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Seawater carbonate chemistry and particulate organic and inorganic carbon, growth of Emiliania huxleyi

Coccolithophore responses to changes in carbonate chemistry speciation such as CO2 and H+ are highly modulated by light intensity and temperature. Here, we fit an analytical equation, accounting for simultaneous changes in carbonate chemistry speciation, light and temperature, to published and original data for Emiliania huxleyi, and compare the projections with those for Gephyrocapsa oceanica. Based on our analysis, the two most common bloom-forming species in present-day coccolithophore communities appear to be adapted for a similar fundamental light niche but slightly different ones for temperature and CO2, with E. huxleyi having a tolerance to lower temperatures and higher CO2 levels than G. oceanica. Based on growth rates, a dominance of E. huxleyi over G. oceanica is projected below temperatures of 22 °C at current atmospheric CO2 levels. This is similar to a global surface sediment compilation of E. huxleyi and G. oceanica coccolith abundances suggesting temperature-dependent dominance shifts. For a future Representative Concentration Pathway (RCP) 8.5 climate change scenario (1000 µatm fCO2), we project a CO2 driven niche contraction for G. oceanica to regions of even higher temperatures. However, the greater sensitivity of G. oceanica to increasing CO2 is partially mitigated by increasing temperatures. Finally, we compare satellite-derived particulate inorganic carbon estimates in the surface ocean with a recently proposed metric for potential coccolithophore success on the community level, i.e. the temperature-, light- and carbonate-chemistry-dependent CaCO3 production potential (CCPP). Based on E. huxleyi alone, as there was interestingly a better correlation than when in combination with G. oceanica, and excluding the Antarctic province from the analysis, we found a good correlation between CCPP and satellite-derived particulate inorganic carbon (PIC) with an R2 of 0.73, p < 0.01 and a slope of 1.03 for austral winter/boreal summer and an R2 of 0.85, p < 0.01 and a slope of 0.32 for austral summer/boreal winter.

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Cite this as

Gafar, Natasha A, Schulz, Kai Georg (2018). Dataset: Seawater carbonate chemistry and particulate organic and inorganic carbon, growth of Emiliania huxleyi. https://doi.org/10.1594/PANGAEA.924611

DOI retrieved: 2018

Additional Info

Field Value
Imported on November 30, 2024
Last update November 30, 2024
License CC-BY-4.0
Source https://doi.org/10.1594/PANGAEA.924611
Author Gafar, Natasha A
Given Name Natasha A
Family Name Gafar
More Authors
Schulz, Kai Georg
Source Creation 2018
Publication Year 2018
Resource Type text/tab-separated-values - filename: Gafar-Schulz_2018_BG
Subject Areas
Name: BiologicalClassification

Name: Chemistry

Name: Ecology

Name: Lithosphere

Related Identifiers
Title: A three-dimensional niche comparison of Emiliania huxleyi and Gephyrocapsa oceanica: reconciling observations with projections
Identifier: https://doi.org/10.5194/bg-15-3541-2018
Type: DOI
Relation: References
Year: 2018
Source: Biogeosciences
Authors: Gafar Natasha A , Schulz Kai Georg , Gattuso Jean-Pierre , Epitalon Jean-Marie , Lavigne Héloïse , Orr James , Gentili Bernard , Hagens Mathilde , Hofmann Andreas , Mueller Jens-Daniel , Proye Aurélien , Rae James , Soetaert Karline .

Title: seacarb: seawater carbonate chemistry with R. R package version 3.2.14
Identifier: https://CRAN.R-project.org/package=seacarb
Type: DOI
Relation: References
Year: 2020
Authors: Gafar Natasha A , Schulz Kai Georg , Gattuso Jean-Pierre , Epitalon Jean-Marie , Lavigne Héloïse , Orr James , Gentili Bernard , Hagens Mathilde , Hofmann Andreas , Mueller Jens-Daniel , Proye Aurélien , Rae James , Soetaert Karline .