Earth Science Frontiers ›› 2022, Vol. 29 ›› Issue (4): 113-122.DOI: 10.13745/j.esf.sf.2022.1.12
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HU Bingyao1,2,3(), LONG Feijiang1,2,3, HAN Xibin2,3,*(
), ZHANG Yongcong2,3, HU Liangming2,3, XIANG Bo1,2,3, GE Qian2,3, BIAN Yeping2,3
Received:
2021-09-22
Revised:
2021-12-19
Online:
2022-07-25
Published:
2022-07-28
Contact:
HAN Xibin
CLC Number:
HU Bingyao, LONG Feijiang, HAN Xibin, ZHANG Yongcong, HU Liangming, XIANG Bo, GE Qian, BIAN Yeping. The evolution of paleoproductivity since the Middle Holocene in the Cosmonaut Sea, Antarctic[J]. Earth Science Frontiers, 2022, 29(4): 113-122.
Fig.1 Location of sediment core ANT36-C4-05, oceanic circulation and front in the Cosmonaut Sea, and modern-day sea ice range during summer and winter in Antarctica. Modified after [25-26]. EDML-EPICA ice cores from Dronning Maud Land
实验室编号 | 样品深 度编号 | 测试 材料 | 测试值/ a BP | 校正年 龄/a | 老碳年 龄/a | 日历年龄/ Cal a BP |
---|---|---|---|---|---|---|
Beta-567729 | C4-05-00 | 有机碳 | 3 820±30 | 2 233 | 2 233 | 0 |
Beta-567729 | C4-05-05 | 有机碳 | 5 700±30 | 4 512 | 2 233 | 2 279 |
Beta-567729 | C4-05-11 | 有机碳 | 8 280±30 | 7 432 | 2 233 | 5 199 |
Beta-567729 | C4-05-17 | 有机碳 | 9 860±40 | 9 200 | 2 233 | 6 967 |
Beta-567729 | C4-05-23 | 有机碳 | 9 490±40 | 8 733 | 2 233 | 6 500 |
Table 1 AMS14C dating results and calibrated ages of sediment samples from core ANT36-C4-05
实验室编号 | 样品深 度编号 | 测试 材料 | 测试值/ a BP | 校正年 龄/a | 老碳年 龄/a | 日历年龄/ Cal a BP |
---|---|---|---|---|---|---|
Beta-567729 | C4-05-00 | 有机碳 | 3 820±30 | 2 233 | 2 233 | 0 |
Beta-567729 | C4-05-05 | 有机碳 | 5 700±30 | 4 512 | 2 233 | 2 279 |
Beta-567729 | C4-05-11 | 有机碳 | 8 280±30 | 7 432 | 2 233 | 5 199 |
Beta-567729 | C4-05-17 | 有机碳 | 9 860±40 | 9 200 | 2 233 | 6 967 |
Beta-567729 | C4-05-23 | 有机碳 | 9 490±40 | 8 733 | 2 233 | 6 500 |
Fig.4 Paleoproductivity proxies in core ANT36-C4-05 (g-m) compared with solar insolation (a), sea surface temperature change (b), EDML CH4 (c), EDML ssNa+(d), EDML δ18O (e), and Taylor Dome δ18O (f)
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