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全新世冲绳海槽北部陆源输入物变化及其古气候意义

黄小慧 王汝建 翦知湣

黄小慧, 王汝建, 翦知湣. 全新世冲绳海槽北部陆源输入物变化及其古气候意义[J]. 海洋地质与第四纪地质, 2009, 29(5): 73-82. doi: 10.3724/SP.J.1140.2009.05073
引用本文: 黄小慧, 王汝建, 翦知湣. 全新世冲绳海槽北部陆源输入物变化及其古气候意义[J]. 海洋地质与第四纪地质, 2009, 29(5): 73-82. doi: 10.3724/SP.J.1140.2009.05073
HUANG Xiaohui, WANG Rujian, JIAN Zhimin. HOLOCENE TERRIGENOUS INPUT CHANGES IN THE NORTHERN OKINAWA TROUGH AND THEIR PALEOCLIMATIC IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 73-82. doi: 10.3724/SP.J.1140.2009.05073
Citation: HUANG Xiaohui, WANG Rujian, JIAN Zhimin. HOLOCENE TERRIGENOUS INPUT CHANGES IN THE NORTHERN OKINAWA TROUGH AND THEIR PALEOCLIMATIC IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 73-82. doi: 10.3724/SP.J.1140.2009.05073

全新世冲绳海槽北部陆源输入物变化及其古气候意义


doi: 10.3724/SP.J.1140.2009.05073
详细信息
    作者简介:

    黄小慧(1987-),女,学士,海洋地质专业,E-mail:erer053241@gmail.com

  • 基金项目:

    同济大学国家大学生创新训练计划项目

    国家重点基础研究发展规划项目(G2007CB815903)

    国家自然科学创新研究群体科学基金项目(40321603)

  • 中图分类号: P736.21

HOLOCENE TERRIGENOUS INPUT CHANGES IN THE NORTHERN OKINAWA TROUGH AND THEIR PALEOCLIMATIC IMPLICATIONS

More Information
  • 摘要: 运用多种方法,重建了全新世以来冲绳海槽北部地区陆源输入物以及火山碎屑物的沉积历史。在11.0~6.0 kaBP期间,北部冲绳海槽的陆源物质供应量主要受控于海平面变化。由于该时期海平面上涨了50~60 m,东海陆架上的海岸线快速后退,导致输入北部冲绳海槽的陆源碎屑物和有机质明显减少,沉积物粒度变细。在8.1~7.8 kaBP期间,沉积物中的火山玻璃数目显著增加,导致该时段沉积物粒度急剧增大。经对比分析,该火山玻璃层即为源自日本南部Kikai火山的K-Ah火山灰层。但深海沉积序列中该火山灰层年龄比陆相记录中的7.3 kaBP偏老几百年,推测这是由海洋14C测年的校正问题引起的。早全新世冲绳海槽地区的碳储库年龄应该比现在偏老300~500 a,导致14C测年的校正值出现偏移。一些陆源烷烃的参数指标显示,全新世以来东亚地区草本植物不断增多,而木本植物逐步减少,表明陆地干旱化程度逐渐加强,这与全新世东亚夏季风减弱相对应。
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  • 收稿日期:  2009-07-13
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全新世冲绳海槽北部陆源输入物变化及其古气候意义

doi: 10.3724/SP.J.1140.2009.05073
    作者简介:

    黄小慧(1987-),女,学士,海洋地质专业,E-mail:erer053241@gmail.com

基金项目:

同济大学国家大学生创新训练计划项目

国家重点基础研究发展规划项目(G2007CB815903)

国家自然科学创新研究群体科学基金项目(40321603)

  • 中图分类号: P736.21

摘要: 运用多种方法,重建了全新世以来冲绳海槽北部地区陆源输入物以及火山碎屑物的沉积历史。在11.0~6.0 kaBP期间,北部冲绳海槽的陆源物质供应量主要受控于海平面变化。由于该时期海平面上涨了50~60 m,东海陆架上的海岸线快速后退,导致输入北部冲绳海槽的陆源碎屑物和有机质明显减少,沉积物粒度变细。在8.1~7.8 kaBP期间,沉积物中的火山玻璃数目显著增加,导致该时段沉积物粒度急剧增大。经对比分析,该火山玻璃层即为源自日本南部Kikai火山的K-Ah火山灰层。但深海沉积序列中该火山灰层年龄比陆相记录中的7.3 kaBP偏老几百年,推测这是由海洋14C测年的校正问题引起的。早全新世冲绳海槽地区的碳储库年龄应该比现在偏老300~500 a,导致14C测年的校正值出现偏移。一些陆源烷烃的参数指标显示,全新世以来东亚地区草本植物不断增多,而木本植物逐步减少,表明陆地干旱化程度逐渐加强,这与全新世东亚夏季风减弱相对应。

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