Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum

Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum

<p>The Palaeocene&ndash;Eocene Thermal Maximum (PETM) was a global warming event of 5&ndash;6&thinsp;&deg;C around 56 million years ago caused by input of carbon into the ocean and atmosphere. Hydrothermal venting of greenhouse gases produced in contact aureoles surrounding mag...

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Bibliographic Details
Main Authors: Berndt, C, Planke, S, Alvarez Zarikian, CA, Frieling, J, Jones, MT, Millett, JM, Brinkhuis, H, Bünz, S, Svensen, HH, Longman, J, Scherer, RP, Karstens, J, Manton, B, Nelissen, M, Reed, B, Faleide, JI, Huismans, RS, Agarwal, A, Andrews, GDM, Betlem, P, Bhattacharya, J, Chatterjee, S, Christopoulou, M, Clementi, VJ, Ferré, EC, Filina, IY, Guo, P, Harper, DT, Lambart, S, Mohn, G, Nakaoka, R, Tegner, C, Varela, N, Wang, M, Xu, W, Yager, SL
Format: Journal article
Language:English
Published: Springer Nature 2023

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