台湾东黑潮主流区近千年来沉积物稀土元素的变化特征与来源

王越奇; 宋金明; 袁华茂; 李学刚; 李宁; 王启栋

doi:10.16562/j.cnki.0256-1492.2018041601

台湾东黑潮主流区近千年来沉积物稀土元素的变化特征与来源

1.
中国科学院海洋研究所海洋生态与环境科学重点实验室，青岛 266071

2.
中国科学院大学，北京 100049

3.
青岛海洋科学与技术国家实验室海洋生态与环境科学功能实验室，青岛 266237

4.
中国科学院海洋大科学研究中心，青岛 266071

基金项目:
深海专项(预研)“深海典型生境生物多样性与生态系统”(2016ASKJ14)；山东省-国家基金委联合基金“海洋生态环境变化的生物地球化学机制”(U1606404)；中国科学院创新先导专项项目“黑潮向近海生源要素的输送”(XDA11020102)

详细信息

作者简介: 王越奇(1992—)，女，博士生，从事海洋生物地球化学研究，E-mail：iocaswyq@163.com

通讯作者: 宋金明(1964—)，男，研究员，主要从事研究海洋生物地球化学，E-mail: jmsong@qdio.ac.cn

中图分类号: P736.4

蔡秋蓉编辑

收稿日期: 2018-04-16

修回日期: 2018-06-19

刊出日期: 2019-04-28

Variation in rare earth elements and provenances of the sediments along the Kuroshio mainstream to the east of Taiwan over the past millennium

1.
CAS Key Laboratory of Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

2.
University of Chinese Academy of Sciences, Beijing 100049, China

3.
Function Laboratory of Marine Ecology and Environmental Sciences, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China

4.
Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China

More Information

Corresponding author: SONG Jinming, jmsong@qdio.ac.cn

Received Date: 16 April 2018

Revised Date: 19 June 2018

Publish Date: 28 April 2019

摘要

摘要:
基于沉积物AMS¹⁴C定年，研究了近千年来台湾以东黑潮主流区沉积物的稀土元素组成变化特征及赋存形态，探讨了该区近千年来稀土来源。台湾东黑潮主流区近千年来沉积物中稀土元素总量平均为119.82μg/g，低于上陆壳和中国黄土的稀土元素平均含量，与冲绳海槽较为接近；轻重稀土元素比值平均为11.30，明显富集轻稀土，具有明显的陆源属性。研究区沉积物稀土元素对球粒陨石和上地壳标准化配分模式均表现为轻稀土富集重稀土相对亏损，且具有弱的Ce正异常。根据定年结果及稀土元素变化特征趋势将柱状沉积物分为3层：0~8.5、8.5~21.5和21.5~30cm，随深度增加稀土元素总量的平均值逐渐增大，轻重稀土元素比值逐渐减小，Ce正异常程度逐渐减弱。稀土元素赋存形态分析表明，La、Ce、Pr、Nd 4种轻稀土元素主要为天然陆源，其他稀土元素受氧化还原环境影响相对较大。稀土元素主要存在于残渣态中，其次为铁锰氧化物结合态，残渣态对台湾以东黑潮主流区沉积物中总稀土元素的配分模式起决定性作用，也是造成Ce正异常的关键赋存形态。近千年来沉积物中稀土元素变化与沉积物粒度关系不大，物质来源较为稳定，台湾东部河流输入是研究区沉积物中稀土元素的最重要来源，亚洲大陆风尘输送对稀土元素的贡献较小。
- 稀土元素 /
- 物源 /
- 形态 /
- 沉积物 /
- 台湾东黑潮主流区
Abstract:
Rare earth elements (REE) and their fractions in the sediments of Kuroshio mainstream off eastern Taiwan were determined to reveal the REE geochemical characteristics and provenances of the sediments for the past millennium. AMS¹⁴C is used for dating. The average ratio of light REE to heavy REE (LREE/HREE) is 11.30 in the sediments of research core, obviously enriched in light REE. The average total REE content is 119.82 ppm, which was under the REE abundance of upper continental crust (UCC) and China loess, and close to the figure of Okinawa Trough. The chondrite-normalized REE patterns and the UCC-normalized REE patterns show a similar trend: light REE enriched with slightly positive Ce anomalies. The research core may be subdivided into three layers according to the chronohorizon and variation trend of REE: 0~8.5cm, 8.5~21.5cm, 21.5~30cm respectively. The average REE contents increase with depth, while the LREE/HREE ratio decrease and the extent of positive Ce anomalies weaken with depth. The results of REE fractionation show that La, Ce, Pr and Nd come from terrigenous sources, as the other REEs are susceptible to the oxidation-deoxidation conditions. The residual fractions of the sediments of the research area are mainly the uppermost fractions of REE, and followed by the Fe/Mn-oxides fractions as the second. Facts show that the residual fraction of REE play a decisive role in the total REE patterns of the Kuroshio mainstream sediments, as well as the key factor of positive Ce anomalies in the total REE. The REE features show no obvious relations with grain size, and the provenance of REE was relatively stable over the past millennium. It is inferred that the rivers input from eastern Taiwan was the most important source of REE in the sediments of the research area, and input from East Asian monsoon subordinates.
- rare earth element /
- provenance /
- fraction /
- sediment /
- eastern Taiwan

