Using the deuterium isotope composition of permafrost meltwater to constrain thermokarst lake contributions to atmospheric CH4during the last deglaciation

scholarly article

Using the deuterium isotope composition of permafrost meltwater to constrain thermokarst lake contributions to atmospheric CH4during the last deglaciation is …
instance of (P31):
scholarly articleQ13442814

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P819ADS bibcode2012JGRG..117.1022B
P356DOI10.1029/2011JG001810

P50authorGuido GrosseQ42657013
Hanno MeyerQ57084934
Paul OverduinQ58148155
P2093author name stringJ. P. Chanton
K. M. Walter Anthony
L. M. Farquharson
L. S. Brosius
P2860cites workExpansion rate and geometry of floating vegetation mats on the margins of thermokarst lakes, northern Seward Peninsula, Alaska, USAQ58264050
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The late Pleistocene environment of the Eastern West Beringia based on the principal section at the Main River, ChukotkaQ67230872
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Paleoenvironmental and paleoclimatic records from permafrost deposits in the Arctic region of Northern SiberiaQ104246426
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Thermokarst lakes as a source of atmospheric CH4 during the last deglaciationQ28254965
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Late Quaternary atmospheric CH4 isotope record suggests marine clathrates are stableQ28296516
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H2-forming N5,N10-methylenetetrahydromethanopterin dehydrogenase from Methanobacterium thermoautotrophicum. Studies of the catalytic mechanism of H2 formation using hydrogen isotopes.Q53892570
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P433issueG1
P407language of work or nameEnglishQ1860
P921main subjectpermafrostQ179918
thermokarstQ1367339
deglaciationQ3707848
P577publication date2012-02-25
P1433published inJournal of Geophysical ResearchQ2738009
P1476titleUsing the deuterium isotope composition of permafrost meltwater to constrain thermokarst lake contributions to atmospheric CH4during the last deglaciation
P478volume117

Reverse relations

cites work (P2860)
Q5639498921st-century modeled permafrost carbon emissions accelerated by abrupt thaw beneath lakes
Q45000792A shift of thermokarst lakes from carbon sources to sinks during the Holocene epoch.
Q57807027Active layer hydrology in an arctic tundra ecosystem: quantifying water sources and cycling using water stable isotopes
Q35597913Climate change and the permafrost carbon feedback.
Q57070771Deglacial mobilization of pre-aged terrestrial carbon from degrading permafrost
Q57889413Detection and spatiotemporal analysis of methane ebullition on thermokarst lake ice using high-resolution optical aerial imagery
Q58388775Evidence of multiple thermokarst lake generations from an 11 800-year-old permafrost core on the northern Seward Peninsula, Alaska
Q38695401Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records
Q59845690Greenhouse gas emissions from diverse Arctic Alaskan lakes are dominated by young carbon
Q36334265Inland waters and their role in the carbon cycle of Alaska
Q57986289Isotopic identification of soil and permafrost nitrate sources in an Arctic tundra ecosystem
Q58388777Methane emissions proportional to permafrost carbon thawed in Arctic lakes since the 1950s
Q58179660Recent Progress (2007-2012) in Permafrost Isotope Geochemistry
Q28660447Role of megafauna and frozen soil in the atmospheric CH4 dynamics
Q35043501Small thaw ponds: an unaccounted source of methane in the Canadian high Arctic
Q57869478Sources of methane to an Arctic lake in Alaska: An isotopic investigation
Q56269769The origin of methane in the East Siberian Arctic Shelf unraveled with triple isotope analysis

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