Supplemental Material: Larger benthic foraminiferal turnover and carbon isotope excursion during the Paleocene–Eocene Thermal Maximum in the Southern Himalayan carbonate platform (Eastern Neo-Tethys Ocean, Pakistan)

Q: What type of study is this?

This is a Quantitative Study study.

Muhammad Kamran; et al.

doi:10.1130/gsab.s.30300397.v1

October 7, 2025Open Access

Supplemental Material: Larger benthic foraminiferal turnover and carbon isotope excursion during the Paleocene–Eocene Thermal Maximum in the Southern Himalayan carbonate platform (Eastern Neo-Tethys Ocean, Pakistan)

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Key Points

Significant benthic foraminiferal turnover observed during the Paleocene-Eocene Thermal Maximum, indicating major environmental changes.
Stable carbon and oxygen isotopes (δ13C, δ18O) are analyzed from samples collected in the Southern Himalayan region.
Detailed isotopic cross-plots illustrate correlations relevant to environmental conditions during this geological period.
Findings highlight the importance of the Eastern Neo-Tethys Ocean as a significant region for examining ancient climate events.

Implication

Analysis reveals significant changes in benthic foraminifera and carbon isotopes in the Southern Himalayan carbonate platform, suggesting environmental shifts.

Abstract

Stable isotope datasets (δ13C and δ18O) from the Jandran and Sanjawi sections, along with supporting figures illustrating isotopic cross-plots and correlations, and tables of matrix micrite and bulk carbonate values.

Discussion

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Cite This Study

Kamran et al. (2025) studied this question.

synapsesocial.com/papers/68e70da790569dd607ee5ad3 https://doi.org/10.1130/gsab.s.30300397.v1

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Supplemental Material: Larger benthic foraminiferal turnover and carbon isotope excursion during the Paleocene–Eocene Thermal Maximum in the Southern Himalayan carbonate platform (Eastern Neo-Tethys Ocean, Pakistan)

Key Points

Implication

Abstract

Discussion

Cite This Study

Supplemental Material: Larger benthic foraminiferal turnover and carbon isotope excursion during the Paleocene–Eocene Thermal Maximum in the Southern Himalayan carbonate platform (Eastern Neo-Tethys Ocean, Pakistan)

Key Points

Implication

Abstract

Discussion

Cite This Study

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