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图 1 研究站位及海底地形示意图

Figure 1.

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图 2 柱状沉积物稀土元素参数与中值粒径垂直变化

Figure 2.

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图 3 研究区各层沉积物及典型区域沉积物稀土元素球粒陨石标准化曲线

Figure 3.

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图 4 研究区各层沉积物及典型区域沉积物稀土元素上地壳标准化曲线

Figure 4.

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图 5 研究区沉积物中稀土元素不同赋存形态相对百分含量

Figure 5.

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图 6 研究区沉积物中不同赋存形态稀土元素上地壳标准化配分模式

Figure 6.

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图 7 研究区、潜在物源区及典型区域沉积物中Sm/Eu- LREE/HREE相关关系图

Figure 7.

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表 1 不同沉积层次沉积物与邻近海域沉积物稀土元素含量(μg/g)及特征参数

Table 1. Contents (μg/g) of REE and related parameters of from core sediments of different layers and surrounding areas

层位/cm 及样品	La	Ce	Pr	Nd	Sm	Eu	Gd	Tb	Dy	Ho	Er	Tm	Yb	Lu	REE	LREE/ HREE
0~0.5	25.77	58.36	5.62	21.13	4.12	0.94	3.67	0.47	2.41	0.43	1.19	0.16	0.98	0.15	125.40	12.25
0.5~1	20.58	52.54	4.13	15.22	3.08	0.72	2.79	0.38	2.02	0.37	0.97	0.14	0.83	0.13	103.89	12.62
1~1.5	24.99	59.73	5.15	18.88	3.73	0.83	3.26	0.42	2.22	0.40	1.09	0.15	0.95	0.15	121.96	13.09
1.5~2	28.14	62.46	6.16	23.22	4.52	1.02	3.78	0.51	2.69	0.49	1.33	0.18	1.13	0.17	135.80	12.21
2~2.5	21.13	56.88	4.40	16.29	3.32	0.77	3.12	0.41	2.13	0.38	1.06	0.14	0.90	0.14	111.07	12.40
2.5~3	21.92	55.02	4.45	16.82	3.38	0.78	3.15	0.41	2.17	0.39	1.08	0.15	0.91	0.15	110.76	12.18
3~3.5	29.43	49.32	6.53	24.21	4.65	1.01	3.91	0.51	2.64	0.47	1.31	0.18	1.10	0.18	125.43	11.19
3.5~4	26.61	59.11	5.72	21.28	4.22	0.94	3.71	0.47	2.41	0.43	1.21	0.16	1.00	0.16	127.41	12.36
4~4.5	25.66	55.67	5.53	21.01	4.15	0.93	3.85	0.47	2.40	0.43	1.25	0.16	1.00	0.16	122.66	11.62
