Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka

The most explosive volcanic event of the Quaternary was the eruption of Mt. Toba, Sumatra, 75,000 y ago, which produced voluminous ash deposits found across much of the Indian Ocean, Indian Peninsula, and South China Sea. A major climatic downturn observed within the Greenland ice cores has been att...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: Lane, Christine S., Chorn, Ben T., Johnson, Thomas C.
Format: Text
Language:English
Published: National Academy of Sciences 2013
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3657767
http://www.ncbi.nlm.nih.gov/pubmed/23630269
https://doi.org/10.1073/pnas.1301474110
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spelling ftpubmed:oai:pubmedcentral.nih.gov:3657767 2023-05-15T16:29:52+02:00 Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka Lane, Christine S. Chorn, Ben T. Johnson, Thomas C. 2013-05-14 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3657767 http://www.ncbi.nlm.nih.gov/pubmed/23630269 https://doi.org/10.1073/pnas.1301474110 en eng National Academy of Sciences http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3657767 http://www.ncbi.nlm.nih.gov/pubmed/23630269 http://dx.doi.org/10.1073/pnas.1301474110 Physical Sciences Text 2013 ftpubmed https://doi.org/10.1073/pnas.1301474110 2013-11-17T01:27:36Z The most explosive volcanic event of the Quaternary was the eruption of Mt. Toba, Sumatra, 75,000 y ago, which produced voluminous ash deposits found across much of the Indian Ocean, Indian Peninsula, and South China Sea. A major climatic downturn observed within the Greenland ice cores has been attributed to the cooling effects of the ash and aerosols ejected during the eruption of the Youngest Toba Tuff (YTT). These events coincided roughly with a hypothesized human genetic bottleneck, when the number of our species in Africa may have been reduced to near extinction. Some have speculated that the demise of early modern humans at that time was due in part to a dramatic climate shift triggered by the supereruption. Others have argued that environmental conditions would not have been so severe to have such an impact on our ancestors, and furthermore, that modern humans may have already expanded beyond Africa by this time. We report an observation of the YTT in Africa, recovered as a cryptotephra layer in Lake Malawi sediments, >7,000 km west of the source volcano. The YTT isochron provides an accurate and precise age estimate for the Lake Malawi paleoclimate record, which revises the chronology of past climatic events in East Africa. The YTT in Lake Malawi is not accompanied by a major change in sediment composition or evidence for substantial temperature change, implying that the eruption did not significantly impact the climate of East Africa and was not the cause of a human genetic bottleneck at that time. Text Greenland Greenland ice cores PubMed Central (PMC) Greenland Indian Proceedings of the National Academy of Sciences 110 20 8025 8029
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Physical Sciences
spellingShingle Physical Sciences
Lane, Christine S.
Chorn, Ben T.
Johnson, Thomas C.
Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka
topic_facet Physical Sciences
description The most explosive volcanic event of the Quaternary was the eruption of Mt. Toba, Sumatra, 75,000 y ago, which produced voluminous ash deposits found across much of the Indian Ocean, Indian Peninsula, and South China Sea. A major climatic downturn observed within the Greenland ice cores has been attributed to the cooling effects of the ash and aerosols ejected during the eruption of the Youngest Toba Tuff (YTT). These events coincided roughly with a hypothesized human genetic bottleneck, when the number of our species in Africa may have been reduced to near extinction. Some have speculated that the demise of early modern humans at that time was due in part to a dramatic climate shift triggered by the supereruption. Others have argued that environmental conditions would not have been so severe to have such an impact on our ancestors, and furthermore, that modern humans may have already expanded beyond Africa by this time. We report an observation of the YTT in Africa, recovered as a cryptotephra layer in Lake Malawi sediments, >7,000 km west of the source volcano. The YTT isochron provides an accurate and precise age estimate for the Lake Malawi paleoclimate record, which revises the chronology of past climatic events in East Africa. The YTT in Lake Malawi is not accompanied by a major change in sediment composition or evidence for substantial temperature change, implying that the eruption did not significantly impact the climate of East Africa and was not the cause of a human genetic bottleneck at that time.
format Text
author Lane, Christine S.
Chorn, Ben T.
Johnson, Thomas C.
author_facet Lane, Christine S.
Chorn, Ben T.
Johnson, Thomas C.
author_sort Lane, Christine S.
title Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka
title_short Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka
title_full Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka
title_fullStr Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka
title_full_unstemmed Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka
title_sort ash from the toba supereruption in lake malawi shows no volcanic winter in east africa at 75 ka
publisher National Academy of Sciences
publishDate 2013
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3657767
http://www.ncbi.nlm.nih.gov/pubmed/23630269
https://doi.org/10.1073/pnas.1301474110
geographic Greenland
Indian
geographic_facet Greenland
Indian
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Greenland ice cores
genre_facet Greenland
Greenland ice cores
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3657767
http://www.ncbi.nlm.nih.gov/pubmed/23630269
http://dx.doi.org/10.1073/pnas.1301474110
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container_title Proceedings of the National Academy of Sciences
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container_issue 20
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