南黄海浮游植物初级生产力粒级结构与碳流途径分析
Size structure and potential export of phytoplankton primary production in the southern Huanghai(Yellow) Sea
-
摘要: 根据2006年夏季与冬季南黄海真光层内浮游植物初级生产速率的实测数据,对比研究了两种差异显著的水动力条件下,不同粒级浮游植物初级生产力水平、时空分布特征及其环境调控机制,并探讨了真光层生源碳可能的碳流途径。研究结果表明,南黄海夏季总初级生产力(碳)平均为30.69 mg/(m2·h),高值区位于调查海域南部长江冲淡水影响区,冬季总初级生产力低于夏季,平均水平为21.73 mg/(m2·h),高值区北迁至海州湾附近;夏季不同粒径浮游植物对总初级生产的贡献率由高到低的顺序为小型(42.8%)、微型(29.6%)、微微型(27.6%),冬季的为微微型(41.2%)、微型(36.5%)、小型(22.3%);真光层初级生产力与环境因子的相关分析表明,水动力条件(混合与层化)引起的营养盐来源和光照的变化是初级生产力分布的主要控制因素;用生态比值法对南黄海碳流途径的分析表明,微食物环在冬夏两季碳流途径中均占有重要地位,从总体上看,南黄海浮游生态系统的碳输出潜力较弱。Abstract: The distribution and environmental control of total and size-fractionated phytoplankton primary production in the Southern Huanghai(Yellow) Sea were studied based on the investigation conducted under summer stratification and winter mixing conditions in 2006.The mean level of euphotic zone integrated primary production in summer and winter were 30.69 mg/(m2·h) and 21.73 mg/(m2·H) respectively.High levels of primary production were observed in the Changjiang River diluted water influenced area in summer, while in winter the high level zone shifted northerly to the adjacent of Haizhou Bay. The relative contributions of different size fractions of phytoplankton were in the sequence of micro(42.8%) >nano (29.6%)>pico(27.6%) in summer and pico(41.2%)> nano(36.5%) > micro(22.3%) in winter. The relationships between the primary production and environmental factors showed that the variations of nutrients availability and light regimes driven by the hydrodynamic conditions were the main causes of primary production distribution features. The food-web mediated carbon pathway and potential export were also qualitatively analyzed with simple ecological ratios. Microbial food web played important roles both in summer and in winter, and in general the pelagic ecosystem of the southern Huanghai Sea showed a weak carbon export potential.
-
Key words:
- southern Huanghai(Yellow) Sea /
- phytoplankton /
- primary production /
- size structure /
- carbon pathway
-
FORTIER L,LE FeVRE J,LEGENDRE L.Export of biogenic carbon to fish and to the deep ocean,the role of large planktonic mirophages[J].Journal of Plankton Research,1994,16:809-839. LEGENDRE L,RASSOULZADEGAN F.Food-web mediated export of biogenic carbon in oceans:hydrodynamic control[J].Marine Ecology Progressive Series,1996,145:179-193. FALKOWSKI P G,BARBER R T,SMETACEK V.Biochemical controls and feedbacks on ocean primary production[J].Science,1998,281:200-206. FRONEMAN P W,PAKHOMOV E A,BALARIN M G.Size-fractionated phytoplankton biomass,production and biogenic carbon flux in the eastern Atlantic sector of the Southern Ocean in late austral summer 1997-1998[J].Deep-Sea research Ⅱ,2004.51:2715-2729. CERMEÑO P,MARAÑÓN E,PÉREZ V,et al.Phytoplankton size structure and primary production in a highly dynamic coastal ecosystem (Ria de Vigo,NW-Spain): seasonal and short-time scale variability[J].Estuarine,Coastal and Shelf Science,2006,67:251-266. COTTINGHAM K L.Nutrients and zooplankton as multiple stressors of phytoplankton communities,evidence from size structure[J].Limnology and Oceanography,1999,44:810-827. TILSTONE G H,FIGUE1RAS F G,FERMiN E G,et al.Significance of nanophytoplankton photosynthesis and primary production in a coastal upwelling system (Rade Vigo,NW Spain)[J].Marine Ecology Progress Series,1999,183:13-27. JENNINGS S.Size-based analyses of aquatic food webs[M]//BERGRANO A,SCHARLER U M,DUNNE J,ULANOWICZ RE.Aquatic Food Webs.New York:Oxford University Press,2005,86-97. CHEN B Z,LIU H B,WANG Z L.Trophic interacitons within the microbial food web in the South China Sea revealed by size-fraction method[J].Journal of Experimental Marine Biology and Ecology,2009,368:59-66. LE BOUTEILIER A,BLANCHOT J,RODIER M.Size distribution of phytoplankton in the western Pacific:Towards a generalization for the tropical open ocean[J].Deep-Sea Research,1992,39:805-823. SAVIDGE G,GIOPIN L.Seasonal influences on size-fractionated chlorophyll a concentrations and primary production in the north-west Indian Ocean[J].Deep-Sea Research,1999,46:701-723. POULTON A J,HOLLIGAN P M,HICHMAN A,et al.Phytoplankton carbon fixation,chlorophyll-biomass and diagnostic pigments in the Atlantic Ocean[J].Deep-Sea Research Ⅱ,2006,53:1593-1610. CHISHOLM S W.Phytoplankton size[M].FALKOWSKI P G,WOODHEAD A D.Primary Productivity and Biogeochemical Cycles in the Sea.New York:Plenum,1992,213-237. AGAWIN N R S,DUARTE C M,AGUSTi S.Nutrient and temperature control of the contribution of picoplankton to phytoplankton biomass and production[J].Limnology and Oceanography,2000,45:591-600. CULLEN J J,FRANKS P J S,KARL D M,et al.Physical influences on marine ecosystem dynamics[J].ROBINSON A R,MCCARTHY J J,ROTHCHILD B J.The Sea,Vol.12[M].New York:John Wiley,2002,297-336. 