西藏色林错沉积物介壳同位素重建的2000年以来气候变化研究

郭姝雯; 余芳艳; 王哲; 何志兴; 尚发美; 谢曼平

doi:10.11928/j.issn.1001-7410.2023.01.07

西藏色林错沉积物介壳同位素重建的2000年以来气候变化研究

- 1.
  云南师范大学地理学部, 云南省高原地理过程与环境变化重点实验室, 云南昆明 650500
- 2.
  中国电建集团昆明勘测设计研究院有限公司, 云南昆明 650000
- 3.
  云南省澄江县第一中学, 云南澄江 652599
基金项目:
国家自然科学基金项目(批准号: 41961015)和第二次青藏高原综合科学考察研究项目(批准号: 2019QZKK0202)共同资助

详细信息

作者简介:
郭姝雯, 女, 24岁, 硕士研究生, 湖泊沉积与环境演变研究, E-mail: 724828678@qq.com

通讯作者: 谢曼平, E-mail: formelody@126.com

中图分类号: P534.63⁺2;P532

收稿日期: 2022-04-02

修回日期: 2022-09-27

刊出日期: 2023-01-30

The research of climate change of past 2000 years based on isotopes of sediment ostracods shells in Serlin Co, Tibet

- 1.
  Yunnan Key Laboratory of Plateau Geographical Processes and Environmental Change, Faculty of Geography, Yunnan Normal University, Kunming 650500, Yunnan
- 2.
  Power China Kunming Engineering Corporation Limited, Kunming 650000, Yunnan
- 3.
  Yunnan Chengjiang First Middle School, Chengjiang 652599, Yunnan

More Information

Corresponding author: XIE Manping, E-mail: formelody@126.com

Received Date: 02 April 2022

Revised Date: 27 September 2022

Publish Date: 30 January 2023

摘要

摘要:
青藏高原作为印度季风与西风交汇的特殊区域, 对全球气候变化响应敏感, 成为了古气候研究的热点地区。青藏高原湖泊众多, 存在巨厚连续的湖泊沉积物, 为古气候重建提供了优良载体。而介形类壳体在湖泊中沉积连续, 生长过程记录了气候变化, 同时有效屏蔽了湖泊水体中同位素的累积效应, 能够反映介壳生长阶段短时间尺度的同位素水平, 理论上是高精度气候重建的理想载体。基于此, 本研究选取青藏高原中部地区湖泊色林错湖芯(SL16-1-1)顶部0~107cm部分为对象, 对其中的介形类壳体进行种属鉴定及碳氧同位素分析, 以期建立高分辨率的古环境变化记录, 结合沉积物Rb/Sr、Ti/Si环境代用指标, 重建色林错湖区近2000年来的气候变化记录, 结果揭示了: 1)介形类壳体碳氧稳定同位素变化对气候变化(尤其冷气候)尤为敏感, 是重建高分辨率环境变化过程的优良载体; 2)色林错地区对小冰期冷事件的响应较早于其他地区; 3)色林错介形类壳体2000年来的气候重建结果与青藏高原研究成果大体一致, 特别是与内地文献记录和物候史料记载高度一致, 说明色林错湖泊记录具有广泛代表性, 同时证实利用湖泊沉积物介形类壳体进行古气候高分辨率重建具有可靠性。
- 介形类 /
- 青藏高原 /
- 湖泊沉积物 /
- 2000年 /
- 气候变化
Abstract:
As the major region of the Indian monsoon and Westerlies circulation, the Tibetan Plateau(TP)is susceptible to climate change and has become an important place for paleoclimate research. The Tibetan Plateau contains numerous lakes, and the thick and continuous lake sediments give excellent climate change records. Research indicates that the deposition of Ostracod shells in lake sediments was multitudinous and continuous, which can guarantee the carrying out of the researching work, and the shells growth processing is short and fast, which can remove the accumulative effect of isotopes and provide precise and reliable isotopic results in water, making it theoretically an ideal proxy for high-precision climate reconstruction. This study focuses on the largest lake in the middle of TP, Serlin Co(31.34°~31.57°N, 88.31°~89.21°E)is located in the transition zone between the Indian monsoon and Westerlies domains of the central TP. We used a sedimentary core(SL16-1-1, collected in 31°45.210'N, 88°58.484'E)that was obtained in the water depth of 41.2m in the center of Serlin Co in 2016 and Ostracod shells, Rb/Sr, Ti/Si from it. The total length of the core was 191cm, we used SL16-1-1 from top to 107cm, samples of 2cm intervals were used to analyze paleoclimate over the past 2000 years. Sedimentological chronology based on AMS ¹⁴C and ²¹⁰Pb dating. With Ostracod assemblages and stable carbon and oxygen isotopes from shells, it is anticipated that high-resolution records of environmental change can be compiled. The results document climate change information in the middle of TP as well as on a worldwide scale. The results showed that: (1)In particular for cold climates, the change of stable carbon and oxygen isotopes in ostracod shells gives a reliable record of climate change and can be used to reconstruct high-resolution paleoclimate; (2)Serlin Co was earlier entered the Little Ice Age(LIA); (3)Ostracod shell paleoclimate results were discovered as TP prior research results, and when compared to historical records, these results are identical. These findings showed that the reconstruction of paleoclimate in plateau lake using Ostracod shell isotopes is reliable and that climate change is broadly representative.
- Ostracods /
- Tibetan Plateau /
- lake sediments /
- 2000 years /
- climate change

