The acclimation process of phytoplankton biomass, carbon fixation and respiration to the combined effects of elevated temperature and pCO2 in the northern South China Sea

被引:36
|
作者
Gao, Guang [1 ,2 ]
Jin, Peng [1 ]
Liu, Nana [1 ]
Li, Futian [1 ]
Tong, Shanying [1 ]
Hutchins, David A. [3 ]
Gao, Kunshan [1 ]
机构
[1] Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen 361005, Peoples R China
[2] Huaihai Inst Technol, Marine Resources Dev Inst Jiangsu, Lianyungang 222005, Peoples R China
[3] Univ Southern Calif, Dept Biol Sci, Marine Environm Biol, 3616 Trousdale Pkwy, Los Angeles, CA 90089 USA
关键词
Ocean acidification; Ocean warming; Photosynthesis; Primary productivity; Respiration; South China Sea; CO2-INDUCED SEAWATER ACIDIFICATION; SOLAR UV-RADIATION; OCEAN ACIDIFICATION; CONCENTRATING MECHANISMS; PHYSIOLOGICAL-RESPONSES; CO2; CONCENTRATION; GROWTH-RATE; PHOTOSYNTHESIS; COASTAL; DIATOMS;
D O I
10.1016/j.marpolbul.2017.02.063
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We conducted shipboard microcosm experiments at both off-shore (SEATS) and near-shore (D001) stations in the northern South China Sea (NSCS) under three treatments, low temperature and low pCO(2) (LTLC), high temperature and low pCO(2) (HTLC), and high temperature and high pCO(2) (HTHC). Biomass of phytoplankton at both stations were enhanced by HT. HTHC did not affect phytoplankton biomass at station D001 but decreased it at station SEATS. HT alone increased net primary productivity by 234% at station SEATS and by 67% at station D001 but the stimulating effect disappeared when HC was combined. HT also increased respiration rate by 236% at station SEATS and by 87% at station D001 whereas HTHC reduced it by 61% at station SEATS and did not affect it at station D001. Overall, our findings indicate that the positive effect of ocean warming on phytoplankton assemblages in NSCS could be damped or offset by ocean acidification. (C) 2017 Elsevier Ltd. All rights reserved.
引用
收藏
页码:213 / 220
页数:8
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