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Speleological and environmental history of Lida Ajer cave, western Sumatra

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 Af...

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Autores principales: Louys, Julien, Duval, Mathieu, Price, Gilbert J., Westaway, Kira, Zaim, Yahdi, Rizal, Yan, Puspaningrum, Mika, Trihascaryo, Agus, Breitenbach, Sebastian F. M., Kwiecien, Ola, Cai, Yanjun, Higgins, Penny, Albers, Paul C. H., de Vos, John, Roberts, Patrick
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8922409/
https://www.ncbi.nlm.nih.gov/pubmed/35249388
http://dx.doi.org/10.1098/rstb.2020.0494
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author Louys, Julien
Duval, Mathieu
Price, Gilbert J.
Westaway, Kira
Zaim, Yahdi
Rizal, Yan
Puspaningrum, Mika
Trihascaryo, Agus
Breitenbach, Sebastian F. M.
Kwiecien, Ola
Cai, Yanjun
Higgins, Penny
Albers, Paul C. H.
de Vos, John
Roberts, Patrick
author_facet Louys, Julien
Duval, Mathieu
Price, Gilbert J.
Westaway, Kira
Zaim, Yahdi
Rizal, Yan
Puspaningrum, Mika
Trihascaryo, Agus
Breitenbach, Sebastian F. M.
Kwiecien, Ola
Cai, Yanjun
Higgins, Penny
Albers, Paul C. H.
de Vos, John
Roberts, Patrick
author_sort Louys, Julien
collection PubMed
description 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’.
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spelling pubmed-89224092022-03-17 Speleological and environmental history of Lida Ajer cave, western Sumatra Louys, Julien Duval, Mathieu Price, Gilbert J. Westaway, Kira Zaim, Yahdi Rizal, Yan Puspaningrum, Mika Trihascaryo, Agus Breitenbach, Sebastian F. M. Kwiecien, Ola Cai, Yanjun Higgins, Penny Albers, Paul C. H. de Vos, John Roberts, Patrick Philos Trans R Soc Lond B Biol Sci Articles 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’. The Royal Society 2022-04-25 2022-03-07 /pmc/articles/PMC8922409/ /pubmed/35249388 http://dx.doi.org/10.1098/rstb.2020.0494 Text en © 2022 The Authors. https://creativecommons.org/licenses/by/4.0/Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) , which permits unrestricted use, provided the original author and source are credited.
spellingShingle Articles
Louys, Julien
Duval, Mathieu
Price, Gilbert J.
Westaway, Kira
Zaim, Yahdi
Rizal, Yan
Puspaningrum, Mika
Trihascaryo, Agus
Breitenbach, Sebastian F. M.
Kwiecien, Ola
Cai, Yanjun
Higgins, Penny
Albers, Paul C. H.
de Vos, John
Roberts, Patrick
Speleological and environmental history of Lida Ajer cave, western Sumatra
title Speleological and environmental history of Lida Ajer cave, western Sumatra
title_full Speleological and environmental history of Lida Ajer cave, western Sumatra
title_fullStr Speleological and environmental history of Lida Ajer cave, western Sumatra
title_full_unstemmed Speleological and environmental history of Lida Ajer cave, western Sumatra
title_short Speleological and environmental history of Lida Ajer cave, western Sumatra
title_sort speleological and environmental history of lida ajer cave, western sumatra
topic Articles
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8922409/
https://www.ncbi.nlm.nih.gov/pubmed/35249388
http://dx.doi.org/10.1098/rstb.2020.0494
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