HTML全文

图 1

色林错湖盆地形及位置(a)和色林错水系与钻孔采样点(b)

Figure 1.

Lake basin and topography (a), and river system and SL16-1-1 core position (b) of Serlin Co

下载: 全尺寸图片幻灯片

图 2

色林错SL16-1-1岩芯年代确定

Figure 2.

The chronology of SL16-1-1 core in Serlin Co.

下载: 全尺寸图片幻灯片

图 3

色林错SL16-1-1孔介形类壳体碳氧同位素和全样元素Rb/Sr与Ti/Si变化

Figure 3.

Variations of δ¹⁸O and δ¹³C of ostracods shells and Rb/Sr and Ti/Si of total examples in SL16-1-1 core of Serlin Co

下载: 全尺寸图片幻灯片

表 1

色林错湖芯SL16-1-1的AMS ¹⁴C测年结果

Table 1.

AMS ¹⁴C dating results of SL16-1-1 core from Serlin Co in Tibet

Beta编号	样品	深度 (cm)	材料	¹⁴C年代±误差 (cal.aB. P.)	δ¹³C (‰)	碳库校正¹⁴C年代±误差 (cal.a B. P.)	日历年年代(2σ) (cal.a B. P.)
575632	SL16-1-1(0-2)-6	6	全有机质	3902±30	-21.3	0±30	0
575633	SL16-1-1(0-2)-28	28	全有机质	3634±30	-23.2	434±30	434
575634	SL16-1-1(0-2)-68	68	全有机质	4572±30	-21.3	1372±30	1372
575635	SL16-1-1(0-2)-95	95	全有机质	4861±30	-22	1661±30	1660.5
575636	SL16-1-1(0-2)-120	120	全有机质	5517±30	-24	2317±30	2316.5
575637	SL16-1-1(0-2)-146	146	全有机质	5894±30	-23.7	2694±30	2694
575638	SL16-1-1(0-2)-166	166	全有机质	6479±30	-22.5	3279±30	3279

下载: 导出CSV

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西藏色林错沉积物介壳同位素重建的2000年以来气候变化研究

作者简介: 郭姝雯, 女, 24岁, 硕士研究生, 湖泊沉积与环境演变研究, E-mail: 724828678@qq.com

通讯作者: 谢曼平, E-mail: formelody@126.com

The research of climate change of past 2000 years based on isotopes of sediment ostracods shells in Serlin Co, Tibet

Corresponding author: XIE Manping, E-mail: formelody@126.com

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作者简介:
郭姝雯, 女, 24岁, 硕士研究生, 湖泊沉积与环境演变研究, E-mail: 724828678@qq.com