Image_1_Effect of Ocean Acidification on Bacterial Metabolic Activity and Community Composition in Oligotrophic Oceans, Inferred From Short-Term Bioassays.TIF

• Main Authors: Caiqin Hu, Xiangfu Li, Maoqiu He, Peng Jiang, Aimin Long, Jie Xu
• Format: Still Image
• Language: unknown
• Published: 2021
• Subjects: Microbiology; Microbial Genetics; Microbial Ecology; Mycology; bacterial metabolic activity; bacterial community composition; microbial carbon cycling; ocean acidification; the northern South China Sea; Ocean acidification
• Online Access: https://doi.org/10.3389/fmicb.2021.583982.s001; https://figshare.com/articles/figure/Image_1_Effect_of_Ocean_Acidification_on_Bacterial_Metabolic_Activity_and_Community_Composition_in_Oligotrophic_Oceans_Inferred_From_Short-Term_Bioassays_TIF/14122115

Increasing anthropogenic CO 2 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-pCO 2 (400 ppm) and high-pCO 2 (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-pCO 2 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-pCO 2 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 2 .