全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
科学通报  2014 

2008年夏季南海北部浮游藻类生物量和群落组成特征及其影响因素:生物标记物研究

DOI: 10.1360/csb2014-59-11-1016, PP. 1016-1025

Keywords: 藻类标志物,生物量,生物群落,南海海洋水文动态

Full-Text   Cite this paper   Add to My Lib

Abstract:

利用海水悬浮颗粒物中的藻类标志物分子,探讨了以生物标志物为基础的海洋生物群落和生物量的变化特征及其影响因素.研究表明,2008年夏季南海北部典型海域浮游植物生物标志物真实地反映了该海域现代浮游植物群落生物量的变化和更替规律.受南海不同水文状况等因素的影响和制约,表现为典型的区域分布特征高丰度的浮游植物主要出现在珠江口海域、台湾岛西南岸外、海南岛东南附近海域;而海盆和海峡海域的含量相对较低.硅藻在整个研究海域的生物量占绝对优势,其次为甲藻,但随着离岸距离的增加,颗石藻的生物量和相对比例逐渐增多.本文研究显示脂类标志物分子真实地记录了调研季节南海浮游藻类的生物量和群落组成变化特征及其与海洋水文特征的关联,该研究不仅为脂类分子的现代海洋生态及结构变化应用提供基础,更将为古海洋群落结构的真实重建提供重要的科学依据.

