HAL (France)
open access
Volcanic controls on smectite authigenesis and paleoclimate signals across the Paleocene-Eocene Thermal Maximum (PETM) sedimentary record from the Norwegian-Greenland Sea.
Clay mineral records provide archives of continental weathering and paleohydrology, but these paleoclimate signals can be obscured by authigenic or diagenetic overprinting. International Ocean Discovery Program Expedition 396 drilled an expanded Paleocene–Eocene Thermal Maximum (PETM) succession fro
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