南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录

李小艳

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录

李小艳

文章导航 > 沉积学报 > 2011 > 29(3): 572-579

李小艳. 南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录[J]. 沉积学报, 2011, 29(3): 572-579.

引用本文:

李小艳. 南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录[J]. 沉积学报, 2011, 29(3): 572-579.

LI Xiaoyan. Evolutionary Paleoceanographic Characteristics in the Northern South China Sea Since Late Pleistocene: Evidence from Core N31[J]. Acta Sedimentologica Sinica, 2011, 29(3): 572-579.

Citation:

LI Xiaoyan. Evolutionary Paleoceanographic Characteristics in the Northern South China Sea Since Late Pleistocene: Evidence from Core N31[J]. Acta Sedimentologica Sinica, 2011, 29(3): 572-579.

李小艳. 南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录[J]. 沉积学报, 2011, 29(3): 572-579.

引用本文:

李小艳. 南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录[J]. 沉积学报, 2011, 29(3): 572-579.

Citation:

南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录

李小艳

海洋沉积与环境地质国家海洋局重点实验室山东青岛 266061

详细信息

通讯作者:
李小艳

计量

文章访问数: 2031
HTML全文浏览量: 25
PDF下载量: 1207
被引次数: 0

Evolutionary Paleoceanographic Characteristics in the Northern South China Sea Since Late Pleistocene: Evidence from Core N31

LI Xiaoyan

Key Lab of Marine Sedimentology and Environmental Geology, SOA, Qingdao Shandong 266061

More Information

Corresponding author: LI Xiaoyan

摘要

摘要: 对南海北部N31柱状样沉积物进行了浮游有孔虫定量分析鉴定、氧碳同位素、碳酸盐含量和粒度测试以及AMS14C测年，并采用古生态转换函数计算了表层海水古温度和温跃层深度，揭示了该海区约55 ka以来的古海洋环境特征。转换函数计算的表层海水古温度结果表明，夏季温度的变化范围为27.0~29.6℃，变化幅度为2.6℃，冬季温度变化范围为18.2~27.0℃，变化幅度为8.8℃。与南海南部转换函数温度对比表明，南海南部的温度比南海北部要高，这种差异在冬季时表现更为突出。温跃层转换函数计算的温跃层深度结果表明，MIS3~MIS2期时温跃层深度没有大的变化，而从冰期向冰后期过渡时，温跃层深度逐渐增大。
- 古海洋环境浮游有孔虫晚更新世南海
Abstract: The South China Sea is the largest marginal sea in the western Pacific Ocean and its' north and south are wide continental shelf. There are many rivers flow into the South China Sea. The highresolution sediment records abundant environmental information of land and sea. This area has become one of hotspots on paleoceanography research and made a lot of research results. Planktonic foraminifera are very sensitive to changes of marine environment. Sea water temperature changes can directly affect the migration and succession of biota. Therefore, research the distribution of planktonic foraminifera in core sediment to analyze the evolution of paleoclimate. In this paper, a sediment Core N31 located in the northern South China Sea had been researched including quantitative analysis and identification of planktonic foraminifera, oxygen and carbon isotopes, carbonate content and grain size, AMS14C dating, sea surface temperature and thermocline depth calculated by paleoecological transfer function. The following conclusions have been attained:
1) The bottom age of Core N31 was about 55ka BP and this core accepted deposition since marine isotope stage 3.
2) Planktonic foraminifera species analysis showed that changes in abundance as the glacialinterglacial cycles and change. Tropical and subtropical species appeared in lager numbers in interglacial and its maximum percentage in MIS3 or MIS1, but temperate species appeared in larger numbers in the glacial period.
3) The sea surface temperature (SST) estimated by the transfer function FP12E shows that the summer SST ranges from 27.0 to 29.6℃ and the winter SST from 18.2 to 27.0℃. The comparison of SST data between the southern and northern SCS shows that SST in the southern SCS is higher than that in the northern SCS. The SST difference is more obvious in winter.
4) The thermocline data show no obvious fluctuations during MIS3MIS2, but the depth deepened gradually during the transitional period from the glacial to the postglacial.
- paleoceanography

HTML全文

参考文献(0)

