ArticlePaleoceanography and paleoclimatology2019
Widespread Warming Before and Elevated Barium Burial During the Paleocene-Eocene Thermal Maximum: Evidence for Methane Hydrate Release?
Article in Paleoceanography and paleoclimatology, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 12 papers.
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Who cites it
12 citing papers in PubMed, 72 citations in OpenAlex.
- Recognition of two potential warming events in the Paleocene terrestrial record of North America and associated mammalian responses.PNAS nexus · 2026Article
- Widespread terrestrial ecosystem disruption at the onset of the Paleocene-Eocene Thermal Maximum.Proceedings of the National Academy of Sciences of the United States of America · 2026Article
- Loss of vegetation functions during the Paleocene-Eocene Thermal Maximum.Nature communications · 2025Article
- Marine mammals as indicators of Anthropocene Ocean Health.npj biodiversity · 2024Review
- Loss of Earth system resilience during early Eocene transient global warming events.Science advances · 2023Article
- Volcanic COScience advances · 2023Article
- Evidence for massive methane hydrate destabilization during the penultimate interglacial warming.Proceedings of the National Academy of Sciences of the United States of America · 2022Article
- Surface ocean warming and acidification driven by rapid carbon release precedes Paleocene-Eocene Thermal Maximum.Science advances · 2022Article
- Eutrophication and Deoxygenation Forcing of Marginal Marine Organic Carbon Burial During the PETM.Paleoceanography and paleoclimatology · 2022Article
- Paleocene/Eocene carbon feedbacks triggered by volcanic activity.Nature communications · 2021Article
- Archaeal lipid biomarker constraints on the Paleocene-Eocene carbon isotope excursion.Nature communications · 2019Article
- Widespread Warming Before and Elevated Barium Burial During the Paleocene-Eocene Thermal Maximum: Evidence for Methane Hydrate Release?Paleoceanography and paleoclimatology · 2019Article
Corrections and comments
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Authors and funding
7 authors at 3 institutions in 3 countries.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Current climate change may induce positive carbon cycle feedbacks that amplify anthropogenic warming on time scales of centuries to millennia. Similar feedbacks might have been active during a phase of carbon cycle perturbation and global warming, termed the Paleocene-Eocene Thermal Maximum (PETM, 56 million years ago). The PETM may help constrain these feedbacks and their sensitivity to warming. We present new high-resolution carbon isotope and sea surface temperature data from Ocean Drilling Program Site 959 in the Equatorial Atlantic. With these and existing data from the New Jersey Shelf and Maud Rise, Southern Ocean, we quantify the lead-lag relation between PETM warming and the carbon input that caused the carbon isotope excursion (CIE). We show ~2 °C of global warming preceded the CIE by millennia, strongly implicating CO
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