Rising atmospheric CO2 and deliberate CO2 sequestration in the ocean change
seawater carbonate chemistry in a similar way, lowering seawater pH, carbonate ion
concentration and carbonate saturation state and increasing dissolved CO2 concentration.
These changes affect marine plankton in various ways. On the organismal
level, a moderate increase in CO2 facilitates photosynthetic carbon fixation of some
phytoplankton groups. It also enhances the release of dissolved carbohydrates, most
notably during the decline of nutrient-limited phytoplankton blooms. A decrease in
the carbonate saturation state represses biogenic calcification of the predominant
marine calcifying organisms, foraminifera and coccolithophorids. On the ecosystem
level these responses influence phytoplankton species composition and succession,
favouring algal species which predominantly rely on CO2 utilization. Increased
phytoplankton exudation promotes particle aggregation and marine snow formation,
enhancing the vertical flux of biogenic material. A decrease in calcification may affect
the competitive advantage of calcifying organisms, with possible impacts on their
distribution and abundance. On the biogeochemical level, biological responses to CO2
enrichment and the related changes in carbonate chemistry can strongly alter the
cycling of carbon and other bio-active elements in the ocean. Both decreasing calcification
and enhanced carbon overproduction due to release of extracellular carbohydrates
have the potential to increase the CO2 storage capacity of the ocean. Although
the significance of such biological responses to CO2 enrichment becomes increasingly
evident, our ability to make reliable predictions of their future developments and to
quantify their potential ecological and biogeochemical impacts is still in its infancy.
It's the other way around. Plankton can increase the CO2 uptake of the oceans. There's been some attempted geoengineering studies of the phenomenon, seeding the ocean with iron.
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That's not what they said. They said (and titled their paper) "High tolerance of microzooplankton to ocean acidification in an Arctic coastal plankton community".
In the same way that a study on droughts in Australia cannot be extrapolated to the rest of the world, a study on Arctic coastal plankton cannot be described (as you and über deniers and industry funded the Idso family do) as being applicable to all of the world's oceans.
Well CO2 Science is a denier site so they most likely take the most damaging info and bypass the reality
http://news.google.com/news/url?sa=t&fd=R&usg=AFQjCNG5_FehFCrBQeUaXdJNn4kzSomgZw&url=http://www.co2science.org/articles/V16/N43/C3.php
The six scientists report that they "found almost no direct effects of OA on microzooplankton composition and diversity," and that "both the relative shares of ciliates and heterotrophic dinoflagellates as well as the taxonomic composition of microzooplankton remained unaffected by changes in pCO2/pH."