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.
Main Authors: | , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Nature Portfolio
2023-03-01
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Series: | Communications Earth & Environment |
Online Access: | https://doi.org/10.1038/s43247-023-00740-6 |