Hu Caiqin, Li Xiangfu, He Maoqiu, Jiang Peng, Long Aimin, Xu Jie
State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China.
College of Marine Science, University of Chinese Academy of Sciences, Beijing, China.
Front Microbiol. 2021 Feb 26;12:583982. doi: 10.3389/fmicb.2021.583982. eCollection 2021.
Increasing anthropogenic CO emissions in recent decades cause ocean acidification (OA), affecting carbon cycling in oceans by regulating eco-physiological processes of plankton. Heterotrophic bacteria play an important role in carbon cycling in oceans. However, the effect of OA on bacteria in oceans, especially in oligotrophic regions, was not well understood. In our study, the response of bacterial metabolic activity and community composition to OA was assessed by determining bacterial production, respiration, and community composition at the low-CO (400 ppm) and high-CO (800 ppm) treatments over the short term at two oligotrophic stations in the northern South China Sea. Bacterial production decreased significantly by 17.1-37.1 % in response to OA, since bacteria with high nucleic acid content preferentially were repressed by OA, which was less abundant under high-CO treatment. Correspondingly, shifts in bacterial community composition occurred in response to OA, with a high fraction of the small-sized bacteria and high bacterial species diversity in a high-CO scenario at K11. Bacterial respiration responded to OA differently at both stations, most likely attributed to different physiological responses of the bacterial community to OA. OA mitigated bacterial growth efficiency, and consequently, a larger fraction of DOC entering microbial loops was transferred to CO.
近几十年来,人为排放的二氧化碳不断增加,导致海洋酸化(OA),通过调节浮游生物的生态生理过程影响海洋中的碳循环。异养细菌在海洋碳循环中起着重要作用。然而,海洋酸化对海洋细菌的影响,尤其是对贫营养区域细菌的影响,尚未得到充分了解。在我们的研究中,通过在南海北部两个贫营养站点对低二氧化碳(400 ppm)和高二氧化碳(800 ppm)处理进行短期测定细菌生产力、呼吸作用和群落组成,评估了细菌代谢活性和群落组成对海洋酸化的响应。由于高核酸含量的细菌优先受到海洋酸化的抑制,而在高二氧化碳处理下这类细菌数量较少,细菌生产力因海洋酸化显著下降了17.1%-37.1%。相应地,细菌群落组成因海洋酸化而发生变化,在K11站点的高二氧化碳环境下,小型细菌比例较高且细菌物种多样性也较高。两个站点的细菌呼吸作用对海洋酸化的响应不同,这很可能归因于细菌群落对海洋酸化的不同生理反应。海洋酸化降低了细菌生长效率,因此,进入微生物环的溶解有机碳中更大比例被转化为二氧化碳。