南海北部沉积物中浮游有孔虫<i>Globigerinoides ruber</i>壳体氧同位素指示的冬季表层海水温度

许慎栋; 陈文煌; 邓文峰; 贾国东

doi:10.16562/j.cnki.0256-1492.2016.02.012

南海北部沉积物中浮游有孔虫Globigerinoides ruber壳体氧同位素指示的冬季表层海水温度

doi: 10.16562/j.cnki.0256-1492.2016.02.012

详细信息

1. 中国科学院广州地球化学研究所, 广州 510640;

2. 广西大学海洋学院, 南宁 530004;

3. 广西大学珊瑚礁研究中心, 南宁 530004;

4. 同济大学海洋地质国家重点实验室, 上海 200092

作者简介:
许慎栋(1987-),男,主要从事海洋沉积和生物地球化学研究,E-mail:sdxu6379@163.com

基金项目:
国家重点基础研究发展计划项目(2009CB421206)
中图分类号: P736.22

WINTER SURFACE SEAWATER TEMPERATURE IN THE NORTHERN SOUTH CHINA SEA INDUCED FROM TEMPERATURE INDEX OF SHELL OXYGEN ISOTOPE OF GLOBIGERINOIDES RUBER

More Information

1. Guangzhou Institute of Geochemistry, Guangzhou 510640;

2. School of Marine Sciences, Guangxi University, Nanning 530004;

3. Coral Reef Research Center of China, Guangxi University, Nanning 530004;

4. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092

摘要: 有孔虫壳体的氧同位素值(δ¹⁸O)是由其生长时海水δ¹⁸O和温度决定的,在海水δ¹⁸O已知的情况下,可以由壳体的δ¹⁸O值估算海水温度。本文以南海北部沿岸地区9个站位的柱状沉积物中浮游有孔虫Globigerinoides ruber为研究对象,测试了其壳体的δ¹⁸O值。分别以相应站点夏季与冬季表层海水的实测δ¹⁸O值代入温度公式,估算了对应的夏季与冬季的海水温度值。然后把计算结果与World Ocean Atlas (WOA)数据库相应站点的海水温度数据作比较。结果表明,计算出的夏季海水温度与WOA的夏季温度有较大差别,而计算出的冬季海水温度则与WOA的冬季海水温度基本相当。这说明δ¹⁸O_ruber记录的是该区域冬季表层海水的温度,此区域内G.ruber这一属种的生产力和沉积通量在东亚冬季风盛行期间出现了最高值。
- 浮游有孔虫 /
- 氧同位素 /
- 表层海水温度 /
- 南海北部
Abstract: The oxygen isotope value (δ¹⁸O) of foraminiferal shell depends upon the δ¹⁸O and temperature of sea water. The seawater temperature, therefore, can be extracted from foraminiferal δ¹⁸O if the δ¹⁸O composition of sea water is known. In this paper, the planktonic foraminifera Globigerinoides ruber picked out from the nine sediment cores in the northern South China Sea were analyzed for δ¹⁸O. Using the published summer and winter sea water δ¹⁸O values at each site, we calculated the sea water temperature (T_ruber), and then comparison was made for T_ruber and the 0~30m water temperature download from the World Ocean Atlas (WOA) database. Our data shows that there is a large difference between T_WOA and T_ruber when summer water δ¹⁸O was used in calculation, however, the difference was in a reasonable range when winter water δ¹⁸O was used. It suggests that δ¹⁸O_ruber reflects better the temperature and δ¹⁸O composition of winter seawater, and further implies that the productivity and deposition flux of G.ruber may reach the maximum when the East Asian Winter Monsoon prevails.
- planktonic foraminifera /
- oxygen isotope /
- sea surface temperature /
- northern South China Sea

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南海北部沉积物中浮游有孔虫Globigerinoides ruber壳体氧同位素指示的冬季表层海水温度

doi: 10.16562/j.cnki.0256-1492.2016.02.012

1. 中国科学院广州地球化学研究所, 广州 510640;

2. 广西大学海洋学院, 南宁 530004;

3. 广西大学珊瑚礁研究中心, 南宁 530004;

4. 同济大学海洋地质国家重点实验室, 上海 200092

作者简介:
许慎栋(1987-),男,主要从事海洋沉积和生物地球化学研究,E-mail:sdxu6379@163.com

WINTER SURFACE SEAWATER TEMPERATURE IN THE NORTHERN SOUTH CHINA SEA INDUCED FROM TEMPERATURE INDEX OF SHELL OXYGEN ISOTOPE OF GLOBIGERINOIDES RUBER

