南海南部上层水体浮游有孔虫的组成与分布特征

安佰正, 李铁刚, 刘健, 孙晗杰, 于心科, 常凤鸣. 南海南部上层水体浮游有孔虫的组成与分布特征[J]. 海洋地质与第四纪地质, 2019, 39(1): 124-133. doi: 10.16562/j.cnki.0256-1492.2018052302
引用本文: 安佰正, 李铁刚, 刘健, 孙晗杰, 于心科, 常凤鸣. 南海南部上层水体浮游有孔虫的组成与分布特征[J]. 海洋地质与第四纪地质, 2019, 39(1): 124-133. doi: 10.16562/j.cnki.0256-1492.2018052302
AN Baizheng, LI Tiegang, LIU Jian, SUN Hanjie, YU Xinke, CHANG Fengming. Assemblage and distribution of planktonic foraminifera in the upper water layer of southern South China Sea[J]. Marine Geology & Quaternary Geology, 2019, 39(1): 124-133. doi: 10.16562/j.cnki.0256-1492.2018052302
Citation: AN Baizheng, LI Tiegang, LIU Jian, SUN Hanjie, YU Xinke, CHANG Fengming. Assemblage and distribution of planktonic foraminifera in the upper water layer of southern South China Sea[J]. Marine Geology & Quaternary Geology, 2019, 39(1): 124-133. doi: 10.16562/j.cnki.0256-1492.2018052302

南海南部上层水体浮游有孔虫的组成与分布特征

  • 基金项目:
    国家自然科学基金项目“15万年以来热带西太平洋颗石藻碳酸钙输出通量演变及其影响因素”(41706070);国家自然科学基金项目“80万年来热带西太平洋上层水体pH和pCO2演变及影响机理”(41230959);青岛海洋科学与技术国家实验室鳌山科技创新计划项目(2016ASKJ13);中国科学院海洋地质与环境重点实验室开放基金“西太平洋上层水体现代颗石藻碳酸钙分布特征”(MGE2017KG03);山东省自然科学基金面上项目“山东半岛东部近岸中、晚全新世高分辨率环境演化过程研究”(ZR2016DM12)
详细信息
    作者简介: 安佰正(1984—), 男,博士,主要从事古海洋学与古环境研究,E-mail: an_baizheng@126.com
    通讯作者: 李铁刚,研究员,主要从事古海洋与古环境方面研究,E-mail: tgli@fio.org.ac.cn
  • 中图分类号: P736.2

  • 周立君编辑

Assemblage and distribution of planktonic foraminifera in the upper water layer of southern South China Sea

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  • 通过分析2012年4月在南海南部获取的浮游生物拖网样品,对水体中浮游有孔虫的区域分布特征及其影响因素进行了初步探讨。南海南部上层水体中共鉴定出现代浮游有孔虫19种,其中优势种为Globigerinoides sacculiferGlobigerinoides ruberGlobigerinella calidaGlobigerinella siphoniferaGloborotalia menardiiOrbulina universaNeogloboquadrina dutertrei。浮游有孔虫种属组成整体上呈现为热带-亚热带群落特征,浮游有孔虫生物丰度与西太平洋北赤道流区域的生物丰度相当。南海南部春季上层水体中浮游有孔虫整体表现为西高东低的区域分布特征,在垂直分布上浮游有孔虫集中分布在上部0~50m水层中,50m以深水体中浮游有孔虫生物丰度迅速降低。认为浮游有孔虫的分布受到温度、水体层化、初级生产力等多方面环境因子的综合作用。个别深水种(如Globorotalia menardii)出现了主要分布在0~50 m水深的特殊现象。

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  • 图 1  南海南部采样站位分布图

    Figure 1. 

    图 2  调查区浮游有孔虫各种属百分含量

    Figure 2. 

    图 3  调查区不同站位浮游有孔虫群落简单分异度

    Figure 3. 

    图 4  调查区不同站位浮游有孔虫生物丰度(单位:inds·m-3)

    Figure 4. 

    图 5  调查区不同站位浮游有孔虫常见种属垂直分布特征

    Figure 5. 

    图 6  各站位实测温盐数据(a.温度;b.盐度)

    Figure 6. 

    图 7  基于WOA2009的环境参数剖面(纬度6.5°N, 使用Ocean DataView软件绘制)

    Figure 7. 

