Preprints
https://doi.org/10.5194/egusphere-2025-325
https://doi.org/10.5194/egusphere-2025-325
13 Feb 2025
 | 13 Feb 2025
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Accelerated export of terrestrial organic carbon to the Chukchi Sea since pre-industrial times

Bassem Jalali, Marie-Alexandrine Sicre, Jian Ren, Zhongqiao Li, Youcheng Bai, Liang Su, Vincent Klein, and Jianfang Chen

Abstract. The on-going global warming is causing rapid changes in the carbon cycle of the Arctic. Yet the response of the Arctic to these environmental changes are not fully understood. In this study, we investigate bulk organic parameters (TOC, TN, δ13Corg, δ15N, C/N) and terrestrial n-alkanes (TERR-alkanes) from 19 surface sediments and 5 210Pb-dated sediment cores covering up to the last three centuries from the Chukchi Sea. Downcore profiles indicate increasing OC since the beginning of the Industrial Era in all cores. They also show higher TOC and TN values in southern Chukchi Sea cores coincident with decreasing δ13Corg indicating an increasing contribution of terrestrial OC that is confirmed by TERR-alkanes. Comparison with regional paleo-records and instrumental data emphasize the key role of air temperature and sea ice cover on the OC cycle and vegetation of the surrounding landmasses.

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Bassem Jalali, Marie-Alexandrine Sicre, Jian Ren, Zhongqiao Li, Youcheng Bai, Liang Su, Vincent Klein, and Jianfang Chen

Status: open (until 01 Apr 2025)

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  • RC1: 'Comment on egusphere-2025-325', Anonymous Referee #1, 28 Feb 2025 reply
Bassem Jalali, Marie-Alexandrine Sicre, Jian Ren, Zhongqiao Li, Youcheng Bai, Liang Su, Vincent Klein, and Jianfang Chen
Bassem Jalali, Marie-Alexandrine Sicre, Jian Ren, Zhongqiao Li, Youcheng Bai, Liang Su, Vincent Klein, and Jianfang Chen

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Short summary
This work investigates the spatiotemporal variations of terrestrial material from surface and core sediments from the Chukchi Sea using bulk parameters and biomarkers. We found a growing imprint of terrestrial material at higher latitudes resulting from the transport of eroded matter or remobilized from shelf sediments by sea ice. The 300 year TERR-alkanes and ACL27-31 composites from 5 cores evidence increasing export of terrestrial carbon since the early 20th century accelerating after 1980.
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