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Onset of North Atlantic deep water production coincident with inception of the C...
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Upper ocean mixing controls the seasonality of planktonic foraminifer fluxes and...
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Expedition 342: Paleogene Newfoundland Sediment Drifts; 1 June 2012 – 30 July 20...
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Iterative evolution of digitate planktonic foraminifera
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Adaptive ecological niche migration does not negate extinction susceptibility
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Adaptive ecological niche migration does not negate extinction susceptibility
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Symbiont 'bleaching' in planktic foraminifera during the Middle Eocene Climatic...
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Symbiont ‘bleaching’ in planktic foraminifera during the Middle Eocene Climatic...
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Symbiont 'bleaching' in planktic foraminifera during the Middle Eocene Climatic...
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New biostratigraphic, magnetostratigraphic and isotopic insights into the Middle...
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New biostratigraphic, magnetostratigraphic and isotopic insights into the Middle...
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New biostratigraphic, magnetostratigraphic and isotopic insights into the Middle...
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New biostratigraphic, magnetostratigraphic and isotopic insights into the Middle...
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Insensitivity of alkenone carbon isotopes to atmospheric CO₂ at low to moderate...
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Symbiont 'bleaching' in planktic foraminifera during the Middle Eocene Climatic...
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An abyssal carbonate compensation depth overshoot in the aftermath of the Paleoc...
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Causes of ice age intensification across the Mid-Pleistocene Transition
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Cenozoic evolution of deep ocean temperature from clumped isotope thermometry
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Cenozoic evolution of deep ocean temperature from clumped isotope thermometry
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Cenozoic evolution of deep ocean temperature from clumped isotope thermometry
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Related Subjects
Eocene
Carbon
Circulation changes
Climactic Optimum (EECO)
Foraminifera
Oxygen
Paleocene
Sea-level
Seawater
Southern-ocean
GC Oceanography
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PALEOCENE THERMAL MAXIMUM
SOUTHERN-OCEAN
Site 1051
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Atl Biostratigraphy
Biostratigraphy
CALIBRATION
CARBON
CCD
CIRCULATION CHANGES
CLIMATIC OPTIMUM EECO
COMPONENT WATER
CORES
DAS
DEEP-WATER PRODUCTION
DELTA-C-13
DELTA-O-18
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