A natural pH gradient caused by marine CO2 seeps off Vulcano Island (Italy) was used to assess the effects of ocean acidification on coccolithophores, which are abundant planktonic unicellular calcifiers. Such seeps are used as natural laboratories to study the effects of ocean acidification on marine ecosystems, since they cause longterm changes in seawater carbonate chemistry and pH, exposing the organisms to elevated CO2 concentrations and therefore mimicking future scenarios. Previous work at CO2 seeps has focused exclusively on benthic organisms. Here we show progressive depletion of 27 coccolithophore species, in terms of cell concentrations and diversity, along a calcite saturation gradient from Ωcalcite6.4 to 1. Water 98848 Nouméa, New Caledonia, France. changes correspond to increases of both [CO2] and [H ], and decreases of pH, [CO32-], and of carbonate saturation states (). This process, called ocean acidification, has raised concerns about long-term effects on marine ecosys...
Ziveri, P., Passaro, M., Incarbona, A., Milazzo, M., Rodolfo Metalpa, R., Hall Spencer, J. (2014). Decline in coccolithophore diversity and impact on coccolith morphogenesis along a natural CO2 gradient. THE BIOLOGICAL BULLETIN, 226(226), 282-290 [10.1086/bblv226n3p282].
Decline in coccolithophore diversity and impact on coccolith morphogenesis along a natural CO2 gradient
INCARBONA, Alessandro;MILAZZO, Marco;
2014-01-01
Abstract
A natural pH gradient caused by marine CO2 seeps off Vulcano Island (Italy) was used to assess the effects of ocean acidification on coccolithophores, which are abundant planktonic unicellular calcifiers. Such seeps are used as natural laboratories to study the effects of ocean acidification on marine ecosystems, since they cause longterm changes in seawater carbonate chemistry and pH, exposing the organisms to elevated CO2 concentrations and therefore mimicking future scenarios. Previous work at CO2 seeps has focused exclusively on benthic organisms. Here we show progressive depletion of 27 coccolithophore species, in terms of cell concentrations and diversity, along a calcite saturation gradient from Ωcalcite6.4 to 1. Water 98848 Nouméa, New Caledonia, France. changes correspond to increases of both [CO2] and [H ], and decreases of pH, [CO32-], and of carbonate saturation states (). This process, called ocean acidification, has raised concerns about long-term effects on marine ecosys...| File | Dimensione | Formato | |
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