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《Acta Oceanologica Sinica》 2005-01
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Natural thermoluminescence characteristics of carbonate in deep sea cores

LIU Hai-sheng~1, FANG Nian-qiao~2, AI Xing-tao~1, MA Wan-yun~1, CHEN Die-yan~1 (1. Key Laboratory of Atomic and Molecular Nanosciences of Ministry of Education of Department of Physics, Tsinghua University, Beijing 100084, China; 2. China University of Geosciences, Beijing 100083, China)  
The natural thermoluminescence (NTL) of foraminiferal shells from piston cores MD81349 and MD77181 from the Ninetyeast Ridge and the Bengal Fan of the Indian Ocean were studied for the climate changes during the past 300 ka. It has been found that the TL fluctuations are closely correlated to the oxygen isotope curves. The high and low TL intensities correspond to the interglacial and glacial stages respectively. The spectrum analysis of TL profile reveals several significant periodicities at 99, 46, 23, 20 and 11 ka. Apparently, the periodicities of 99, 46, 23 and 20 ka coincide with the orbital eccentricity, obliquity and processional cycles respectively. The results of spectrum analysis and TL fluctuations indicate that glacial-interglacial climatic cycles are controlled by the change in the solar insolation. The TL intensities of planktonic foraminiferal shells can be used to indicate the paleoclimate changes and the solar insolation.
【Fund】: 国家自然科学基金资助项目(40306017;40272074);; 中国博士后基金资助项目.
【CateGory Index】: P532
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