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珊瑚生长率重建西沙海域中晚全新世海温变化

DOI: 10.3969/j.issn.1001-7410.2014.06.19, PP. 1296-1305

Keywords: 珊瑚生长率,SST,中晚全新世,西沙海域,滨珊瑚(Poriteslutea)

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Abstract:

珊瑚生长率是记录海洋表层海水温度(SST)的重要指标之一。本文在测量西沙永兴岛海域1个现代滨珊瑚(Poriteslutea)和4个中-晚全新世滨珊瑚样品生长率基础上,定量重建了中晚全新世5个特征时段的SST:1887~2007A.D.(27.27℃)、1993~1936aB.P.(26.73℃)、2985~2904aB.P.(26.5℃)、4004~3962aB.P.(26.8℃)和5514~5398aB.P.(27.0℃)。这些结果表明5.5~1.9kaB.P.期间西沙海域SST总体上呈下降趋势,与中国大陆的平均温度基本同步变化。西沙海域中晚全新世SST的降低趋势受东亚夏季风强度减弱的控制,也可能与这一时期逐渐活跃的ENSO存在联系,而岁差引起的北半球太阳辐射量的减少可能是SST变化的根本驱动因素。

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