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Fossil-bound nitrogen isotope and foraminifera size evidence for oxygenated tropical subsurface waters during the Paleocene-Eocene Thermal Maximum

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Moretti,  Simone
Climate Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Schiebel,  Ralf
Climate Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Haug,  Gerald Hermann
Climate Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

/persons/resource/persons192213

Martinez-Garcia,  Alfredo
Climate Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Moretti, S., Auderset, A., Deutsch, C. A., Schmitz, R., Thomas, E., Gerber, L., et al. (2024). Fossil-bound nitrogen isotope and foraminifera size evidence for oxygenated tropical subsurface waters during the Paleocene-Eocene Thermal Maximum. Poster presented at Ocean Sciences Meeting, New Orleans, LA.


Cite as: https://hdl.handle.net/21.11116/0000-000E-9D26-7
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