4.5~5	24.67	51.14	5.28	19.58	4.08	0.90	3.83	0.48	2.51	0.45	1.33	0.18	1.09	0.18	115.72	10.51
5~5.5	25.21	57.50	5.37	20.07	4.10	0.92	3.88	0.47	2.41	0.43	1.23	0.16	1.01	0.16	122.93	11.60
5.5~6	20.80	53.91	4.25	16.09	3.27	0.76	3.16	0.40	2.03	0.37	1.04	0.14	0.85	0.14	107.20	12.20
6~6.5	21.47	55.62	4.29	16.01	3.20	0.75	3.52	0.41	2.12	0.39	1.13	0.15	0.96	0.15	110.17	11.49
6.5~7	20.37	54.64	4.25	15.98	3.34	0.76	3.55	0.41	2.10	0.38	1.15	0.15	0.94	0.16	108.18	11.24
7~7.5	25.13	51.83	5.19	19.04	3.76	0.86	3.68	0.46	2.37	0.43	1.26	0.17	1.03	0.17	115.38	11.06
7.5~8	17.04	54.07	3.55	13.46	2.87	0.69	3.15	0.38	1.97	0.36	1.08	0.14	0.89	0.15	99.78	11.32
8~9	21.95	59.60	4.67	17.39	3.51	0.81	4.06	0.45	2.23	0.41	1.30	0.17	1.03	0.17	117.76	11.00
9~10	22.63	57.87	4.70	17.56	3.49	0.81	3.67	0.43	2.22	0.40	1.19	0.15	0.97	0.16	116.26	11.64
10~11	22.70	59.19	4.68	17.79	3.66	0.84	3.52	0.44	2.25	0.41	1.14	0.15	0.95	0.15	117.85	12.09
11~12	33.22	53.69	7.35	27.35	5.27	1.12	4.53	0.55	2.85	0.51	1.43	0.20	1.18	0.19	139.43	11.19
12~13	30.03	50.81	6.76	25.04	4.87	1.04	4.11	0.52	2.69	0.49	1.38	0.19	1.15	0.19	129.26	11.07
13~14	30.93	54.02	6.80	25.40	4.88	1.03	4.18	0.53	2.79	0.51	1.45	0.19	1.23	0.19	134.14	11.10
14~15	19.78	60.62	3.74	13.63	2.79	0.65	2.79	0.35	1.86	0.34	0.93	0.13	0.79	0.13	108.54	13.81
15~16	17.31	55.48	3.33	12.62	2.67	0.65	2.90	0.36	1.93	0.36	1.02	0.14	0.87	0.14	99.78	11.92
16~17	18.77	62.56	3.62	13.48	2.82	0.68	3.02	0.37	1.94	0.36	1.00	0.13	0.85	0.13	109.72	13.07
17~18	31.71	57.44	7.01	26.27	4.92	1.05	4.23	0.52	2.63	0.48	1.35	0.18	1.12	0.18	139.07	12.02
18~19	17.30	63.17	3.44	13.33	2.99	0.72	3.17	0.39	2.07	0.38	1.09	0.15	0.90	0.14	109.24	12.16
19~20	20.89	54.78	4.08	14.89	2.98	0.71	3.05	0.39	2.02	0.36	1.02	0.14	0.85	0.14	106.30	12.34
