Implications of the glacial CO2“iron hypothesis” for Quaternary climate change
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Southern Ocean dust-climate coupling over the past four million years.Causes of ice age intensification across the Mid-Pleistocene Transition.Lowering of glacial atmospheric CO2in response to changes in oceanic circulation and marine biogeochemistryImplications of coral reef buildup for the controls on atmospheric CO2since the Last Glacial MaximumA model-based interpretation of low-frequency changes in the carbon cycle during the last 120,000 years and its implications for the reconstruction of atmospheric Δ14CQuantitative interpretation of atmospheric carbon records over the last glacial termination
P2860
Implications of the glacial CO2“iron hypothesis” for Quaternary climate change
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wetenschappelijk artikel
@nl
наукова стаття, опублікована у вересні 2003
@uk
name
Implications of the glacial CO2“iron hypothesis” for Quaternary climate change
@en
Implications of the glacial CO2“iron hypothesis” for Quaternary climate change
@nl
type
label
Implications of the glacial CO2“iron hypothesis” for Quaternary climate change
@en
Implications of the glacial CO2“iron hypothesis” for Quaternary climate change
@nl
prefLabel
Implications of the glacial CO2“iron hypothesis” for Quaternary climate change
@en
Implications of the glacial CO2“iron hypothesis” for Quaternary climate change
@nl
P2860
P356
P1476
Implications of the glacial CO2“iron hypothesis” for Quaternary climate change
@en
P2093
Andy J. Ridgwell
P2860
P356
10.1029/2003GC000563
P577
2003-09-01T00:00:00Z