References

[1]  2 Falkowski P G, Laws E A, Barber R T, et al. Phytoplankton and their role in primary, new, and export production. In: Fasham M J R, ed. Ocean Biogeochemistry: The Role of the Ocean Carbon Cycle in Global Change. New York: Springer, 2003. 99-121
[2]  4 Harrison K G. Role of increased marine silica input on paleo-pCO2 levels. Paleoceanography, 2000, 15: 292-298
[3]  9 Zhao M X, Mercer J L, Eglinton G, et al. Comparative molecular biomarker assessment of phytoplankton paleoproductivity for the last 160 kyr off Cap Blanc, NW Africa. Org Geochem, 2006, 37: 72-97
[4]  10 丁玲, 邢磊, 赵美训. 生物标志物重建浮游植物生产力及群落结构研究进展. 地球科学进展, 2010, 25: 981-989
[5]  11 Volkman J K, Barrett S M, Blackburn S, et al. Microalgal biomarkers, a review of recent research developments. Org Geochem, 1998, 29: 1163-1179
[6]  12 李丽, 王慧, 李健如, 等. 南海西部45万年来的表层水温变化. 科学通报, 2009, 54: 1269-1277
[7]  14 Ning X, Chai F, Xue H, et al. Physical-biological oceanographic coupling influencing phytoplankton and primary production in the South China Sea. J Geophys Res, 2004, 109, doi: 10.1029/2004JC002365
[8]  18 郝锵, 宁修仁, 刘诚刚, 等. 南海北部初级生产力遥感反演及其环境调控机制. 海洋学报, 2007, 29: 58-68
[9]  23 Jing Z Y, Qi Y Q, Hua Z L, et al. Numerical study on the summer upwelling system in the northern continental shelf of the South China Sea. Cont Shelf Res, 2009, 29: 467-478
[10]  24 Ning X, Lin C, Hao Q, et al. Long term changes in the ecosystem in the northern South China Sea during 1976-2004. Biogeosciences, 2009, 6: 2227-2243
[11]  29 Chen Y L. Spatial and seasonal variations of nitrate-based new production and primary production in the South China Sea. Deep-Sea Res Part I-Oceanogr Res Pap, 2005, 52: 319-340
[12]  30 Gan J P, Li L, Wang D X, et al. Interaction of a river plume with coastal upwelling in the northeastern South China Sea. Cont Shelf Res, 2009, 29: 728-740
[13]  35 李涛, 刘胜, 王桂芬, 等. 2004年秋季南海北部浮游植物组成及其数量分布特征. 热带海洋学报, 2010, 29: 65-73
[14]  36 Jiang Y W, Chai F, Wan Z W, et al. Characteristics and mechanisms of the upwelling in the southern Taiwan Strait: A three-dimensional numerical model study. J Oceanogr, 2011, 67: 699-708
[15]  37 赵美训, 赵晓晨, 陈建芳, 等. 南海表层沉积物生物标志物的分布特征及古生产力重建意义. 热带海洋学报, 2009, 28: 45-53
[16]  38 Chu P C, Li R. South China Sea isopycnal-surface circulation. J Phys Oceanogr, 2000, 30: 2419-2438
[17]  41 Xu J P, Shi M, Zhu B K, et al. Several characteristics of water exchange in the Luzon Strait. Acta Oceanol Sin, 2004, 23: 11-22
[18]  49 Li K Z, Yin J Q, Huang L M, et al. Monsoon-forced distribution and assemblages of appendicularians in the northwestern coastal waters of South China Sea. Estuar Coast Shelf Sci, 2010, 89: 145-153
[19]  1 Falkowski P G, Barber R T, Smetacek V. Biogeochemical controls and feedbacks on ocean primary production. Science, 1998, 281: 200-206
[20]  3 Martin J H, Coale K, Johnson K, et al. Testing the iron hypothesis in ecosystems of the equatorial Pacific Ocean. Nature, 1994, 371: 123-129
[21]  5 李丽, 汪品先. 大洋"生物泵"——海洋浮游植物生物标志物. 海洋地质与第四纪地质, 2004, 24: 73-79
[22]  6 Kohfeld K E, Quéré C L, Anderson R F, et al. Role of marine biology in glacial-interglacial CO2 cycles. Science, 2005, 308: 74-78
[23]  7 Cerme?o P, Dutkiewicz S, Harris R P, et al. The role of nutricline depth in regulating the ocean carbon cycle. Proc Natl Acad Sci USA, 2008, 105: 20344-20349
[24]  8 刘杰, 李丽, 贺娟. 南海海域浮游植物分布特征及研究进展. 海洋地质与第四纪地质, 2010, 30: 133-142
[25]  13 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. 海洋学报, 2003, 25: 8-23
[26]  15 Chen Y L, Chen H Y. Seasonal dynamics of primary and new production in the northern South China Sea: The significance of river discharge and nutrient advection. Deep-Sea Res Part I-Oceanogr Res Pap, 2006, 53: 971-986
[27]  16 乐凤凤, 孙军, 宁修仁, 等. 2004年夏季中国南海北部的浮游植物. 海洋与湖沼, 2006, 37: 238-248
[28]  17 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. 生态学报, 2006, 26: 3960-3967
[29]  19 陈纪新, 黄帮钦, 刘媛, 等. 应用特征光合色素研究东海和南海北部浮游植物的群落结构. 地球科学进展, 2006, 21: 738-746
[30]  20 孙军, 宋书群, 乐凤凤, 等. 2004年冬季南海北部浮游植物. 海洋学报, 2007, 29: 132-145
[31]  21 Han A, Dai M, Kao S-J, et al. Nutrient dynamics and biological consumption in a large continental shelf system under the influence of both a river plume and coastal upwelling. Limnol Oceanogr, 2012, 57: 486-502
[32]  22 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. 海洋学报, 2005, 27: 45-52
[33]  25 Chen Y L, Chen H Y, Karl D M, et al. Nitrogen modulates phytoplankton growth in spring in the South China Sea. Cont Shelf Res, 2004, 24: 527-541
[34]  26 Xu J. Nutrient limitation in the Pearl River Estuary, Hong Kong waters and adjacent South China Sea waters. Doctor Dissertation. Hong Kong: Hong Kong University of Science and Technology, 2007
[35]  27 龙爱民, 陈绍勇, 周伟华. 南海北部秋季营养盐溶解氧, pH值和叶绿素a分布特征及相互关系. 海洋通报, 2006, 25: 10-15
[36]  28 刘玉, 李适宇, 吴仁海, 等. 珠江口四大口门及近滩水域浮游藻类和关键水质因子的监测和分析. 中国环境监测, 2002, 18: 26-29
[37]  31 Gan J P, Lu Z M, Dai M H, et al. Biological Response to intensified upwelling and to a river plume in the northeastern South China Sea: A modeling study. J Geophys Res, 2010, 115: C09001, doi: 10.1029/2009JC005569
[38]  32 Zhao H, Tang D L, Wang D X. Phytoplankton blooms near the Pearl River Estuary induced by Typhoon Nuri. J Geophys Res, 2009, 114: C12027, doi: 10.1029/2009JC005384
[39]  33 Chow C H, Hu J H, Centurioni L R, et al. Mesoscale Dongsha Cyclonic Eddy in the northern South China Sea by drifter and satellite observations. J Geophys Res, 2008, 113: C04018, doi: 10.1029/2007JC004542
[40]  34 宋星宇, 刘华雪, 黄良民, 等. 南海北部夏季基础生物生产力分布特征及影响因素. 生态学报, 2010, 30: 6409-6417
[41]  39 Qu T. Upper-layer circulation in the South China Sea. J Phys Oceanogr, 2000, 30: 1450-1460
[42]  40 Qu T. Evidence for water exchange between the South China Sea and the Pacific Ocean through the Luzon Strait. Acta Oceanol Sin, 2002, 21: 175-185
[43]  42 Tian J W, Yang Q, Liang X, et al. Observation of Luzon Strait transport. Geophys Res Lett, 2006, 33: L19607, doi: 10.1029/2006GL026272.
[44]  43 Yang Q X, Tian J W, Zhao W. Observation of Luzon Strait transport in summer 2007. Deep-Sea Res Part I-Oceanogr Res Pap, 2010, 57: 670-676
[45]  44 Chen G X, Hu P, Hou Y J, et al. Intrusion of the Kuroshio into the South China Sea in September 2008. J Oceanogr, 2011, 67: 439-448
[46]  45 Nan F, Xue H J, Chai F, et al. Identification of different types of Kuroshio intrusion into the South China Sea. Ocean Dyn, 2011, 61: 1291-1304
[47]  46 Su J, Pohlmann T. Wind and topography influence on an upwelling system at the eastern Hainan coast. J Geophys Res, 2009, 114: C06017, doi: 10.1029/2008JC005018
[48]  47 Su J, Wang J, Pohlmann T, et al. Theinfluence of meteorological variation on the upwelling system off eastern Hainan during summer 2007-2008. Ocean Dyn, 2011, 61: 717-730
[49]  48 谢玲玲, 张书文, 赵辉. 琼东上升流研究概述. 热带海洋学报, 2012, 31: 35-41
[50]  50 Xiu P, Chai F, Shi L, et al. A census of eddy activities in the South China Sea during 1993-2007. J Geophys Res, 2010, 115: C03012, doi: 10.1029/2009J C005657

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133