Description: One of the options to mitigate atmospheric CO2 increase is CO2 Capture and Storage in sub-seabed geological formations. Since predicting long-term storage security is difficult, different CO2 leakage scenarios and impacts on marine ecosystems require evaluation. Submarine CO2 vents may serve as natural analogues and allow studying the effects of CO2 leakage in a holistic approach. At the study site east of Basiluzzo Islet off Panarea Island (Italy), gas emissions (90-99% CO2) occur at moderate flows (80-120 L m-2 h-1). We investigated the effects of acidified porewater conditions (pHT range: 5.5-7.7) on the diversity of benthic bacteria and invertebrates by sampling natural sediments in three subsequent years and by performing a transplantation experiment with a duration of one year, respectively. Both multiple years and one year of exposure to acidified porewater conditions reduced the number of benthic bacterial operational taxonomic units and invertebrate species diversity by 30-80%. Reduced biodiversity at the vent sites increased the temporal variability in bacterial and nematode community biomass, abundance and composition. While the release from CO2 exposure resulted in a full recovery of nematode species diversity within one year, bacterial diversity remained affected. Overall our findings showed that seawater acidification, induced by seafloor CO2 emissions, was responsible for loss of diversity across different size-classes of benthic organisms, which reduced community stability with potential relapses on ecosystem resilience.

Description: The area around the Antarctic Peninsula is projected to undergo rapid climatic changes affecting seasonal sea ice cover, water column stratification, terrestrial meltwater run-off, and related nutrient input and thus the conditions for primary production and organic carbon export. The impact of such environmental changes on benthic microbial communities is poorly understood. In this study, we investigated the impact of different sea ice cover and redox conditions on microbial community compositions from 7 different stations (330–450 m water depth) along a 400-mile transect from the eastern shelf of the Antarctic Peninsula to the west of the South Orkney Islands. Two deep stations (3000 m depth) were sampled for comparison. Samples were collected from 6 different intervals down to a depth of 16 cm. The diversity and composition of microbial communities were determined by 16S ribosomal RNA (rRNA) gene sequencing. Redox conditions in sediments with long ice-free periods showed that iron and sulfate reduction are dominant anaerobic pathways for carbon mineralization. In contrast, sediments at a heavily ice-covered station were dominated by the aerobic pathway, which accounted for 〉94 % of the total carbon degradation. Our results reveal that the microbial community composition at the station under heavy ice-cover differs significantly from stations under low ice-cover and tends to cluster separately, suggesting that sea ice cover is the main driver for changes in microbial community composition in the shelf sediments. Further, the frequency of marginal sea ice conditions (here defined as 5-35% sea ice cover) is significantly different between stations (p 0.001) and can explain 5 to 13% of the variation between microbial communities. The bacterial communities at stations under low ice-cover co-varied significantly with TOC content and porewater concentrations of ammonia, dissolved iron, and sulfide. This was reflected in the microbial community composition, where stations with low ice-cover were dominated by Desulfuromonadia, a taxon including many iron and sulfate reducers. At the station with heavy ice-cover, this class showed very low abundances. Our findings demonstrate that the benthic microbial composition and mediated-processes at various sites around the eastern Antarctic Peninsula are regulated by sea ice cover.