[图书][B] Biogeochemistry of marine dissolved organic matter
DA Hansell, CA Carlson - 2014 - books.google.com
Marine dissolved organic matter (DOM) is a complex mixture of molecules found throughout
the world's oceans. It plays a key role in the export, distribution, and sequestration of carbon …
the world's oceans. It plays a key role in the export, distribution, and sequestration of carbon …
Carbon sequestration during the Palaeocene–Eocene Thermal Maximum by an efficient biological pump
A perturbation of the carbon cycle and biosphere, linked to globally increased temperatures
about 55.9 million years ago, characterized the Palaeocene–Eocene Thermal Maximum. Its …
about 55.9 million years ago, characterized the Palaeocene–Eocene Thermal Maximum. Its …
I/Ca evidence for upper ocean deoxygenation during the PETM
Anthropogenic global warming affects marine ecosystems in complex ways, and declining
ocean oxygenation is a growing concern. Forecasting the geographical and bathymetric …
ocean oxygenation is a growing concern. Forecasting the geographical and bathymetric …
[HTML][HTML] Coccolithophore calcification response to past ocean acidification and climate change
Anthropogenic carbon dioxide emissions are forcing rapid ocean chemistry changes and
causing ocean acidification (OA), which is of particular significance for calcifying organisms …
causing ocean acidification (OA), which is of particular significance for calcifying organisms …
Middle Eocene to late Oligocene Antarctic glaciation/deglaciation and Southern Ocean productivity
G Villa, C Fioroni, D Persico, AP Roberts… - …, 2014 - Wiley Online Library
Abstract During the Eocene‐Oligocene transition, Earth cooled significantly from a
greenhouse to an icehouse climate. Nannofossil assemblages from Southern Ocean sites …
greenhouse to an icehouse climate. Nannofossil assemblages from Southern Ocean sites …
The spread of marine anoxia on the northern Tethys margin during the Paleocene‐Eocene Thermal Maximum
Records of the paleoenvironmental changes that occurred during the Paleocene‐Eocene
Thermal Maximum (PETM) are preserved in sedimentary rocks along the margins of the …
Thermal Maximum (PETM) are preserved in sedimentary rocks along the margins of the …
Deep‐sea redox across the Paleocene‐Eocene thermal maximum
C Pälike, ML Delaney, JC Zachos - Geochemistry, Geophysics …, 2014 - Wiley Online Library
Large amounts of 13C‐depleted carbon were released to the oceans and atmosphere
during a period of abrupt global warming at the Paleocene‐Eocene thermal maximum …
during a period of abrupt global warming at the Paleocene‐Eocene thermal maximum …
Enhanced primary productivity and magnetotactic bacterial production in response to middle Eocene warming in the Neo-Tethys Ocean
Earth's climate experienced a warming event known as the Middle Eocene Climatic
Optimum (MECO) at~ 40 Ma, which was an abrupt reversal of a long-term Eocene cooling …
Optimum (MECO) at~ 40 Ma, which was an abrupt reversal of a long-term Eocene cooling …
Rapid fluctuations in mid-latitude siliceous plankton production during the Middle Eocene Climatic Optimum (ODP Site 1051, western North Atlantic)
Abstract The Middle Eocene Climatic Optimum (MECO;~ 40 million years ago [Ma]) is one of
the most prominent transient global warming events in the Paleogene. Although the event is …
the most prominent transient global warming events in the Paleogene. Although the event is …
Impact of dissolution on the sedimentary record of the Paleocene–Eocene thermal maximum
TJ Bralower, DC Kelly, S Gibbs, K Farley… - Earth and Planetary …, 2014 - Elsevier
The input of massive amounts of carbon to the atmosphere and ocean at the Paleocene–
Eocene Thermal Maximum (PETM;∼ 55.53 Ma) resulted in pervasive carbonate dissolution …
Eocene Thermal Maximum (PETM;∼ 55.53 Ma) resulted in pervasive carbonate dissolution …