冬季南海北部陆架锋区悬浮颗粒态硅的分析

鲁超; 刘素美; 任景玲; 陈琪; 罗忻; 李建兵; 张经

冬季南海北部陆架锋区悬浮颗粒态硅的分析

1.
中国海洋大学海洋化学理论与工程技术教育部重点实验室, 山东青岛 266100
2.
国家海洋局第二海洋研究所海洋动力和卫星遥感重点实验室, 浙江杭州 310012
3.
中国海洋大学海洋化学理论与工程技术教育部重点实验室, 山东青岛 266100;华东师范大学, 河口海岸动力沉积和动力地貌综合国家重点实验室, 上海 200062

基金项目: 国家自然科学基金与香港研究资助局联合资助项目(40218001;N-HKUST609/32);科技部国际科技合作交流专项(No.2007DFB20380)资助

计量
- 文章访问数: 1089
- HTML全文浏览量: 19
- PDF下载量: 1124
- 被引次数: 0
出版历程
- 收稿日期: 2009-04-01
- 修回日期: 2009-06-12

A study on particulate silica in the northern part of the South China Sea in winter

1.
Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao 266100, China
2.
Laboratory of Ocean Dynamic Processes and Satellite Oceanography, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China
3.
Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao 266100, China;State Key Laboratory of Estuary and Coast, Eastchina Normal of University, Shanghai 200062, China

摘要

摘要: 对冬季南海北部陆架锋区的悬浮颗粒态生物硅(Particulate Biogenic Silica,PBSi)和成岩硅(Lithogenic Silica,LSi)含量进行了调查分析,讨论了悬浮颗粒态生物硅分布及其影响因素。结果表明,南海北部陆架区悬浮颗粒态生物硅和成岩硅平均含量分别为0.59和8.93μmol/dm³。生物硅分布与水团关系密切:在营养盐充足的沿岸水生物硅含量高(1.0μmol/dm³);而在营养盐缺乏的陆架表层水生物硅含量低(0.23μmol/dm³);在两种水团过渡区生物硅含量居中(0.65μmol/dm³)并与溶解硅酸盐(Dissolved Silicate,DSi)成显著正相关(R=0.48,N=44,P=0.001,a=0.01)。此外锋面位置也直接影响生物硅的含量与分布。大部分调查海区被高温高盐低营养盐海水占据,因此导致了调查海区以低浓度的生物硅和成岩硅为特征,且与世界其他海区相比,生物硅含量处于低值区。
- 生物硅 /
- 成岩硅 /
- 分布 /
- 陆架锋 /
- 南海北部
Abstract: The distribution of particulate biogenic silica (PBSi) and lithogenic silica (LSi) were studied in the northern part of South China Sea in winter 2004.The average concent rations of PBSi and LSi were 0.59 and 8.93 μmol/dm³,respectively.Due to the intrusion of off shore seawater,the concentrations of PBSi decreased greatly from the coastal water (1.0μmol/dm³) to the offshore water (0.23μmol/dm³),just like the distribution of dissolved silicate (DSi),which is related to the water mass and shelf front.The concentration of PBSi in the northern part of South China Sea is ranked at the lower end among the world coastal areas.
- biogenic silica /
- lithogenic silica /
- distribution /
- shelf front /
- South China Sea

HTML全文

参考文献(57)

RAGUENEAU O,TREGUER P,LEYNAERT A,et al.A review of the Si cycle in the modern ocean:recent progress and missing gaps in the application of biogenic opal as a paleoproductivity proxy[J].Global and Planetary Change,2000,26(4):317-365.

BUESSELER K O.The decoupling of production and particulate export in the surface ocean[J].Global Biogeochemistry Cycles,1998,12:297-310.

LIU S M,YE X W,ZHANG J,et al.The silicon balance in Jiaozhou Bay,North China[J].Journal of Marine Systems,2008,74(1/2):639-648.

GOLDMAN J G.Spatial and temporal discontinuities of biological processes in pelagic surface waters[M]// Rothschild B J.Toward a Theory of Biological-Physical Interactions in the World Ocean.Dordrecht:Kluwer Academic Publishing,1988:273-296.

GOLDMAN J C.Potential role of large oceanic diatoms in new primary production[J].Deep-Sea Res,1993,40:159-168.

NELSON D M,TREGUER P,BRZEZINSKI M A,et al.Production and dissolution of biogenic silica in the oceans revised global esti-mates,comparison with regional data and relationship to biogenic sedimentation[J].Global Biogeochemistry Cycles,1995,9:359-372.