[1]	葛小瞳, 汪远征, 陈代钊, 张恭境, 黄泰誉, 李王鹏. 川东北地区二叠纪晚期古海洋环境与有机质富集 . 沉积学报, 2024, 42(3): 757-773. doi: 10.14027/j.issn.1000-0550.2023.115
[2]	刘欣宇, 李永祥. 晚塞诺曼期东特提斯洋古海洋环境探析 . 沉积学报, 2021, 39(5): 1171-1184. doi: 10.14027/j.issn.1000-0550.2020.045
[3]	徐承芬, 张勇, 孔祥淮, 胡刚, 毕世普, 牟秀娟, 宁泽, 张晓波. 闽北近岸海域晚更新世以来沉积地层特征及其演化 . 沉积学报, 2020, 38(2): 331-339. doi: 10.14027/j.issn.1000-0550.2019.095
[4]	郭沫贞, 吕福亮, 侯福斗, 李林, 杨涛涛, 李东. 东爪哇盆地抱球虫灰岩浮游有孔虫组成及指相意义 . 沉积学报, 2020, 38(4): 747-758. doi: 10.14027/j.issn.1000-0550.2019.070
[5]	高胜美, 卓海腾, 王英民, 王星星, 贾凯育, 周伟. 南海北部白云峡谷群富有孔虫砂层沉积特征及发育机制 . 沉积学报, 2019, 37(4): 798-811. doi: 10.14027/j.issn.1000-0550.2018.187
[6]	杨向荣, 严德天, 张利伟, 张宝, 徐翰文, 刘文慧, 郧嘉琳. 赫南特冰期古海洋环境转变及其成因机制研究现状 . 沉积学报, 2018, 36(2): 319-332. doi: 10.14027/j.issn.1000-0550.2018.037
[7]	王鹏万, 斯春松, 张润合, 李娴静, 马立桥, 黄羚, 徐云俊, 鲁慧丽. 滇黔北坳陷寒武系碳酸盐岩古海洋环境特征及地质意义 . 沉积学报, 2016, 34(5): 811-818. doi: 10.14027/j.cnki.cjxb.2016.05.001
[8]	于革, 叶良涛, 廖梦娜. 晚更新世江苏海岸带沉积分布模拟研究 . 沉积学报, 2016, 34(4): 670-678. doi: 10.14027/j.cnki.cjxb.2016.04.007
[9]	杨剑萍, 庞效林, 王海峰, 贾军涛, 刘玲. 山东广饶地区晚更新世以来沉积演化与古气候变迁 . 沉积学报, 2016, 34(1): 79-89. doi: 10.14027/j.cnki.cjxb.2016.01.007
[10]	蓝先洪, 秦亚超, 王中波, 陈晓辉, 密蓓蓓, 黄龙. 渤海东部晚更新世以来的沉积物地球化学特征 . 沉积学报, 2016, 34(5): 892-901. doi: 10.14027/j.cnki.cjxb.2016.05.008
[11]	. 南海北部近6 Ma以来中层水体演化的底栖有孔虫证据 . 沉积学报, 2014, 32(3): 527-536.
[12]	王利波, 李军, 陈正新, 赵京涛, 白凤龙, 胡邦琦, 窦衍光, 翟滨. 晚更新世以来台湾浅滩西部地层结构与古环境演化 . 沉积学报, 2014, 32(6): 1089-1099.
[13]	周开胜. 长江口北支有孔虫组合及其环境意义 . 沉积学报, 2009, 27(2): 334-342.
[14]	程红光. 龙门山地区早泥盆世古海洋环境——来自腕足类壳体的地球化学证据 . 沉积学报, 2008, 26(6): 897-903.
[15]	张强, 朱诚, 房迎三. 宁镇地区中更新世环境演变的沉积学研究 . 沉积学报, 2002, 20(2): 307-313.
[16]	章伟艳, 张富元, 陈荣华, 张霄宇. 南海深水区晚更新世以来沉积速率、沉积通量与物质组成 . 沉积学报, 2002, 20(4): 668-674.
[17]	李玉成, 黄宝玉, 徐永昌. 利用贝类(Lamprotula)化石碳氧同位素再建山西丁村地区晚更新世气候环境 . 沉积学报, 2001, 19(4): 648-651.
[18]	秦蕴珊, 赵松龄. 晚更新世以来长江水下三角洲的沉积结构与环境变迁 . 沉积学报, 1987, 5(3): 105-112.
[19]	王开发, 蒋辉. 黄海晚更新世以来的硅藻组合及其沉积环境 . 沉积学报, 1987, 5(1): 94-103.
[20]	杨振强, 林甲兴. 从鄂西二叠纪碳酸盐岩微相探讨有孔虫的生态环境 . 沉积学报, 1983, 1(4): 93-105.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 2031
HTML全文浏览量: 25
PDF下载量: 1207
被引次数: 0

南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录

李小艳

海洋沉积与环境地质国家海洋局重点实验室山东青岛 266061

通讯作者: 李小艳

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2011-06-10

关键词:

