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Titel Calcifying phytoplankton biomass and CO2: A striking balance
VerfasserIn Jorijntje Henderiks, Bjarte Hannisdal, Lee Hsiang Liow
Konferenz EGU General Assembly 2010
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 12 (2010)
Datensatznummer 250041098
 
Zusammenfassung
Calcifying phytoplankton play a fundamental role in marine ecosystems and global biogeochemical cycles. Their cell size and abundance modulate the strength of the biological carbon and carbonate “pumps”, which represent important feedbacks in the Earth System. Phytoplankton biomass is thus coupled to climate variability, but the behavior of this coupling on geological time scales remains unknown. We compared fossil time series of coccolithophore relative abundance and cell size to geochemical proxy records of global climate change over much of the Cenozoic (~45-5 million years ago). We show that the Cenozoic decline in atmospheric carbon dioxide levels (pCO2) caused a reduction in calcifying phytoplankton biomass. Our results demonstrate that long-term variation in CO2 availability and concomitant shifts in ocean carbonate chemistry have been important drivers of planktonic ecosystems beyond their association with ocean temperature and stratification. This supports the hypothesis that large-celled coccolithophores lacking a carbon concentrating mechanism were disadvantaged in a low-pCO2 world (Henderiks & Pagani 2008). In addition, decreasing biomass of calcifying phytoplankton may have represented a negative feedback during global cooling by reducing carbon drawdown and burial fluxes, potentially contributing to the stabilization of atmospheric CO2 concentrations over the past 24 million years (Pagani et al. 2009). References Henderiks, J. and M. Pagani (2008), Coccolithophore cell size and the Paleogene decline in atmospheric CO2, Earth and Planetary Science Letters, 269, 575-583. Pagani, M., K. Caldeira, R. Berner and D. J. Beerling (2009), The role of terrestrial plants in limiting atmospheric CO2 decline over the past 24 million years, Nature, 460, 85-88.