20~21	22.51	51.97	4.72	17.63	3.52	0.82	3.34	0.43	2.19	0.40	1.09	0.15	0.90	0.14	109.80	11.73
21~22	34.37	57.43	7.76	28.85	5.49	1.16	5.60	0.60	2.92	0.52	1.71	0.21	1.30	0.22	148.16	10.31
22~23	28.71	57.21	6.33	23.66	4.74	1.03	4.45	0.52	2.67	0.48	1.44	0.19	1.17	0.19	132.79	10.95
23~24	20.02	60.32	4.27	16.22	3.37	0.79	3.59	0.41	2.13	0.38	1.13	0.15	0.90	0.15	113.84	11.88
24~25	21.02	60.26	4.48	16.89	3.50	0.82	4.37	0.46	2.27	0.42	1.34	0.17	1.09	0.18	117.27	10.38
25~26	21.32	57.37	4.45	16.65	3.49	0.78	4.65	0.46	2.22	0.41	1.37	0.17	1.10	0.19	114.64	9.84
26~27	20.19	60.88	4.07	15.28	3.14	0.73	4.25	0.42	2.01	0.37	1.22	0.14	0.95	0.16	113.82	10.94
27~28	31.44	62.39	6.95	25.89	5.00	1.10	4.22	0.53	2.77	0.50	1.39	0.19	1.14	0.19	143.70	12.14
28~29	29.77	56.54	6.59	24.56	4.74	1.05	4.06	0.52	2.65	0.47	1.30	0.17	1.05	0.17	133.63	11.86
29~30	31.03	53.86	6.87	25.72	5.00	1.08	4.35	0.54	2.72	0.49	1.36	0.18	1.12	0.17	134.49	11.30
平均值	24.38	56.72	5.17	19.33	3.86	0.87	3.74	0.45	2.33	0.42	1.22	0.16	1.01	0.16	119.82	11.69
A层(0~8.5cm) 均值	23.58	55.73	4.97	18.57	3.72	0.85	3.53	0.44	2.28	0.41	1.18	0.16	0.98	0.16	116.56	11.76
B层(8.5~21.5cm) 均值	24.58	57.05	5.19	19.37	3.85	0.86	3.73	0.45	2.33	0.42	1.22	0.16	1.01	0.16	120.38	11.69
C层(21.5~30cm) 均值	26.43	58.47	5.75	21.52	4.27	0.95	4.39	0.50	2.48	0.45	1.36	0.17	1.09	0.18	128.04	11.04
台湾东部河流^[22] n=12	44.12	86.61	9.81	36.30	6.53	1.40	6.23	0.92	5.28	0.99	2.92	0.44	2.89	0.45	204.88	9.07
中国黄土^[20]n=45	34.00	66.8	7.97	37.30	6.20	1.18	4.43	0.83	4.53	1.17	2.61	0.52	2.69	0.43	103.86	5.03
吕宋岛弧^[23] n=5	6.81	14.23	1.90	8.38	1.99	0.74	1.85	0.32	1.91	0.41	1.24	0.18	1.19	0.22	41.35	4.80
冲绳海槽^[14]n=30	25.84	51.18	5.95	23.77	4.58	0.95	4.12	0.62	3.39	0.75	1.96	0.28	1.91	0.30	125.61	8.42
南海^[24] n=3	41.00	58.00	10.20	36.80	5.69	1.35	5.81	0.83	3.21	0.34	1.95	0.13	1.59	0.26	167.16	10.84
注：n为样品数

