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  • Abaiang_Kiribati; Acid-base regulation; Aitutaki_Cook_New_Zeland; Alkalinity, total; Anakena_Isla_de_Pascua_Chile; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Biomass/Abundance/Elemental composition; Boron/Calcium ratio; Calcification/Dissolution; Calcification rate; Calcifying fluid, aragonite saturation state; Calcifying fluid, carbonate ion; Calcifying fluid, dissolved inorganic carbon; Calcifying fluid, pH; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Clipperton_France; Cnidaria; Coast and continental shelf; Coiba_Panama; CSR_11_Wallis_France; Date/Time of event; Density; DEPTH, water; Diploastrea heliopora; E_Vangunu_Salomon; Event label; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Green_Island_Taiwan; Growth/Morphology; Guam_USA; Helen_Reef_Palau_1; Helen_Reef_Palau_2; Heron_S_GBR_Australia; Identification; Kimbe_Hoskins_District_PNG; Koror_Palau; LATITUDE; Linear extension; Location; LONGITUDE; Losuia_Tabungora_Island_PNG; Moorea_French_Polynesia_1; Moorea_French_Polynesia_2; Motu_Taka_Rua_Isla_de_Pascua_Chile; N_Hoskins_District_PNG; North_Palau; North Pacific; Noumea_Lagoon_New_Caledonia; NW_Fiji; OA-ICC; Ocean Acidification International Coordination Centre; Ogasawara_Japan; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Pisinun_Chuuk_Micronesia; Porites sp.; Potentiometric titration; S_Niue_New_Zeland; Salinity; Sample ID; Secas_islands_Panama; Sesoko_Okinawa_Japan; Single species; South Pacific; Species; SW_Cockatoo_Reef_GBR_Australia; Tekava_Gambier_French_Polynesia; Temperate; Temperature, water; Tropical; Type of study; Upolu_Samoa; W_Niue_New_Zeland; δ11B  (1)
  • Ciliates  (1)
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  • 1
    Publication Date: 2024-05-07
    Description: The Tara Pacifc expedition (2016–2018) provided an opportunity to investigate calcifcation patterns in extant corals throughout thePacifc Ocean. Cores from colonies of the massive Porites and Diploastrea genera were collected fromdiferent environments to assess calcifcation parameters of long-lived reef-building corals. In this study, we compared the calcifcation and carbonate chemistryup-regulation of Diploastrea heliopora and Porites corals from across a range of environments. To this, we analyzed the skeletal geochemistry and growth parameters of 39 colonies of Porites (n=33) and Diploastrea (n=6) collected across the tropical Pacifc Ocean during the Tara Pacifc expedition (2016–2018). Te collected corals represent a suite of cores exposed to various hydrological conditions of seawater temperature (SST: 22.4–29.8 °C), salinity (SSS: 31.5–36.1), and carbonate chemistry (total scale pHsw: 8.01–8.09). Te average chemical composition of the calcifying fuid (pHcf, [CO32−]cf, DICcf, Ωcf) was derived from paired boron isotope (δ11B) and B/Ca analyses of core-top samples corresponding to the last 6 years of growth (2010–2016). Based on these data, we assessed the impact of the ambient seawater properties (SST, salinity, carbonate chemistry) on the cf composition of these slow-growing reef-building genera at the Pacifc basin scale.
    Keywords: Abaiang_Kiribati; Acid-base regulation; Aitutaki_Cook_New_Zeland; Alkalinity, total; Anakena_Isla_de_Pascua_Chile; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Biomass/Abundance/Elemental composition; Boron/Calcium ratio; Calcification/Dissolution; Calcification rate; Calcifying fluid, aragonite saturation state; Calcifying fluid, carbonate ion; Calcifying fluid, dissolved inorganic carbon; Calcifying fluid, pH; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Clipperton_France; Cnidaria; Coast and continental shelf; Coiba_Panama; CSR_11_Wallis_France; Date/Time of event; Density; DEPTH, water; Diploastrea heliopora; E_Vangunu_Salomon; Event label; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Green_Island_Taiwan; Growth/Morphology; Guam_USA; Helen_Reef_Palau_1; Helen_Reef_Palau_2; Heron_S_GBR_Australia; Identification; Kimbe_Hoskins_District_PNG; Koror_Palau; LATITUDE; Linear extension; Location; LONGITUDE; Losuia_Tabungora_Island_PNG; Moorea_French_Polynesia_1; Moorea_French_Polynesia_2; Motu_Taka_Rua_Isla_de_Pascua_Chile; N_Hoskins_District_PNG; North_Palau; North Pacific; Noumea_Lagoon_New_Caledonia; NW_Fiji; OA-ICC; Ocean Acidification International Coordination Centre; Ogasawara_Japan; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Pisinun_Chuuk_Micronesia; Porites sp.; Potentiometric titration; S_Niue_New_Zeland; Salinity; Sample ID; Secas_islands_Panama; Sesoko_Okinawa_Japan; Single species; South Pacific; Species; SW_Cockatoo_Reef_GBR_Australia; Tekava_Gambier_French_Polynesia; Temperate; Temperature, water; Tropical; Type of study; Upolu_Samoa; W_Niue_New_Zeland; δ11B
    Type: Dataset
    Format: text/tab-separated-values, 1532 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-05-26
    Description: Author Posting. © Inter-Research, 2009. This article is posted here by permission of Inter-Research for personal use, not for redistribution. The definitive version was published in Aquatic Microbial Ecology 57 (2009): 279-310, doi:10.3354/ame01340.
    Description: Acquisition of phototrophy is widely distributed in the eukaryotic tree of life and can involve algal endosymbiosis or plastid retention from green or red origins. Species with acquired phototrophy are important components of diversity in aquatic ecosystems, but there are major differences in host and algal taxa involved and in niches of protists with acquired phototrophy in marine and freshwater ecosystems. Organisms that carry out acquired phototrophy are usually mixotrophs, but the degree to which they depend on phototrophy is variable. Evidence suggests that ‘excess carbon’ provided by acquired phototrophy has been important in supporting major evolutionary innovations that are crucial to the current ecological roles of these protists in aquatic ecosystems. Acquired phototrophy occurs primarily among radiolaria, foraminifera, ciliates and dinoflagellates, but is most ecologically important among the first three. Acquired phototrophy in foraminifera and radiolaria is crucial to their contributions to carbonate, silicate, strontium, and carbon flux in subtropical and tropical oceans. Planktonic ciliates with algal kleptoplastids are important in marine and fresh waters, whereas ciliates with green algal endosymbionts are mostly important in freshwaters. The phototrophic ciliate Myrionecta rubra can be a major primary producer in coastal ecosystems. Our knowledge of how acquired phototrophy influences trophic dynamics and biogeochemical cycles is rudimentary; we need to go beyond traditional concepts of ‘plant’ and ‘animal’ functions to progress in our understanding of aquatic microbial ecology. This is a rich area for exploration using a combination of classical and molecular techniques, laboratory and field research, and physiological and ecosystem modeling.
    Description: F.N. and C.dV were supported by a SAD grant SYMFORAD from the Région Bretagne (France) and the BioMarKs project funded by the European ERA-net program BiodivERsA.
    Keywords: Mixotrophy ; Radiolaria ; Foraminifera ; Ciliates ; Dinoflagellates ; Kleptoplastidy ; Karyoklepty ; Endosymbiosis ; Myrionecta rubra
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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