Evidence for late winter biogeochemical connectivity in permafrost soils

Longer periods of biogeochemical connectivity in soil porewaters with a deeper active layer suggest early organic carbon transport during the dormant season, according to silicon isotope compositions of permafrost soil porewaters in Alaska.

Bibliographic Details
Main Authors: Catherine Hirst, Arthur Monhonval, Elisabeth Mauclet, Maxime Thomas, Maëlle Villani, Justin Ledman, Edward. A. G. Schuur, Sophie Opfergelt
Format: Article
Language:English
Published: Nature Portfolio 2023-03-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-023-00740-6