南京大学学报(自然科学版) ›› 2019, Vol. 55 ›› Issue (2): 320–331.doi: 10.13232/j.cnki.jnju.2019.02.017

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北部湾全新世UK37的古海水表面温度重建研究

杨　博1，殷　勇1*，高　抒1，贾培宏1，夏　真2   

  1. 1.南京大学地理与海洋科学学院，南京，210023； 2.中华人民共和国自然资源部广州海洋地质调查局，广州，510075
  • 接受日期:2018-04-27 出版日期:2019-04-01 发布日期:2019-03-31
  • 通讯作者: 殷　勇 E-mail:yinyong@nju.edu.cn
  • 基金资助:
    江苏省重点基金(BK20130056)，国家自然科学基金(40776023)

A Holocene UK37 based paleo－sea surface temperature reconstruction，the Beibu Gulf，Southwestern China

Yang Bo1，Yin Yong1*，Gao Shu1，Jia Peihong1，Xia Zhen2   

  1. 1.School of Geography and Ocean Science，Nanjing University，Nanjing，210023，China 2.Guangzhou Marine Geological Survey，Ministry of Natural Resources of the People’s Republic of China，Guangzhou，510075，China
  • Accepted:2018-04-27 Online:2019-04-01 Published:2019-03-31
  • Contact: Yin Yong E-mail:yinyong@nju.edu.cn

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摘要： 通过海洋沉积物有机温标UK37反演了北部湾地区一万年以来的海水表面温度(Sea Surface Temperature，SST)变化. 结果表明，北部湾一万年以来的SST变化范围为22.0 ℃～28.0 ℃，平均25.4 ℃，整体呈现波动升高的趋势，其中1300年来的SST升高更为明显. 此外，钻孔还记录到了八次具有区域意义的温度变化事件. 北部湾一万年来的海表温度变化主要受到太阳总辐照度和东亚冬季风的控制，一些冷事件还受到高纬度融冰事件的影响，而暖事件可能受到赤道太平洋低纬度驱动的影响．

关键词: 北部湾, 全新世, 海水表面温度, 太阳总辐照度, 东亚冬季风, UK37

Abstract: The South China Sea(SCS)is one of the largest marginal seas in the Western Pacific and sensitive to climate changes. Emilimia Huxley and Gephyrocapsa Oceanica can produce a compound with 37～39 carbon atoms which we call long chain alkenones in the process of growth and metabolism. The unsaturation of this alkenones is UK37. The sea surface temperature(SST) variation process of the Beibu Gulf during the last 10 thousand years has been reconstructed based on the sediment core SO－31(location 18°36′46.45″N，107°22′43.20″E，core length 7.34 m)by using the organic thermometer UK37. Overall，the SST of the Beibu Gulf has been increasing gradually for the last 10 thousand years. The highest temperature is 28.0 ℃ at 255 a BP and the lowest is about 22.0 ℃ at 2658 a BP with an average of 25.4 ℃. The SST has an overall increasing trend during the Holocene，but increasing obviously during the last 1.3 ka. The fluctuation amplitude is low between 10.0 ka BP and 5.3 ka BP，but becoming large since 5.3 ka BP. For the last 5300 years，SST has a one hundred scale periodic time，which might be related to the double century cycle of total solar irradiance. In addition，the core has recorded 8 temperature events with regional significance including 6 cold events at 9.2 ka BP，5.3 ka BP，4.3 ka BP，2.7 ka BP，1.3 ka BP，0.6～0.2 ka BP and 2 warm events at 6.9 ka BP，0.9 ka BP. The Beibu Gulf SST fluctuation during the last 10 ka is mainly controlled total solar irradiance，East Asia Winter Monsoon and even high latitudinal ice melting events. Meanwhile，volcanic eruptions and reducing cosmic rays are also important to SST changes during the last 1 ka.

Key words: The Beibu Gulf, Holocene, Sea Surface Temperature(SST), Total Solar Irradiance(TSI), East Asia Winter Monsoon(EAWM), UK37

中图分类号: 

  • P736.4
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