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Hermoso, Michael (2015): Control of ambient pH on growth and stable isotopes in phytoplanktonic calcifying algae [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.861380, Supplement to: Hermoso, M (2015): Control of ambient pH on growth and stable isotopes in phytoplanktonic calcifying algae. Paleoceanography, 30(8), 1100-1112, https://doi.org/10.1002/2015PA002844

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Abstract:
The present work examines the relationship between pH-induced changes in growth and stable isotopic composition of coccolith calcite in two coccolithophore species with a geological perspective. These cells (Gephyrocapsa oceanica and Coccolithus pelagicus) with differing physiologies and vital effects possess a growth optimum corresponding to average pH of surface seawater in the geological period during their first known occurrence. Diminished growth rates outside of their optimum pH range are explained by the challenge of proton translocation into the extracellular environment at low pH, and enhanced aqueous CO2 limitation at high pH. These diminished growth rates correspond to a lower degree of oxygen isotopic disequilibrium in G. oceanica. In contrast, the slower growing and ancient species C. pelagicus, which typically precipitates near-equilibrium calcite, does not show any modulation of oxygen isotope signals with changing pH. In CO2-utilizing unicellular algae, carbon and oxygen isotope compositions are best explained by the degree of utilization of the internal dissolved inorganic carbon (DIC) pool and the dynamics of isotopic re-equilibration inside the cell. Thus, the "carbonate ion effect" may not apply to coccolithophores. This difference with foraminifera can be traced to different modes of DIC incorporation into these two distinct biomineralizing organisms. From a geological perspective, these findings have implications for refining the use of oxygen isotopes to infer more reliable sea surface temperatures (SSTs) from fossil carbonates, and contribute to a better understanding of how climate-relevant parameters are recorded in the sedimentary archive.
Keyword(s):
Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (<20 L); Chromista; Coccolithus pelagicus; Gephyrocapsa oceanica; Growth/Morphology; Haptophyta; Laboratory experiment; Laboratory strains; Not applicable; Pelagos; Phytoplankton; Single species
Further details:
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse (2015): seacarb: seawater carbonate chemistry with R. R package version 3.0.8. https://cran.r-project.org/package=seacarb
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1TypeTypeHermoso, Michaelstudy
2SpeciesSpeciesHermoso, Michael
3StrainStrainHermoso, Michael
4Registration number of speciesReg spec noHermoso, MichaelWoRMS Aphia ID
5Uniform resource locator/link to referenceURL refHermoso, Michael
6pHpHHermoso, Michaelinitial, total scale
7pHpHHermoso, Michaelfinal, total scale
8Time in daysTimedaysHermoso, Michael
9Cell densityCells#/mlHermoso, Michaelinitial
10Cell densityCells#/mlHermoso, Michaelfinal
11Growth rateµ1/dayHermoso, Michael
12δ13C, calciteδ13C cal‰ PDBHermoso, Michael
13δ18O, calciteδ18O cal‰ PDBHermoso, Michael
14Coccosphere, diameterCoccosp diamµmHermoso, Michael
15Carbon utilization indexµ/CO2kg*µm/µmol/dayHermoso, Michael
16Temperature, waterTemp°CHermoso, Michael
17SalinitySalHermoso, Michael
18Alkalinity, totalATµmol/kgHermoso, Michael
19Carbon dioxideCO2µmol/kgHermoso, Michael
20Bicarbonate ion[HCO3]-µmol/kgHermoso, Michael
21Carbonate ion[CO3]2-µmol/kgHermoso, Michael
22Calcite saturation stateOmega CalHermoso, Michael
23δ13C, carbon dioxide, aquaticδ13C CO2 aqHermoso, Michael
24δ18O, waterδ18O H2O‰ SMOWHermoso, Michaelseawater
25δ18O, calciteδ18O cal‰ PDBHermoso, Michaelinorganic calcite after Kim and O'Neil [1997] without pH effect
26δ18O, calciteδ18O cal‰ PDBHermoso, Michaelinorganic calcite after Kim and O'Neil [1997] accounting for the pH by Zeebe [2007]
27δ18O, calciteδ18O cal‰ PDBHermoso, Michaelequilibrium calcite after Watkins et al. [2014]
28δ18O, calciteδ18O cal‰ PDBHermoso, Michaelequilibrium calcite after Watkins et al. [2014] accounting for kinetic effect
29Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
30Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
31Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
32Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
33Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
34Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
35Carbon, inorganic, dissolvedDICµmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
36Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
37Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
1153 data points

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