地学前缘 ›› 2022, Vol. 29 ›› Issue (4): 113-122.DOI: 10.13745/j.esf.sf.2022.1.12
胡栟铫1,2,3(), 龙飞江1,2,3, 韩喜彬2,3,*(), 张泳聪2,3, 胡良明2,3, 向波1,2,3, 葛倩2,3, 边叶萍2,3
收稿日期:
2021-09-22
修回日期:
2021-12-19
出版日期:
2022-07-25
发布日期:
2022-07-28
通讯作者:
韩喜彬
作者简介:
胡栟铫(1997—),男,硕士研究生,古生物学与地层学专业,主要从事海洋沉积研究。E-mail: 1564779815@qq.com
基金资助:
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
摘要:
本文通过对南极宇航员海ANT36-C4-05岩心的放射性核素210Pb、AMS14C测年、XRF岩心扫描、多参数物性扫描和主、微量元素的测试分析,重建了该海区中全新世(6 500 Cal a BP)以来的古生产力演变及其制约因素。研究结果表明,中全新世以来宇航员海古生产力波动较强,其演变趋势与南极气温变化基本一致,受海冰范围变化制约较大。在6 500~5 200 Cal a BP期间宇航员海古生产力随着温度升高和海冰范围减小而快速上升;在5 200~3 350 Cal a BP期间宇航员海的古生产力处于高值期,波动较小;在3 350~2 000 Cal a BP期间随着温度降低和海冰范围的扩大,硅质、钙质生产力下降;在2 000~0 Cal a BP期间古生产力水平变化复杂,变化程度相较于之前小。同时,中全新世以来宇航员海区沉积记录较好地反映了5 500 Cal a BP冷事件、DACP冷事件、MWP暖期和LIA冷事件的气候变化,受冷、暖事件影响导致的古生产力的变化最为明显。
中图分类号:
胡栟铫, 龙飞江, 韩喜彬, 张泳聪, 胡良明, 向波, 葛倩, 边叶萍. 中全新世以来南极宇航员海的古生产力演变[J]. 地学前缘, 2022, 29(4): 113-122.
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.
图1 ANT36-C4-05岩心位置及宇航员海域环流、锋面、现代冬夏季海冰范围示意图(据文献[25-26]补充修改)
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 |
表1 ANT36-C4-05岩心AMS14C测年数据及其校正年龄
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 |
图4 ANT36-C4-05古生产力替代指标与65°S一月光照、海洋表层温度变化、EDML CH4、EDML ssNa+、EDML δ18O、Taylor Dome δ18O对比图 1—5 500 Cal a BP冷事件;2—黑暗时代冷期;3—中世纪暖期;4—小冰期;a—65°S一月光照[40];b—南极半岛JPC-10站位SST[41];c—EDML C H 4 [ 42 ];d—EDML ssN a + [ 43 ];e—EDML δ18O[42];f—Taylor Dome δ18O[44];g至m各古生产力替代指标。
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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