    表 1  南海南部各站位采样信息

    Table 1.  Samplinginformation in the Southern South China Sea

    站位 取样位置 取样日期和时间
    DS10 7.2°N,112.3°E 2012-05-08-21:01
    DS17 7.2°N,114.2°E 2012-04-20-16:16
    DS19 7.2°N,114.7°E 2012-04-21-10:39
    DS13 6.7°N,113.1°E 2012-05-04-17:14
    DS02 6.4°N,110.3°E 2012-05-03-01:17
    DS15 5.6°N,113.7°E 2012-04-25-13:30
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  • [1]

    Schiebel R.Plankticforaminiferal sedimentation and the marine calcite budget[J]. Glob.Biogeochem. Cycle, 2002, 16: 1-21. doi: 10.1029/2001GB001398

    [2]

    Kuroyanagi A, Kawahata H. Vertical distribution of living planktonic foraminifera in the seas around Japan[J]. Marine Micropaleontology, 2004, 53: 173-196. doi: 10.1016/j.marmicro.2004.06.001

    [3]

    Manno C, Pavlov A. Living planktonic foraminifera in the Fram Strait (Arctic): absence of diel vertical migration during the midnight sun[J].Hydrobiologia, 2014, 721: 285-295. doi: 10.1007/s10750-013-1669-4

    [4]

    Kucera M. Planktonic foraminifera as tracers of past oceanic environments[J]. Developments in Marine Geology, 2007, 1: 213-262. doi: 10.1016/S1572-5480(07)01011-1

    [5]

    Pflaumann U, Jian Z, Modern distribution patterns of planktonic foraminifera in the South China Sea and western Pacific: A new transfer technique to estimate regional sea-surface temperatures[J]. Marine Geology, 1999, 156: 41-83. doi: 10.1016/S0025-3227(98)00173-X

    [6]

    Darling K F, Kucera M, Pudsey C J, et al. Molecular evidence links cryptic diversification in polar planktonic protists to Quaternary climate dynamics[J]. Proceedings of the National Academy of Sciences of the United States of America, 2004, 101: 7657-7662. doi: 10.1073/pnas.0402401101

    [7]

    Chen M T, Wang C H, Huang C Y, et al. A late Quaternary planktonic foraminifer faunal record of rapid climatic changes from the South China Sea[J]. Marine Geology, 1999, 156: 85-108. doi: 10.1016/S0025-3227(98)00174-1

    [8]

    Xiang R, Chen M, Li Q, et al. Planktonic foraminiferal records of East Asia monsoon changes in the southern South China Sea during the last 40000 years[J]. Marine Micropaleontology, 2009, 73: 1-13. doi: 10.1016/j.marmicro.2009.06.004

    [9]

    Katz M E, Cramer B S, Franzese A, et al. Traditional and emerging geochemical proxies in foraminifera[J]. Journal of Foraminiferal Research, 2010, 40: 165-192. doi: 10.2113/gsjfr.40.2.165

    [10]

    Mix A C, Morey A E, Pisias N G, et al. Foraminiferal faunal estimates of paleotemperature: Circumventing the no-analog problem yields cool ice age tropics[J]. Paleoceanography, 1999, 14: 350-359. doi: 10.1029/1999PA900012

    [11]

    Barker S, Elderfield H, Foraminiferal calcification response to glacial-interglacial changes in atmospheric CO2[J]. Science, 2002, 297: 833-836. doi: 10.1126/science.1072815

    [12]

    Bijma J, Spero H, Lea D. Reassessing foraminiferal stable isotope geochemistry: Impact of the oceanic carbonate system (experimental results) [C]// Fischer G, Wefer G, eds.Use of proxies in paleoceanography-Examples from the South Atlantic. Springer, Berlin, Heidelberg, 1999: 489-512.

    [13]

    Foster G. Seawater pH, pCO2 and [CO32-] variations in the Caribbean Sea over the last 130 kyr: a boron isotope and B/Ca study of plankticforaminifera[J]. Earth and Planetary Science Letters, 2008, 271: 254-266. doi: 10.1016/j.epsl.2008.04.015

    [14]

    Hall J M, Chan L H. Ba/Ca in Neogloboquadrina pachyderma as an indicator of deglacial meltwater discharge into the western Arctic Ocean[J]. Paleoceanography, 2004, 19(1), doi:10.1029/2003PA000910.

