Growth rate relationships to physiological, indices of nutrient status in marine diatoms

被引:15
作者
Clark, DR [1 ]
机构
[1] Univ Coll Swansea, Sch Biol Sci, Ecol Res Unit, Swansea SA2 8PP, W Glam, Wales
关键词
carbon; chl a : C; nutrient limitation; N : C ratio; nitrogen; stress; Thalassiosira;
D O I
10.1046/j.1529-8817.2001.037002249.x
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
The growth of two species of marine diatom, Thalassiosira weissflogii (Grunow) and Thalassiosira pseudonana (Hustedt), was followed in batch cultures at four concentrations of dissolved inorganic carbon from N- and C-replete lag phase into N- and/or C-deplete stationary phase. Results describe the relationship between carbon-specific growth rate (mu (C)) and chi EI:carbon (chl a:C) and glutamine:glutamate (gln:glu) ratios with changes in the cells' nutritional status (N:C), during the utilization of either NO(3)(-) or NH(4)(+). The use of the gln:glu ratio as an index of N:C requires further clarification. For both species and N sources, N stress resulted in a decrease in mu (C), chi a:C, and N:C relative to mu (Cmax) values, whereas C stress resulted in a decrease in mu (C) and an increase in chi a:C and N:C relative to mu (Cmax) values. Both species attained a chi a:C ratio of approximately 15 mug.g(-1) at mu (Cmax) using either N source. However, this value was not necessarily an indicator of maximal growth rate. NC colimitation resulted in decreased mu (C) to values less than 20% of mu (Cmax) with only minor changes in chi a:C and N:C relative to mu (Cmax) values. Chi a:C results suggest a similarity between the light stress and C stress responses of marine diatoms, The potential for C stress in the marine environment needs to be addressed.
引用
收藏
页码:249 / 256
页数:8
相关论文
共 40 条
[1]   CARBONIC-ANHYDRASE AND CO2 CONCENTRATING MECHANISMS IN MICROALGAE AND CYANOBACTERIA [J].
AIZAWA, K ;
MIYACHI, S .
FEMS MICROBIOLOGY LETTERS, 1986, 39 (03) :215-233
[2]  
BADGER MR, 1992, PHYSIOL PLANTARUM, V84, P606, DOI 10.1111/j.1399-3054.1992.tb04711.x
[3]   Biomass, growth rates and limitation of Equatorial Pacific diatoms [J].
Blain, S ;
Leynaert, A ;
Treguer, P ;
ChretiennotDinet, MJ ;
Rodier, M .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 1997, 44 (07) :1255-1275
[4]  
BUTLER NB, 1982, CARBON DIOXIDE EQUIL, P44
[5]   Utilization of dissolved inorganic carbon (DIC) and the response of the marine flagellate Isochrysis galbana to carbon nitrogen stress [J].
Clark, DR ;
Merrett, MJ ;
Flynn, KJ .
NEW PHYTOLOGIST, 1999, 144 (03) :463-470
[6]   The relationship between the dissolved inorganic carbon concentration and growth rate in marine phytoplankton [J].
Clark, DR ;
Flynn, KJ .
PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES, 2000, 267 (1447) :953-959
[7]   TEMPORAL CHANGES IN THE INORGANIC CARBON SYSTEM OF THE SOUTHEASTERN BERING SEA DURING SPRING 1980 [J].
CODISPOTI, LA ;
FRIEDERICH, GE ;
IVERSON, RL ;
HOOD, DW .
NATURE, 1982, 296 (5854) :242-245
[8]  
COLMAN JR, 1991, PLANT CELL ENVIRON, V14, P861
[9]   THE DEEP CHLOROPHYLL MAXIMUM - COMPARING VERTICAL PROFILES OF CHLOROPHYLL-A [J].
CULLEN, JJ .
CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES, 1982, 39 (05) :791-803
[10]   CHLOROPHYLL-A FLUORESCENCE IN PHYTOPLANKTON - RELATIONSHIP TO PHOTOSYNTHESIS AND BIOMASS [J].
FALKOWSKI, P ;
KIEFER, DA .
JOURNAL OF PLANKTON RESEARCH, 1985, 7 (05) :715-731