A molybdenum isotope record of Eocene Thermal Maximum 2: Implications for global ocean redox during the early Eocene
During the early Eocene, a series of short-term global warming events ("hyperthermals") occurred in response to the rapid release of carbon into the oceans and atmosphere. In order to investigate the response of ocean redox to global warming, we have determined the molybdenum isotope compo...
Main Authors: | Dickson, A, Cohen, A |
---|---|
Formato: | Journal article |
Idioma: | English |
Publicado: |
2012
|
Títulos similares
-
Constraints on ocean circulation at the Paleocene–Eocene Thermal Maximum from neodymium isotopes
por: A. N. Abbott, et al.
Publicado: (2016-04-01) -
Seawater oxygenation during the Paleocene-Eocene Thermal Maximum
por: Dickson, A, et al.
Publicado: (2012) -
Shallow-water carbonate record of the Paleocene-Eocene Thermal maximum from a Pacific Ocean Guyot
por: Robinson, SA
Publicado: (2011) -
Expanded subsurface ocean anoxia in the Atlantic during the Paleocene-Eocene Thermal Maximum
por: Weiqi Yao, et al.
Publicado: (2024-10-01) -
Mercury anomalies across the Palaeocene–Eocene Thermal Maximum
por: M. T. Jones, et al.
Publicado: (2019-02-01)