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Predicting long‐term carbon mineralization and trace gas production from thawing permafrost of N ortheast S iberia
Author(s) -
Knoblauch Christian,
Beer Christian,
Sosnin Alexander,
Wagner Dirk,
Pfeiffer EvaMaria
Publication year - 2013
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/gcb.12116
Subject(s) - permafrost , mineralization (soil science) , organic matter , environmental chemistry , total organic carbon , methane , carbon dioxide , thermokarst , carbon cycle , environmental science , carbon fibers , soil science , geology , chemistry , ecology , oceanography , ecosystem , soil water , materials science , organic chemistry , biology , composite number , composite material
The currently observed A rctic warming will increase permafrost degradation followed by mineralization of formerly frozen organic matter to carbon dioxide ( CO 2 ) and methane ( CH 4 ). Despite increasing awareness of permafrost carbon vulnerability, the potential long‐term formation of trace gases from thawing permafrost remains unclear. The objective of the current study is to quantify the potential long‐term release of trace gases from permafrost organic matter. Therefore, H olocene and P leistocene permafrost deposits were sampled in the L ena R iver D elta, N ortheast S iberia. The sampled permafrost contained between 0.6% and 12.4% organic carbon. CO 2 and CH 4 production was measured for 1200 days in aerobic and anaerobic incubations at 4 °C. The derived fluxes were used to estimate parameters of a two pool carbon degradation model. Total CO 2 production was similar in Holocene permafrost (1.3 ± 0.8 mg CO 2 ‐C gdw −1 aerobically, 0.25 ± 0.13 mg CO 2 ‐C gdw −1 anaerobically) as in 34 000–42 000‐year‐old P leistocene permafrost (1.6 ± 1.2 mg CO 2 ‐C gdw −1 aerobically, 0.26 ± 0.10 mg CO 2 ‐C gdw −1 anaerobically). The main predictor for carbon mineralization was the content of organic matter. Anaerobic conditions strongly reduced carbon mineralization since only 25% of aerobically mineralized carbon was released as CO 2 and CH 4 in the absence of oxygen. CH 4 production was low or absent in most of the P leistocene permafrost and always started after a significant delay. After 1200 days on average 3.1% of initial carbon was mineralized to CO 2 under aerobic conditions while without oxygen 0.55% were released as CO 2 and 0.28% as CH 4 . The calibrated carbon degradation model predicted cumulative CO 2 production over a period of 100 years accounting for 15.1% (aerobic) and 1.8% (anaerobic) of initial organic carbon, which is significantly less than recent estimates. The multiyear time series from the incubation experiments helps to more reliably constrain projections of future trace gas fluxes from thawing permafrost landscapes.