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...

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Bibliographic Details
Main Authors: Owens, Jeremy D, Lyons, Timothy W, Li, Xiaona N, MacLeod, Kenneth G, Gordon, Gwenyth, Kuypers, Marcel MM, Anbar, Ariel D, Kuhnt, Wolfgang, Severmann, Silke
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2012
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.824952
https://doi.org/10.1594/PANGAEA.824952