The impact of disturbed peatlands on river outgassing in Southeast Asia

被引:57
作者
Wit, Francisca [1 ]
Mueller, Denise [1 ,2 ]
Baum, Antje [1 ]
Warneke, Thorsten [2 ]
Pranowo, Widodo Setiyo [3 ]
Mueller, Moritz [4 ]
Rixen, Tim [1 ,5 ]
机构
[1] Leibniz Ctr Trop Marine Ecol ZMT, D-28359 Bremen, Germany
[2] Univ Bremen, Inst Environm Phys, D-28359 Bremen, Germany
[3] Res & Dev Ctr Marine & Coastal Resources P3SDLP, Jakarta 14430, Indonesia
[4] Swinburne Univ Technol, Kuching 93350, Sarawak, Malaysia
[5] Univ Hamburg, Inst Geol, D-20146 Hamburg, Germany
关键词
DISSOLVED ORGANIC-CARBON; GAS-EXCHANGE; TROPICAL PEATLANDS; CENTRAL SUMATRA; PEAT; DIOXIDE; EMISSIONS; WETLANDS; FLUXES; EXPORT;
D O I
10.1038/ncomms10155
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
River outgassing has proven to be an integral part of the carbon cycle. In Southeast Asia, river outgassing quantities are uncertain due to lack of measured data. Here we investigate six rivers in Indonesia and Malaysia, during five expeditions. CO2 fluxes from Southeast Asian rivers amount to 66.9 +/- 15.7 Tg C per year, of which Indonesia releases 53.9 +/- 12.4 Tg C per year. Malaysian rivers emit 6.2 +/- 1.6 Tg C per year. These moderate values show that Southeast Asia is not the river outgassing hotspot as would be expected from the carbon-enriched peat soils. This is due to the relatively short residence time of dissolved organic carbon (DOC) in the river, as the peatlands, being the primary source of DOC, are located near the coast. Limitation of bacterial production, due to low pH, oxygen depletion or the refractory nature of DOC, potentially also contributes to moderate CO2 fluxes as this decelerates decomposition.
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页数:9
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