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Potential carbon release from permafrost soils of Northeastern Siberia
Koushik Dutta
,
E. A.G. Schuur
, J. C. Neff
, S. A. Zimov
Research output
:
Contribution to journal
›
Article
›
peer-review
344
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Keyphrases
Respiration
100%
Carbon Release
100%
Northeastern Siberia
100%
Permafrost Soils
100%
Organic Matter
50%
Bulk Soil
50%
Mineral Soil
50%
C Concentration
50%
C Pools
25%
14C Age
25%
Tundra
25%
Positive Feedback
25%
Carbon C
25%
Boreal Forest
25%
Global Temperature
25%
Permafrost
25%
Boreal Ecosystems
25%
Lability
25%
Organic Matter Decomposition
25%
Dissolved Organic C
25%
Arctic Ecosystems
25%
Q10 Value
25%
Radiocarbon 14C
25%
Labile C Pools
25%
C-component
25%
Loess Deposits
25%
Controlled Temperature
25%
Siberian Permafrost
25%
Strongly Correlated
25%
Earth and Planetary Sciences
Siberia
100%
Carbon Dioxide
100%
Protective Atmosphere
60%
Organic Matter
40%
Pleistocene
20%
Boreal Forest
20%
Positive Feedback
20%
Mineral Surface
20%
Decomposition of Organic Matter
20%
Reference Sample
20%
Arctic Ecosystem
20%
Agricultural and Biological Sciences
Permafrost
100%
Carbon Dioxide
83%
Bulk Soil
33%
Mineral Soils
33%
Boreal Forest
16%
Decomposition of Organic Matter
16%