Reduced calcification of marine plankton in response to increased atmospheric CO2

By U. Riebesell, I. Zondervan, B. Rost, P. Tortell, R. Zeebe, François M. M. Morel. Nature, 2000

1,546 citations recorded by the source corpus.

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Citations in the corpus

Pelagic functional group modeling: Progress, challenges and prospects (2006, positive): “…changes dramatically in both time and space, and it does not account for variability in PIC/POC ratios due to changing CO2 concentrations, as shown for corals (Gattuso et al., 1998; Kleypas et al., 1999; Langdon et al., 2000) and coccolithophores (Riebesell et al., 2000; Zondervan et al., 2002).”
CO2 control of Trichodesmium N2 fixation, photosynthesis, growth rates, and elemental ratios: Implications for past, present, and future ocean biogeochemistry (2007, background): “Marine phytoplankton respond to anthropogenic CO2 increases and sea-surface warming by altering their physiology (Riebesell et al. 2000), relative abundance (Tortell et al. 2002), and biogeography (Boyd and Doney 2002).”
Poleward expansion of the coccolithophore Emiliania huxleyi (2014, background): “The effects of OA on E. huxleyi calcification are still hotly debated primarily because both laboratory (e.g. Riebesell et al., 2000 vs. Iglesias-Rodriguez et al., 2008) and observational data (e.g. Beaufort et al., 2011 vs. Smith et al., 2012) give contradictory results.”
Environmental controls on coccolithophore calcification (2012, background): “…higher than those found today (390 ppm) or at least a decrease in PIC:POC and a corresponding increase in calcification in low CO2 concentrations such as the 190 ppm or so seen at the last glacial maximum 18 000 yr ago (e.g. Riebesell et al. 2000a,b, Zon - dervan et al. 2001, Casareto et al. 2009).”
Effect of pH on Gene Expression and Thermal Tolerance of Early Life History Stages of Red Abalone (Haliotis rufescens) (2010, background): “KEY WORDS: abalone, ocean acidification, early development, pH, Haliotis, climate change, gene expression”
Pore‐scale simulation of mixing‐induced calcium carbonate precipitation and dissolution in a microfluidic pore network (2012, background): “, 2004], biogeochemical behavior in marine environments [Riebesell et al., 2000], biomineralization of products from microorganisms [De Yoreo and Vekilov, 2003], growth of calcite concretions in fractured and porous media [Mozley and Davis, 2005], and the formation of scale in boilers and cooling to”
The impacts of climate change in coastal marine systems. (2006, background): “Decreased calcification rates in response to increased CO2 has been shown in taxa including coccolithophorid zooplankters, coralline algae, reef-building scleractinian corals and pteropod molluscs (Kleypas et al. 1999; Riebesell et al. 2000; Feely et al. 2004).”
Response of sea urchin pluteus larvae (Echinodermata: Echinoidea) to reduced seawater pH: a comparison among a tropical, temperate, and a polar species (2009, methodology): “Tests for sphericity were made using the Mauchly's sphericity test a Degrees of freedom and P-value adjusted by Greenhouse-Geisser e algae (Gattuso et al. 1999; Gao et al. 1993; Borowitzka 1981) and coccolithophores (Sciandra et al. 2003; Riebesell et al. 2000).”
Effects of ocean acidification and high temperatures on the bryozoan Myriapora truncata at natural CO2 vents (2010, result): “…measured at B1 is consistent with laboratory and mesocosm observations of reduced calcification rates in other calcitic groups such as coralline algae (Kuffner et al. 2008; Martin & Gattuso 2009), foraminifera (Spero et al. 1997) and coccolithophores (Riebesell et al. 2000; Delille et al. 2005).”
Testing the effect of CO2 concentration on the dynamics of marine heterotrophic bacterioplankton (2006, background): “A doubling in present CO2 levels will result in a significant reduction of biogenic calcification of Foraminifera and coccolithophores (Bijma et al. 1999; Riebesell et al. 2000).”
Plankton functional type modelling : running before we can walk? (2005, background): “Or changes in seawater carbonate chemistry as a result of anthropogenic CO2 invading the ocean may decrease calcification in major planktonic groups such as the coccolithophores and foraminiferans (Riebesell et al., 2000; Barker and Elderfield, 2002).”
A simple model for the CaCO3 saturation state of the ocean: The “Strangelove,” the “Neritan,” and the “Cretan” Ocean (2003, background): “This assumption is probably reasonable at high supersaturation [Riebesell et al., 2000; Zondervan et al., 2001; Bijma et al., 1999; Wolf-Gladrow et al., 1999].”