1. Guangzhou Institute of Geochemistry, Guangzhou 510640;

2. School of Marine Sciences, Guangxi University, Nanning 530004;

3. Coral Reef Research Center of China, Guangxi University, Nanning 530004;

4. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092

计量

南海北部沉积物中浮游有孔虫Globigerinoides ruber壳体氧同位素指示的冬季表层海水温度

doi: 10.16562/j.cnki.0256-1492.2016.02.012

1. 中国科学院广州地球化学研究所, 广州 510640;

2. 广西大学海洋学院, 南宁 530004;

3. 广西大学珊瑚礁研究中心, 南宁 530004;

4. 同济大学海洋地质国家重点实验室, 上海 200092

作者简介:
许慎栋(1987-),男,主要从事海洋沉积和生物地球化学研究,E-mail:sdxu6379@163.com

English Abstract

WINTER SURFACE SEAWATER TEMPERATURE IN THE NORTHERN SOUTH CHINA SEA INDUCED FROM TEMPERATURE INDEX OF SHELL OXYGEN ISOTOPE OF GLOBIGERINOIDES RUBER

1. Guangzhou Institute of Geochemistry, Guangzhou 510640;

2. School of Marine Sciences, Guangxi University, Nanning 530004;

3. Coral Reef Research Center of China, Guangxi University, Nanning 530004;

4. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092

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南海北部沉积物中浮游有孔虫Globigerinoides ruber壳体氧同位素指示的冬季表层海水温度

doi: 10.16562/j.cnki.0256-1492.2016.02.012

1. 中国科学院广州地球化学研究所, 广州 510640; 2. 广西大学海洋学院, 南宁 530004; 3. 广西大学珊瑚礁研究中心, 南宁 530004; 4. 同济大学海洋地质国家重点实验室, 上海 200092

作者简介: 许慎栋(1987-),男,主要从事海洋沉积和生物地球化学研究,E-mail:sdxu6379@163.com

WINTER SURFACE SEAWATER TEMPERATURE IN THE NORTHERN SOUTH CHINA SEA INDUCED FROM TEMPERATURE INDEX OF SHELL OXYGEN ISOTOPE OF GLOBIGERINOIDES RUBER

1. Guangzhou Institute of Geochemistry, Guangzhou 510640; 2. School of Marine Sciences, Guangxi University, Nanning 530004; 3. Coral Reef Research Center of China, Guangxi University, Nanning 530004; 4. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092

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南海北部沉积物中浮游有孔虫Globigerinoides ruber壳体氧同位素指示的冬季表层海水温度

doi: 10.16562/j.cnki.0256-1492.2016.02.012

1. 中国科学院广州地球化学研究所, 广州 510640; 2. 广西大学海洋学院, 南宁 530004; 3. 广西大学珊瑚礁研究中心, 南宁 530004; 4. 同济大学海洋地质国家重点实验室, 上海 200092

作者简介: 许慎栋(1987-),男,主要从事海洋沉积和生物地球化学研究,E-mail:sdxu6379@163.com

English Abstract

WINTER SURFACE SEAWATER TEMPERATURE IN THE NORTHERN SOUTH CHINA SEA INDUCED FROM TEMPERATURE INDEX OF SHELL OXYGEN ISOTOPE OF GLOBIGERINOIDES RUBER

1. Guangzhou Institute of Geochemistry, Guangzhou 510640; 2. School of Marine Sciences, Guangxi University, Nanning 530004; 3. Coral Reef Research Center of China, Guangxi University, Nanning 530004; 4. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092

全文HTML

目录

链接

关于期刊

关于我们

1. 中国科学院广州地球化学研究所, 广州 510640;

2. 广西大学海洋学院, 南宁 530004;

3. 广西大学珊瑚礁研究中心, 南宁 530004;

4. 同济大学海洋地质国家重点实验室, 上海 200092

作者简介:
许慎栋(1987-),男,主要从事海洋沉积和生物地球化学研究,E-mail:sdxu6379@163.com

1. Guangzhou Institute of Geochemistry, Guangzhou 510640;

2. School of Marine Sciences, Guangxi University, Nanning 530004;

3. Coral Reef Research Center of China, Guangxi University, Nanning 530004;

4. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092

1. 中国科学院广州地球化学研究所, 广州 510640;

2. 广西大学海洋学院, 南宁 530004;

3. 广西大学珊瑚礁研究中心, 南宁 530004;

4. 同济大学海洋地质国家重点实验室, 上海 200092

作者简介:
许慎栋(1987-),男,主要从事海洋沉积和生物地球化学研究,E-mail:sdxu6379@163.com

1. Guangzhou Institute of Geochemistry, Guangzhou 510640;

2. School of Marine Sciences, Guangxi University, Nanning 530004;

3. Coral Reef Research Center of China, Guangxi University, Nanning 530004;

4. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092