南海北部ZHS-176孔古海洋学记录：氧同位素和有机碳
对南海北部陆坡ZHS-176孔进行浮游有孔虫氧同位素和有机碳的研究,重建了末次冰期以来的古气候演化历史。ZHS-176孔浮游有孔虫氧同位素分析揭示了末次冰期期间的气候波动,如末次盛冰期、Heinrich事件1、Bølling-Allerød暖期与新仙女木事件在南海北部陆坡均有响应。同时,在全新世阶段存在3个强降水期和3个弱降水期。ZHS-176孔有机碳以生物成因为主,随着夏季风的增强,陆源物质含量增加,但在3 kaBP以后由于华南地区夏季风减弱而导致陆源输入减少。...
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| Published in | Hăiyang dĭzhĭ yu dĭsĭjĭ dĭzhĭ Vol. 32; no. 5; p. 73 |
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| Main Authors | , , , , |
| Format | Journal Article |
| Language | Chinese |
| Published |
Beijing
Marine Geology and Quaternary Geology
01.01.2012
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| Subjects | |
| Online Access | Get full text |
| ISSN | 0256-1492 |
| DOI | 10.3724/SP.J.1140.2012.05073 |
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| Abstract | 对南海北部陆坡ZHS-176孔进行浮游有孔虫氧同位素和有机碳的研究,重建了末次冰期以来的古气候演化历史。ZHS-176孔浮游有孔虫氧同位素分析揭示了末次冰期期间的气候波动,如末次盛冰期、Heinrich事件1、Bølling-Allerød暖期与新仙女木事件在南海北部陆坡均有响应。同时,在全新世阶段存在3个强降水期和3个弱降水期。ZHS-176孔有机碳以生物成因为主,随着夏季风的增强,陆源物质含量增加,但在3 kaBP以后由于华南地区夏季风减弱而导致陆源输入减少。 |
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| AbstractList | 对南海北部陆坡ZHS-176孔进行浮游有孔虫氧同位素和有机碳的研究,重建了末次冰期以来的古气候演化历史。ZHS-176孔浮游有孔虫氧同位素分析揭示了末次冰期期间的气候波动,如末次盛冰期、Heinrich事件1、Bølling-Allerød暖期与新仙女木事件在南海北部陆坡均有响应。同时,在全新世阶段存在3个强降水期和3个弱降水期。ZHS-176孔有机碳以生物成因为主,随着夏季风的增强,陆源物质含量增加,但在3 kaBP以后由于华南地区夏季风减弱而导致陆源输入减少。 |
| Author | Zuo, XUE MENG Xianwei CHU Fengyou GE Qian Jijiang, LEI |
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| DOI | 10.3724/SP.J.1140.2012.05073 |
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| Snippet | 对南海北部陆坡ZHS-176孔进行浮游有孔虫氧同位素和有机碳的研究,重建了末次冰期以来的古气候演化历史。ZHS-176孔浮游有孔虫氧同位素分析揭示了末次冰期期间的气候波动,如末... |
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| SubjectTerms | Carbon Foraminifera Glacial periods Heinrich events Holocene Ice ages Isotopes Monsoons Organic carbon Oscillations Oxygen Oxygen isotopes Precipitation Records Summer |
| Title | 南海北部ZHS-176孔古海洋学记录：氧同位素和有机碳 |
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