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Zooxanthellae that open calcium channels: implications for reef corals
Toxins that open cell membrane calcium channels have been found in the dinoflagellate genusSymbiodinium, and likely occur in most zooxanthellae. I used published observations to examine some potentially far-reaching consequences to reef corals. Algal toxins may stimulate coral calcification by openi...
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Published in: | Marine ecology. Progress series (Halstenbek) 2012-07, Vol.460, p.277-287 |
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creator | McConnaughey, Ted A. |
description | Toxins that open cell membrane calcium channels have been found in the dinoflagellate genusSymbiodinium, and likely occur in most zooxanthellae. I used published observations to examine some potentially far-reaching consequences to reef corals. Algal toxins may stimulate coral calcification by opening Ca2+channels on the calcifying ectoderm. The coral discharges the resulting protons (Ca2++ HCO₃⁻ → CaCO₃⁺ H+) into its coelenteron cavity, where they improve algal bicarbonate and nutrient assimilation. Coupling calcification with autotrophic physiologies contributes to the success of highly calcareous zooxanthellar symbioses, and to their associations with nutrient-poor tropical waters. Nutrient shortages freeze zooxanthellae in the G1 phase of the cell cycle. Dinoflagellates are often most toxic at such times, perhaps because toxins modulate their nuclear mix of cations, to control DNA conformation and activity. Increased Ca2+influx into host cells disrupts cell adhesion and induces apoptosis. Zooxanthellae assimilate host nutrients, complete G1, divide, and disperse to new hosts. Nutrient shortages associate with high sea surface temperatures (SST), producing correlations between SST, calcification, and algal exit. Zooxanthellae proliferate when nutrients are abundant, but when nutrients later disappear, usually as SST warms, toxins and the departure of over-abundant zooxanthellae potentially overwhelm the coral and cause coral bleaching. |
doi_str_mv | 10.3354/meps09776 |
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Nutrient shortages associate with high sea surface temperatures (SST), producing correlations between SST, calcification, and algal exit. Zooxanthellae proliferate when nutrients are abundant, but when nutrients later disappear, usually as SST warms, toxins and the departure of over-abundant zooxanthellae potentially overwhelm the coral and cause coral bleaching.</description><identifier>ISSN: 0171-8630</identifier><identifier>EISSN: 1616-1599</identifier><identifier>DOI: 10.3354/meps09776</identifier><language>eng</language><publisher>Inter-Research</publisher><subject>Algae ; Bleaching ; Carbon dioxide ; Cell cycle ; Coral reefs ; Corals ; Marine ; Nutrients ; Photosynthesis ; REVIEW ; Symbiodinium ; Symbiosis ; Toxins</subject><ispartof>Marine ecology. 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Increased Ca2+influx into host cells disrupts cell adhesion and induces apoptosis. Zooxanthellae assimilate host nutrients, complete G1, divide, and disperse to new hosts. Nutrient shortages associate with high sea surface temperatures (SST), producing correlations between SST, calcification, and algal exit. Zooxanthellae proliferate when nutrients are abundant, but when nutrients later disappear, usually as SST warms, toxins and the departure of over-abundant zooxanthellae potentially overwhelm the coral and cause coral bleaching.</description><subject>Algae</subject><subject>Bleaching</subject><subject>Carbon dioxide</subject><subject>Cell cycle</subject><subject>Coral reefs</subject><subject>Corals</subject><subject>Marine</subject><subject>Nutrients</subject><subject>Photosynthesis</subject><subject>REVIEW</subject><subject>Symbiodinium</subject><subject>Symbiosis</subject><subject>Toxins</subject><issn>0171-8630</issn><issn>1616-1599</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNo90M1KxDAUBeAgCtbRhQ8gdDkuqrlJmp-lDI4KA2504yak6S3t0Da1aUHf3hkqszqbj8PhEHIL9IHzXDx2OERqlJJnJAEJMoPcmHOSUFCQacnpJbmKcU8pSKFkQtZfIfy4fqqxbR2mU-2mNAzYp961vpm71Neu77GN1-Sicm3Em_9ckc_t88fmNdu9v7xtnnaZ52CmTMiK0pILpXLPwAinKbDKSFlqJb32DhV6Y8qKIYJAl6uCeeM1lVIVlBV8RdZL7zCG7xnjZLsm-uO6HsMcLQBwxpjK-YHeL9SPIcYRKzuMTefGXwvUHt-wpzcO9m6x-ziF8QSZOMziSvM_fOlbIw</recordid><startdate>20120724</startdate><enddate>20120724</enddate><creator>McConnaughey, Ted A.</creator><general>Inter-Research</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QP</scope><scope>7SN</scope><scope>7TN</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>L.G</scope><scope>M7N</scope></search><sort><creationdate>20120724</creationdate><title>Zooxanthellae that open calcium channels</title><author>McConnaughey, Ted A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c319t-46f00d34775c2194a8012f966d876c8cae7ec99df2ee14ea57b2c9c80667b02b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Algae</topic><topic>Bleaching</topic><topic>Carbon dioxide</topic><topic>Cell cycle</topic><topic>Coral reefs</topic><topic>Corals</topic><topic>Marine</topic><topic>Nutrients</topic><topic>Photosynthesis</topic><topic>REVIEW</topic><topic>Symbiodinium</topic><topic>Symbiosis</topic><topic>Toxins</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>McConnaughey, Ted A.</creatorcontrib><collection>CrossRef</collection><collection>Calcium & Calcified Tissue Abstracts</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><jtitle>Marine ecology. 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The coral discharges the resulting protons (Ca2++ HCO₃⁻ → CaCO₃⁺ H+) into its coelenteron cavity, where they improve algal bicarbonate and nutrient assimilation. Coupling calcification with autotrophic physiologies contributes to the success of highly calcareous zooxanthellar symbioses, and to their associations with nutrient-poor tropical waters. Nutrient shortages freeze zooxanthellae in the G1 phase of the cell cycle. Dinoflagellates are often most toxic at such times, perhaps because toxins modulate their nuclear mix of cations, to control DNA conformation and activity. Increased Ca2+influx into host cells disrupts cell adhesion and induces apoptosis. Zooxanthellae assimilate host nutrients, complete G1, divide, and disperse to new hosts. Nutrient shortages associate with high sea surface temperatures (SST), producing correlations between SST, calcification, and algal exit. Zooxanthellae proliferate when nutrients are abundant, but when nutrients later disappear, usually as SST warms, toxins and the departure of over-abundant zooxanthellae potentially overwhelm the coral and cause coral bleaching.</abstract><pub>Inter-Research</pub><doi>10.3354/meps09776</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
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source | JSTOR Archival Journals and Primary Sources Collection |
subjects | Algae Bleaching Carbon dioxide Cell cycle Coral reefs Corals Marine Nutrients Photosynthesis REVIEW Symbiodinium Symbiosis Toxins |
title | Zooxanthellae that open calcium channels: implications for reef corals |
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