珠江口沉积地球化学特征与古环境演化过程

王珊珊; 曹志敏; 兰东兆; 郑志昌

doi:10.3799/dqkx.2010.026

珠江口沉积地球化学特征与古环境演化过程

doi: 10.3799/dqkx.2010.026

王珊珊^1,,
曹志敏²,
兰东兆^{2, 3},
郑志昌⁴

1.
浙江省水利河口研究院, 浙江杭州 310020
2.
中国海洋大学海洋地球科学学院, 山东青岛 266100
3.
国家海洋局第三海洋研究所, 福建厦门 590100
4.
国土资源部广州海洋地质调查局, 广东广州 510760

基金项目:

国家海洋局"908"专项"重要三角洲演变规律及重大事件的沉积记录与可持续发展研究" No.908-02-02-05

详细信息

作者简介:
王珊珊(1980-), 女, 博士, 主要从事海洋环境地质学和海洋工程研究.E-mail: shanshwang@gmail.com

中图分类号: P628;P59
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- 被引次数: 0
出版历程
- 收稿日期: 2009-02-15
- 刊出日期: 2010-03-01

Geochemical Characteristics of Sediment of Pearl River Estuary and Its Paleoenvironmental Evolution

1.
Zhejiang Institute of Hydraulics & Estuary, Hangzhou 310020, China
2.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
3.
Third Institute of Oceanography, SOA, Xiamen 590100, China
4.
Guangzhou Marine Geological Survey, Ministry of Land and Resources, Guangzhou 510760, China

摘要

摘要: 利用ICP-AES法和重铬酸钾氧化还原容量法测定珠江口沉积物中的微量元素和总有机质含量, 结合沉积物粒度参数, 采用因子分析方法识别控制沉积物化学组成和元素行为的3个因子: 流域侵蚀因子、表生沉积作用控制因子和海洋环境控制因子.研究发现, 3个控制因子的得分曲线基本反映了该地区气候干湿、冷暖的强弱变化, 可作为恢复古气候环境的代用曲线; 在本岩心所代表的沉积年代中共有5次较为明显的环境变化, 为深入研究珠江三角洲区域古环境、古气候演化提供了重要的参考依据.
- 珠江口 /
- 因子分析 /
- 地球化学 /
- 古环境
Abstract: The trace metal elements and average grain size were determined for sediments of Pearl River Estuary and three important factors were identified using factor analysis method, which controls chemical compositions of sediments, such as catchment erosion, biogenic deposit, marine dominated condition. Moreover, further research indicates that the factor score curves of the three factors can be used to represent the changes of humidity, temperature and the hydrodynamics, respectively, which provides a good effective approach to paleoenviromental reconstruction. On the basis of the study, the evolution history of the regional climate and environment is evaluated and it is revealed that the basic climate succession in the region of Pearl River Delta is the cool-humid, cool-dry, warm-dry, warm-dry, warm-humid and warm-dry successively.
- Pearl River Estuary /
- factor analysis /
- geochemistry /
- paleoenvironment

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图 1 研究区环境和采样站位图

Fig. 1. Setting and sampling station of core ZXZ2

下载: 全尺寸图片幻灯片

图 2 沉积柱地球化学和粒度参数指标垂直剖面图

Fig. 2. Vertical profiles of chemical elements and mean grain size in the sediments of core ZXZ2

下载: 全尺寸图片幻灯片

图 3 珠江口ZXZ2孔沉积物因子得分曲线图

Fig. 3. Curves of factor scores of sediments of core ZXZ2

下载: 全尺寸图片幻灯片

表 1 因子分析结果

Table 1. Results of factor analysis

公因子	变量及公因子负载	方差贡献(%)
F₁	Co 0.873 Cu 0.906 Ni 0.925 Zn 0.807 Cr 0.628 平均粒径 0.710	42.06
F₂	Sr 0.885 Ba 0.949	21.95
F₃	Zr 0.748 有机质 -0.937	21.58

下载: 导出CSV

表 2 沉积物因子得分

Table 2. Factor scores of sediments of core ZXZ2

编号	深度(m)	F₁因子	F₂因子	F₃因子
1	0.0~0.2	0.814	1.005	0.561
2	0.2~0.4	0.714	-0.473	1.197
3	0.4~0.6	0.995	-0.137	2.616
4	0.6~0.8	1.720	0.351	-0.090
5	0.8~1.0	0.482	-0.245	-0.046
6	1.0~1.2	0.252	0.272	-0.962
7	1.2~1.4	-0.145	0.720	-0.318
8	1.4~1.6	-0.356	0.495	-0.552
9	1.6~1.8	-0.380	0.082	-0.242
10	1.8~2.0	0.134	0.241	-1.359
11	2.0~2.2	-0.488	0.418	-0.566
12	2.2~2.4	-0.523	1.597	-0.155
13	2.4~2.6	-2.109	-0.342	1.076
14	2.6~2.8	-1.899	-1.134	0.486
15	3.0~3.2	0.839	-2.920	-1.008
16	3.3~3.5	-0.052	0.070	-0.639

