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斑兰叶的果壳为澳大利亚北部的马杰比比(Madjedbebe)提供了人类居住的古降水记录。

Pandanus nutshell generates a palaeoprecipitation record for human occupation at Madjedbebe, northern Australia.

机构信息

School of Social Science, The University of Queensland, Brisbane, Queensland, Australia.

Australian Research Council Centre of Excellence for Australian Biodiversity and Heritage, University of Wollongong, Wollongong, New South Wales, Australia.

出版信息

Nat Ecol Evol. 2021 Mar;5(3):295-303. doi: 10.1038/s41559-020-01379-8. Epub 2021 Jan 25.

DOI:10.1038/s41559-020-01379-8
PMID:33495592
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7929916/
Abstract

Little is known about the Pleistocene climatic context of northern Australia at the time of early human settlement. Here we generate a palaeoprecipitation proxy using stable carbon isotope analysis of modern and archaeological pandanus nutshell from Madjedbebe, Australia's oldest known archaeological site. We document fluctuations in precipitation over the last 65,000 years and identify periods of lower precipitation during the penultimate and last glacial stages, Marine Isotope Stages 4 and 2. However, the lowest effective annual precipitation is recorded at the present time. Periods of lower precipitation, including the earliest phase of occupation, correspond with peaks in exotic stone raw materials and artefact discard at the site. This pattern is interpreted as suggesting increased group mobility and intensified use of the region during drier periods.

摘要

关于早期人类定居时澳大利亚北部更新世的气候背景,我们知之甚少。在这里,我们使用现代和考古潘达努斯果壳的稳定碳同位素分析,在澳大利亚最古老的已知考古遗址 Madjedbebe 生成了一个古降水代理。我们记录了过去 65000 年来降水的波动情况,并确定了倒数第二个和最后一个冰河期阶段(海洋同位素阶段 4 和 2)期间降水较少的时期。然而,目前记录到的有效年降水量最低。降水较少的时期,包括最早的居住阶段,与该地点外来石器原料和文物丢弃的高峰期相对应。这种模式表明,在较干燥的时期,群体的流动性增加,对该地区的使用强度加大。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/27f4d1dd2da1/41559_2020_1379_Fig8_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/ce57d2bca401/41559_2020_1379_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/b80fa58a74fe/41559_2020_1379_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/ff52d9e5d5a6/41559_2020_1379_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/3972a267c912/41559_2020_1379_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/3d32330c4eaf/41559_2020_1379_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/94d9cfcba342/41559_2020_1379_Fig6_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/b5ad55bf7d2f/41559_2020_1379_Fig7_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/27f4d1dd2da1/41559_2020_1379_Fig8_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/ce57d2bca401/41559_2020_1379_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/b80fa58a74fe/41559_2020_1379_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/ff52d9e5d5a6/41559_2020_1379_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/3972a267c912/41559_2020_1379_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/3d32330c4eaf/41559_2020_1379_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/94d9cfcba342/41559_2020_1379_Fig6_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/b5ad55bf7d2f/41559_2020_1379_Fig7_ESM.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cf2f/7929916/27f4d1dd2da1/41559_2020_1379_Fig8_ESM.jpg

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