黄邦钦,刘嫒,陈纪新,等.东海、黄海浮游植物生物量的粒级结构及时空分布[J].海洋学报,2006,28(2):156-164. 邓春梅,于志刚,姚鹏,等.东海、南黄海浮游植物粒级结构及环境影响因素分析[J].中国海洋大学学报,2008,38(5):791-798. 乐凤凤,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. 宁修仁,刘子琳,蔡昱明,等.渤海晚春浮游植物粒度分级生物量与初级生产力[J].海洋科学集刊,2002,44:22-33. PERISSINOTTO R,DUNCOMBE RAE C M,BODEN B P,et al.Vertical stability as a controlling factor of the marine phytoplankton production at the Prince Edward Archipelago (Southern Ocean)[J].Marine Ecology Progress Series,1990,60:205-209. RODRÍ GUÉZ J,TINTOREJ,ALLEN J T,et al.Mesoscale vertical motion and the size structure of phytoplankton in the ocean[J].Nature,2001,410:360-363. RIEGMAN R,KUIPERS B R,NOORDELOOS A A M,et al.Size-differential control of phytoplankton and the structure of plankton communities[J].Netherlands Journal of Sea Research,1993,31:255-265. KI(O)RBOE T.Turbulence,phytoplankton cell size and the structure of pelagic food webs[J].Advances in Marine Biology,1993,29;1-72. VARELA M,FERNANDEZ E,SERRET P.Size-fractionated phytoplankton biomass and primary production in the Gerlache and south Bransfield Straits (Antarctic Peninsula) in Austral summer 1995-1996[J].Deep-Sea Research Ⅱ,2002,49:749-768. ZHANG S W,WANG Q Y,LÜ Y,et al.Observation of the seasonal evolution of the Yellow Sea Cold Water Mass in 1996-1998[J].Continental Shelf Research,2008,28:442-457. MASK A C,O'BRIEN J J,PRELLER R.Wind-driven effects on the Yellow Sea Warm Current[J].Journal of Geophysical Research,1998,103,30713-30729. QIAO F,MA J,XIA C,et al.Influence of the surface wave induced and tidal mixing on vertical temperature of the Yellow and East China Seas in summer[J].Progress in Natural Science,2006,16 (7):739-746. YUAN Y,SU J.Numerical modeling of the circulation in the East China Sea[C]//ICHIYE T.Ocean Hydrodynamics of the Japan and East China Seas,Vol.39.Amsterdam-.Elsevier Oceanography Series,1984:167-176. STEEMAN-NIELSEN E.The use of radioactive carbon (14C) for measuring organic production in the sea[J].Journal Conseil Perm.International Exporation Mer,1952,18:117-140. MOUSSEAU L,KLEIN B,LEGENDRE L,et al.Assessing trophic pathway that dominate planktonic food webs:an approach based on simple ecological ratios[J].Journal of Plankton Research,2001,23(8):765-777. DECEMBRINI F,CAROPPO C,AZZARO M.Size structure and production of phytoplankton community and carbon pathways channeling in the southern Tyrrhenian sea (Western Mediterranean)[J].Deep-Sea Ressearch Ⅱ,doi: 10.1016/j.dsr2.2008.07.022. TREMBLAY J E,LEGENDRE L.A model for the size-fractionated biomass and production of marine phytoplankton[J].Limnology and Oceanography,1994,39:2004-2014. LI W K W.Macroecological patterns of phytoplankton in the northwestern North Atlantic Ocean[J].Nature,2002,149:154-157. FRONEMAN P W,PAKHOMOV E A,PERISSINOTTO R,et al.Dynamics of the plankton communities of the Lazarev Sea (Southern Ocean) during seasonal ice melt[J].Marine Ecology Progress Series,1997,149,201-214. DELGADILLO-H1NOJOSA F,GAXIOLA-CASTRO G,SEGOVIA-ZAVALA J A,et al.The effect of vertical mixing on primary production in a bay of the Gulf of California[J].Estuarine,Coastal and Shelf Science,1997,45:135-148. TOWNSENDDW,SPINRAD R W.Early spring phytoplankton blooms in the Gulf of Maine[J].Continental Shelf Research,1986,6:515-529. COLE J J,CARACO N F,PEIERLS B L.Can phytoplankton maintain a positive carbon balance in a turbid,freshwater,tidal estuary[J]. Limnology and Oceanography,1992,37(8):1608-1617. FINKEL Z V,IRWIN A J,SCHOFIELD O.Resource limitation alters the 3/4 size scaling of metabolic rates in phytoplankton[J].Marine Ecology Progress Series,2004,273:269-279. TREMBLAY J E,KLEIN B,LEGENDRE L.Estimation of f-ratio in oceans based on phytoplankton size structure[J].Limnology and Oceanography,1997,42(3):595-601. 江春渡,张龙军,王峰.南黄海夏季海水pCO2究Ⅱ——下层海水涌升和长江冲淡水对海-气界面CO2通量的贡献[J].中国海洋大学学报,2006,36(Sup.):147-152. RICHARDSON T L,JACKSON G A.Small phytoplankton and carbon export from the surface ocean[J].Science,2007,315:838-840.
点击查看大图
计量
- 文章访问数: 1398
- HTML全文浏览量: 5
- PDF下载量: 1185
- 被引次数: 0