Diel Patterns of Variable Fluorescence and Carbon Fixation of Picocyanobacteria Prochlorococcus-Dominated Phytoplankton in the South China Sea Basin

被引:26
作者
Xie, Yuyuan [1 ]
Laws, Edward A. [2 ]
Yang, Lei [3 ]
Huang, Bangqin [1 ,3 ]
机构
[1] Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen, Peoples R China
[2] Louisiana State Univ, Dept Environm Sci, Baton Rouge, LA 70803 USA
[3] Xiamen Univ, Dept Environm Sci, Xiamen, Peoples R China
基金
国家重点研发计划; 中国国家自然科学基金; 中国博士后科学基金;
关键词
diel variation; variable fluorescence; primary production; photosynthetic parameters; Prochlorococcus; South China Sea basin; nutrient limitation; photosynthetic energetic stoichiometry; CHLOROPHYLL-A FLUORESCENCE; MAXIMUM QUANTUM YIELD; MARINE-PHYTOPLANKTON; PACIFIC-OCEAN; PHOTOSYNTHETIC PARAMETERS; CYANOBACTERIAL PHOTOSYNTHESIS; NATURAL ASSEMBLAGES; COMMUNITY STRUCTURE; ELECTRON-TRANSPORT; IRON LIMITATION;
D O I
10.3389/fmicb.2018.01589
中图分类号
Q93 [微生物学];
学科分类号
071005 ; 100705 ;
摘要
The various photosynthetic apparatus and light utilization strategies of phytoplankton are among the critical factors that regulate the distribution of phytoplankton and primary productivity in the ocean. Active chlorophyll fluorescence has been a powerful technique for assessing the nutritional status of phytoplankton by studying the dynamics of photosynthesis. Further studies of the energetic stoichiometry between light absorption and carbon fixation have enhanced understanding of the ways phytoplankton adapt to their niches. To explore the ecophysiology of a Prochlorococcus-dominated phytoplankton assemblage, we conducted studies of the diel patterns of variable fluorescence and carbon fixation by phytoplankton in the oligotrophic South China Sea (SCS) basin in June 2017. We found that phytoplankton photosynthetic performance at stations SEATS and SS1 were characterized by a nocturnal decrease, dawn maximum, and midday decrease of the maximum quantum yield of PSII (F-v(')/F-m('), which has been denoted as both F-v/F-m and F'(v)/F'(m)) in the nutrient-depleted surface layer. That these diel patterns of F-v(')/ F-m(') were similar to those in the tropical Pacific Ocean suggests macro-nutrient and potentially micro-nutrient stress. However, the fact that variations were larger in the central basin than at the basin's edge implied variability in the degree of nutrient limitation in the basin. The estimated molar ratio of gross O-2 production to net production of carbon (GOP:NPC) of 4.9:1 was similar to ratios reported across the world's oceans. The narrow range of the GOP:NPC ratios is consistent with the assumption that there is a common strategy for photosynthetic energy allocation by phytoplankton. That photo-inactivated photosystems or nonphotochemical quenching rather than GOP accounted for most of the radiation absorbed by phytoplankton explains why the maximum quantum yield of carbon fixation was rather low in the oligotrophic SCS.
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页数:15
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