Interpreting transient carbonate compensation depth changes by marine sediment core modeling
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Assessing "dangerous climate change": required reduction of carbon emissions to protect young people, future generations and natureA probabilistic assessment of the rapidity of PETM onset.Climate science: Cracking the palaeoclimate code.Slow release of fossil carbon during the Palaeocene–Eocene Thermal MaximumAn abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene–Eocene Thermal MaximumPatterns and magnitude of deep sea carbonate dissolution during Eocene Thermal Maximum 2 and H2, Walvis Ridge, southeastern Atlantic OceanRecovering the true size of an Eocene hyperthermal from the marine sedimentary recordOcean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescalesPaleoredox changes across the Paleocene-Eocene thermal maximum, Walvis Ridge (ODP Sites 1262, 1263, and 1266): Evidence from Mn and U enrichment factorsEnvironmental and biological controls on size-specific δ13 C and δ18 O in recent planktonic foraminiferaMethane Hydrate Instability: A View from the Palaeogene
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Interpreting transient carbonate compensation depth changes by marine sediment core modeling
description
article
@en
im Oktober 2007 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в жовтні 2007
@uk
name
Interpreting transient carbona ...... marine sediment core modeling
@en
Interpreting transient carbona ...... marine sediment core modeling
@nl
type
label
Interpreting transient carbona ...... marine sediment core modeling
@en
Interpreting transient carbona ...... marine sediment core modeling
@nl
prefLabel
Interpreting transient carbona ...... marine sediment core modeling
@en
Interpreting transient carbona ...... marine sediment core modeling
@nl
P2860
P356
P1433
P1476
Interpreting transient carbona ...... marine sediment core modeling
@en
P2860
P356
10.1029/2006PA001372
P577
2007-10-24T00:00:00Z