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参考文献(37)

[1]	刘伟, 宋金明, 袁华茂, 等.黑潮化学物质输入东海的途径与通量[J].地球科学进展, 2015, 30(8): 904-914. http://d.old.wanfangdata.com.cn/Periodical/dqkxjz201508006 LIU Wei, SONG Jinming, YUAN Huamao, et al. Pathway and flux of inputting chemical substances from the Kuroshio to the East China Sea[J]. Advance in Earth Sciences, 2015, 30(8): 904-914. http://d.old.wanfangdata.com.cn/Periodical/dqkxjz201508006
[2]	Sibuet J C, Hsu S K, Normand A. Tectonic significance of the Taitung canyon, Huatung basin, east of Taiwan [J]. Marine Geophysical Researches, 2006, 27(1): 77-9. doi: 10.1007/s11001-006-8182-3
[3]	Liu C C, Yu S B. Vertical crustal movements in eastern Taiwan and their tectonic implications[J]. Tectonophysics, 1990, 183(1-4): 111-119. doi: 10.1016/0040-1951(90)90191-A
[4]	耿威, 张训华, 温珍河, 等.台湾东部海岸山脉对弧陆碰撞的响应[J].地质论评, 2013, 59(1): 129-136. doi: 10.3969/j.issn.0371-5736.2013.01.014 GENG Wei, ZHANG Xunhua, WEN Zhenhe, et al. A review on response of arc-continent collision in coastal range, eastern taiwan island[J]. Geological Review, 2013, 59(1): 129-136. doi: 10.3969/j.issn.0371-5736.2013.01.014
[5]	Li C, Shi X, Kao S, et al. Clay mineral composition and their sources for the fluvial sediments of Taiwanese rivers[J]. Chinese Science Bulletin, 2012, 57(6): 673-681. doi: 10.1007/s11434-011-4824-1
[6]	孙美静, 高红芳, 李学杰.台湾东部海域台东峡谷沉积特征及其成因[J].地球科学, 2017, DOI: 10.3799/DQKX.2017.515. SUN Meijign, GAO Hongfang, LI Xuejie. Sedimentary characteristics and origin on Taitung Canyon in eastern waters of Taiwan Island[J]. Earth Science, 2017, DOI: 10.3799/DQKX.2017.515.
[7]	Bentahila Y, Othman D B, Luck J M. Strontium, lead and zinc isotopes in marine cores as tracers of sedimentary provenance: A case study around Taiwan orogen[J]. Chemical Geology, 2008, 248(1): 62-82. https://www.sciencedirect.com/science/article/abs/pii/S0009254107004718
[8]	徐勇航, 陈坚, 王爱军, 等.台湾海峡表层沉积物中黏土矿物特征及物质来源[J].沉积学报, 2013, 31(1): 120-129. http://d.old.wanfangdata.com.cn/Periodical/cjxb201301013 XU Yonghang, CHEN Jian, WANG Aijun, et al. Clay minerals in surface sediments of the Taiwan Strait and their provenance[J]. Acta Sedimentologica Sinica, 2013, 31(1): 120-129. http://d.old.wanfangdata.com.cn/Periodical/cjxb201301013
[9]	方建勇, 陈坚, 王爱军, 等.台湾海峡表层沉积物的粒度和碎屑矿物分布特征[J].海洋学报, 2012, 34(5): 91-99. http://d.old.wanfangdata.com.cn/Periodical/hyxb201205011 FANG Jianyong, CHEN Jian, WANG Aijun, et al. Clay minerals in surface sediments of the Taiwan Strait and their provenance[J]. Haiyang Xuebao, 2012, 34(5):91-99. http://d.old.wanfangdata.com.cn/Periodical/hyxb201205011
[10]	Piper D Z. Rare earth elements in the sedimentary cycle: A summary[J]. Chemical Geology, 1974, 14(4): 285-304. http://d.old.wanfangdata.com.cn/NSTLQK/10.1016-0009-2541(74)90066-7/
[11]	徐兆凯, 李安春, 蒋富清, 等.东菲律宾海沉积物的地球化学特征与物质来源[J].科学通报, 2008, 53(6): 695-702. doi: 10.3321/j.issn:0023-074X.2008.06.013 XU Zhaokai, LI Anchun, JIANG Fuqing, et al. Geochemistry and provenance in the sediments of the east Phillippine Sea[J]. Chinese Science Bulletin, 2008, 53(6): 695-702. doi: 10.3321/j.issn:0023-074X.2008.06.013
