Composition and dynamics of the phytoplankton of the Ionian Sea (eastern Mediterranean) -: art. no. 8116

被引:70
作者
Casotti, R
Landolfi, A
Brunet, C
D'Ortenzio, F
Mangoni, O
d'Alcalà, MR
Denis, M
机构
[1] Stn Zool A Dohrn, I-80121 Naples, Italy
[2] Lab Oceanog & Biogeochim, F-13288 Marseille 09, France
关键词
ultraplankton; flow cytometry; primary productivity; Mediterranean Sea; mixing; photoacclimation;
D O I
10.1029/2002JC001541
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
[1] The relationship between phytoplankton distribution and dynamics, and the resident water masses in the Ionian Sea was investigated in the spring of 1999 by flow cytometry, HPLC, microscopy, C-14 incorporation, and serial dilutions. More than 50% of total biomass was represented by ultraphytoplankton, with proportions increasing with depth (up to 80%) and eastward (up to 60%). Synechococcus sp. cyanobacteria dominated ultraphytoplankton numbers and biomass. Hydrological stability explained the relative vertical distribution of Synechococcus sp. and Prochlorococcus sp. cyanobacteria and their degree of photoacclimation. The northwestern area ("Italian Side'') was in a transition from bloom to oligotrophic conditions, reflected in high biological instability in terms of phytoplankton composition, photoacclimative properties, and photosynthetic efficiency (P/B of 11.40 mg C mg chl(-1) h(-1)). The influence of the Adriatic Surface Water, carrying a trace of the spring bloom was visible from satellite imagery (SeaWiFS). The eastern part of the sampled area ("Greek Side,'' GS) was hydrologically more stable (low estimated vertical velocities), resulting in higher photosynthetic efficiency (P/B of 20.47 mg C mg chl(-1) h(-1)) and phytoplankton photoacclimative properties. The Atlantic Water (AW) was the most oligotrophic in terms of nutrient concentration, chla, and productivity (208.0 mg C m(-2) d(-1)), but also the most variable in terms of mesoscale features. Growth of Synechococcus sp. and Prochlorococcus sp. was slow (0.36 d(-1) at max), while picoeukaryotes grew well in the deep chlorophyll maximum (DCM) of the GS (0.67 d(-1)) Picoeukaryote growth was tightly coupled with grazing (0.80 d(-1)), indicating efficient biomass recycling. Biological characterization and DCM dynamics in the three areas are discussed in relation to physical features present at the time of sampling.
引用
收藏
页数:19
相关论文
共 123 条
[81]   Enumeration and cell cycle analysis of natural populations of marine picoplankton by flow cytometry using the nucleic acid stain SYBR Green I [J].
Marie, D ;
Partensky, F ;
Jacquet, S ;
Vaulot, D .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 1997, 63 (01) :186-193
[82]  
MARTIN V, 1997, THESIS U MEDITERR AI
[83]   NITROGENOUS NUTRITION OF MARINE-PHYTOPLANKTON IN NUTRIENT-DEPLETED WATERS [J].
MCCARTHY, JJ ;
GOLDMAN, JC .
SCIENCE, 1979, 203 (4381) :670-672
[84]   Oceanic 18S rDNA sequences from picoplankton reveal unsuspected eukaryotic diversity [J].
Moon-van der Staay, SY ;
De Wachter, R ;
Vaulot, D .
NATURE, 2001, 409 (6820) :607-610
[85]   COMPARATIVE PHYSIOLOGY OF SYNECHOCOCCUS AND PROCHLOROCOCCUS - INFLUENCE OF LIGHT AND TEMPERATURE ON GROWTH, PIGMENTS, FLUORESCENCE AND ABSORPTIVE PROPERTIES [J].
MOORE, LR ;
GOERICKE, R ;
CHISHOLM, SW .
MARINE ECOLOGY PROGRESS SERIES, 1995, 116 (1-3) :259-275
[86]   Physical-biological coupling in the Algerian Basin (SW Mediterranean):: Influence of mesoscale instabilities on the biomass and production of phytoplankton and bacterioplankton [J].
Morán, XAG ;
Taupier-Letage, I ;
Vázquez-Dominguez, E ;
Ruiz, S ;
Arin, L ;
Raimbault, P ;
Estrada, M .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 2001, 48 (02) :405-437
[87]  
MOREL A, 2000, IBBP BOOK SER, V5, P338
[88]   Primary production, carbon export and nutrients availability in western and eastern Mediterranean Sea in early summer 1996 (MINOS cruise) [J].
Moutin, T ;
Raimbault, P .
JOURNAL OF MARINE SYSTEMS, 2002, 33 :273-288
[89]   Does competition for nanomolar phosphate supply explain the predominance of the cyanobacterium Synechococcus? [J].
Moutin, T ;
Thingstad, TF ;
Van Wambeke, F ;
Marie, D ;
Slawyk, G ;
Raimbault, P ;
Claustre, H .
LIMNOLOGY AND OCEANOGRAPHY, 2002, 47 (05) :1562-1567
[90]  
NEVEUX J, 1987, ARCH HYDROBIOL, V109, P567