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利达阿杰尔洞的洞穴学和环境史,西苏门答腊。

Speleological and environmental history of Lida Ajer cave, western Sumatra.

机构信息

Australian Research Centre for Human Evolution, Griffith University, Brisbane 4111 Australia.

Centro Nacional de Investigación sobre la Evolución Humana (CENIEH), Burgos 09002, Spain.

出版信息

Philos Trans R Soc Lond B Biol Sci. 2022 Apr 25;377(1849):20200494. doi: 10.1098/rstb.2020.0494. Epub 2022 Mar 7.

DOI:10.1098/rstb.2020.0494
PMID:35249388
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8922409/
Abstract

Some of the earliest evidence for the presence of modern humans in rainforests has come from the fossil deposits of Lida Ajer in Sumatra. Two human teeth from this cave were estimated to be 73-63 thousand years old, which is significantly older than some estimates of modern human migration out of Africa based on genetic data. The deposits were interpreted as being associated with a rainforest environment based largely on the presence of abundant orangutan fossils. As well as the main fossil-bearing chamber, fossil-bearing passages are present below a sinkhole, although the relationship between the different fossil deposits has only been tenuously established. Here, we provide significant new sedimentological, geochronological and palaeoecological data aimed at reconstructing the speleological and environmental history of the cave and the clastic and fossil deposits therein. Our data suggest that the Lida Ajer fossils were deposited during Marine Isotope Stage 4, with fossils from the lower passages older than the main fossil chamber. Our use of stable carbon and oxygen isotope analyses of mammalian tooth enamel demonstrates that early humans probably occupied a closed-canopy forest very similar to those present in the region today, although the fossil orangutans may have occupied a slightly different niche. This article is part of the theme issue 'Tropical forests in the deep human past'.

摘要

一些关于现代人出现在热带雨林中的最早证据来自苏门答腊的力达·阿杰尔化石沉积物。从这个洞穴中发现的两颗人类牙齿估计有 7.3 万至 6.3 万年的历史,这比一些基于遗传数据的现代人类离开非洲的估计要早得多。这些沉积物被解释为与热带雨林环境有关,主要是因为有大量的猩猩化石。除了主要的含化石洞穴外,一个陷坑下面还有含化石的通道,尽管不同化石沉积物之间的关系只是初步确定的。在这里,我们提供了重要的新沉积学、年代学和古生态学数据,旨在重建洞穴的洞穴学和环境历史以及其中的碎屑和化石沉积物。我们的数据表明,力达·阿杰尔化石是在海洋同位素阶段 4 期间沉积的,下部通道的化石比主化石室还要古老。我们利用哺乳动物牙齿珐琅质的稳定碳和氧同位素分析表明,早期人类可能占据了一个类似于今天该地区存在的封闭树冠森林,尽管化石猩猩可能占据了一个略有不同的生态位。本文是主题为“远古时期的热带森林”的一部分。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/373f/8922409/74fc0a781eda/rstb20200494f03.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/373f/8922409/8178ccce2314/rstb20200494f01.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/373f/8922409/8561cdf4531b/rstb20200494f02.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/373f/8922409/74fc0a781eda/rstb20200494f03.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/373f/8922409/8178ccce2314/rstb20200494f01.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/373f/8922409/8561cdf4531b/rstb20200494f02.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/373f/8922409/74fc0a781eda/rstb20200494f03.jpg

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