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辽宁暖和洞石笋δ13C记录的古气候环境意义初探

顾 宁 吴江滢

顾 宁, 吴江滢. 辽宁暖和洞石笋δ13C记录的古气候环境意义初探[J]. 中国岩溶, 2012, 31(2): 107-114.
引用本文: 顾 宁, 吴江滢. 辽宁暖和洞石笋δ13C记录的古气候环境意义初探[J]. 中国岩溶, 2012, 31(2): 107-114.
GU Ning, WU Jiang-ying. Pale climate significance of δ13C in stalagmite from Nuanhe Cave, Liaoning[J]. CARSOLOGICA SINICA, 2012, 31(2): 107-114.
Citation: GU Ning, WU Jiang-ying. Pale climate significance of δ13C in stalagmite from Nuanhe Cave, Liaoning[J]. CARSOLOGICA SINICA, 2012, 31(2): 107-114.

辽宁暖和洞石笋δ13C记录的古气候环境意义初探

基金项目: 国家自然科学基金项目(40972111)

Pale climate significance of δ13C in stalagmite from Nuanhe Cave, Liaoning

  • 摘要: 基于辽宁暖和洞石笋NH33铀系测年结果,利用900条年纹层及302个碳、氧同位素和灰度数据,建立全新世大暖期内近1000年的石笋δ13C与灰度序列(8638±60 - 7748±53 aBP)。碳同位素与灰度序列细节特征变化趋势上的一致性,证实了δ13C所指示的古气候意义。在百年尺度上,石笋δ13C主要响应于温度变化,由地表生物量的变化驱动。石笋δ13C序列可进一步划分为3个气候段:(1)8655 – 8366 aBP,气候偏热;(2)8366 – 8048 aBP,气候转冷;(3)8048 – 7756 aBP,气候相对温暖。这与同时段孢粉记录具有很好的一致性。其中,8366-8048aBP的冷期与北大西洋地区“8.2 kaBP冷事件”相吻合。石笋δ13C记录中也包含一定的非气候因素,主要由渗水速率变化引起围岩CaCO3溶解量的变化造成。将石笋δ13C和灰度数据进行回归分析,可有效地剔除这一水动力因素的影响。

     

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  • 收稿日期:  2011-12-29
  • 刊出日期:  2012-06-25

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