Late glacial (17,060–13,400 cal yr BP) sedimentary and paleoenvironmental evolution of the Sekhokong Range (Drakensberg), southern Africa
Southern Africa sits at the junction of tropical and temperate systems, leading to the formation of seasonal precipitation zones. Understanding late Quaternary paleoclimatic change in this vulnerable region is hampered by a lack of available, reliably-dated records. Here we present a sequence from a...
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ftpubmed:oai:pubmedcentral.nih.gov:7968709 2023-05-15T13:31:40+02:00 Late glacial (17,060–13,400 cal yr BP) sedimentary and paleoenvironmental evolution of the Sekhokong Range (Drakensberg), southern Africa Kylander, Malin E. Holm, Mikaela Fitchett, Jennifer Grab, Stefan Martinez Cortizas, Antonio Norström, Elin Bindler, Richard 2021-03-17 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7968709/ http://www.ncbi.nlm.nih.gov/pubmed/33730018 https://doi.org/10.1371/journal.pone.0246821 en eng Public Library of Science http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7968709/ http://www.ncbi.nlm.nih.gov/pubmed/33730018 http://dx.doi.org/10.1371/journal.pone.0246821 © 2021 Kylander et al http://creativecommons.org/licenses/by/4.0/ This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/) , which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. CC-BY PLoS One Research Article Text 2021 ftpubmed https://doi.org/10.1371/journal.pone.0246821 2021-04-04T00:42:21Z Southern Africa sits at the junction of tropical and temperate systems, leading to the formation of seasonal precipitation zones. Understanding late Quaternary paleoclimatic change in this vulnerable region is hampered by a lack of available, reliably-dated records. Here we present a sequence from a well-stratified sedimentary infill occupying a lower slope basin which covers 17,060 to 13,400 cal yr BP with the aim to reconstruct paleoclimatic variability in the high Drakensberg during the Late Glacial. We use a combination of pollen, total organic carbon and nitrogen, δ(13)C, Fourier transform infrared spectroscopy attenuated total reflectance (FTIR-ATR) spectral and elemental data on contiguous samples with high temporal resolution (10 to 80 years per sample). Our data support a relatively humid environment with considerable cold season precipitation during what might have been the final stage of niche-glaciation on the adjoining southern aspects around 17,000 cal yr BP. Then, after an initial warmer and drier period starting ~15,600 cal yr BP, we identify a return to colder and drier conditions with more winter precipitation starting ~14,380 cal yr BP, which represents the first local evidence for the Antarctic Cold Reversal (ACR) in this region. On decadal to centennial timescales, the Late Glacial period was one marked by considerable climatic fluctuation and bi-directional environmental change, which has not been identified in previous studies for this region. Our study shows complex changes in both moisture and thermal conditions providing a more nuanced picture of the Late Glacial for the high Drakensburg. Text Antarc* Antarctic PubMed Central (PMC) Antarctic The Antarctic PLOS ONE 16 3 e0246821 |
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Research Article Kylander, Malin E. Holm, Mikaela Fitchett, Jennifer Grab, Stefan Martinez Cortizas, Antonio Norström, Elin Bindler, Richard Late glacial (17,060–13,400 cal yr BP) sedimentary and paleoenvironmental evolution of the Sekhokong Range (Drakensberg), southern Africa |
topic_facet |
Research Article |
description |
Southern Africa sits at the junction of tropical and temperate systems, leading to the formation of seasonal precipitation zones. Understanding late Quaternary paleoclimatic change in this vulnerable region is hampered by a lack of available, reliably-dated records. Here we present a sequence from a well-stratified sedimentary infill occupying a lower slope basin which covers 17,060 to 13,400 cal yr BP with the aim to reconstruct paleoclimatic variability in the high Drakensberg during the Late Glacial. We use a combination of pollen, total organic carbon and nitrogen, δ(13)C, Fourier transform infrared spectroscopy attenuated total reflectance (FTIR-ATR) spectral and elemental data on contiguous samples with high temporal resolution (10 to 80 years per sample). Our data support a relatively humid environment with considerable cold season precipitation during what might have been the final stage of niche-glaciation on the adjoining southern aspects around 17,000 cal yr BP. Then, after an initial warmer and drier period starting ~15,600 cal yr BP, we identify a return to colder and drier conditions with more winter precipitation starting ~14,380 cal yr BP, which represents the first local evidence for the Antarctic Cold Reversal (ACR) in this region. On decadal to centennial timescales, the Late Glacial period was one marked by considerable climatic fluctuation and bi-directional environmental change, which has not been identified in previous studies for this region. Our study shows complex changes in both moisture and thermal conditions providing a more nuanced picture of the Late Glacial for the high Drakensburg. |
format |
Text |
author |
Kylander, Malin E. Holm, Mikaela Fitchett, Jennifer Grab, Stefan Martinez Cortizas, Antonio Norström, Elin Bindler, Richard |
author_facet |
Kylander, Malin E. Holm, Mikaela Fitchett, Jennifer Grab, Stefan Martinez Cortizas, Antonio Norström, Elin Bindler, Richard |
author_sort |
Kylander, Malin E. |
title |
Late glacial (17,060–13,400 cal yr BP) sedimentary and paleoenvironmental evolution of the Sekhokong Range (Drakensberg), southern Africa |
title_short |
Late glacial (17,060–13,400 cal yr BP) sedimentary and paleoenvironmental evolution of the Sekhokong Range (Drakensberg), southern Africa |
title_full |
Late glacial (17,060–13,400 cal yr BP) sedimentary and paleoenvironmental evolution of the Sekhokong Range (Drakensberg), southern Africa |
title_fullStr |
Late glacial (17,060–13,400 cal yr BP) sedimentary and paleoenvironmental evolution of the Sekhokong Range (Drakensberg), southern Africa |
title_full_unstemmed |
Late glacial (17,060–13,400 cal yr BP) sedimentary and paleoenvironmental evolution of the Sekhokong Range (Drakensberg), southern Africa |
title_sort |
late glacial (17,060–13,400 cal yr bp) sedimentary and paleoenvironmental evolution of the sekhokong range (drakensberg), southern africa |
publisher |
Public Library of Science |
publishDate |
2021 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7968709/ http://www.ncbi.nlm.nih.gov/pubmed/33730018 https://doi.org/10.1371/journal.pone.0246821 |
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Antarctic The Antarctic |
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Antarctic The Antarctic |
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Antarc* Antarctic |
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Antarc* Antarctic |
op_source |
PLoS One |
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7968709/ http://www.ncbi.nlm.nih.gov/pubmed/33730018 http://dx.doi.org/10.1371/journal.pone.0246821 |
op_rights |
© 2021 Kylander et al http://creativecommons.org/licenses/by/4.0/ This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/) , which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. |
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CC-BY |
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https://doi.org/10.1371/journal.pone.0246821 |
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16 |
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e0246821 |
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