al., 1998; Huoponen et al., 2001; Ingman & Gyllensten,
2003; Ingman et al., 2000; Kivisild et al., 2006; Kayser et al., 2006;
van Holst Pellekaan et al.,
2006; Friedlaender et al., 2007; Underhill et al., 2001; Underhill et
al., 2000).
Conclusions
A single early founding group occupying both Australia and New Guinea a
relatively short period of time following the exodus from Africa ≈50-70
ka, at a time when Australia and New Guinea were joined into a single
continent, Sahul, which made it necessary to make crossings only across
narrow straits, as in crossing Wallacea, is pointed to by the results of
the mitochondrial and Y chromosome analysis that have been presented in
this paper. A small founding population and subsequent isolation of
Australia and, to a lesser extent, New Guinea, from the remainder of the
world, is indicated by the deep, specific lineages of the present within
the former landmass of +. Hudjashov et
al. suggests that these
founder events could possibly underlie the divergent morphological
development that is seen in the Australian human fossil record, and
might also explain the remarkably restricted range of Australian
Pleistocene
lithic industries and bone artefacts compared to contemporaneous
cultures in other parts of the world (Mellars, 2006).
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| Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading | ||||||||||||||