[12]	Xu Z, Li T, Wan S, et al. Geochemistry of rare earth elements in the mid-late Quaternary sediments of the western Philippine Sea and their paleoenvironmental significance[J]. Science China-Earth Sciences, 2014, 57(4): 802-812. doi: 10.1007/s11430-013-4786-z
[13]	吴明清.我国台湾浅滩海底沉积物稀土元素地球化学[J].地球化学, 1983, (3): 303-313. doi: 10.3321/j.issn:0379-1726.1983.03.010 WU Mingqing. Geochemistry of rare earth element in the sediments of Taiwan Shoal[J]. Geochemica, 1983, (3): 303-313. doi: 10.3321/j.issn:0379-1726.1983.03.010
[14]	刘娜, 孟宪伟.冲绳海槽中段表层沉积物中稀土元素组成及其物源指示意义[J].海洋地质与第四纪地质, 2004, 24(4): 37-43. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=532e329f-d868-4bd5-9a02-65a6d3c0d8c5 LIU Na, MENG Xianwei. Characteristics of rare earth elements in surface sediments from the middle Okinawa Trough: Implications for provenance of mixed sediments[J]. Marine Geology & Quaternary Geology, 2004, 24(4): 37-43. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=532e329f-d868-4bd5-9a02-65a6d3c0d8c5
[15]	褚征, 胡宁静, 刘季花, 等.西菲律宾海表层沉积物稀土元素地球化学特征及物源指示意义[J].海洋地质与第四纪地质, 2016, 36(5): 53-62. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=024ae3d2-9c01-4431-ac49-456752742b2d ZHU Zheng, HU Ningjing, LIU Jihua, et al. Rare earth elements in sediments of west Phillippine Sea and their implications for sediment provenance[J], Marine Geology & Quaternary Geology, 2016, 36 (5): 53-62. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=024ae3d2-9c01-4431-ac49-456752742b2d
[16]	徐兆凯, 李安春, 徐方建, 等.东菲律宾海表层沉积物中元素的赋存状态[J].海洋地质与第四纪地质, 2007, 27(2): 51-58. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=bb6d5a38-70b6-4049-a7e6-48f239d0390b XU Zhaokai, LI Anchun, XU Fangjian, et al. Elemental occurrence phases of surface sediments from the east Phillippine Sea[J], Marine Geology & Quaternary Geology, 2007, 27(2): 51-58. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=bb6d5a38-70b6-4049-a7e6-48f239d0390b
[17]	贾建军, 高抒, 薛允传.图解法与矩法沉积物粒度参数的对比[J].海洋与湖沼, 2002, 33(6): 577-582. doi: 10.3321/j.issn:0029-814X.2002.06.002 JIA Jianjun, GAO Shu, XUE Yunchuan, et al. Grain-size parameters derived from graphic and moment methods: a comparative study[J]. Oceanolgia et Limnologia Sinica, 2002, 33(6): 577-582. doi: 10.3321/j.issn:0029-814X.2002.06.002
[18]	Rauret G, Rubio R, López-Sánchez J F. Optimization of tessier procedure for metal solid speciation in river sediments[J]. International Journal of Environmental Analytical Chemistry, 1989, 36(2): 69-83. doi: 10.1080/03067318908026859
[19]	傅飘儿, 庄畅, 刘坚, 等.南海西沙海槽XH-CL16柱状沉积物稀土元素特征及其物源[J].海洋地质与第四纪地质, 2015, 35(4): 63-71. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=3e58d193-cfe8-45dc-aeb8-751f97bb6e22 FU Piaoer, ZHUANG Chang, LIU Jian, et al. Rare earth elements geochemistry and provenance of the sediments from core XH-CL16 in the Xisha Though, South China Sea[J]. Marine Geology and Quaternary Geology, 2015, 35(4): 63-71. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=3e58d193-cfe8-45dc-aeb8-751f97bb6e22
