Organic matter distribution and origin in marine surface sediments on the Canadian Beaufort Sea Shelf ...

The continental shelves of the Arctic Ocean are undergoing profound changes because of climate warming. Large amounts of previously freeze-locked carbon and nutrients are released towards the shelves due to increasing river discharge, deeper permafrost thaw and accelerated coastal erosion. Still, th...

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Bibliographic Details
Main Authors: Schwarzkopf, Katharina, Fritz, Michael, Bröder, Lisa, Haghipour, Negar, O'Regan, Matt, Juhls, Bennet, Priest, Taylor, Lattaud, Julie, Whalen, Dustin, Matsuoka, Atushi, Pellerin, André, Bossé-Demers, Thomas, Rudbäck, Daniel, Rodriquez-Cuicas, Maria-Emilia, Overduin, Pier Paul, Vonk, Jorien E.
Format: Conference Object
Language:unknown
Published: Zenodo 2023
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.10260175
https://zenodo.org/doi/10.5281/zenodo.10260175
Description
Summary:The continental shelves of the Arctic Ocean are undergoing profound changes because of climate warming. Large amounts of previously freeze-locked carbon and nutrients are released towards the shelves due to increasing river discharge, deeper permafrost thaw and accelerated coastal erosion. Still, their interactions and their effects on carbon turnover and greenhouse gas fluxes between sediment, ocean, and atmosphere are poorly understood. This study aims to investigate the origin and depositional patterns of organic matter in the Canadian Beaufort Sea. To address this, long and short sediment cores were taken in fall 2021 from twenty-five positions along five major transects that spanned the Beaufort Sea Shelf. We discuss the concentration and regional distribution of organic carbon, nitrogen, mercury, and grain size in surface sediments (upper 2 cm). In addition, bulk 14C radiocarbon ages and stable isotope ratios (δ13C and δ15N) are used to help distinguish sources and degradation status of terrigenous ...