    [15]

    Moy A D, Howard W R, Bray S G, et al. Reduced calcification in modern Southern Ocean planktonic foraminifera[J]. Nature Geoscience, 2009, 2: 276-280. doi: 10.1038/ngeo460

    [16]

    Russell A D, Hönisch B, Spero H J, et al. Effects of seawater carbonate ion concentration and temperature on shell U, Mg, and Sr in cultured planktonic foraminifera[J]. Geochimica et Cosmochimica Acta, 2004, 68: 4347-4361. doi: 10.1016/j.gca.2004.03.013

    [17]

    Weinkauf M F G, Kunze J G, Waniek J J, et al. Seasonal variation in shell calcification of planktonic foraminifera in the NE Atlantic reveals species-specific response to temperature, product ivity, and optimum growth conditions[J]. Plos One, 2016, 11: e0148363. doi: 10.1371/journal.pone.0148363

    [18]

    Weldeab S, Lea D W, Schneider R R, et al. 155000 years of West African monsoon and ocean thermal evolution[J]. Science, 2007, 316: 1303-1307. doi: 10.1126/science.1140461

    [19]

    Yu J, Elderfield H. Benthic foraminiferal B/Ca ratios reflect deep water carbonate saturation state[J]. Earth and Planetary Science Letters, 2007, 258: 73-86. doi: 10.1016/j.epsl.2007.03.025

    [20]

    Bé A W H. An ecological, zoogeographic and taxonomic review of recent planktonic foraminifera[M]// Ramsay A T S. Oceanic Micropaleontology. London: Academic Press, 1977.

    [21]

    崔喜江, 向荣, 郑范, 等.南海南部活体浮游有孔虫分布特征及其影响因素初探[J].热带海洋学报, 2006, 25:25-30. doi: 10.3969/j.issn.1009-5470.2006.04.005

    CUI Xijiang, XIANG Rong, ZHENG Fan, et al. A preliminary study of living planktonic foraminifera distribution and its affecting factors in southern South China Sea[J]. Journal of Tropical Oceanography.2006, 25: 25-30. doi: 10.3969/j.issn.1009-5470.2006.04.005

    [22]

    向荣, 陈木宏, 张兰兰, 等.南海北部秋季活体浮游有孔虫的组成与分布[J].地球科学:中国地质大学学报, 2010(1):10. http://d.old.wanfangdata.com.cn/Periodical/dqkx201001001

    XIANG Rong, CHEN Muhong, ZHANG Lanlan, et al. Compositions and distribution of living planktonic foraminifera in Autumn waters of the Northern South China Sea [J]. Earth Science-Journal of China University of Geosciences, 2010(1):10. http://d.old.wanfangdata.com.cn/Periodical/dqkx201001001

    [23]

    罗琼一, 金海燕, 翦知湣, 等.南海现代浮游有孔虫的垂直分布及其古海洋学意义[J].第四纪研究, 2015, 35: 1342-1353. doi: 10.11928/j.issn.1001-7410.2015.06.04

    LUO Qiongyi, JIN Haiyan, JIAN Zhimin, et al. Vertical distribution of living planktonic foraminifera in the northern South China Sea and its paleoceanographic implications [J]. Quarternary Sciences, 2015, 35: 1342-1353. doi: 10.11928/j.issn.1001-7410.2015.06.04

    [24]

    方文东, 黄企洲, 邱章, 等.春夏季季风转换期南海南部的异常表层水[J].热带海洋学报, 2001, 20: 77-81. doi: 10.3969/j.issn.1009-5470.2001.01.010

    FANG Wendong, HUANG Qizhou, QIU Zhang, et al. Anomalous sea surface water in southern South China Sea during spring to summer monsoon transition[J]. Journal of Tropical Oceanography, 2001, 20: 77-81. doi: 10.3969/j.issn.1009-5470.2001.01.010

    [25]

    Garcia H, Locarnini R, Boyer T, et al. Nutrients (Phosphate, Nitrate, Silicate) [M]//World Ocean Atlas. US Gov. Printing Office, Washington, DC, 2010: 71.

    [26]

    万随, 翦知湣, 成鑫荣, 等.南沙海区浮游有孔虫通量及其壳体化学性质的季节变化[J].中国科学:地球科学, 2010, 40: 881-892. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZUGS200910001326.htm

    WAN Sui, JIAN Zhimin, CHENG Xinrong, et al. Seasonal variations in planktonic foraminiferal flux and the chemical properties of their shells in the southern South China Sea[J]. Science China:Earth Science, 2010, 40: 881-892. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZUGS200910001326.htm

    [27]

    Lin H L, Hsieh H Y. Seasonal variations of modern planktonic foraminifera in the South China Sea[J]. Deep Sea Research Part Ⅱ: Topical Studies in Oceanography, 2007, 54: 1634-1644. doi: 10.1016/j.dsr2.2007.05.007

