Permafrost collapse alters soil carbon stocks, respiration, CH4, and N2O in upland tundra

Author:

Abbott Benjamin W.12,Jones Jeremy B.2

Affiliation:

1. OSUR; CNRS; UMR 6553 ECOBIO; Université de Rennes 1; Rennes France

2. Department of Biology and Wildlife and Institute of Arctic Biology; University of Alaska Fairbanks; Fairbanks AK USA

Funder

National Science Foundation ARCSS

Publisher

Wiley

Subject

General Environmental Science,Ecology,Environmental Chemistry,Global and Planetary Change

Reference106 articles.

1. Elevated dissolved organic carbon biodegradability from thawing and collapsing permafrost;Abbott;Journal of Geophysical Research: Biogeosciences,2014

2. Patterns and persistence of hydrologic carbon and nutrient export from collapsing upland permafrost;Abbott;Biogeosciences,2015

3. A shift of thermokarst lakes from carbon sources to sinks during the Holocene epoch;Anthony;Nature,2014

4. Riverine coupling of biogeochemical cycles between land, oceans, and atmosphere;Aufdenkampe;Frontiers in Ecology and the Environment,2011

5. Timing of retrogressive thaw slump initiation in the Noatak Basin, northwest Alaska, USA;Balser;Journal of Geophysical Research: Earth Surface,2014

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