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      Coralline algae (Rhodophyta) in a changing world: integrating ecological, physiological, and geochemical responses to global change

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          Abstract

          Coralline algae are globally distributed benthic primary producers that secrete calcium carbonate skeletons. In the context of ocean acidification, they have received much recent attention due to the potential vulnerability of their high‐Mg calcite skeletons and their many important ecological roles. Herein, we summarize what is known about coralline algal ecology and physiology, providing context to understand their responses to global climate change. We review the impacts of these changes, including ocean acidification, rising temperatures, and pollution, on coralline algal growth and calcification. We also assess the ongoing use of coralline algae as marine climate proxies via calibration of skeletal morphology and geochemistry to environmental conditions. Finally, we indicate critical gaps in our understanding of coralline algal calcification and physiology and highlight key areas for future research. These include analytical areas that recently have become more accessible, such as resolving phylogenetic relationships at all taxonomic ranks, elucidating the genes regulating algal photosynthesis and calcification, and calibrating skeletal geochemical metrics, as well as research directions that are broadly applicable to global change ecology, such as the importance of community‐scale and long‐term experiments in stress response.

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          Most cited references39

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          Dynamic patterns and ecological impacts of declining ocean pH in a high-resolution multi-year dataset.

          Increasing global concentrations of atmospheric CO(2) are predicted to decrease ocean pH, with potentially severe impacts on marine food webs, but empirical data documenting ocean pH over time are limited. In a high-resolution dataset spanning 8 years, pH at a north-temperate coastal site declined with increasing atmospheric CO(2) levels and varied substantially in response to biological processes and physical conditions that fluctuate over multiple time scales. Applying a method to link environmental change to species dynamics via multispecies Markov chain models reveals strong links between in situ benthic species dynamics and variation in ocean pH, with calcareous species generally performing more poorly than noncalcareous species in years with low pH. The models project the long-term consequences of these dynamic changes, which predict substantial shifts in the species dominating the habitat as a consequence of both direct effects of reduced calcification and indirect effects arising from the web of species interactions. Our results indicate that pH decline is proceeding at a more rapid rate than previously predicted in some areas, and that this decline has ecological consequences for near shore benthic ecosystems.
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            Chemically rich seaweeds poison corals when not controlled by herbivores.

            Coral reefs are in dramatic global decline, with seaweeds commonly replacing corals. It is unclear, however, whether seaweeds harm corals directly or colonize opportunistically following their decline and then suppress coral recruitment. In the Caribbean and tropical Pacific, we show that, when protected from herbivores, approximately 40 to 70% of common seaweeds cause bleaching and death of coral tissue when in direct contact. For seaweeds that harmed coral tissues, their lipid-soluble extracts also produced rapid bleaching. Coral bleaching and mortality was limited to areas of direct contact with seaweeds or their extracts. These patterns suggest that allelopathic seaweed-coral interactions can be important on reefs lacking herbivore control of seaweeds, and that these interactions involve lipid-soluble metabolites transferred via direct contact. Seaweeds were rapidly consumed when placed on a Pacific reef protected from fishing but were left intact or consumed at slower rates on an adjacent fished reef, indicating that herbivory will suppress seaweeds and lower frequency of allelopathic damage to corals if reefs retain intact food webs. With continued removal of herbivores from coral reefs, seaweeds are becoming more common. This occurrence will lead to increasing frequency of seaweed-coral contacts, increasing allelopathic suppression of remaining corals, and continuing decline of reef corals.
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              Scleractinian coral species survive and recover from decalcification.

              Anthropogenic-driven accumulation of carbon dioxide in the atmosphere and projected ocean acidification have raised concerns regarding the eventual impact on coral reefs. This study demonstrates that skeleton-producing corals grown in acidified experimental conditions are able to sustain basic life functions, including reproductive ability, in a sea anemone-like form and will resume skeleton building when reintroduced to normal modern marine conditions. These results support the existence of physiological refugia, allowing corals to alternate between nonfossilizing soft-body ecophenotypes and fossilizing skeletal forms in response to changes in ocean chemistry. This refugia, however, does not undermine the threats to reef ecosystems in a high carbon dioxide world.
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                Author and article information

                Journal
                J Phycol
                J. Phycol
                10.1111/(ISSN)1529-8817
                JPY
                Journal of Phycology
                John Wiley and Sons Inc. (Hoboken )
                0022-3646
                1529-8817
                23 January 2015
                February 2015
                : 51
                : 1 ( doiID: 10.1111/jpy.2015.51.issue-1 )
                : 6-24
                Affiliations
                [ 1 ] Department of Ecology and EvolutionThe University of Chicago 1101 E. 57th Street Chicago Illinois 60637USA
                [ 2 ] School of Geographical and Earth SciencesUniversity of Glasgow University Avenue Glasgow G12 8QQUK
                [ 3 ]Present address: Plymouth Marine Laboratory Prospect Place, The Hoe Plymouth PL1 3DHUK
                Author notes
                [*] [* ]Author for correspondence: e‐mail mccoy@ 123456uchicago.edu .
                Article
                JPY12262
                10.1111/jpy.12262
                4964943
                26986255
                1e7e8fd7-4ac9-4523-b6e7-cd6e436b3be8
                © 2015 The Authors. Journal of Phycology published by Wiley Periodicals, Inc. on behalf of Phycological Society of America.

                This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.

                History
                : 18 April 2014
                : 03 October 2014
                Page count
                Pages: 19
                Categories
                Review
                Review
                Custom metadata
                2.0
                jpy12262
                February 2015
                Converter:WILEY_ML3GV2_TO_NLMPMC version:4.9.2 mode:remove_FC converted:28.07.2016

                calcification,climate change,coralline algae,crustose coralline algae,ecology,ecosystem services,ocean acidification,paleoclimate,paleoclimate proxies,photosynthesis,physiology

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