北极楚克奇陆架边缘“大西洋水层”钕同位素示踪

杨映; 叶黎明; 倪建宇; 于晓果; 原超; 葛倩; 宋赛; 张泳聪

doi:10.3799/dqkx.2023.045

Volume 49 Issue 8

Aug. 2024

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Article Navigation > Earth Science > 2024 > 49(8): 2938-2951

Yang Ying, Ye Liming, Ni Jianyu, Yu Xiaoguo, Yuan Chao, Ge Qian, Song Sai, Zhang Yongcong, 2024. Arctic Neodymium Isotope Traces for the Atlantic Water Layer at the Chukchi Continental Margin. Earth Science, 49(8): 2938-2951. doi: 10.3799/dqkx.2023.045

Citation:

Yang Ying, Ye Liming, Ni Jianyu, Yu Xiaoguo, Yuan Chao, Ge Qian, Song Sai, Zhang Yongcong, 2024. Arctic Neodymium Isotope Traces for the Atlantic Water Layer at the Chukchi Continental Margin. Earth Science, 49(8): 2938-2951. doi: 10.3799/dqkx.2023.045

Citation:

Yang Ying, Ye Liming, Ni Jianyu, Yu Xiaoguo, Yuan Chao, Ge Qian, Song Sai, Zhang Yongcong, 2024. Arctic Neodymium Isotope Traces for the Atlantic Water Layer at the Chukchi Continental Margin. Earth Science, 49(8): 2938-2951. doi: 10.3799/dqkx.2023.045

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Arctic Neodymium Isotope Traces for the Atlantic Water Layer at the Chukchi Continental Margin

doi: 10.3799/dqkx.2023.045

Yang Ying^{1
,
,},
Ye Liming^{1
,
,
,},
Ni Jianyu¹,
Yu Xiaoguo¹,
Yuan Chao¹,
Ge Qian¹,
Song Sai^{1, 2},
Zhang Yongcong¹

1.
Key Laboratory of Submarine Geosciences & Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
2.
School of Geography and Ocean Science, Nanjing University, Nanjing 210023, China

Received Date: 2023-01-23
Available Online: 2024-08-27
Publish Date: 2024-08-25

Abstract

Abstract

In the Arctic Ocean, the Atlantic water layer is an essential source of heat that regulates sea ice, ice shelves, and surrounding ice sheets. By analyzing the content and pattern of rare earth elements (REE) and Nd isotopic composition (ε_Nd) in the sediments of Hole M04 and its distribution pattern and Nd isotopic composition of Fe-Mn oxide fraction, this study explores the enrichment mechanism of REE on the edge of Chukchi shelf since Late Pleistocene, the effectiveness of ε_Nd tracer water mass properties, and the strength and weakness of the "Atlantic water layer".The records indicate that Fe-Mn oxides were the primary carriers for dissolved REE during the interglacial period, but a large quantity of dissolved REE was also enriched in the gray layer lacking Fe-Mn oxides. In addition, there is a significant spike of ε_Nd in Fe-Mn oxide leachate during the glacial period and a drop during the interglacial period corresponding to values between -5.50 and -8.74. Therefore, we conclude that the Atlantic water layer strengthened during the interglacial period, which allowed re-oxidation of Fe²⁺ and Mn²⁺ input from the shelf, but withdrew almost entirely from the Chukchi continental margin during the glacial period. Similar to the chemical composition of modern glacial meltwater, the development of the East Siberian ice sheet and its subglacial drainage are more likely to lead to the REE enrichment and ε_Nd positive bias in Core M04 Fe-Mn oxide extraction solution than sea ice production brine. These findings further illustrate the process of enrichment of REEs in the Arctic Ocean, demonstrate the effectiveness of ε_Nd as a marker of the Atlantic water layer, and contribute to an understanding of the Atlantic water layer evolution.
- neodymium isotope,
- rare earth element,
- Atlantic water layer,
- Chukchi continental margin,
- Arctic Ocean,
- marine geology

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References(61)

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