On the sediment age estimated by 210Pb dating: probably misleading “prolonging” and multiple-factor-caused “loss”

JIA Jianjun YANG Yang CAI Tinglu GAO Jianhua XIA Xiaoming LI Yan GAO Shu

贾建军, 杨旸, 蔡廷禄, 高建华, 夏小明, 李炎, 高抒. 210Pb测年的“延年”与“折寿”[J]. 海洋学报英文版, 2018, 37(6): 30-39. doi: 10.1007/s13131-018-1214-4
引用本文: 贾建军, 杨旸, 蔡廷禄, 高建华, 夏小明, 李炎, 高抒. 210Pb测年的“延年”与“折寿”[J]. 海洋学报英文版, 2018, 37(6): 30-39. doi: 10.1007/s13131-018-1214-4
JIA Jianjun, YANG Yang, CAI Tinglu, GAO Jianhua, XIA Xiaoming, LI Yan, GAO Shu. On the sediment age estimated by 210Pb dating: probably misleading “prolonging” and multiple-factor-caused “loss”[J]. Acta Oceanologica Sinica, 2018, 37(6): 30-39. doi: 10.1007/s13131-018-1214-4
Citation: JIA Jianjun, YANG Yang, CAI Tinglu, GAO Jianhua, XIA Xiaoming, LI Yan, GAO Shu. On the sediment age estimated by 210Pb dating: probably misleading “prolonging” and multiple-factor-caused “loss”[J]. Acta Oceanologica Sinica, 2018, 37(6): 30-39. doi: 10.1007/s13131-018-1214-4

210Pb测年的“延年”与“折寿”

doi: 10.1007/s13131-018-1214-4
基金项目: The National Natural Science Foundation of China under contract Nos 41376068 and 41776068.

On the sediment age estimated by 210Pb dating: probably misleading “prolonging” and multiple-factor-caused “loss”

  • 摘要: 放射性同位素210Pb适于百年尺度的定年和沉积速率计算,已经在冰芯、土壤、湖泊、水库、河口、潮滩、潟湖、海湾和浅海陆架等多种环境得到广泛应用。目前,210Pb测年方法的应用有两种现象值得注意:一种是“延年”,即根据测算的沉积速率回溯定年的时间,有时回溯的时间跨度可达二、三百年;另一种是“折寿”,即根据测算的表观沉积速率计算得到的210Pb本底层位之上的时间跨度不足百年。根据210Pb测年的原理和有关仪器的检出限来分析,本文作者认为,210Pb直接定年的上限以110 yr~155 yr为宜。因此,“延年”的运用有一定的前提条件,即研究区的沉积环境在回溯的数百年尺度内应该保持稳定,同时回溯的定年结果最好有其他独立的定年方法(如历史文献记录或生物标志物等)来印证、以增加其可靠性。对于210Pb测年的“折寿”现象,可能的原因有四种。第一,沉积及取样的压实效应没有在分析和计算过程中得到校正。第二,210Pb活度测量的精度和不确定度影响了对本底的判断;为稳妥起见,研究者选定的本底层位一般会比真实的本底年龄要年轻一些,导致定年结果的时间跨度缩小。第三,210Pb定年计算模式决定了本底活度值的微小差异将带来计算出来的时间跨度产生显著差异。第四,沉积过程事实上发生了后期的侵蚀和迁移,导致保存在柱样中的沉积记录不完整。为了有效地减少210Pb测年法的结果误差,可以采取减小210Pb活度测量子样的间距、并同步测量226Ra活度等技术手段;另外,在计算时应该使用沉积通量而不是表观沉积速率。我们相信,210Pb测年方法的正确运用和解译将对物源判断、沉降后的侵蚀和扰动等问题提供一些有益的信息。
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  • 收稿日期:  2018-01-05
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