LI Zhongqiao, WANG Xinyi, JIN Haiyan, JI Zhongqiang, BAI Youcheng. Variations in organic carbon loading of surface sediments from the shelf to the slope of the Chukchi Sea, Arctic Ocean[J]. Acta Oceanologica Sinica, 2017, 36(8): 131-136. doi: 10.1007/s13131-017-1026-y
Citation: LI Zhongqiao, WANG Xinyi, JIN Haiyan, JI Zhongqiang, BAI Youcheng. Variations in organic carbon loading of surface sediments from the shelf to the slope of the Chukchi Sea, Arctic Ocean[J]. Acta Oceanologica Sinica, 2017, 36(8): 131-136. doi: 10.1007/s13131-017-1026-y

Variations in organic carbon loading of surface sediments from the shelf to the slope of the Chukchi Sea, Arctic Ocean

doi: 10.1007/s13131-017-1026-y
  • Received Date: 2016-03-30
  • The content of organic carbon (OC) normalized to the specific surface area (SSA) of sediment is widely used to trace variations in OC loading (OC/SSA). This study presents observations of OC/SSA of surface sediments collected in the Chukchi Sea, a typical Arctic marginal sea. Shelf sediments exhibit much higher OC/SSA values than slope sediments in the study area. Compared with OC/SSA values reported from the East Siberian Shelf and Mackenzie River, the slope sediments possess lower OC loading. This abrupt decrease in OC/SSA is mostly related to the lower primary production on slope as well as possible oxidization processes. The results of linear regression analysis between OC and SSA indicate a sedimentary source rock for the OC in the Chukchi Sea sediments. Moreover, shelf sediments with low SSA possess a larger rock OC fraction than slope sediments do. The dataset of the present study enables a more thorough understanding of regional OC cycling in the Chukchi Sea.
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