CUSHING D H.A difference in structure between ecosystems in strongly stratified waters and in those that are only weakly stratified[J].Journal of Plankton Research,1989,11(1):1-13.

NIXON S W,AMMERMAN J W,Atkinson L,et al.The fate of nitrogen and phosphorus at the land-sea margin of the North Atlantic Ocean[J].Biogeochemistry,1996,35:141-180.

HOWARTH R W,BILLEN G,SWANEY D,et al.Regional nitrogen budgets and riverine inputs of N &P for the drainages to the North Atlantic Ocean:natural and human influences[J].Biogeochemistry,1996,35:75-139.

Conley D J,Schelske C L,Stoermer E P.Modification of the biogeochemical cycle of silica with eutrophication[J].Marine Ecology Pro-gress Series,1993,101:179-192.

HUMBORG C,ITTEKOT V,COCIASU A,et al.Effect of Danube river dam on Black Sea biogeoehemistry and ecosystem structure[J].Nature,1997,386:385-388.

HUMBORG C,SEMDBERG E,MEDINA M R,et al.Changes in dissovled silicate loads to the Baltic Sea-The effects of lakes and reservoirs[J].Journal of Marine Systems,2007,73:223-235.

DELAMO Y,QUEGUINER B,Tréguer P,et al.Impacts of high-nitrate freshwater inputs on macrotidal ecosystems:Ⅱ.Specific role of the silicic acid pump in the year-round dominance of diatoms in the Bay of Brest(France)[J].Marine Ecology Progress Series,1997,161:225-237.

RAGUENEAU O,CHAUVAND L,LEYNAERT A,et al.Direct evidence of a biologically active coastal silicate pump:Ecological im-plications[J].Limnology and Oceanography,2002,47(6):1849-1854.

TREGUER P,NELSON D M,Van BENNEKOM A J,et al.The silica balance in the world ocean:A reestimate[J].Science,1995,268:375-379.

SÁNCHEZ G E,PANTOJA S,LANGE C B,et al.Seasonal changes in particulate biogenic silica and lithogenic silica in the upwelling system off concepcion(～36°S),Chile,and their relationship to fluctuations in marine productivity and continental input[J].Continen-tal Shelf Research,2008,28:2594-2600.

DERRY L A.KURTZ A C.ZIEGLER K,et al.Biological control of terrestial silica cycling and export fluxes to watersheds[J].Na-ture,2005,433:728-731.

NELSON D M,BRZEZINSKI M A.Diatom growth and productivity in an oligotrophic midocean gyre:A3-yr record from the Sargasso Sea near Bermuda[J].Limnology and Oceanography,1997,42:473-486.

OWEN R W.Fronts and eddies in the sea:mechanisms,interactions and biological effects[M]//Longhurst A R.Analysis of Marine E-cosystems.Orlandol Academic Press,1981:197-233.

Le FÈVRE J.Aspects of the biology of frontal systems[J].Advances in Marine Biology,1986.23:163-299.

FEDOROV K N.The physical nature and structure of oceanic fronts[M].New York:Springer-Verlag,1986:1-7.

冯士筰.李风歧,李少普.海洋科学导论[M].北京:高等教育出版社,1999:477-479.

SU J.Overview of the South China Sea circulation and its influence on the coastal physical oceanography outside the Pearl River Estuary[J].Continent Shelf Research,2004,24:1745-1760.

许建平,苏纪兰.黑潮水人侵南海的水文分析:Ⅱ.1994年8-9月观测结果[J].热带海洋,1997,16(2),1-23.

OILSON D B,HITCHCOCK G L,MARIANO A J,et al.Life on the edge:marine life and fronts[J].Oceanography.1994.7(2):52-60.

周菊珍,谷国传.长江河口夏季营养盐的分布、变化及锋面对营养盐的影响[J].广州环境科学,2002,17(1):1-5.

刘桂梅,孙松,王辉,等.春秋季黄海海洋锋对中华哲水蚤分布的影响[J].自然科学进展,2002,12(11):1150-1154.

陈长胜.海洋生态系统动力学与模型[M].北京:高等教育出版社,2003:133-182.

李洪波,等.南黄海潮汐锋对浮游细菌生物量分布的影响[J].生态学报,2004.24(11):2608-2615.

万小芳,潘爱军.郭小刚.台湾海峡表层叶绿素含量的季节、年际变化特征研究[J].台湾海峡.2007,26(l):36-45.

