Composition and biodegradability of dissolved organic matter leached from eroding coastal soils and permafrost in seawater, from Drew Point, Alaska ...

Eroding permafrost coastlines export significant quantities of organic carbon (OC) to the marine environment, similar in magnitude to riverine particulate OC fluxes to the Arctic Ocean. Moreover, erosion rates are predicted to increase due to warming temperatures, declines in sea ice, and increasing...

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Bibliographic Details
Main Authors: Bristol, Emily M, Behnke, Megan I, Spencer, Robert G. M., McKenna, Amy, Jones, Benjamin M, Bull, Diana L, McClelland, James W
Format: Dataset
Language:English
Published: Environmental Data Initiative 2024
Subjects:
Ice
Online Access:https://dx.doi.org/10.6073/pasta/bffc3d4e9cdc255ff0e8582d668c006e
https://portal.edirepository.org/nis/mapbrowse?packageid=knb-lter-ble.32.1
Description
Summary:Eroding permafrost coastlines export significant quantities of organic carbon (OC) to the marine environment, similar in magnitude to riverine particulate OC fluxes to the Arctic Ocean. Moreover, erosion rates are predicted to increase due to warming temperatures, declines in sea ice, and increasing waves. While erosion primarily mobilizes organic matter in the particulate form, this material can be leached to dissolved organic matter (DOM). This DOM may be incorporated by microbial communities and fuel marine food webs or decomposed to form greenhouse gases like carbon dioxide and methane. Many studies show that permafrost-derived organic matter can be rapidly decomposed in soils and freshwater, but few studies examine the fate of permafrost organic matter in seawater. To address this knowledge gap, we designed a laboratory experiment to leach coastal soils and permafrost in seawater and examine the composition and biodegradability of leached DOM. Coastal soil/sediment was cored near Drew Point, Alaska in ...