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参考文献(40)

[1]	Chen, J.A., Wan, G.J., Chen, Z.L., et al., 1999. Chemical elements in sediments of Lake Erhai and palaeoclimate evolution. Geochimica, 28(6): 562-570 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-DQHX199906005.htm
[2]	Chen, J.A., Wan, G.J., Huang, R.G., 1998. Geochemical phases and pollution history of heavy metals in sediments of Lake Erhai. Geology Geochemistry, 26(2): 1-8 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZDQ199802000.htm
[3]	Dypvik, H., Harris, N.B., 2001. Geochemical facies analysis of fine-grained siliciclastics using Th/U, Zr/Rb and (Zr+Rb)/Sr ratios. Chemical Geology, 181(1-4): 131-146. doi: 10.1016/S0009-2541(01)00278-9
[4]	Huang, B.Q., Jian, Z.M., Zhao, Q.H., et al., 2005. Variations in deep-water masses from the northern South China Sea since the Late Pliocene. Earth Science—Journal of China University of Geosciences, 30(5): 529-533 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200505002.htm
[5]	Jiang, F.Q., Li, A.C., Li, T.G., 2002. Geochemical characteristics for core sediments of the southern Okinawa trough and their paleoenvironment implication. Marine Geology & Quaternary Geology, 22(3): 11-17 (in Chinese with English abstract). http://www.researchgate.net/publication/311962723_Geochemical_characteristics_for_core_sediments_of_the_southern_Okinawa_trough_and_their_paleoenvironment_implication
[6]	Li, P.R., Qiao, P.N., Zheng, H.H., et al., 1991. Envolution of Zhujiang Delta in the past 10 000 years. Ocean Press, Beijing (in Chinese).
[7]	Li, X.M., 1997. Sedimentary characteristics of the Dalianpao sediment in southern Liaoning and its paleoenvironment changes. Acta Sedimentologica Sinica, 15(1): 80-84 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB701.014.htm
[8]	Liu, Y.J., 1984. Element geochemistry. Science Press, Beijing (in Chinese).
[9]	Luo, C.X., Pan, A.D., Shi, R.Q., 2005. The environmentary significance of granularity of the Quaternary sediments in Jiangcun ZK2 core of the Pearl River Delta. Journal of Stratigraphy, 29(Suppl. ): 631-634 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DCXZ2005S1031.htm
[10]	Luo, C., Peng, Z.C., Liu, W.G., et al., 2008. Evidence from the lacustrine sediments of Lop-Nur Lake, North west China for the Younger Dryas event. Earth Science—Journal of China University of Geosciences, 33(2): 190-196 (in Chinese with English abstract). doi: 10.3799/dqkx.2008.025
[11]	Ma, Y.J., Liu, C.Q., 1999. Trace element geochemistry in chemical weathering. Chinese Science Bulletin, 44(22): 2433-2437 (in Chinese). doi: 10.1360/csb1999-44-22-2433
[12]	Meng, X.W., Du, D.W., Cheng, Z.B., 2001. Trace elemental and Sr-Nd isotopic geochemistry of foraminifera shell of the Okinawa Trough. Acta Oceanologica Sinica, 23(2): 62-68 (in Chinese with English abstract). http://www.cqvip.com/Main/Detail.aspx?id=5024568
[13]	Nechaev, V.P., Isphording, W.C., 1993. Heavy-mineral assemblages of continental margins as indicators of plate-tectonic environments. Journal of Sedimentary Research, 63(6): 1110-1117. http://www.onacademic.com/detail/journal_1000036006494310_43d1.html
[14]	Shi, Y.F., Yu, G., 2003. Warm-humid climate and transgressions during 40-30 ka BP and their potential mechanisms. Quaternary Sciences, 23(1): 1-11 (in Chinese with English abstract). http://www.cqvip.com/main/zcps.aspx?c=1&id=7532765
