Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations

© 2015 Elsevier Ltd. Ocean acidification (OA), induced by rapid anthropogenic CO2 rise and its dissolution in seawater, is known to have consequences for marine organisms. However, knowledge on the evolutionary responses of phytoplankton to OA has been poorly studied. Here we examined the coccolitho...

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Bibliographic Details
Published in:Marine Pollution Bulletin
Main Authors: Jin, Peng, Gao, Kunshan
Other Authors: Biological and Environmental Sciences and Engineering (BESE) Division, Environmental Science and Engineering Program, Red Sea Research Center (RSRC), State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen, China
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier BV 2015
Subjects:
Coccolithophore
Evolution
Fitness
Ocean acidification
Phenotypic plasticity
Online Access:http://hdl.handle.net/10754/621459
https://doi.org/10.1016/j.marpolbul.2015.12.039
Description
Summary:© 2015 Elsevier Ltd. Ocean acidification (OA), induced by rapid anthropogenic CO2 rise and its dissolution in seawater, is known to have consequences for marine organisms. However, knowledge on the evolutionary responses of phytoplankton to OA has been poorly studied. Here we examined the coccolithophore Gephyrocapsa oceanica, while growing it for 2000 generations under ambient and elevated CO2 levels. While OA stimulated growth in the earlier selection period (from generations ~700 to ~1550), it reduced it in the later selection period up to 2000 generations. Similarly, stimulated production of particulate organic carbon and nitrogen reduced with increasing selection period and decreased under OA up to 2000 generations. The specific adaptation of growth to OA disappeared in generations 1700 to 2000 when compared with that at 1000 generations. Both phenotypic plasticity and fitness decreased within selection time, suggesting that the species' resilience to OA decreased after 2000 generations under high CO2 selection. This study was supported by the National Natural Science Foundation (No. 41430967 & No. 41120164007), the Joint Project of the NSFC and Shandong province (No. U1406403), and the Strategic Priority Research Program of the Chinese Academy of Sciences (No. XDA11020302). The authors are grateful to Shanying Tong and Nana Liu (students) for their technical assistance and to Wenyan Zhao, Xianglan Zeng and Liting Peng for their kind help with the laboratory logistics. Professor John Hodgkiss is thanked for his help with English.

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