Seasonally resolved stratigraphy at Jwalapuram India shows regional surface warming after the Toba volcanic super-eruption

Understanding the nature and tempo of global environmental responses to the ∼74,000 BP (∼74 ka) Toba volcanic super-eruption is based primarily on historical analogies and climate models that lack ground-truthing in regions distal to eruptions. Here, we report the first proxy-based terrestrial record of the immediate environmental impact of the Younger Toba Tuff (YTT) eruption on the hominin-occupied ecosystem in peninsular India, spanning six annual monsoonal cycles directly following the YTT event. We present a multiproxy paleoclimate dataset from Jwalapuram in southern India, featuring a geochemical characterization of multiple YTT tephra and hardpan layers, complemented by detailed stratigraphic observations, sedimentological insights, and stable carbon isotope data. Taken together, these multiple lines of evidence show a progressive trend of tephra weathering and strong evapotranspiration in the immediate aftermath of the YTT, suggesting multiannual regional warming. Our results underline the complex responses of regional environments to the Toba super-eruption, which extend beyond a simple widespread "volcanic winter."

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Publication Details

Journal
PNAS Nexus
Published
2025-03-27
DOI
https://doi.org/10.1093/pnasnexus/pgaf109
Citations
2
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
2.21

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article

Seasonally resolved stratigraphy at Jwalapuram India shows regional surface warming after the Toba volcanic super-eruption

Deepak Kumar Jha, Anna Tsoupra, Jack Longman, Peter Ditchfıeld et al.
2 citations
PNAS Nexus
Climate variability and models
2.21
article

Seasonally resolved stratigraphy at Jwalapuram India shows regional surface warming after the Toba volcanic super-eruption

Deepak Kumar Jha, Anna Tsoupra, Jack Longman, Peter Ditchfıeld, Roshan Paladugu, Sebastian F. M. Breitenbach, GK Jha, Rachel Rudd, Michael D. Petraglia, Patrick Roberts, Nicole Boivin, Rachna Raj, Mafalda Costa, Ola Kwiecien, Hema Achyuthan, K. Krishnan, Cristina Barrocas Dias, Sindu Shree, Devara Anilkumar
article en
2 citations

Abstract

Understanding the nature and tempo of global environmental responses to the ∼74,000 BP (∼74 ka) Toba volcanic super-eruption is based primarily on historical analogies and climate models that lack ground-truthing in regions distal to eruptions. Here, we report the first proxy-based terrestrial record of the immediate environmental impact of the Younger Toba Tuff (YTT) eruption on the hominin-occupied ecosystem in peninsular India, spanning six annual monsoonal cycles directly following the YTT event. We present a multiproxy paleoclimate dataset from Jwalapuram in southern India, featuring a geochemical characterization of multiple YTT tephra and hardpan layers, complemented by detailed stratigraphic observations, sedimentological insights, and stable carbon isotope data. Taken together, these multiple lines of evidence show a progressive trend of tephra weathering and strong evapotranspiration in the immediate aftermath of the YTT, suggesting multiannual regional warming. Our results underline the complex responses of regional environments to the Toba super-eruption, which extend beyond a simple widespread "volcanic winter."

PNAS NexusVol. 4(4)
Smithsonian Institution (US), Maharaja Sayajirao University of Baroda (IN), Griffith University (AU), Jawaharlal Nehru University (IN), The University of Queensland (AU), University of Évora (PT), Hochschule für Angewandte Wissenschaften Kiel (DE), Christian-Albrechts-Universität zu Kiel (DE), Northumbria University (GB), Anna University, Chennai (IN), University of Oxford (GB), Max Planck Institute for Evolutionary Anthropology (DE), Oxford Archaeology (GB), Max Planck Institute for the Science of Human History (DE), Max Planck Institute of Geoanthropology, University of Tübingen (DE)
Maharaja Sayajirao University of Baroda, Fundação para a Ciência e a Tecnologia
Openalex Percentile: Top 14%
Climate variability and models
2.21
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