TY - JOUR
T1 - Late Holocene climate change an d human behavioural variability in the coastal wet -dry tropics of northern Australia
T2 - Evidence from a pilot study of oxygen isotopes in marine bivalve shells from archaeological sites
AU - Brockwell, Sally
AU - Marwick, Ben
AU - Bourke, Patricia
AU - Faulkner, Patrick
AU - Willan, Richard
PY - 2013/6
Y1 - 2013/6
N2 - Previously it has been argued that midden analysis from three geographically distinct coastal regions of tropical northern Australia (Hope Inlet, Blyth River, Blue Mud Bay) demonstrates that changes through time in Aboriginal mollusc exploitation reflect broader coastal environmental transformations associated with late Holocene climatic variability (Bourke et al. 2007). It was suggested that, while a direct link between environmental change and significant cultural change in the archaeological record has yet to be demonstrated unambiguously, midden analysis has the potential to provide the as-yet missing link between changes in climate, environment and human responses over past millennia. We test this hypothesis with a preliminary sclerochronological analysis (i.e. of sequential stable isotopes of oxygen) of archaeological shell samples from all three regions. Our findings suggest the existence of variations in temperature and rainfall indicative of an increasing trend to aridity from 2000 to 500 cal. BP, consistent with previous palaeoenvironmental work across northern Australia.
AB - Previously it has been argued that midden analysis from three geographically distinct coastal regions of tropical northern Australia (Hope Inlet, Blyth River, Blue Mud Bay) demonstrates that changes through time in Aboriginal mollusc exploitation reflect broader coastal environmental transformations associated with late Holocene climatic variability (Bourke et al. 2007). It was suggested that, while a direct link between environmental change and significant cultural change in the archaeological record has yet to be demonstrated unambiguously, midden analysis has the potential to provide the as-yet missing link between changes in climate, environment and human responses over past millennia. We test this hypothesis with a preliminary sclerochronological analysis (i.e. of sequential stable isotopes of oxygen) of archaeological shell samples from all three regions. Our findings suggest the existence of variations in temperature and rainfall indicative of an increasing trend to aridity from 2000 to 500 cal. BP, consistent with previous palaeoenvironmental work across northern Australia.
UR - http://www.scopus.com/inward/record.url?scp=84880200320&partnerID=8YFLogxK
U2 - 10.1080/03122417.2013.11681962
DO - 10.1080/03122417.2013.11681962
M3 - Article
SN - 0312-2417
VL - 76
SP - 21
EP - 33
JO - Australian Archaeology
JF - Australian Archaeology
ER -