Evidence for a reduction in the carbonate ion content of the deep sea during the course of the Holocene
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Holocene peatland and ice-core data constraints on the timing and magnitude of CO2 emissions from past land use.Timing and nature of AMOC recovery across Termination 2 and magnitude of deglacial CO2 change.Negligible glacial-interglacial variation in continental chemical weathering rates.Late Holocene climate: Natural or anthropogenic?Implications of coral reef buildup for the controls on atmospheric CO2since the Last Glacial MaximumAssessing divergent SST behavior during the last 21 ka derived from alkenones andG. ruber-Mg/Ca in the equatorial PacificCarbon sequestration in western Canadian peat highly sensitive to Holocene wet-dry climate cycles at millennial timescalesHolocene radiative forcing impact of northern peatland carbon accumulation and methane emissions
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P2860
Evidence for a reduction in the carbonate ion content of the deep sea during the course of the Holocene
description
article
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im Dezember 1999 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована в грудні 1999
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Evidence for a reduction in th ...... ing the course of the Holocene
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Evidence for a reduction in th ...... ing the course of the Holocene
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Evidence for a reduction in th ...... ing the course of the Holocene
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Evidence for a reduction in th ...... ing the course of the Holocene
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Evidence for a reduction in th ...... ing the course of the Holocene
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Evidence for a reduction in th ...... ing the course of the Holocene
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P2093
P356
P1433
P1476
Evidence for a reduction in th ...... ing the course of the Holocene
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P2093
Daniel C. McCorkle
Elizabeth Clark
Georges Bonani
Irena Hajdas
Tsung-Hung Peng
Wallace S. Broecker
P304
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10.1029/1999PA900038
P577
1999-12-01T00:00:00Z