A 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 Δ14C
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Carbon isotope constraints on the deglacial CO₂ rise from ice cores.Radiocarbon constraints on the extent and evolution of the South Pacific glacial carbon poolRapid global ocean-atmosphere response to Southern Ocean freshening during the last glacial.Permafrost thawing as a possible source of abrupt carbon release at the onset of the Bølling/Allerød.Marine radiocarbon reservoir age simulations for the past 50,000 yearsThe impact of atmosphericpCO2on carbon isotope ratios of the atmosphere and oceanNorth Atlantic ventilation of “southern-sourced” deep water in the glacial oceanConstraint of the CO2rise by new atmospheric carbon isotopic measurements during the last deglaciationImpact of the ocean's Overturning circulation on atmospheric CO2
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P2860
A 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 Δ14C
description
article
@en
wetenschappelijk artikel
@nl
наукова стаття, опублікована в листопаді 2006
@uk
name
A model-based interpretation o ...... nstruction of atmospheric Δ14C
@en
A model-based interpretation o ...... nstruction of atmospheric Δ14C
@nl
type
label
A model-based interpretation o ...... nstruction of atmospheric Δ14C
@en
A model-based interpretation o ...... nstruction of atmospheric Δ14C
@nl
prefLabel
A model-based interpretation o ...... nstruction of atmospheric Δ14C
@en
A model-based interpretation o ...... nstruction of atmospheric Δ14C
@nl
P2860
P356
P1476
A model-based interpretation o ...... nstruction of atmospheric Δ14C
@en
P2093
Raimund Muscheler
P2860
P356
10.1029/2005GC001228
P577
2006-11-01T00:00:00Z