Downstream Evolution of Particulate Organic Matter Composition From Permafrost Thaw Slumps

Permafrost soils, which store almost half of the global belowground organic carbon (OC), are susceptible to thaw upon climate warming. On the Peel Plateau of northwestern Canada, the number and size of retrogressive thaw slumps (RTS) has increased in recent decades due to rising temperatures and hig...

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Bibliografske podrobnosti

Principais autores:	Kirsi H. Keskitalo, Lisa Bröder, Sarah Shakil, Scott Zolkos, Suzanne E. Tank, Bart E. van Dongen, Tommaso Tesi, Negar Haghipour, Timothy I. Eglinton, Steven V. Kokelj, Jorien E. Vonk
Format:	Artigo
Jezik:	Inglês
Izdano:	Frontiers Media S.A. 2021-03-01
Serija:	Frontiers in Earth Science
Teme:	Arctic climate carbon lipid biomarkers Peel Plateau permafrost
Online dostop:	https://www.frontiersin.org/articles/10.3389/feart.2021.642675/full
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