50,000 years of archaeological site stratigraphy and micromorphology in Boodie Cave, Barrow Island, Western Australia

Ward, Ingrid, Veth, Peter Marius, Prossor, L., Denham, T., Ditchfield, Kane, Manne, T., Kendrick, P., Byrne, C., Hook, F. and Troitzcsh, U. (2017) 50,000 years of archaeological site stratigraphy and micromorphology in Boodie Cave, Barrow Island, Western Australia. Journal of Archaeological Science: Reports, 15 344-369. doi:10.1016/j.jasrep.2017.08.012


Author Ward, Ingrid
Veth, Peter Marius
Prossor, L.
Denham, T.
Ditchfield, Kane
Manne, T.
Kendrick, P.
Byrne, C.
Hook, F.
Troitzcsh, U.
Title 50,000 years of archaeological site stratigraphy and micromorphology in Boodie Cave, Barrow Island, Western Australia
Journal name Journal of Archaeological Science: Reports
ISSN 2352-409X
Publication date 2017-10-01
Year available 2017
Sub-type Article (original research)
DOI 10.1016/j.jasrep.2017.08.012
Open Access Status Not yet assessed
Volume 15
Start page 344
End page 369
Total pages 26
Place of publication Amsterdam, Netherlands
Publisher Elsevier BV
Language eng
Abstract This study explores the application of soil micromorphological and automated scanning electron microscopy mineralogical analysis to characterise lithological boundaries and site formation history from an archaeological cave site on Barrow Island, northwestern Australia. The high-resolution characterisation is used to document the changing depositional context within Boodie Cave from the earliest period of occupation around 50 ky BP through to when transgressing seas isolated the island around 7 ky BP. Comparisons are made between excavations at the front of the cave - where stratigraphic integrity is high and a thicker, more comprehensive early Holocene sequence is preserved, with excavations inside the cave - where stratigraphic integrity is lower but an older Pleistocene record is preserved. The combination of these depositional scenarios provides a complete stratigraphic sequence for Boodie Cave, with depositional contacts defined at macro-, meso- and micro-scale levels. These contacts include erosive surfaces and trampled (ground) surfaces, such as the upper interface of SU5 and SU4. Based on the mineralogical and textural variations (microfacies) preserved within each unit, the vertical mixing zone is estimated to be between 1 and 5 cm. This reworking has not affected the general sequence of sedimentological (including grain size and mineralogy) and macro-cultural changes, which record an increasingly marine-dominated assemblage as the coastline encroaches. The integration of microscopic observations with anthracological, archaeomalacological, zooarchaeological and lithic analyses provides a more dynamic and comprehensive dialogue for interpreting the formation history of Boodie Cave and likely other early occupation sites from northern Australia.
Keyword Northwestern Australia
Sediments
Occupation
Indonesia
History
Q-Index Code C1
Q-Index Status Provisional Code
Grant ID DP150104604 | DE150101597 | DP130100802
Institutional Status UQ
Additional Notes http://www.sciencedirect.com/science/article/pii/S2352409X1730408X

Document type: Journal Article
Sub-type: Article (original research)
Collections: HERDC Pre-Audit
School of Social Science Publications
 
Versions
Version Filter Type
Citation counts: Scopus Citation Count Cited 0 times in Scopus Article
Google Scholar Search Google Scholar
Created: Wed, 13 Sep 2017, 10:25:13 EST by Tiina Manne on behalf of School of Social Science