Iron isotope and trace metal record of Cenomanian-Turonian sediments
he global carbon cycle during the mid-Cretaceous (~125-88 million years ago, Ma) experienced numerous major perturbations linked to increased organic carbon burial under widespread, possibly basin-scale oxygen deficiency and episodes of euxinia (anoxic and H2S-containing). The largest of these episo...
Main Authors: | , , , , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2012
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.824952 https://doi.org/10.1594/PANGAEA.824952 |