地球科学进展

地球科学进展 ›› 2016, Vol. 31 ›› Issue (3): 310 -319. doi: 10.11867/j.issn.1001-8166.2016.03.0310.

所属专题： IODP研究；

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利用有孔虫氧同位素重建古海平面变化的研究进展
李悦 1( ), 王汝建 1,,A; *( ), 李文宝 2   
  1. 1.同济大学海洋地质国家重点实验室,上海 020092
    2.内蒙古农业大学水资源保护与利用自治区重点实验室,内蒙古 呼和浩特 010018
  • 收稿日期:2016-01-31 修回日期:2016-02-20 出版日期:2016-03-20
  • 通讯作者: 王汝建 E-mail:1335140liyue@tongji.edu.cn;rjwang@tongji.edu.cn
  • 基金资助:
    国家重大科学研究计划项目“近百年极地冰盖冰架变化对全球海平面上升的总体贡献定量研究”(编号:2012CB957701);南极专项项目“2016年度南极周边海域海洋地质考察”(编号:CHINARE2016-01-02)资助

Review on Research on Paleo-Sea Level Reconstruction Based on Foraminiferal Oxygen Isotope in Deep Sea Sediments

Yue Li 1( ), Rujian Wang 1, *( ), Wenbao Li 2   

  1. 1.State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092,China
    2.IMARK Key Laboratory of Water Resources Protection and Utilization,Inner Mongolia Agriculture University, Hohhot 010018,China
  • Received:2016-01-31 Revised:2016-02-20 Online:2016-03-20 Published:2016-03-10
  • Contact: Rujian Wang E-mail:1335140liyue@tongji.edu.cn;rjwang@tongji.edu.cn
  • About author:

    First author:Li Yue(1989-), male, Tianjin City, Master student. Research area include Paleoceanography and paleoclimatology.E-mail:1335140liyue@tongji.edu.cn

    Corresponding author:Wang Rujian(1959-), male, Kunming City, Yunnan Province,Professor. Research area include Paleoceanography and paleoclimatology.E-mail:rjwang@tongji.edu.cn

  • Supported by:
    Project supported by the State Key Project of Scientific Research and Plan “Quantitative research on total contribution of polar ice-sheet change during the last 100 year to global sea-level rise”(No.2012CB957701);Antarctic and Arctic Special Project “Marine geology investigation around Antarctic in 2016”(No.CHINARE2016-01-02)
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海平面变化重建结果是一个重要的气候变化指标,可以被用来与其他气候指示要素以及基于计算机模型的重建结果进行比较,从而可以更好地理解海平面变化以及与其气候系统其他要素之间的关系。从深海沉积物中的钙质有孔虫得到的氧同位素记录包含着全球大陆冰量的变化过程,因此可以用来重建地质历史时期海平面演化的历史。尽管诸多研究者利用海洋沉积物中有孔虫氧同位素比值作为基础数据重建了长时间尺度上连续的海平面变化记录,但是,在未来的海平面重建过程中,还需要与其他学科领域结合,并对海平面重建结果和其他气候指标进行对比和相互验证,才能获得可靠的海平面变化记录。

关键词: 海平面变化, 有孔虫氧同位素, 极地冰盖

Sea level reconstruction is an important proxy for climate change. It can be compared with other reconstructed climatic factors as well as the results of the computer model-based reconstruction to offer a better recognition of the relationship between sea-level changes and other factors in the climate system. Oxygen isotope record obtained from calcium foraminiferal shell in deep-sea sediments contains global continental ice volume signal which can be used to reconstruct the evolution of paleo-sea level. Researchers reconstructed many long time scale and continuous records of sea level change by using foraminiferal oxygen isotope ratio data. In the future of paleo-sea level reconstruction, however, researchers need to contrast the sea level reconstruction with other climate proxy results to validate its accuracy and employ the interdisciplinary study method to acquire further development.

Key words: Paleo-sea level, Foraminiferal oxygen isotope, Polar ice sheet.

中图分类号: 

图1 水文循环对氧同位素比值影响的示意图(据参考文献[25]修改)
对海水的影响用斜体表示
Fig.1 Schematic diagram of the hydrological cycle influences on oxygen isotope ratios(modified after reference[25])
Effects on seawater are described in italics
图2 逆过程方法的图解纲要
该过程计算了模拟氧同位素值和0.1 ka之后的观测氧同位素值的平均地表空气温度异常值。平均地表温度异常(DT)的计算结果,会被导入到2个物理系统当中:①左侧的冰川和质量平衡模块;②右侧的大气深层海水温度耦合模块。质量平衡模块利用现在的降水中的同位素含量( Ip)、地表空气温度( T) 和降水量( P) 以及受轨道引起的随时间变化的太阳辐射( Q),计算了在空间上( x),季节上( s)和时间( t)上的变化的质量平衡( M)变化场和降水中的同位素含量( Ip)。 M和 Ip被冰川模块用来计算新的冰川表层高度( H)和表层反射率( α)的分布,该新的计算结果将会返回代入质量平衡过程。 I o为观测氧同位素值,冰川过程决定了平均冰盖同位素含量( Ii),冰川体积( Vi)和全球海平面( S)。以上这些值,与深海温度( DT o)一起,被海洋过程用来计算代入逆过程的海水氧同位素值( Im)。这一过程产生了相互一致的 DT、 DT o、 Vi、 S 和 Ii的时间序列观测获得的数值用红色标注,模拟结果值用黑色标注(据参考文献[55]修改)
Fig.2 Schematic outline of the inverse procedure
The routine calculates a mean surface air temperature anomaly (DT) based on the difference between the modelled marine isotope value and the observed value 0.1 ka later. The value of DT feeds into two physical systems:① the ice-sheet and mass-balance module to the left and ② the atmosphere-deep ocean temperature coupling module to the right. The mass-balance module calculates spatially ( x), seasonally ( s) and temporally ( t) varying fields of surface mass balance ( M) and isotope content of precipitation ( Ip) using initial, present-day fields of Ip, surface air temperature ( T) and precipitation ( P) and temporally varying orbitally induced insolation ( Q) . M and Ip are used by the ice-sheet module to calculate new distributions of ice-sheet surface height ( H) and surface albedo ( α), which feed back into the mass balance routine. Io denotes observed value of oxygen isobope.The ice-sheet routine determines the mean ice-sheet isotope content ( Ii), the ice-sheet volume ( Vi) and global sea level ( S). These values, together with the deep ocean temperature ( DT o), are used by the ocean routine to evaluate the marine isotope value ( Im) that feeds into the inverse routine. This procedure yields mutually consistent time series of DT, DT o, Vi, S, and Ii. Observed variables are in red, modelled ones in black (modified after reference[55])
图3 全球相对海平面重建结果时间序列
蓝色曲线为全球平均海平面的重建结果,绿色曲线为北美大陆冰盖对海平面变化的贡献量,红色曲线为欧亚大陆冰盖对海平面变化的贡献量(据参考文献[55]修改)
Fig.3 Time series of past global sea level
Reconstructed global sea level (blue), and the contributions from Eurasia (red) and North America (green) in sea level equivalents (modified after reference[55])
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