地球科学进展 ›› 2004, Vol. 19 ›› Issue (4): 545 -551. doi: 10.11867/j.issn.1001-8166.2004.04.0545

所属专题: IODP研究

IODP研究 上一篇    下一篇

深海研究中的底栖有孔虫:回顾与展望
张江勇,汪品先   
  1. 同济大学海洋地质教育部重点实验室,上海 200092
  • 收稿日期:2004-05-20 修回日期:2004-06-14 出版日期:2004-08-01
  • 通讯作者: 张江勇(1978-),男,山西晋城人,硕士研究生,主要从事第四纪古海洋学与古环境研究. E-mail:E-mail:zjy905@hotmail.com
  • 基金资助:

    国家重点基础研究发展规划项目“地球圈层相互作用中的深海过程和深海记录”(编号:G2000078500)资助

BENTHIC FORAMINIFERA IN DEEPSEA RESERCH:RETROSPECT AND PROSPECT

ZHANG Jiang-yong; WANG Pin-xian   

  1. Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
  • Received:2004-05-20 Revised:2004-06-14 Online:2004-08-01 Published:2004-08-01

底栖有孔虫在古环境研究中的应用先是用作古水深或水团的标志物。随着新技术的应用,识别出了2种不同的底栖有孔虫微生境:外生种和内生种;认识到甚至深海底栖有孔虫,也能对表层浮游生物勃发的季节性短暂事件作出响应,因为沉降到海底的有机物质供养着底栖有孔虫。目前,底栖有孔虫被广泛应用于估算海洋表层生产力和底层水团的含氧量。回顾了深海底栖有孔虫生态研究的历史和其在古海洋学中的应用,并强调研究、应用中的新方法、新技术。中国已经加入了诸如IODP等深海研究计划,有必要向我国学术界提供底栖有孔虫研究的新方向,以资参考。

The use of benthic foraminifera in paleoenvironmental studies was started as indicators of paleowater depth or water mass. With application of new technology, two different microhabitats of benthic foraminifera have been distinguished: epifauna vs〖KG*2〗infauna, and it was found that even deepwater benthic foraminifera respond to seasonal ephemeral changes caused by surface planktonic bloom for the supply of organic matter to the sea bottom. Benthic foraminifera are now widely used for estimation of surface productivity of the ocean and the oxygen content of the bottom water. This paper reviews the historical development of ecological studies on deepsea benthic foraminifera and their use in paleoceanography, with emphasis on new approaches and new technology. Since China has joined such deepsea research programs as IODP, some new directions in benthic foraminiferal studies are proposed to the Chinese community.

中图分类号: 

