Increasing atmospheric carbon dioxide (CO2) is changing seawater chemistry towards reduced pH,
which affects various properties of marine organisms. Coastal and brackish
water communities are expected to be less affected by ocean acidification
(OA) as these communities are typically adapted to high fluctuations in
CO2 and pH. Here we investigate the response of a coastal brackish water
plankton community to increasing CO2 levels as projected for the coming
decades and the end of this century in terms of community and biochemical
fatty acid (FA) composition. A Baltic Sea plankton community was enclosed in
a set of offshore mesocosms and subjected to a CO2 gradient ranging from
natural concentrations ( ∼ 347 µatm fCO2) up to
values projected for the year 2100 ( ∼ 1333 µatm
fCO2). We show that the phytoplankton community composition was
resilient to CO2 and did not diverge between the treatments. Seston FA
composition was influenced by community composition, which in turn was driven
by silicate and phosphate limitation in the mesocosms and showed no
difference between the CO2 treatments. These results suggest that
CO2 effects are dampened in coastal communities that already experience
high natural fluctuations in pCO2. Although this coastal plankton
community was tolerant of high pCO2 levels, hypoxia and CO2
uptake by the sea can aggravate acidification and may lead to pH changes
outside the currently experienced range for coastal organisms
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