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      The requirement for calcification differs between ecologically important coccolithophore species

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          Summary

          • Coccolithophores are globally distributed unicellular marine algae that are characterized by their covering of calcite coccoliths. Calcification by coccolithophores contributes significantly to global biogeochemical cycles. However, the physiological requirement for calcification remains poorly understood as non‐calcifying strains of some commonly used model species, such as Emiliania huxleyi, grow normally in laboratory culture.

          • To determine whether the requirement for calcification differs between coccolithophore species, we utilized multiple independent methodologies to disrupt calcification in two important species of coccolithophore: E. huxleyi and Coccolithus braarudii. We investigated their physiological response and used time‐lapse imaging to visualize the processes of calcification and cell division in individual cells.

          • Disruption of calcification resulted in major growth defects in C. braarudii, but not in E. huxleyi. We found no evidence that calcification supports photosynthesis in C. braarudii, but showed that an inability to maintain an intact coccosphere results in cell cycle arrest.

          • We found that C. braarudii is very different from E. huxleyi as it exhibits an obligate requirement for calcification. The identification of a growth defect in C. braarudii resulting from disruption of the coccosphere may be important in considering their response to future changes in ocean carbonate chemistry.

          Abstract

          See also the Commentary on this article by https://doi.org/10.1111/nph.15409.

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          Production and accumulation of calcium carbonate in the ocean: Budget of a nonsteady state

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            Pan genome of the phytoplankton Emiliania underpins its global distribution

            Coccolithophores have influenced the global climate for over 200 million years. These marine phytoplankton can account for 20 per cent of total carbon fixation in some systems. They form blooms that can occupy hundreds of thousands of square kilometres and are distinguished by their elegantly sculpted calcium carbonate exoskeletons (coccoliths), rendering them visible from space. Although coccolithophores export carbon in the form of organic matter and calcite to the sea floor, they also release CO2 in the calcification process. Hence, they have a complex influence on the carbon cycle, driving either CO2 production or uptake, sequestration and export to the deep ocean. Here we report the first haptophyte reference genome, from the coccolithophore Emiliania huxleyi strain CCMP1516, and sequences from 13 additional isolates. Our analyses reveal a pan genome (core genes plus genes distributed variably between strains) probably supported by an atypical complement of repetitive sequence in the genome. Comparisons across strains demonstrate that E. huxleyi, which has long been considered a single species, harbours extensive genome variability reflected in different metabolic repertoires. Genome variability within this species complex seems to underpin its capacity both to thrive in habitats ranging from the equator to the subarctic and to form large-scale episodic blooms under a wide variety of environmental conditions.
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              Reduced calcification of marine plankton in response to increased atmospheric CO2.

              The formation of calcareous skeletons by marine planktonic organisms and their subsequent sinking to depth generates a continuous rain of calcium carbonate to the deep ocean and underlying sediments. This is important in regulating marine carbon cycling and ocean-atmosphere CO2 exchange. The present rise in atmospheric CO2 levels causes significant changes in surface ocean pH and carbonate chemistry. Such changes have been shown to slow down calcification in corals and coralline macroalgae, but the majority of marine calcification occurs in planktonic organisms. Here we report reduced calcite production at increased CO2 concentrations in monospecific cultures of two dominant marine calcifying phytoplankton species, the coccolithophorids Emiliania huxleyi and Gephyrocapsa oceanica. This was accompanied by an increased proportion of malformed coccoliths and incomplete coccospheres. Diminished calcification led to a reduction in the ratio of calcite precipitation to organic matter production. Similar results were obtained in incubations of natural plankton assemblages from the north Pacific ocean when exposed to experimentally elevated CO2 levels. We suggest that the progressive increase in atmospheric CO2 concentrations may therefore slow down the production of calcium carbonate in the surface ocean. As the process of calcification releases CO2 to the atmosphere, the response observed here could potentially act as a negative feedback on atmospheric CO2 levels.
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                Author and article information

                Contributors
                glw@mba.ac.uk
                Journal
                New Phytol
                New Phytol
                10.1111/(ISSN)1469-8137
                NPH
                The New Phytologist
                John Wiley and Sons Inc. (Hoboken )
                0028-646X
                1469-8137
                19 June 2018
                October 2018
                : 220
                : 1 ( doiID: 10.1111/nph.2018.220.issue-1 )
                : 147-162
                Affiliations
                [ 1 ] Marine Biological Association Plymouth PL1 2PB UK
                [ 2 ] School of Ocean and Earth Science University of Southampton Southampton SO14 3ZH UK
                [ 3 ] Department of Biology and Marine Biology University of North Carolina Wilmington Wilmington NC 28403‐591 USA
                [ 4 ] Station Biologique de Roscoff Place Georges Teisser 29680 Roscoff France
                Author notes
                [*] [* ] Author for correspondence:

                Glen L. Wheeler

                Tel: +44 01752 426360

                Email: glw@ 123456mba.ac.uk

                Author information
                http://orcid.org/0000-0002-8570-2399
                Article
                NPH15272 2018-2219
                10.1111/nph.15272
                6175242
                29916209
                d7f2d880-1337-429c-a5b0-bc77adedf3a6
                © 2018 The Authors. New Phytologist © 2018 New Phytologist Trust

                This is an open access article under the terms of the http://creativecommons.org/licenses/by/4.0/ License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.

                History
                : 15 January 2018
                : 07 May 2018
                Page count
                Figures: 9, Tables: 0, Pages: 16, Words: 10807
                Funding
                Funded by: Natural Environment Research Council Doctoral Training Partnership
                Award ID: NE/L002531/1
                Award ID: NE/N011708/1
                Funded by: National Science Foundation
                Award ID: 1638838
                Funded by: European Research Council
                Award ID: ERC‐ADG 670390
                Categories
                Full Paper
                Research
                Full Papers
                Custom metadata
                2.0
                nph15272
                October 2018
                Converter:WILEY_ML3GV2_TO_NLMPMC version:version=5.5.0 mode:remove_FC converted:08.10.2018

                Plant science & Botany
                calcification,coccolithophore,coccolithus braarudii,emiliania huxleyi,phytoplankton

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