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Warming and CO2 Enhance Arctic Heterotrophic Microbial Activity
Dolors Vaqué1, Elena Lara1, Jesús M Arrieta2
1Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar (CSIC), Barcelona, Spain.
Rising Arctic temperatures and CO2 levels will decrease phytoplankton biomass and boost bacterial production, weakening the ocean's carbon sink capacity. This impacts microbial food webs and biogeochemical cycles.
Area of Science:
- Marine microbial ecology
- Climate change science
- Arctic Oceanography
Background:
- Ocean acidification and warming are key climate change impacts on marine ecosystems.
- The Arctic Ocean is warming faster than other regions globally.
- Marine planktonic microorganisms are crucial for ocean biogeochemical cycles.
Purpose of the Study:
- To investigate the combined effects of warming and elevated CO2 on Arctic microbial communities.
- To assess changes in phototrophic and heterotrophic microbial abundances and processes.
- To examine viral activity (lytic and lysogenic) under simulated future Arctic conditions.
Main Methods:
- Experimental microcosms simulating Arctic fjord conditions (Svalbard).
- Controlled temperature treatments (1°C, 6°C, 10°C) with elevated CO2 concentrations (135–2,318 μatm).
- Measurements of chlorophyll a, bacterial production (BP), bacterial mortality, and viral lytic/lysogenic activity.
Main Results:
- Chlorophyll a decreased with increasing temperature.
- Bacterial production significantly increased with pCO2 at 6°C and 10°C.
- Lysogeny increased with pCO2, especially at 10°C, and protistan grazing showed a positive interaction with temperature.
Conclusions:
- Future Arctic warming and CO2 increase will reduce phytoplankton biomass.
- Bacterial production will be enhanced, altering microbial food web carbon fluxes.
- The Arctic plankton community's capacity to act as a CO2 sink will likely diminish.
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