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The sedimentary record of palaeoenvironments and sea-level change in the Gulf of Carpentaria, Australia, through the last glacial cycle

Reeves, Jessica M., Chivas, Allan R., García, Adriana, Holt, Sabine, Couapel, Martine J.J., Jones, Brian G., Cendón, Dioni I., Fink, David·2008·Quaternary International
DOI 10.1016/j.quaint.2007.11.019
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  • During the millennia following human arrival, the hydroclimate at the continental scale cycled several times through conditions similar to modern conditions, toward both wetter and drier periods, potentially with different timing and to differing degrees from the south to the north of the continent.

    “However, during the millennia following human arrival, the hydroclimate at the continental scale cycled several times through conditions similar to modern conditions, toward both wetter and drier periods, potentially with different timing and to differing degrees from the south to the north of the continent (48–51).”

    From Humans, water, and the colonization of Australia (2016) · cites this paper as [50]

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Metadata

Authors
Reeves, J. M., Chivas, A. R., García, A., Holt, S., Couapel, M. J. J., Jones, B. G., Cendón, D. I., & Fink, D.
Venue
Quaternary International
Publisher
Elsevier BV
Published
2008-05
Volume
183
Issue
1
Pages
3-22
ISSN
1040-6182
DOI
10.1016/j.quaint.2007.11.019
Cited by
87
References
1
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)

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