Understanding the overestimated impact of the Toba volcanic super-eruption on global environments and ancient hominins
Understanding the overestimated impact of the Toba volcanic super-eruption on global environments and ancient hominins
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了解多巴火山超级喷发对全球环境和古代人类的高估影响
DOI:
10.1016/j.quaint.2020.06.021
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发表时间:
2020-07
影响因子:
2.2
通讯作者:
Gao Xing
中科院分区:
文献类型:
--
作者:
Ge Yong;Gao Xing
The ~74 ka Toba super-eruption was the largest known explosive volcanic event of the past 2.5 million years and has been held responsible for presumed dramatic global cooling and large-scale hominin extinction. The hypothesis that the Toba super-eruption resulted in human extinction outside of tropical Africa has been cited as a mechanism to support models of a Middle Pleistocene African origin for modern humans. This hypothesis has prevailed for decades and drawn the attention of researchers from many fields. Recently, this proposition has been debated or refuted because of the development of more precise dating techniques and higher-resolution geological records that provide new data to reevaluate the climatic influence of the Toba event. Relevant archaeological evidence also indicates the survival of hominin groups in Eurasia immediately after the Toba event, even in India and Sumatra, which were covered by thick deposits of volcanic ash. Here, we correlate high-resolution geological records with the most precise available ages for the Toba event (ca. 74 ka), including ice cores, stalagmites, and lake and deep-sea sediments, concluding only limited influence of the Toba super-eruption on the Earth's climate. We also assemble archaeological data demonstrating continuity of human activity before and after the Toba event, ancient DNA and fossil evidences also testify the survival of other archaic humans after the eruption. The preponderance of the evidence dictates rejection of previous “population bottleneck” hypotheses and the total replacement model for the origins of modern humans. Although the Toba super-eruption was the largest such event of the Quaternary period, it did not have a devastating impact on the Earth's climate and human activity.
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影响因子:
56.9
作者:
M. Rampino;S. Self;R. Fairbridge
通讯作者:
M. Rampino;S. Self;R. Fairbridge
DOI:
10.1016/j.palaeo.2005.03.042
发表时间:
2005-08
期刊:
Palaeogeography, Palaeoclimatology, Palaeoecology
影响因子:
--
作者:
W. Kuhnt;S. Hess;A. Holbourn;Harald Paulsen;Brigitte Salomon
通讯作者:
W. Kuhnt;S. Hess;A. Holbourn;Harald Paulsen;Brigitte Salomon
DOI:
10.1126/science.1224344
发表时间:
2012-10-12
期刊:
Science (New York, N.Y.)
影响因子:
--
作者:
Meyer M;Kircher M;Gansauge MT;Li H;Racimo F;Mallick S;Schraiber JG;Jay F;Prüfer K;de Filippo C;Sudmant PH;Alkan C;Fu Q;Do R;Rohland N;Tandon A;Siebauer M;Green RE;Bryc K;Briggs AW;Stenzel U;Dabney J;Shendure J;Kitzman J;Hammer MF;Shunkov MV;Derevianko AP;Patterson N;Andrés AM;Eichler EE;Slatkin M;Reich D;Kelso J;Pääbo S
通讯作者:
Pääbo S
影响因子:
56.9
作者:
Solomon, Susan;Rosenlof, Karen H.;Plattner, Gian-Kasper
通讯作者:
Plattner, Gian-Kasper
影响因子:
5.8
作者:
R. Larson
通讯作者:
R. Larson