[1]Boltovskoy E, Wright R. Recent Foraminifera [M]. Hague: Dr. W Junk b v-Publishers, 1976. 113-122.
[2]Phleger F BEcology and Distribution of Recent Foramnifera[M].Baltimore:John Hopkins Press, 1960.
[3]Wang Pinxian(汪品先), Zhang Jijun(章纪军), Zhao Quanhong(赵泉鸿), et al. Foraminifera and Ostracoda in Bottom Sediments of the East China Sea[M]. Beijing: China Ocean Press, 1988. 105-114(in Chinese).
[4]Murry J W. Ecology and distribution of benthic foraminifera: A review[A]. In:Takayanagi Y, Saito T, eds. Studies in Benthic Foraminifera[C]. Japan:Tokai University Press, 1992. 33-41.
[5]Douglas R,Woodruff F.Deep-sea benthic foraminifera[A]. In: Emiliani C, eds.The sea,7 [C].  New York: Wiley-Interscience Publication,1981.1 233-1 327.
[6]Buzas M A,Culver S J.Foraminifera, distribution of provinces in the western North Atlantic [J]. Science, 1980, 209:687-689.
[7]Corliss B H. Microhabitats of benthic foraminifera within deep-sea sediments[J]. Nature, 1985, 314:435-438.
[8]Corliss B H, Chen C. Morphotype patterns of Norwegian Sea deep-sea benthic foraminifera and ecological implications[J]. Geology, 1988, 16:716-719.
[9]Corliss B H, Fois E. Morphotype analysis of deep-sea benthic foraminifera from the northwest gulf of Mexico[J]. Research Reports, 1991,(5):589-605.
[10]Kaiho K. Benthic foraminiferal dissoved-oxygen index and dissoved-oxygen levels in the modern ocean[J]. Geology, 1994, 22:719-722.
[11]Jorissen F J, de Stigter H C, Widmark J G V. A conceptual model explaining benthic foraminiferal microhabitats[J]. Marine Micropaleontology, 1995, 26:3-15.
[12]Kitazato H, Shirayama Y, Nakatsuka T, et al. Seasonal phytodetritus deposition and respones of bathyal benthic foraminiferal populations in Sagami Bay, Japan: Preliminary results from “Project Sagami 1996-1999”[J].Marine Micropaleontology, 2000, 40:135-149.
[13]Herguara J C, Berger W H. Paleoproductivity from benthic foraminifera abundance: Glacial to postglacial change in the west-equatorial pacific[J]. Marine Micropaleontology, 1991, 19:1 173-1 176.
[14]Gooday A J. A response by benthic foraminifera to the deposition of phytodetritus in the deep sea[J].Nature, 1988, 332(3):70-73.
[15]Danovaro R, Dell'Anno A, Fabiano M, et al. Deep-sea ecosystem response to climate changes: The eastern Mediterranean case study[J].Trends in Ecology & Evolution, 2001, 16(9):505-510.
[16]Tenbach A V. Short term processes and patterns in the foraminiferal response to organic flux rates[J]. Marine Micropaleontology, 1992, 19:119-129.
[17]Gooday A J. Biological responses to seasonally varying fluxes of organic matter to the ocean floor: A review[J].Journal of Oceanography, 2002, 58:305-332.
[18]Gooday A J, Rathburn A E. Temporal variabiliity in living deep-sea benthic foraminifera: A review[J].Earth-Science Review,1999,46: 187-212.
[19]Altenbach A V. Short term processes and patterns in the foraminiferal response to organic flux rates[J].Marine Micropaleontology,1992, 19:119-129.
[20]De Rijk s, Jorissen F J, Rohling E J, et al. Organic flux control on bathymetric zonation of Mediterranean benthic foraminifera[J].Marine Micropaleontology, 2000, 40:151-166.
[21]Bernhard J M, Sen Gupta B K, Borne P F. Benthic foramiferal proxy to estimate dysoxic bottom-water oxygen concentrations: Sante Barbara Basin, U.S. Pacific continental margin[J]. Journal of Foraminiferal Research, 1997, 27:301-310.
[22]Sen Gupta B K, Platon E, Bernhard J M, et al. Foraminiferal colonization of hydrocarbon-seep bacterial mats and underlying sediment, Gulf of Mexico[J].Journal of Foraminiferal Research, 1997, 27:292-300.
[23]Boyle E A. Limits on benthic foraminiferal chemical analyses as precise measures of environmental properties[J].Journal of Foraminiferal Research, 1995, 25:4-13.
[24]IODP Planning Sub-Committee. Earth, Oceans, and Life: IODP Initial Science Plan[M]. International Working Group Support Office, 2001.35-52.
[25]Jian Z, Wang L, Kienast M, et al. Benthic foraminiferal paleoceanography of the South China Sea over the last 40 000 years[J].Marine Geology, 1999, 156:159-186.

[1] 徐昭萌, 刘素美. 底栖有孔虫体内储存硝酸盐和反硝化研究进展[J]. 地球科学进展, 2017, 32(9): 949-958.
[2] 陈春, 高峰, 鲁景亮, 陈松丛. 日本海洋科技战略计划与重点研究布局及其对我国的启示[J]. 地球科学进展, 2016, 31(12): 1247-1254.
[3] 汪品先. 我国参加大洋钻探的近十年回顾与展望[J]. 地球科学进展, 2014, 29(3): 322-326.
[4] 秦蕴珊,尹宏. 西太平洋——我国深海科学研究的优先战略选区[J]. 地球科学进展, 2011, 26(3): 245-248.
[5] 向 荣,刘 芳,陈 忠,颜 文,陈木宏. 冷泉区底栖有孔虫研究进展[J]. 地球科学进展, 2010, 25(2): 193-202.
[6] 李清,王家生,王晓芹,陈祈,陈洪仁. IODP 311航次底栖有孔虫碳稳定同位素对天然气水合物地质系统的指示[J]. 地球科学进展, 2008, 23(11): 1161-1166.
[7] 汪品先,翦知湣,刘志飞. 地球圈层相互作用中的深海过程和深海记录(I):研究进展与成果[J]. 地球科学进展, 2006, 21(4): 331-337.
阅读次数
全文


摘要