WEST KIMBERLEY PLACE REPORT - Department of Sustainability ...
WEST KIMBERLEY PLACE REPORT - Department of Sustainability ...
WEST KIMBERLEY PLACE REPORT - Department of Sustainability ...
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Evidence for uninterrupted occupation spanning the Pleistocene into the Holocene is<br />
also not unique in the Australian archaeological record. Puritjarra rock shelter<br />
provides evidence <strong>of</strong> continued human occupation, albeit <strong>of</strong> varying intensity, dating<br />
from about 32,000 BP through to the late Holocene (Smith, 2006). Evidence from<br />
Willandra Lakes also shows continuous occupation beginning in the Pleistocene and<br />
persisting into the late Holocene (Allen et al. 2007).<br />
Culturally deposited botanical material dating to the Pleistocene has also been<br />
uncovered at Devil's Lair (Dortch 2004) and at Puritjarra rock shelter (Smith et al.<br />
1995). However, in both cases, only hearth charcoal is present (Smith et al. 1995;<br />
Shackley 1978). In terms <strong>of</strong> evidence on human adaptation to climate change,<br />
Puritjarra rock shelter again <strong>of</strong>fers some insights through stone tool development<br />
(Smith 2006). Several sites in Arnhem Land also record evidence <strong>of</strong> human<br />
adaptation to smaller climate change events caused by the el Niño/la Niña<br />
phenomenon during the Holocene (Bourke et al. 2007).<br />
The evidence provided by Carpenter's Gap 1 is exceptional as it has provided<br />
researchers with a micro and macro-botanical collection <strong>of</strong> incomparable antiquity<br />
and breadth <strong>of</strong> botanical variation, spanning 40,000 years. The micro-botanical<br />
material, including phytoliths carried in the air and by water flows, are likely to<br />
represent the vegetation <strong>of</strong> an extremely large catchment area, whilst the macrobotanical<br />
remains including stems, leaves and seeds are likely to have been deposited<br />
by human cultural actions or faunal activity from sources in closer proximity to the<br />
rock shelter (Wallis 2001, 107-109). The combined botanical record allows for the<br />
Carpenter's Gap 1 material to be used in creating both a broad geographic spectrum<br />
and a predominantly localised model <strong>of</strong> the changing Kimberley environment over<br />
time.<br />
Carpenter's Gap 1 rock shelter has outstanding heritage value to the nation<br />
under criterion (b) for its rare archaeological sequence <strong>of</strong> micro and macrobotanical<br />
remains spanning 40,000 years that contributes to our understanding<br />
<strong>of</strong> the impacts <strong>of</strong> climate change on flora composition though time, and the rare<br />
evidence it provides <strong>of</strong> plant procurement strategies used by Aboriginal people<br />
from the Pleistocene, through the last glacial maximum, a period when many<br />
occupation sites were abandoned across Australia, and into the Holocene.<br />
CONTACT, CHANGE AND CONTINUITY<br />
European explorers<br />
Karrakatta Bay<br />
The association <strong>of</strong> Karrakatta Bay with William Dampier has been addressed under<br />
criteria (a) and (h).<br />
Careening Bay<br />
Just as Dampier has an important place in the process <strong>of</strong> accumulating knowledge<br />
about the Australian continent as the first to make direct information about Australia<br />
widely available to the European public, so too Phillip Parker King has a pivotal role<br />
as the man who completed that process through his work in charting the majority <strong>of</strong><br />
the last unmapped areas <strong>of</strong> the Australian coast. With King, the last uncharted parts <strong>of</strong><br />
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