Lukas Gerber
0009-0008-8721-6889
Heidelberg University
3 papers found
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Holocene Variability of the AMOC as derived from 231Pa/230Th
Foraminifera nitrogen isotopes and body size reveal an oxygen rise in the tropical upper ocean during the Paleocene-Eocene Thermal Maximum (PETM)
Oxygen rise in the tropical upper ocean during the Paleocene-Eocene Thermal Maximum
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