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西太平洋马尔库斯-威克海山区沉积物中生物硅含量分布
引用本文:孟凡盛,倪建宇,姚旭莹. 西太平洋马尔库斯-威克海山区沉积物中生物硅含量分布[J]. 海洋学研究, 2019, 37(4): 60-67. DOI: 10.3969/j.issn.1001-909X.2019.04.006
作者姓名:孟凡盛  倪建宇  姚旭莹
作者单位:自然资源部第二海洋研究所,浙江杭州310012;国家海洋局海底科学重点实验室,浙江杭州310012;自然资源部第二海洋研究所,浙江杭州310012;国家海洋局海底科学重点实验室,浙江杭州310012;自然资源部第二海洋研究所,浙江杭州310012;国家海洋局海底科学重点实验室,浙江杭州310012
基金项目:中国大洋矿产资源研究与开发专项基金资助(DY135-S1-1-08)
摘    要:分析了大洋40航次在西太平洋马尔库斯-威克海山区山间海盆采集的表层沉积物中生物硅和有机质的含量,并对其分布特征和来源进行了初步的研究。结果表明,马尔库斯-威克海山区附近海域深海表层沉积物中生物硅含量总体较低,含量在0.88%~12.41%之间,平均含量为2.19%,分布上呈现西南含量高,向东北方向递减的趋势;深海表层沉积物中有机碳含量较低,δ13C同位素组成分布与生物硅相同。沉积物柱状样的研究表明研究区在过去的100~200 ka期间表层水体中硅质生物的初级生产力是逐渐增加的。

关 键 词:西太平洋  生物硅  沉积物
收稿时间:2019-03-18

Biogenic silica content and distribution in deep sea sediments at Marcus-Wake Seamounts area in the western Pacific Ocean
MENG Fan-sheng,NI Jian-yu,YAO Xu-ying. Biogenic silica content and distribution in deep sea sediments at Marcus-Wake Seamounts area in the western Pacific Ocean[J]. Journal of Marine Sciences, 2019, 37(4): 60-67. DOI: 10.3969/j.issn.1001-909X.2019.04.006
Authors:MENG Fan-sheng  NI Jian-yu  YAO Xu-ying
Affiliation:1. Second Institute of Oceanography, MNR, Hangzhou 310012, China;2. Key Laboratory of Submarine Geosciences, SOA, Hangzhou 310012, China
Abstract:In this study, the content of bio-silicon and organic matter in the surface sediments were analyzed, which were collected by the Ocean 40 voyage in the mountain basin of the Marcus-Wick Sea area in the western Pacific, and the preliminary research on its distribution characteristics and sources were also conducted. The results show that the content of bio-silicon in the deep sea surface sediments near the Marcus-Wicker Sea area is generally low, ranging from 0.88% to 12.41%, with an average content of 2.19%. The distribution shows a high content in the southwest and a diminishing trend toward the northeast. The content of organic carbon in the surface sediments is low, and the distribution of δ13C is the same as that of bio-silicon. Sediment core studies show that the primary production of siliceous organisms in the surface waters of the study area during the past 100-200 ka is gradually increasing.
Keywords:western Pacific Ocean  biogenic silica  sediments  
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