Magnetic recordings of millennium-scale climate events in the northern Japan Sea since the early MIS 3

Zou Qingchao; Shi Xuefa; Ge Shulan; Wu Yonghua; Zou Jianjun; He Xiangfeng; Sergey A. Gorbarenko; Liu Jianxing

doi:10.12284/hyxb2024029

Volume 46 Issue 4

Jun. 2024

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Article Navigation > Haiyang Xuebao > 2024 > 46(4): 106-121

Zou Qingchao，Shi Xuefa，Ge Shulan, et al. Magnetic recordings of millennium-scale climate events in the northern Japan Sea since the early MIS 3[J]. Haiyang Xuebao，2024, 46(4)：106–121 doi: 10.12284/hyxb2024029

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Magnetic recordings of millennium-scale climate events in the northern Japan Sea since the early MIS 3

doi: 10.12284/hyxb2024029

Zou Qingchao^1
,,
Shi Xuefa^{1, 2},
Ge Shulan^{1, 2},
Wu Yonghua^{1, 2},
Zou Jianjun^{1, 2},
He Xiangfeng³,
Sergey A. Gorbarenko⁴,
Liu Jianxing^{1, 2
,
,}

1.
Key Laboratory of Marine Geology and Metallogeny, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China
2.
Laboratory of Marine Geology, Qingdao Marine Science and Technology Center, Qingdao 266237, China
3.
School of Geography and Marine Science, Nanjing University, Nanjing 210023, China
4.
Institute of Pacific Ocean Research, Far Eastern Branch of Russian Academy of Sciences, Vladivostok 690041, Russia

Received Date: 2024-01-15
Rev Recd Date: 2024-03-07

Available Online: 2024-05-20

Publish Date: 2024-06-30

Abstract

Abstract

The Japan Sea is the largest marginal sea in the northwestern Pacific Ocean. For a long time, it has been widely believed that the sediments are deposited in strongly reducing environment, which results in extremely weak magnetic signals and then restricts the application of frequently-used magnetic method in this region. To investigate deeply the availability of magnetic indicators in paleoenvironmental and paleoceanographic studiesin the Japan Sea, we conducted systematic rock magnetic analyses, high-resolution accelerator mass spectrometer (AMS) ¹⁴C dating, and grain-size analysis on a 626-cm-long sediment core (LV87-2-3, water depth 740 m) recovered from the northern Japan Sea that has been studied in relatively low level. The results indicate that the studied core corresponds to a sedimentary record since approximately 48.3 ka BP. The majority of primary ferrimagnetic minerals, mainly magnetite, in the sediments below 55 cm, had been reduced into pyrite, which caused weakly magnetic intensity. This is associated closely with the intensified stratification of water body and the increase in surface productivity during interstadials in the Dansgaard-Oeschger (D-O) cycles. Nevertheless, there are still four strong magneticlayers characterized by elevated percentages of high-coercivity minerals (i.e., hematite and goethite), which are termed as ‘hard-magnetic abnormal’ layers and correspond well with the Heinrich Events. This indicatesrelatively weak reducing conditions that were resulted from the enhanced East Asian Winter Monsoon (EAWM) and injection of high salinity Tsushima Warm Current (TWC). These changes, however, are not reflected by the grain-size of sediment. Our study therefore not only indicates that the role of magnetic parameters in the paleoenvironmental and palaeoceanographic reconstructions of the Japan Sea during the last glacial, but also provides new perspectives and ideasfor relevant investigations in the future.
- sediments of the Japan Sea,
- magnetic minerals,
- rock magnetism,
- paleoenvironment,
- the Heinrich Events

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