MUELBERT J H,ACHA M,MIANZAN H,et al.Biological,physical and chemical properties at the subtrophical shelf front zone in the SW Atlantic continental shelf[J]Continental Shelf Research,2008,28:1662-1673.

王汝建,房殿勇,邵磊,等.南海北部陆坡渐新世的蛋白石沉积[J].中国科学D辑,2001.31(10):867-872.

贾国东,彭平安,傅家谟.珠江口近百年来富营养化加剧的沉积记录[J].第四纪研究,2002,22(2):158-165.

李家英.南海北部陆坡ODP 1144站位第四纪硅藻及其古环境演变[J].地质论评,2002,48(5);542-551.

黄元辉.蓝东兆.南海东北部末次冰期以来的沉积环境演变[J].海洋地质与第四纪地质,2005.25(4):9-14.

HU J,ZHANG G,LI K,et al.Increased eutrophication offshore Hong Kong.China during the past 75 yearsl Evidence from high-reso-lution sedimentary records[J].Marine Chemistry,2008,110(1/2):7-17.

RAGYENEAU O,SAUOYE N,AMO Y D,et al.A new method for the measurement of biogenic silica in suspended matter of coastal waters:using Si:AI ratios to correct for the mineral interference[J].Continental Shelf Research,2005.25:697-710.

罗忻.胶州湾、东海悬浮颗粒态生物硅的研究[D].青岛:中国海洋大学.2006.

MULLIN J B,RILEY J P.The colorimetric determination of silicate with special reference to sea and natural waters[J].Analytica Chimica Acta,1955,12:162-176.

REN J L.ZHANG J,LUO J Q,et al.Improved fluorimetric determination of dissolved aluminium by micelle-enhaced lumogallion com-plex in natural waters[J].The Royal Society of Chemistry:The Analyst,2001,126:698-702.

陈洪涛,张欣泉,米铁柱,等.悬浮颗粒物中生物硅测定方法的改进与应用[J].海洋学报,2007,29(4):156-160.

王磊.南海北部陆架区域的海洋锋及锋面涡旋研究[D].青岛:中国海洋大学.2004.

程岩.胶州湾、东海和南海部分海区中溶解态砷的行为[D].青岛:中国海洋大学,2005.

GBW07334,南海海洋沉积物成分分析标准物质[S].

李凤岐,苏育嵩.海洋水团分析[M].青岛:青岛海洋大学出版社.2000.

彭欣,宁修仁,孙军,等.南海北部浮游植物生长对营养盐的响应[J].生态学报,2006.26(12):3959-3968.

袁梁英.南海北部营养盐结构特征[D].厦门:厦门大学,2005.

孙军,宋书群,乐风凤,等.2004年冬季南海北部浮游植物[J].海洋学报,2007,29(5):132-145.

乐风凤,宁修仁,刘诚刚,等.2006年冬季南海北部浮游植物生物量和初级生产力及其环境调控[J].生态学报.2008,28(11):5775-5784.

YIN K.Influence of monsoons and oceanographic process on red tides in Hong Kong wtaers[J].Marine Ecology Progress Series.2003.262:27-41.

PARTENSKY F,BLANCHOT J.VAULOT D.Differential distribution and ecology of Prochloroccus and Synechococcus in ocenic wa-ters:a review[J].Bulletin de l'Institut océanographique,Monaco(n°spécial),1999,19:457-475.

PAN L A,ZHANG J.CHEN Q,et al.Picoplankton community structure at a coastal front region in the northern part of the South China Sea[J].Journal of Plankton Research,2005,28(3):337-343.

李小斌,陈楚群,施平,等.南海1998-2002年初级生产力遥感估算及其时空演化机制[J].热带海洋学报,2006.25(3):52-57.

庞海龙.珠江冲淡水扩散路径分析[D].青岛:中国海洋大学,2006.

罗忻,刘索美,张经,等.胶州湾悬浮颗粒态生物硅的研究[J].中国海洋大学学报(自然科学版),2008,38(4):627-634.

LIU SM,ZHANG J,LI R X.Ecological significance of biogenic silica in the East China Sea[J].Marine Ecology Progress Series,2005,290:15-26.

FIRME G,RUE E,WEEKS D,et al.Spatial and temporal variability in phytoplankton iron limitation along the California coast and consequences for Si,N,and C biogeochemistry[J].Global Biogeochemical Cycle,2003,17:1016-1029.

施引文献

资源附件(0)

访问统计