globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6448490
论文题名:
用南黄海沉积岩心中氮同位素重建海水营养盐利用率的历史变化
其他题名: Historical changes of nutrient utilization of seawater reconstructed with nitrogen isotopes in sedimentary cores from the southern Yellow Sea
作者: 蔡德陵1; 杨庶2; 王玉堃3; 杨茜3; 孙耀3
刊名: 海洋学报
ISSN: 0253-4193
出版年: 2019
卷: 41, 期:2, 页码:855-863
语种: 中文
中文关键词: 沉积岩心 ; 南黄海 ; 营养盐利用率
英文关键词: C/N ; delta~(15) N ; sediment core ; the southern Yellow Sea ; C/N ; delta~(15) N ; nutrient usability
WOS学科分类: GEOLOGY
WOS研究方向: Geology
中文摘要: 基于2006年黄东海航次获得的表层沉积物和2009年航次南黄海3个柱状沉积物岩心,分析了表层沉积物总氮(TN)、C/N比值和氮稳定同位素比值(delta~(15) N)的分布特征及南黄海柱状沉积物中这些参数的长期变化规律。结果表明,黄海、东海表层沉积物TN含量、C/N比值和delta~(15) N的变化范围分别为0.023%~0.33%、1.4~50.3和4.0~16.0。其中,TN与C/N比值存在较显著的负相关性,而TN与delta~(15) N以及C/N比值与delta~(15) N之间无明显的相关性,这反映出黄海和东海陆架边缘海中氮循环的复杂性。对南黄海柱状沉积物的分析结果表明:3个柱状岩心中的TN、C/N比值和delta~(15) N随年代的波动均呈现一定的周期性变化趋势。3个岩心中TN随年代的变化趋势基本一致,100a来总体呈波动上升趋势,且3个岩心中C/N比值也呈较为类似的变化趋势。柱状沉积物中delta~(15) N的平均变化周期约为24a左右。由此,重建200a来南黄海海水中营养盐利用率的历史变化,并初步探讨了其对气候变化的响应。
英文摘要: The distributions of total nitrogen(TN),C/N,and nitrogen stable isotope ratio(delta~(15) N)in surface sediments are first studied in the Yellow Sea and East China Sea.The content of TN in surface sediment ranges from 0.023%to 0.33%,while C/N anddelta~(15) N are about 1.4-50.3and 4.0-16.0respectively.Significant negative correlation exists between TN and C/N,and no correlation is found between TN anddelta~(15) N or between C/N anddelta~(15) N.These relationships reflect the complexity of the nitrogen cycles in the Yellow Sea and the East China Sea,both belonging to typical continental shelf marginal sea.Then,three sediment cores collected from the southern Yellow Sea were analyzed for TN,C/N anddelta~(15) N values.And the long-term change trends of TN,C/N and delta~(15) N were subsequently rebuilt combing with 210Pb chronological study.The results indicate that the long-term changes of TN,C/N anddelta~(15) N show some periodical trends.The temporal changes of TN show similar change trends in the three sea areas,with generally increasing trends over the past 100years.And C/N trends also follow relatively similar patterns in the three sediment cores,while the average cycle ofdelta~(15) N is about 24years.Finally, the historical changes of nutrient usability in the upper water of the southern Yellow Sea over the past 200years are reconstructed,and their responses to climate change are discussed preliminarily.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/155801
Appears in Collections:气候变化事实与影响

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作者单位: 1.中国水产科学研究院黄海水产研究所
2.自然资源部第一海洋研究所, 农业农村部海洋渔业可持续发展重点实验室
3., 青岛
4.青岛, 山东
5.山东 266071
6.266061, 中国
7.中国水产科学研究院黄海水产研究所
8.山东大学海洋研究院, 农业农村部海洋渔业可持续发展重点实验室
9., 青岛
10.青岛, 山东
11.山东 266071
12.266237, 中国
13.中国水产科学研究院黄海水产研究所, 农业农村部海洋渔业可持续发展重点实验室, 青岛, 山东 266071, 中国

Recommended Citation:
蔡德陵,杨庶,王玉堃,等. 用南黄海沉积岩心中氮同位素重建海水营养盐利用率的历史变化[J]. 海洋学报,2019-01-01,41(2):855-863
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