[20]	文启忠.中国黄土地球化学[M].北京:科学出版社, 1989. WEN Qizhong. Geochemistry of Chinese Losess[M]. Beijing: Science Press, 1989.
[21]	蒋富清, 孟庆勇, 徐兆凯, 等.冲绳海槽北部15ka B.P.以来沉积物源及控制因素——稀土元素的证据[J].海洋与湖沼, 2008, 39(2): 112-118. doi: 10.3321/j.issn:0029-814X.2008.02.003 JIANG Fuqing, MENG Qingyong, XU Zhaokai, et al. The REE imprint on sediment provenance of the northern Okinawa Trough since the last 15ka B.P. [J]. Oceanolgia et Limnologia Sinica, 2008, 39(2): 112-118. doi: 10.3321/j.issn:0029-814X.2008.02.003
[22]	Li C S, Shi X F, Kao S J, et al. Rare earth elements in fine-grained sediments of major rivers from the high-standing island of Taiwan[J]. Journal of Asian Earth Sciences, 2013, 69(12): 39-47. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=fc9a6b8ad7b40f65d30173f7a999918a
[23]	Iii T A T, Yumul G P, Ramos E G L, et al. Rare earth element geochemistry of the Zigzag Klondyke sedimentary rock formations: Clues to the evolution of the Baguio mineral district (Luzon), Philippines[J]. Resource Geology, 2010, 55(3): 217-224.
[24]	赵一阳, 王金土, 秦朝阳, 等.中国大陆架海底沉积物中的稀土元素[J].沉积学报, 1990, 8 (1): 37-43. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB199001004.htm ZHAO Yiyang, WANG Jinshi, QIN Zhaoyang, et al. Rare-earth elements in continental shelf sediments of the China Seas[J], Acta Sedimentologica Sinica, 1990, 8(1): 37-43. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB199001004.htm
[25]	Xu Y, Song J, Duan L, et al. Fraction characteristics of rare earth elements in the surface sediment of Bohai Bay, North China[J]. Environmental Monitoring & Assessment, 2012, 184(12): 7275-7292. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=67874fdc8fc73956dd6ce03fba4199ff
[26]	Xu Y, Song J, Duan L, et al. Environmental geochemistry reflected by rare earth elements in Bohai Bay (North China) core sediments[J]. Journal of Environmental Monitoring, 2010, 12(8): 1547-1555. doi: 10.1039/c0em00013b
[27]	徐亚岩, 宋金明, 李学刚, 等.渤海湾各形态重金属的地球化学特征及其环境意义[J].农业环境科学学报, 2011, 30(12): 2560-2570. http://d.old.wanfangdata.com.cn/Periodical/nyhjbh201112025 XU Yayan, SONG Jinming, LI Xuegang, et al. Geochemical characteristics of heavy metals in different fractions and their environmental significance in Bohai Bay sediment cores, China[J]. Journal of Agro-Environment Science, 2011, 30(12): 2560-2570. http://d.old.wanfangdata.com.cn/Periodical/nyhjbh201112025
[28]	宋金明, 段丽琴.渤黄东海微/痕量元素的环境生物地球化学[M].北京:科学出版社, 2017. SONG Jinming, DUAN Liqin. Environmental Biogeochemistry of Trace Elements in Bohai, Yellow Sea and East China Sea[M]. Beijign: Science Press, 2017.
[29]	杨守业, 李从先. REE示踪沉积物物源研究进展[J].地球科学进展, 1999, 14(2): 164-167. doi: 10.3321/j.issn:1001-8166.1999.02.010 YANG Shouye, LI Congxian. Research progress in REE tracer for sediment source[J]. Advance in Earth Sciences, 1999, 14(2): 164-167. doi: 10.3321/j.issn:1001-8166.1999.02.010