    [28]

    张凯南, 王珍岩, 王保铎. 2012年春季南海南部不同水团上层海水中悬浮体分布特征及其物源分析[J].海洋科学, 2014, 38(3):26-36. http://d.old.wanfangdata.com.cn/Periodical/hykx201403005

    ZHANG Kainan, WANG Zhenyan, WANG Baoduo.Distribution characteristic and provenance of suspended matter in upper water of the southern South China Sea during the spring of 2012[J]. Marine Sciences, 2014, 38(3): 26-36. http://d.old.wanfangdata.com.cn/Periodical/hykx201403005

    [29]

    柯志新, 黄良民, 李刚, 等.春末夏初巽他陆架表层水体的叶绿素粒级结构及其和营养盐的关系[J].海洋学报, 2012, 34: 190-196. http://d.old.wanfangdata.com.cn/Periodical/hyxb201203024

    KE Zhixin, HUANG Liangmin, LI Gang, et al. Size structure of chlorophyll a in relation to environmental factors in surface waters of Sunda shelf during late spring and early summer[J]. Acta Oceanological Sinica, 2012, 34: 190-196. http://d.old.wanfangdata.com.cn/Periodical/hyxb201203024

    [30]

    赵辉, 齐义泉, 王东晓, 等.南海叶绿素浓度季节变化及空间分布特征研究[J].海洋学报, 2005, 27(4):45-52. doi: 10.3321/j.issn:0253-4193.2005.04.006

    ZHAO Hui, QI Yiquan, WANG Dongxiao, et al. Study on the features of chlorophyll-a derived from SeaWiFS in the South China Sea[J]. Acta Oceanological Sinica, 2005, 27(4):45-52. doi: 10.3321/j.issn:0253-4193.2005.04.006

    [31]

    朱根海, 宁修仁, 蔡昱明, 等.南海浮游植物种类组成和丰度分布的研究[J].海洋学报, 2003, 25:8-23. http://cdmd.cnki.com.cn/Article/CDMD-10384-1014227619.htm

    ZHU Genhai, NING Xiuren, CAI Yuming, et al. Studies on species composition and abundance distribution of phytoplankton in the South China Sea[J]. Acta Oceanologica Sinica, 2003, 25: 8-23. http://cdmd.cnki.com.cn/Article/CDMD-10384-1014227619.htm

    [32]

    张兰兰, 陈木宏, 陆钧, 等.南海南部上层水体中多孔放射虫的组成与分布特征[J].热带海洋学报, 2005, 24: 55-64. doi: 10.3969/j.issn.1009-5470.2005.03.008

    ZHANG Lanlan, CHEN Muhong, LU Jun, et al. Living polycystine radiolarian fauna in upper water column of southern South China Sea and its distribution[J]. Journal of Tropical Oceanography, 2005, 24: 55-64. doi: 10.3969/j.issn.1009-5470.2005.03.008

    [33]

    Li B H, Jian Z M, Wang P X.Pulleniatinaobliquiloculata as a paleoceanographic indicator in the southern Okinawa Trough during the last 20000 years[J]. Marine Micropaleontology, 1997, 32(1-2): 59-69. doi: 10.1016/S0377-8398(97)00013-3

    [34]

    Xu J, Wang P X, Huang B Q, et al. Response of planktonic foraminifera to glacial cycles: Mid-Pleistocene change in the Southern South China Sea[J]. Marine Micropaleontology, 2005, 54(1-2): 89-105. doi: 10.1016/j.marmicro.2004.09.005

    [35]

    An B, Li T, Liu J, et al. Spatial distribution and controlling factors of planktonic foraminifera in the modern western Pacific[J]. Quaternary International, 2018, 468: 14-23. doi: 10.1016/j.quaint.2018.01.003

    [36]

    万随, 翦知湣, 成鑫荣.赤道西太平洋冬季浮游有孔虫分布与壳体同位素特征[J].第四纪研究, 2011, 31:284-291. doi: 10.3969/j.issn.1001-7410.2011.02.10

    WAN Sui, JIAN Zhimin, CHENG Xinrong. Distribution of winter living planktonic foraminifers and characteristics to their shell's stable isotopic in the western equatorial Pacific[J]. Quaternary Sciences, 2011, 31: 284-291. doi: 10.3969/j.issn.1001-7410.2011.02.10

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出版历程
收稿日期:  2018-05-23
修回日期:  2018-08-08
刊出日期:  2019-02-28

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