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作 者:王汝建 Andrea Abelmann
机构地区:[1]Alfred Wegener Institute for Polar and Marine Research, 27515 Bremerhaven, Germany
出 处:《Science China Earth Sciences》1999年第5期536-543,共8页中国科学(地球科学英文版)
基 金:Project supported by the National Natural Science Foundation of China (Grant No. 49291100);by the German Federal Ministry for Education, Science, Research and Technology (BMBF) as part of a German/Chinese scientific cooperation Program. This is Alfred
摘 要:Based on a quantitative radiolarian analysis, 5 radiolarian zones (NR1-NR5) have been defined at Core 17957-2 from the South China Sea, considering radiolarian zonations from low latitudes. The absolute age assignment of the radiolarian zones and the ranges of the six marker species is based on the direct correlation with the paleomagnetic and isotopic record, respectively. A comparison of the radiolarian stratigraphic data obtained from Core 17957-2 from the South China Sea with those from the equatorial Pacific and the tropical Indian Ocean shows a close similarity to the ages defined in the equatorial Pacific. The obtained biostratigraphic data provide an excellent tool for further dating of Pleistocene sediments in the China Sea.Based on a quantitative radiolarian analysis, 5 radiolarian zones (NR1-NR5) have been defined at Core. 17957-2 from the South China Sea, considering radiolarian zonations from low latitudes. The absolute age assignment of the radiolarian zones and the ranges of the six marker species is based on the direct correlation with the paleomagnetic and isotopic record, respectively. A comparison of the radiolarian stratigraphic data obtained from Core 17957-2 from the South China Sea with those from the equatorial Pacific and the tropical Indian Ocean shows a close similarity to the ages defined in the equatorial Pacific. The obtained biostratigraphic data provide an excellent tool for further dating of Pleistocene sediments in the China Sea.
关 键 词:RADIOLARIAN BIOSTRATIGRAPHY RADIOLARIAN ZONES PLEISTOCENE SOUTH China Sea.
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