Marine Science Faculty Publications

Document Type

Article

Publication Date

2017

Keywords

Arctic, permafrost, pyrolysis, lignin, Colville River, carbon cycling

Digital Object Identifier (DOI)

https://doi.org/10.1002/2017GL075543

Abstract

The deposition of terrestrial-derived permafrost particulate organic carbon (POC) has been recorded in major Arctic river deltas. However, associated transport pathways of permafrost POC from the watershed to the coast have not been well constrained. Here we utilized a combination of ramped pyrolysis-oxidation radiocarbon analysis (RPO 14C) along with lignin biomarkers, to track the linkages between soils and river and delta sediments. Surface and deep soils showed distinct RPO thermographs which may be related to degradation and organo-mineral interaction. Soil material in the bed load of the river channel was mostly derived from deep old permafrost. Both surface and deep soils were transported and deposited to the coast. Hydrodynamic sorting and barrier island protection played important roles in terrestrial-derived permafrost POC deposition near the coast. On a large scale, ice processes (e.g., ice gauging and strudel scour) and ocean currents controlled the transport and distribution of permafrost POC on the Beaufort Shelf.

Was this content written or created while at USF?

Yes

Citation / Publisher Attribution

Geophysical Research Letters, v. 44, issue 22, p. 11491-11500

©2017. American Geophysical Union. All Rights Reserved.

grl56665-sup-0001-2017gl075543-si.docx (1087 kB)
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