Siberian peatlands a net carbon sink and global methane source since the early Holocene.
about
Thermokarst lakes as a source of atmospheric CH4 during the last deglaciationMassive remobilization of permafrost carbon during post-glacial warmingRapid deglacial and early Holocene expansion of peatlands in AlaskaThe current state of knowledge of ecosystems and ecosystem services in Russia: A status report.Carbon accumulation in a permafrost polygon peatland: steady long-term rates in spite of shifts between dry and wet conditions.Polygonal tundra geomorphological change in response to warming alters future CO2 and CH4 flux on the Barrow Peninsula.Methane bubbling from northern lakes: present and future contributions to the global methane budget.Temperature-induced increase in methane release from peat bogs: a mesocosm experimentNorthern peatland initiation lagged abrupt increases in deglacial atmospheric CH4.Cultivating uncultured bacteria from northern wetlands: knowledge gained and remaining gaps.Atmospheric nitrogen deposition promotes carbon loss from peat bogs.Abundant Trimethylornithine Lipids and Specific Gene Sequences Are Indicative of Planctomycete Importance at the Oxic/Anoxic Interface in Sphagnum-Dominated Northern Wetlands.Pyrosequencing-based assessment of the bacteria diversity in surface and subsurface peat layers of a northern wetland, with focus on poorly studied phyla and candidate divisions.Tropical/Subtropical Peatland Development and Global CH4 during the Last GlaciationEnhanced silicon availability leads to increased methane production, nutrient and toxicant mobility in peatlands.A catchment-scale carbon and greenhouse gas budget of a subarctic landscape.Carbon storage and potential methane production in the Hudson Bay Lowlands since mid-Holocene peat initiation.Methanogenesis and methanogenic pathways in a peat from subarctic permafrost.Differential arthropod responses to warming are altering the structure of Arctic communities.A note on the relationship between ice core methane concentrations and insolationSoil drainage facilitates earthworm invasion and subsequent carbon loss from peatland soilVulnerability of Permafrost Carbon to Climate Change: Implications for the Global Carbon CycleReconstructing Disturbances and Their Biogeochemical Consequences over Multiple TimescalesAbundance, distribution and potential activity of methane oxidizing bacteria in permafrost soils from the Lena Delta, SiberiaMethanotrophic symbionts provide carbon for photosynthesis in peat bogsModelling of growing season methane fluxes in a high-Arctic wet tundra ecosystem 1997–2010 using in situ and high-resolution satellite dataLand-atmosphere exchange of methane from soil thawing to soil freezing in a high-Arctic wet tundra ecosystemImpact of snow deposition on major and trace element concentrations and elementary fluxes in surface waters of the Western Siberian Lowland across a 1700 km latitudinal gradientDissolved organic carbon and major and trace elements in peat porewater of sporadic, discontinuous, and continuous permafrost zones of western SiberiaSeasonal and spatial variability of elemental concentrations in boreal forest larch foliage of Central Siberia on continuous permafrostHeterotrophic bacterio‐plankton in thawed lakes of the northern part of Western Siberia controls the CO2flux to the atmosphereWestern Siberia wetlands as indicator and regulator of climate change on the global scaleA vertical representation of soil carbon in the JULES land surface scheme (vn4.3_permafrost) with a focus on permafrost regionsVulnerability of high-latitude soil organic carbon in North America to disturbanceDecadal vegetation changes in a northern peatland, greenhouse gas fluxes and net radiative forcingFossil organic matter characteristics in permafrost deposits of the northeast Siberian ArcticMap-based inventory of wetland biomass and net primary production in western SiberiaLinkages among runoff, dissolved organic carbon, and the stable oxygen isotope composition of seawater and other water mass indicators in the Arctic OceanIssues Related to Incorporating Northern Peatlands into Global Climate ModelsHolocene radiative forcing impact of northern peatland carbon accumulation and methane emissions
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P2860
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
description
2004 nî lūn-bûn
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2004 թուականի Յունուարին հրատարակուած գիտական յօդուած
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2004 թվականի հունվարին հրատարակված գիտական հոդված
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2004年の論文
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2004年学术文章
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2004年学术文章
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2004年学术文章
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2004年学术文章
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2004年学术文章
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2004年學術文章
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name
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
@ast
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
@en
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
@nl
type
label
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
@ast
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
@en
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
@nl
prefLabel
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
@ast
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
@en
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
@nl
P2093
P356
P1433
P1476
Siberian peatlands a net carbon sink and global methane source since the early Holocene.
@en
P2093
Beilman DW
Borisova OK
Kremenetski KV
MacDonald GM
Velichko AA
P304
P356
10.1126/SCIENCE.1090553
P407
P577
2004-01-01T00:00:00Z