Exploring variations in upper ocean structure for the last 2 Ma of the Nansha area by means of calca

来源 :Science in China(Series D:Earth Sciences) | 被引量 : 0次 | 上传用户:eric_vl
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A great number of calcareous nannofossils have been found in the deep-sea sediments of 2.32 Ma at ODP Site 1143 located in the Nansha area, the southern South China Sea. The number of coccoliths varies from about 0.5×10~6 up to almost 53×10~6 coccoliths/g sediment, with an average of 16×10~6 coccoliths/g sediment. The accumulation rate of total coccoliths varies from 1×10~6 to 278×10~6coccoliths/cm2 ka. The nannofossil assemblages are usually dominated by a lower-photic species-Florisphaera profunda, of which the average percentage is about 70% in all samples. The absolute abundance and the accumulation rate of nannofossils as well as the percentage of F. profunda display significant oscillations on two different time scales. One is the fluctuation coincident with the glacial-interglacial cycle, and the other is the long-term changes on a time scale longer than 100 ka. Six evolutionary stages of calcareous nannofossils could be divided for the last 2.32 Ma, from which we can reconstruct the changes A great number of calcareous nannofossils have been found in the deep-sea sediments of 2.32 Ma at ODP Site 1143 located in the Nansha area, the southern South China Sea. The number of coccoliths varies from about 0.5 × 10 ~ 6 up to almost 53 × 10 ~ 6 coccoliths / g sediment with an average of 16 × 10 ~ 6 coccoliths / g sediment. The accumulation rate of total coccoliths varies from 1 × 10 ~ 6 to 278 × 10 ~ 6 coccoliths / cm 2 ka. The nannofossil assemblages are usually dominated by a lower-photic species-Florisphaera profunda, of which the average percentage is about 70% in all samples. The absolute abundance and the accumulation rate of nannofossils as well as the percentage of F. profunda display significant oscillations on two different time scales. One is the fluctuation coincident with the glacial-interglacial cycle, and the other is the long-term changes on a time scale longer than 100 ka. Six evolutionary stages of calcareous nannofossils could be divided for the last 2.32 Ma, from which we can recon struct the changes
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