Table_1_Warming and CO2 Enhance Arctic Heterotrophic Microbial Activity.DOCX

• Main Authors: Dolors Vaqué, Elena Lara, Jesús M. Arrieta, Johnna Holding, Elisabet L. Sà, Iris E. Hendriks, Alexandra Coello-Camba, Marta Alvarez, Susana Agustí, Paul F. Wassmann, Carlos M. Duarte
• Format: Dataset
• Language: unknown
• Published: 2019
• Subjects: Microbiology; Microbial Genetics; Microbial Ecology; Mycology; pCO2; temperature; microbial food-webs; viral life cycle; Arctic Ocean; Arctic; Longyearbyen; Svalbard; Climate change; Ocean acidification; UNIS
• Online Access: https://doi.org/10.3389/fmicb.2019.00494.s003; https://figshare.com/articles/Table_1_Warming_and_CO2_Enhance_Arctic_Heterotrophic_Microbial_Activity_DOCX/7868549

Ocean acidification and warming are two main consequences of climate change that can directly affect biological and ecosystem processes in marine habitats. The Arctic Ocean is the region of the world experiencing climate change at the steepest rate compared with other latitudes. Since marine planktonic microorganisms play a key role in the biogeochemical cycles in the ocean it is crucial to simultaneously evaluate the effect of warming and increasing CO 2 on marine microbial communities. In 20 L experimental microcosms filled with water from a high-Arctic fjord (Svalbard), we examined changes in phototrophic and heterotrophic microbial abundances and processes [bacterial production (BP) and mortality], and viral activity (lytic and lysogenic) in relation to warming and elevated CO 2 . The summer microbial plankton community living at 1.4°C in situ temperature, was exposed to increased CO 2 concentrations (135–2,318 μatm) in three controlled temperature treatments (1, 6, and 10°C) at the UNIS installations in Longyearbyen (Svalbard), in summer 2010. Results showed that chlorophyll a concentration decreased at increasing temperatures, while BP significantly increased with pCO 2 at 6 and 10°C. Lytic viral production was not affected by changes in pCO 2 and temperature, while lysogeny increased significantly at increasing levels of pCO 2 , especially at 10°C (R 2 = 0.858, p = 0.02). Moreover, protistan grazing rates showed a positive interaction between pCO 2 and temperature. The averaged percentage of bacteria grazed per day was higher (19.56 ± 2.77% d -1 ) than the averaged percentage of lysed bacteria by virus (7.18 ± 1.50% d -1 ) for all treatments. Furthermore, the relationship among microbial abundances and processes showed that BP was significantly related to phototrophic pico/nanoflagellate abundance in the 1°C and the 6°C treatments, and BP triggered viral activity, mainly lysogeny at 6 and 10°C, while bacterial mortality rates was significantly related to bacterial abundances at 6°C. Consequently, our ...