Permafrost Hydrology Drives the Assimilation of Old Carbon by Stream Food Webs in the Arctic
Permafrost thaw in the Arctic is mobilizing old carbon (C) from soils to aquatic ecosystems and the atmosphere. Little is known, however, about the assimilation of old C by aquatic food webs in Arctic watersheds. Here, we used C isotopes (d13C, D14C) to quantify C assimilation by biota across 12 str...
Main Authors: | , , , , , , |
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Format: | Text |
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DigitalCommons@University of Nebraska - Lincoln
2019
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Online Access: | https://digitalcommons.unl.edu/natlpark/205 https://digitalcommons.unl.edu/context/natlpark/article/1209/viewcontent/ODonnell_ECOSYSTEMS_2010_Permafrost_Hydrology.pdf |