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Organic carbon in water, particulate matter, and upper layer of bottom sediments of the central part of the Kara Sea

机译:卡拉海中部的水中的有机碳,颗粒物和底部沉积物的上层

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摘要

Based on data obtained in the course of the 59th cruise of RV Akademik Mstislav Keldysh, the content of organic carbon was determined in water (dissolved organic carbon, DOC), particulate matter (particulate organic carbon, POC), and bottom sediments of the Yenisei estuary and of the central part of the Kara Sea during the summer-autumn season of 2011. The decisive impact of the waters of riverine runoff upon the variability of DOC and POC concentrations in the marine aquatic area is shown. POC enrichment in the autochthonous component is revealed for the frontal zones, as well as the increase of DOC concentrations in the area of the northern extremity of the Novaya Zemlya Islands. The distribution map of organic carbon (C-org) in the upper layer of bottom sediments of the central part of the Kara Sea is plotted on the basis of the analysis of the authors' and published data. A pronounced enrichment of the thin upper layer (0-0.5 cm) of bottom sediments in organic carbon (> 20%) is registered at most of the stations and depends neither on lithological composition of sediments nor on the location of sampling sites.
机译:根据第59轮RV Akademik Mstislav Keldysh航行中获得的数据,确定水(溶解的有机碳,DOC),颗粒物(颗粒有机碳,POC)和叶尼塞河底部沉积物中的有机碳含量图为2011年夏秋季节的河口和卡拉海中部地区。显示了河流径流水域对海洋水域DOC和POC浓度变化的决定性影响。额叶区域的原生质成分中的POC富集以及Novaya Zemlya群岛北端区域的DOC浓度增加。在对作者和发表的数据进行分析的基础上,绘制了卡拉海中部底部沉积物上层中有机碳的分布图(C-org)。在大多数测站中,有机碳(> 20%)中底部沉积物的薄上层(0-0.5 cm)有明显的富集,既不取决于沉积物的岩性组成,也不取决于采样点的位置。

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