中全新世以来南极宇航员海的古生产力演变

doi:10.13745/j.esf.sf.2022.1.12

地学前缘 ›› 2022, Vol. 29 ›› Issue (4): 113-122.DOI: 10.13745/j.esf.sf.2022.1.12

• 深海生物地球化学过程 • 上一篇下一篇

中全新世以来南极宇航员海的古生产力演变

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

1.成都理工大学沉积地质研究院, 四川成都 610059
2.自然资源部海底科学重点实验室, 浙江杭州 310012
3.自然资源部第二海洋研究所, 浙江杭州 310012

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
通信作者: 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:
自然资源部专项“南极重点海域对气候变化的响应和影响(IRASCC2020-2022);中央级公益性科研院所基本科研业务费专项资金项目(SZ2102);中央级公益性科研院所基本科研业务费专项资金项目(YJJC2001);中央级公益性科研院所基本科研业务费专项资金项目(YJJC2003);上海交通大学“深蓝计划”基金(SL2002)

The evolution of paleoproductivity since the Middle Holocene in the Cosmonaut Sea, Antarctic

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

1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
2. Key Laboratory of Submarine Geosciences, Ministry of Natural Resources, Hangzhou 310012, China
3. Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China

Received:2021-09-22 Revised:2021-12-19 Online:2022-07-25 Published:2022-07-28
Contact: HAN Xibin

摘要/Abstract

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。

关键词: 宇航员海, 古生产力, 气候变化, 沉积环境

Abstract:

Aiming to reconstruct the paleoproductivity evolution and its constraints in the Cosmonaut Sea since the Middle Holocene (6500 Cal a BP), a series of experiments including AMS¹⁴C dating, radionuclide ²¹⁰Pb testing, XRF core scan, multi-parameter spectrophotometer probe as well as major and trace elemental analysis were conducted on sediment core ANT36-C4-05 collected from the Cosmonaut Sea, Antarctic. The results showed that paleoproductivity in the Cosmonaut Sea fluctuates strongly since the Middle Holocene, and its evolutionary trend is largely consistent with the temperature change in Antarctic constrained mainly by the change of sea ice range. During the period of 6500-5200 Cal a BP, paleoproductivity increased rapidly with increasing temperature and decreasing sea ice range, and remained high with little fluctuation between 5200-3350 Cal a BP. During 3350-2000 Cal a BP siliceous and calcareous productivity decreased with decreasing temperature and expanding sea ice range. Paleoproductivity variability became complex with smaller fluctuation during 2000-0 Cal a BP. Moreover, sedimentary records of the Cosmonaut Sea since the Middle Holocene showed that the most obvious paleoproductivity fluctuations were associated with the cold period of 5500 Cal a BP, the Dark Age Cold Period, the Medieval Warm Period, and the Little Ice Age.

Key words: Cosmonaut Sea, paleoproductivity, climatic change, sedimentary environment

中图分类号:

P467
P736.21

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/表 5

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

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2 ANT36-C4-05岩心210Pbex垂直剖面图

Fig.2 210Pbex vertical profile of core ANT36-C4-05

图3 ANT36-C4-05岩心日历年龄与沉积速率图

Fig.3 Age model and sedimentation rate of core ANT36-C4-05

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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中全新世以来南极宇航员海的古生产力演变

The evolution of paleoproductivity since the Middle Holocene in the Cosmonaut Sea, Antarctic

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