[30]	Chen M P, Lo S C, Lin K L. Composition and texture of surface sediment indicating the depositional environments off northeast Taiwan [J]. Terrestrial, Atmospheric and Oceanic Sciences, 1992, 3(3):395-418. doi: 10.3319/TAO.1992.3.3.395(KEEP)
[31]	黄永样, 杨慧宁.海底沉积物类型及其地球化学环境对多金属结核形成与分布的控制作用[M].武汉:中国地质大学出版社, 1997. HUANG Yongyang, YANG Huining. The Control Effect of Seabed Sedimetns and Its Geochemical Environment on the Formation and Distribution of Polymetallic Nodules[M]. Wuhan: China University of Geosciences Press, 1997.
[32]	亨德森.稀土元素地球化学[M].北京:地质出版社, 1989. Henderson P. Rare Earth Element Geochemistry[M]. Beijing: Geological Publishing House, 1989.
[33]	王越奇, 宋金明, 袁华茂, 等. 近千年来台湾以东黑潮主流区沉积物来源及其对气候波动的响应[J]. 海洋科学进展(待刊). WANG Yueqi, SONG Jinming, YUAN Huamao, et al. Sedimentary provenance and corresponding to the climate fluctuation of the Kuroshio area of eastern Taiwan for the last 1000 years[J]. Advances in Marine Science (Article in press).
[34]	杨守业, 李从先.长江与黄河沉积物元素组成及地质背景[J].海洋地质与第四纪地质, 1999, 19(2): 19-26. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=c1cfd796-4a1a-4dfd-bea5-6bc812581bdf YANG Shouye, LI Congxian. Characteristic element compositions of the Yangtze and the Yellow river sediments and their geological background[J]. Marine Geology and Quaternary Geology, 1999, 19(2): 19-26. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=c1cfd796-4a1a-4dfd-bea5-6bc812581bdf
[35]	Defant M J. Geochemistry and tectonic setting of the Luzon arc, Philippines[J]. Geological Society of America Bulletin, 1989, 101(5): 663-72. doi: 10.1130/0016-7606(1989)101<0663:GATSOT>2.3.CO;2
[36]	池野, 李安春, 蒋富清, 等.吕宋岛东部海域黏土矿物组合特征及物源分析[J].海洋科学, 2009, 33(9): 80-88. http://d.old.wanfangdata.com.cn/Periodical/hykx200909016 CHI Ye, LI Anchun, JIANG Fuqing, et al. Assemblage and provenance of clay minerals off the east of Luzon Island[J]. Marine Sciences, 2009, 33(9): 80-88. http://d.old.wanfangdata.com.cn/Periodical/hykx200909016
[37]	蓝先洪, 徐晓达, 王中波, 等.渤海西部表层沉积物的稀土元素分布特征与物源约束[J].地球学报, 2018, 39(1): 37-44. http://d.old.wanfangdata.com.cn/Periodical/dqxb201801004 LAN Xianhong, XU Xiaoda, WANG Zhongbo, et al. Distribution characteristics of rare erath elements and their provenance constraints in the surface sedimetns from the western Bohai Sea[J]. Acta Geoscientica Sinica, 2018, 39(1): 37-44. http://d.old.wanfangdata.com.cn/Periodical/dqxb201801004

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台湾东黑潮主流区近千年来沉积物稀土元素的变化特征与来源

1. 中国科学院海洋研究所海洋生态与环境科学重点实验室，青岛 266071 2. 中国科学院大学，北京 100049 3. 青岛海洋科学与技术国家实验室海洋生态与环境科学功能实验室，青岛 266237 4. 中国科学院海洋大科学研究中心，青岛 266071

作者简介: 王越奇(1992—)，女，博士生，从事海洋生物地球化学研究，E-mail：iocaswyq@163.com

通讯作者: 宋金明(1964—)，男，研究员，主要从事研究海洋生物地球化学，E-mail: jmsong@qdio.ac.cn

蔡秋蓉编辑

Variation in rare earth elements and provenances of the sediments along the Kuroshio mainstream to the east of Taiwan over the past millennium

Corresponding author: SONG Jinming, jmsong@qdio.ac.cn

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