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      Inter- and intraspecific phenotypic plasticity of three phytoplankton species in response to ocean acidification

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          Abstract

          Phenotypic plasticity describes the phenotypic adjustment of the same genotype to different environmental conditions and is best described by a reaction norm. We focus on the effect of ocean acidification on inter- and intraspecific reaction norms of three globally important phytoplankton species ( Emiliania huxleyi, Gephyrocapsa oceanica and Chaetoceros affinis). Despite significant differences in growth rates between the species, they all showed a high potential for phenotypic buffering (similar growth rates between ambient and high CO 2 conditions). Only three coccolithophore genotypes showed a reduced growth in high CO 2. Diverging responses to high CO 2 of single coccolithophore genotypes compared with the respective mean species responses, however, raise the question of whether an extrapolation to the population level is possible from single-genotype experiments. We therefore compared the mean response of all tested genotypes with a total species response comprising the same genotypes, which was not significantly different in the coccolithophores. Assessing species reaction norms to different environmental conditions on short time scale in a genotype-mix could thus reduce sampling effort while increasing predictive power.

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          Most cited references17

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          Adaptation to an extraordinary environment by evolution of phenotypic plasticity and genetic assimilation.

          Adaptation to a sudden extreme change in environment, beyond the usual range of background environmental fluctuations, is analysed using a quantitative genetic model of phenotypic plasticity. Generations are discrete, with time lag tau between a critical period for environmental influence on individual development and natural selection on adult phenotypes. The optimum phenotype, and genotypic norms of reaction, are linear functions of the environment. Reaction norm elevation and slope (plasticity) vary among genotypes. Initially, in the average background environment, the character is canalized with minimum genetic and phenotypic variance, and no correlation between reaction norm elevation and slope. The optimal plasticity is proportional to the predictability of environmental fluctuations over time lag tau. During the first generation in the new environment the mean fitness suddenly drops and the mean phenotype jumps towards the new optimum phenotype by plasticity. Subsequent adaptation occurs in two phases. Rapid evolution of increased plasticity allows the mean phenotype to closely approach the new optimum. The new phenotype then undergoes slow genetic assimilation, with reduction in plasticity compensated by genetic evolution of reaction norm elevation in the original environment.
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            Evaluating 'Plasticity-First' Evolution in Nature: Key Criteria and Empirical Approaches.

            Many biologists are asking whether environmentally initiated phenotypic change (i.e., 'phenotypic plasticity') precedes, and even facilitates, evolutionary adaptation. However, this 'plasticity-first' hypothesis remains controversial, primarily because comprehensive tests from natural populations are generally lacking. We briefly describe the plasticity-first hypothesis and present much-needed key criteria to allow tests in diverse, natural systems. Furthermore, we offer a framework for how these criteria can be evaluated and discuss examples where the plasticity-first hypothesis has been investigated in natural populations. Our goal is to provide a means by which the role of plasticity in adaptive evolution can be assessed.
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              Impact of ocean acidification on the structure of future phytoplankton communities

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                Author and article information

                Journal
                Biol Lett
                Biol. Lett
                RSBL
                roybiolett
                Biology Letters
                The Royal Society
                1744-9561
                1744-957X
                February 2017
                February 2017
                : 13
                : 2
                : 20160774
                Affiliations
                GEOMAR, Helmholtz Centre for Ocean Research Kiel , Düsternbrooker Weg 20, 24105 Kiel, Germany
                Author notes
                [†]

                Shared first-authorship.

                [‡]

                Shared last-authorship.

                A contribution to the special feature ‘Ocean acidification’.

                Electronic supplementary material is available online at https://dx.doi.org/10.6084/m9.figshare.c.3667954.

                Author information
                http://orcid.org/0000-0003-4660-7759
                http://orcid.org/0000-0002-8517-8427
                Article
                rsbl20160774
                10.1098/rsbl.2016.0774
                5326507
                28148833
                efc4b9bc-f2f2-4be1-a31c-1445426882db
                © 2017 The Authors.

                Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, provided the original author and source are credited.

                History
                : 30 September 2016
                : 20 December 2016
                Funding
                Funded by: Deutsche Forschungsgemeinschaft, http://dx.doi.org/10.13039/501100001659;
                Award ID: MA5058/2-1
                Award ID: RE5058/2-2
                Categories
                1001
                60
                70
                Special Feature
                Ocean Acidification
                Custom metadata
                February, 2017

                Life sciences
                emiliania huxleyi,gephyrocapsa oceanica,chaetoceros affinis,ocean acidification,plasticity,reaction norm

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