[15]	Xu, F.J., Li, A.C., Wan, S.M., et al., 2009. Terrigenous mineral constrains on the grain-size distribution and geochemical composition of sediments in the inner shelf of the East China Sea. Earth Science—Journal of China University of Geosciences, 34(4): 614-622 (in Chinese with English abstract).
[16]	Yang, X.W., Wang, W.J., 1994. A statistical study on hydrodynamic sedimentation and sand movement Huangmaohai estuary bay. The Ocean Engineering, 12(4): 42-51 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYGC404.005.htm
[17]	Yu, G., 1997.1997 international paleoclimate summer meeting hot points: mid-Holocene Epoch and last ice age of China. Chinese Science Bulletin, 42(17): 1903-1904 (in Chinese). doi: 10.1360/csb1997-42-17-1903
[18]	Zeng, J.H., Zhang, S.W., Qiu, N.S., et al., 2002. Degree of oil-gas charged in lens-shaped sand body in Jiyang depression and its main controlling factors. Earth Science—Journal of China University of Geosciences, 27(6): 729-732 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200206012.htm
[19]	Zhang, H.L., 1994. Math geology. Metallurgical Industry Press, Beijing (in Chinese).
[20]	Zhao, Y.Y., Yan, M.C., 1994. Geochemistry of Sediments of the China shelf sea. Science Press, Beijing (in Chinese).
[21]	Zhu, G.W., Chen, Y.X., 2001. A review of geochemical behaviors and environmental effects of organic matter in sediments. Journal of Lake Science, 13(3): 272-279 (in Chinese with English abstract). doi: 10.18307/20010312
[22]	陈敬安, 万国江, 陈振楼, 等, 1999. 洱海沉积物化学元素与古气候演化. 地球化学, 28(6): 562-570. doi: 10.3321/j.issn:0379-1726.1999.06.006
[23]	陈敬安, 万国江, 黄荣贵, 1998. 洱海沉积物重金属地球化学相及污染历史研究. 地质地球化学, 26(2): 1-8. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ199802000.htm
[24]	黄宝琦, 翦知民, 赵泉鸿, 等, 2005. 晚上新世以来南海北部深部水团演化. 地球科学——中国地质大学学报, 30(5): 529-533. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200505002.htm
[25]	蒋富清, 李安春, 李铁刚, 2002. 冲绳海槽南部柱状沉积物地球化学特征及其古环境意义. 海洋地质与第四纪地质, 22(3): 11-17. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200203002.htm
[26]	李平日, 乔彭年, 郑洪汉, 等, 1991. 珠江三角洲一万年来环境演变. 北京: 海洋出版社.
[27]	李雪铭, 1997. 辽南大莲泡沉积物的沉积特征及古环境变化. 沉积学报, 15(1): 80-84. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB701.014.htm
[28]	刘英俊, 1984. 元素地球化学. 北京: 科学出版社.
[29]	罗传秀, 潘安定, 施汝权, 2005. 珠江三角洲江村ZK2钻孔沉积物粒度的环境意义. 地层学杂志, 29(增刊): 631-634. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ2005S1031.htm
[30]	罗超, 彭子成, 刘卫国, 等, 2008. 新仙女木事件在罗布泊湖相沉积物中的记录. 地球科学——中国地质大学学报, 33(2): 190-196. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200802006.htm
[31]	马英军, 刘丛强, 1999. 化学风化作用中的微量元素地球化学——以江西龙南黑云母花岗岩风化壳为例. 科学通报, 44(22): 2433-2437. doi: 10.3321/j.issn:0023-074X.1999.22.015
[32]	孟宪伟, 杜德文, 程振波, 2001. 冲绳海槽有孔虫壳体的微量元素Sr、Nd同位素地球化学. 海洋学报, 23(2): 62-68. doi: 10.3321/j.issn:0253-4193.2001.02.010
[33]	施雅风, 于革, 2003.40~30 ka BP中国暖湿气候和海侵的特征与成因探讨. 第四纪研究, 23(1): 1-11. doi: 10.3321/j.issn:1001-7410.2003.01.001
[34]	徐方建, 李安春, 万世明, 等, 2009. 东海内陆架陆源物质矿物组成对粒度和地球化学成分的制约. 地球科学——中国地质大学学报, 34(4): 614-622. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200904007.htm
[35]	杨雪舞, 王文介, 1994. 珠江口黄茅海河口湾水动力沉积和泥沙运动的统计研究. 海洋工程, 12(4): 42-51. https://www.cnki.com.cn/Article/CJFDTOTAL-HYGC404.005.htm
[36]	于革, 1997.1997年夏国际古气候会议的热点之一: 中国的中全新世和末次盛冰期. 科学通报, 42 (17): 1903-1904. doi: 10.3321/j.issn:0023-074X.1997.17.035
[37]	曾溅辉, 张善文, 邱楠生, 等, 2002. 济阳坳陷砂岩透镜体油气藏充满度大小及其主控因素. 地球科学——中国地质大学学报, 27(6): 729-732. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200206012.htm
[38]	张华良, 1994. 数学地质. 北京: 冶金工业出版社.
[39]	赵一阳, 鄢明才, 1994. 中国浅海沉积物地球化学. 北京: 科学出版社.
[40]	朱广伟, 陈英旭, 2001. 沉积物中有机质的环境行为研究进展. 湖泊科学, 13(3): 272-279. doi: 10.3321/j.issn:1003-5427.2001.03.012