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西北冰洋表层沉积物中生源和陆源粗组分及其沉积环境

, PP. 103-114

Keywords: 表层沉积物,生源与陆源粗组分,表层生产力与冰筏碎屑,沉积环境,北冰洋西部

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Abstract:

通过中国第1至第3次北极科学考察在北冰洋西部所采集的99个表层沉积物中生源与陆源粗组分的分析,研究了该海域表层生产力的变化,有机质来源以及陆源粗颗粒物质的输入方式和影响因素。研究区域生源组分所反映的表层生产力变化与通过白令海峡进入楚科奇海的3股太平洋洋流密切相关。楚科奇海西侧高盐高营养盐的阿纳德尔流流经区域,表层生产力普遍较高;东侧低盐低营养盐阿拉斯加沿岸流流经区域,浮游硅质生物生产力低,并且受陆源有机质输入影响显著。阿尔法脊和楚科奇海台较高的浮游钙质生物生产力与北大西洋水的注入密切相关。楚科奇海陆架区低的浮游钙质生物生产力与陆源物质的稀释作用和浮游钙质生物生活水深有关;加拿大海盆区低的浮游钙质生物生产力主要受到碳酸钙溶解作用的影响。研究区域表层沉积物中的陆源粗组分-冰筏碎屑(ice-rafteddetritus,IRD)的分布主要受海冰和冰山的搬运,陆缘冰输入,河流输入以及太平洋入流水的影响。白令海峡入口处的陆源粗颗粒沉积主要受太平洋入流水影响;阿拉斯加近岸海域的陆源粗颗粒沉积来自于陆缘冰以及河流的输入;而北风脊高的IRD含量主要是由海冰和冰山所携带,被波弗特环流搬运至此,伴随着海冰和冰山的融化并卸载进入沉积物中。

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