Geochemical characteristics of black carbon in surface sediments of the East Siberian Arctic Shelf and their environmental implications

YU Wenxiu; HU Limin; SHI Xuefa; ZHANG Yuying; YE Jun; BAI Yazhi; XIA Yi; YANG Gang; Anatolii Astakhov

doi:10.16562/j.cnki.0256-1492.2022022001

Marine Geology & Quaternary Geology > 2022 > 42(4): 50-60. > DOI: 10.16562/j.cnki.0256-1492.2022022001

YU Wenxiu，HU Limin，SHI Xuefa，et al. Geochemical characteristics of black carbon in surface sediments of the East Siberian Arctic Shelf and their environmental implications[J]. Marine Geology & Quaternary Geology，2022，42(4)：50-60. DOI: 10.16562/j.cnki.0256-1492.2022022001

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Geochemical characteristics of black carbon in surface sediments of the East Siberian Arctic Shelf and their environmental implications

YU Wenxiu^1,,
HU Limin^1,2,3, ,,
SHI Xuefa^2,3,
ZHANG Yuying¹,
YE Jun^1,3,
BAI Yazhi^2,3,
XIA Yi²,
YANG Gang^2,3,
Anatolii Astakhov⁴

1.
College of Marine Geosciences,Key Laboratory of Submarine Geosciences and Prospecting Technology,Ocean University of China, Qingdao 266100, China
2.
Key Laboratory of Marine Geology and Metallogeny, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China
3.
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
4.
V.I.Il'ichev Pacific Oceanological Institute, Far Eastern Branch of Russian Academy of Sciences, Vladivostok 690041, Russia

More Information

Received Date: February 19, 2022
Revised Date: March 30, 2022
Accepted Date: March 30, 2022
Available Online: April 24, 2022

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Abstract

Abstract

Pyrogenic black carbon (BC) is closely related to climate change and human activities. In the context of global warming, the BC emission and transfer from land to sea and the environmental fate provide important scientific clues for understanding the source-sink course of terrigenous organic carbon and its climate and environmental effects under rapid climate change in the Arctic area. The East Siberian Arctic Shelf is the widest and shallowest shelf in the world, receiving a large amount of terrestrial material input from runoff and coastal erosion. Especially in recent years, frequent occurrence of wildfires around the Arctic makes it an ideal area for studying the course and route of source-sink of BC deposited in the Arctic waters. Based on the data of samples collected from the East Siberian shelf, the content, composition, spatial distribution, and influencing factors of BC in surface sediments were studied. Preliminary results show that the content of BC is 0.1～2.3 mg/g, on average of 0.99 mg/g. Among them, char from biomass combustion contributed more than 70% on average. The spatial distribution of BC is very heterogeneous. BC in the Laptev Sea and the western part of the East Siberian Sea is high, which is closely related to coastal erosion and river input. The eastern part of the shelf (including the Chukchi Sea) has less terrigenous input and relatively low BC content. The spatial variability of different types of BC is obvious. In the nearshore region, runoff and coastal erosion is probably the main input pathway of char.
- black carbon,
- source and sink,
- surface sediments,
- Arctic rapid change,
- East Siberian Arctic Shelf

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References (75)

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Geochemical characteristics of black carbon in surface sediments of the East Siberian Arctic Shelf and their environmental implications