作者: Elena Blanc-Betes , Jeffrey M. Welker , Neil C. Sturchio , Jeffrey P. Chanton , Miquel A. Gonzalez-Meler
DOI: 10.1111/GCB.13242
关键词:
摘要: Arctic winter precipitation is projected to increase with global warming, but some areas will experience decreases in snow accumulation. Although CH4 emissions may represent a significant climate forcing feedback, long-term impacts of changes accumulation on fluxes remain uncertain. We measured ecosystem and soil CO2 concentrations (13) C composition investigate the metabolic pathways transport mechanisms driving moist acidic tundra flux over growing season (Jun-Aug) after 18 years experimental depth increases decreases. Deeper increased wetness reducing %O2 levels increasing thaw depth. Soil moisture, through saturation, determined predominance methanotrophy or methanogenesis, temperature regulating sink source strength. Reduced (RS) fraction oxidized (Fox) by 75-120% compared Ambient, switching system from small net (21 ± 2 -31 ± 1 mg CH4 m(-2) season(-1) at Ambient RS). reduced Fox 35-40% 90-100% medium- (MS) high- (HS) additions relative contributing strength (464 ± 15 3561 ± 97 mg CH4 MS HS). Decreases deeper were partly due plant-mediated associated expansion tall graminoids. enhanced production within newly thawed soils, responding mainly warming rather than acetate fermentation expected thaw-induced SOC availability. Our results suggest that tundra, resulting positive feedback change depend balance between more less they are currently facing.