古海洋环境浮游有孔虫晚更新世南海

摘要: 对南海北部N31柱状样沉积物进行了浮游有孔虫定量分析鉴定、氧碳同位素、碳酸盐含量和粒度测试以及AMS14C测年，并采用古生态转换函数计算了表层海水古温度和温跃层深度，揭示了该海区约55 ka以来的古海洋环境特征。转换函数计算的表层海水古温度结果表明，夏季温度的变化范围为27.0~29.6℃，变化幅度为2.6℃，冬季温度变化范围为18.2~27.0℃，变化幅度为8.8℃。与南海南部转换函数温度对比表明，南海南部的温度比南海北部要高，这种差异在冬季时表现更为突出。温跃层转换函数计算的温跃层深度结果表明，MIS3~MIS2期时温跃层深度没有大的变化，而从冰期向冰后期过渡时，温跃层深度逐渐增大。

English Abstract

Evolutionary Paleoceanographic Characteristics in the Northern South China Sea Since Late Pleistocene: Evidence from Core N31

LI Xiaoyan

Key Lab of Marine Sedimentology and Environmental Geology, SOA, Qingdao Shandong 266061

Corresponding author: LI Xiaoyan

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2011-06-10

Keywords:

paleoceanography

Abstract: The South China Sea is the largest marginal sea in the western Pacific Ocean and its' north and south are wide continental shelf. There are many rivers flow into the South China Sea. The highresolution sediment records abundant environmental information of land and sea. This area has become one of hotspots on paleoceanography research and made a lot of research results. Planktonic foraminifera are very sensitive to changes of marine environment. Sea water temperature changes can directly affect the migration and succession of biota. Therefore, research the distribution of planktonic foraminifera in core sediment to analyze the evolution of paleoclimate. In this paper, a sediment Core N31 located in the northern South China Sea had been researched including quantitative analysis and identification of planktonic foraminifera, oxygen and carbon isotopes, carbonate content and grain size, AMS14C dating, sea surface temperature and thermocline depth calculated by paleoecological transfer function. The following conclusions have been attained:
1) The bottom age of Core N31 was about 55ka BP and this core accepted deposition since marine isotope stage 3.
2) Planktonic foraminifera species analysis showed that changes in abundance as the glacialinterglacial cycles and change. Tropical and subtropical species appeared in lager numbers in interglacial and its maximum percentage in MIS3 or MIS1, but temperate species appeared in larger numbers in the glacial period.
3) The sea surface temperature (SST) estimated by the transfer function FP12E shows that the summer SST ranges from 27.0 to 29.6℃ and the winter SST from 18.2 to 27.0℃. The comparison of SST data between the southern and northern SCS shows that SST in the southern SCS is higher than that in the northern SCS. The SST difference is more obvious in winter.
4) The thermocline data show no obvious fluctuations during MIS3MIS2, but the depth deepened gradually during the transitional period from the glacial to the postglacial.

李小艳. 南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录[J]. 沉积学报, 2011, 29(3): 572-579.

引用本文:

李小艳. 南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录[J]. 沉积学报, 2011, 29(3): 572-579.

Citation:

全文HTML

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录

通讯作者:
李小艳

计量

Evolutionary Paleoceanographic Characteristics in the Northern South China Sea Since Late Pleistocene: Evidence from Core N31

Corresponding author: LI Xiaoyan

计量

目录

南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录

海洋沉积与环境地质国家海洋局重点实验室山东青岛 266061

通讯作者: 李小艳

English Abstract

Evolutionary Paleoceanographic Characteristics in the Northern South China Sea Since Late Pleistocene: Evidence from Core N31

Key Lab of Marine Sedimentology and Environmental Geology, SOA, Qingdao Shandong 266061

Corresponding author: LI Xiaoyan

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录

通讯作者: 李小艳

计量

出版历程

Evolutionary Paleoceanographic Characteristics in the Northern South China Sea Since Late Pleistocene: Evidence from Core N31

Corresponding author: LI Xiaoyan

计量

出版历程

目录

南海北部晚更新世以来的古海洋环境演化特征①——来自N31柱样的沉积记录

海洋沉积与环境地质国家海洋局重点实验室 山东青岛 266061

通讯作者: 李小艳

English Abstract

Evolutionary Paleoceanographic Characteristics in the Northern South China Sea Since Late Pleistocene: Evidence from Core N31

Key Lab of Marine Sedimentology and Environmental Geology, SOA, Qingdao Shandong 266061

Corresponding author: LI Xiaoyan

全文HTML

目录

友情链接

期刊在线

联系我们

通讯作者:
李小艳

海洋沉积与环境地质国家海洋局重点实验室山东青岛 266061