Independent variations of CH4 emissions and isotopic composition over the past 160,000 years
about
Understanding the glacial methane cycle.Minimal geological methane emissions during the Younger Dryas-Preboreal abrupt warming event.Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records.Automated simultaneous measurement of the δ(13) C and δ(2) H values of methane and the δ(13) C and δ(18) O values of carbon dioxide in flask air samples using a new multi cryo-trap/gas chromatography/isotope ratio mass spectrometry system.Permafrost thawing as a possible source of abrupt carbon release at the onset of the Bølling/Allerød.Fully automated, high-throughput instrumentation for measuring the δ13C value of methane and application of the instrumentation to rice paddy samples.Atmospheric methane variability: Centennial-scale signals in the Last Glacial PeriodCarbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2
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Independent variations of CH4 emissions and isotopic composition over the past 160,000 years
description
article
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im August 2013 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
@nl
наукова стаття, опублікована в серпні 2013
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name
Independent variations of CH4 ...... on over the past 160,000 years
@en
Independent variations of CH4 ...... on over the past 160,000 years
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type
label
Independent variations of CH4 ...... on over the past 160,000 years
@en
Independent variations of CH4 ...... on over the past 160,000 years
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prefLabel
Independent variations of CH4 ...... on over the past 160,000 years
@en
Independent variations of CH4 ...... on over the past 160,000 years
@nl
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Independent variations of CH4 ...... on over the past 160,000 years
@en
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Heinrich Miller
Lars Möller
Michael Bock
Renato Spahni
Todd Sowers
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10.1038/NGEO1922
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2013-08-25T00:00:00Z
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1033758210