晚第四纪中西太平洋暖池球粒岩变化及其对环境变化的响应

Dan Liang, Chuanlian Liu, X. Su
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摘要

本文对西太平洋中部暖池KX97321-2站点近380 ka的球石种类和百分比进行了分析。结果表明,近380 ka来,深Florisphaera profunda的相对丰度呈上升趋势,表明营养线深度下降,初级生产力下降。然而,Gephyrocapsa sp .的相对丰度在最近380 ka中有所下降。由于对中布朗什特有环境的适应进化,加勒比巨藻在中布朗什区间数量最多。通过对深叶霉初级生产力的光谱分析,发现了近380 ka的100 ka和30 ka旋回。0~80 ka和320~380 ka有明显的20 ka旋回,80~320 ka有明显的40 ka旋回。
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COCCOLITH VARIATIONS IN CENTRAL WEST PACIFIC WARM POOL AND THEIR RESPONSE TO ENVIRONMENTAL CHANGE DURING LATE QUATERNARY
The analysis of coccolith species and percentage for the past 380 ka from Site KX97321-2 of the central West Pacific Warm Pool has been carried out.The results show that the relative abundance of Florisphaera profunda increased in the last 380 ka,indicating the decline of nutricline depth and the decrease in primary productivity.The relative abundance of Gephyrocapsa spp.however,dropped in the last 380 ka.Gephyrocapsa caribbeanica was the most abundant species in the Mid-Brunhes interval as the result of the adaptive evolution to the Mid-Brunhes peculiar environment.Based on the spectrum analysis of primary productivity converted from F.profunda,100 ka and 30 ka cycles were discovered during the last 380 ka.20 ka cycle was found obvious in the 0~80 ka and 320~380 ka,and 40 ka cycle in the 80~320 ka.
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