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  • 1
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    PANGAEA
    In:  Supplement to: Suzuki, A; Nakamori, T; Kayanne, Hajime (1995): The mechanism of production enhancement in coral reef carbonate systems: model and empirical results. Sedimentary Geology, 99(3-4), 259-280, https://doi.org/10.1016/0037-0738(95)00048-D
    Publication Date: 2024-03-15
    Description: Coral reefs are characterized by enormous carbonate production of the organisms. It is known that rapid calcification is linked to photosynthesis under control of the carbonate equilibrium in seawater. We have established a model simulating the coexisting states of photosynthesis and calcification in order to examine the effects of photosynthesis and calcification on the carbonate system in seawater. Supposing that the rates of photosynthesis and calcification are proportional to concentrations of their inorganic carbon source, the model calculations indicate that three kinds of unique interactions of the organic and inorganic carbon productions are expected. These are photosynthetic enhancement of calcification, calcification which benefits photosynthesis and carbonate dissolution induced by respiration. The first effect appears when the photosynthetic rate is more than approximately 1.2 larger than that of calcification. This effect is caused by the increase of CO3 content and carbonate saturation degree in seawater. If photosynthesis use molecular carbon dioxide, the second effect occurs when the calcification rate is more than approximately 1.6 times larger than that of photosynthesis. Time series model experiments indicate that photosynthesis and calcification potentially enhance each other and that organic and inorganic carbon is produced more efficiently in the coexisting system than in the isolated reactions. These coexisting effects on production enhancement of photosynthesis and calcification are expected to appear not only in the internal pool of organisms but also in a reef environment which is isolated from the outer ocean during low tide. According to the measurements on the fringing type Shiraho Reef in the Ryukyu Islands, the diurnal change of water properties (pH, total alkalinity, total carbon dioxide and carbonate saturation degree) were conspicuous. This environment offers an appropriate condition for the appearance of these coexisting effects. The photosynthetic enhancement of calcification and the respiratory inducement of decalcification were observed during day-time and night-time slack-water periods, respectively. These coexisting effects, especially the photosynthetic enhancement of calcification, appear to play important roles for fluorishing coral reef communities.
    Keywords: Alkalinity, total; Alkalinity anomaly technique (Smith and Key, 1975); Aragonite saturation state; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate of calcium carbonate; Calcite saturation state; Calculated; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbon dioxide; Coast and continental shelf; DATE/TIME; DEPTH, water; Entire community; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Measured; North Pacific; OA-ICC; OCE; Ocean Acidification International Coordination Centre; Oceanography; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Radiation, photosynthetically active; Rocky-shore community; Salinity; Suzuki_etal_94/95; Temperate; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 189 data points
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Agostini, Sylvain; Fujimura, Hiroyuki; Higuchi, Tomihiko; Yuyama, Ikuko; Casareto, Beatriz E; Suzuki, Yoshimi; Nakano, Yoshiyuki (2013): The effects of thermal and high-CO2 stresses on the metabolism and surrounding microenvironment of the coral Galaxea fascicularis. Comptes Rendus Biologies, 336(8), 384-391, https://doi.org/10.1016/j.crvi.2013.07.003
    Publication Date: 2024-03-15
    Description: The effects of elevated temperature and high pCO2 on the metabolism of Galaxea fascicularis were studied with oxygen and pH microsensors. Photosynthesis and respiration rates were evaluated from the oxygen fluxes from and to the coral polyps. High-temperature alone lowered both photosynthetic and respiration rates. High pCO2 alone did not significantly affect either photosynthesis or respiration rates. Under a combination of high-temperature and high-CO2, the photosynthetic rate increased to values close to those of the controls. The same pH in the diffusion boundary layer was observed under light in both (400 and 750 ppm) CO2 treatments, but decreased significantly in the dark as a result of increased CO2. The ATP contents decreased with increasing temperature. The effects of temperature on the metabolism of corals were stronger than the effects of increased CO2. The effects of acidification were minimal without combined temperature stress. However, acidification combined with higher temperature may affect coral metabolism due to the amplification of diel variations in the microenvironment surrounding the coral and the decrease in ATP contents.
    Keywords: Adenosine triphosphate, per unit protein; Alkalinity, total; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); 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; Cnidaria; Coast and continental shelf; Comment; Figure; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Galaxea fascicularis; Gross photosynthesis rate, oxygen; Identification; Laboratory experiment; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; Potentiometric; Potentiometric titration; Primary production/Photosynthesis; Respiration; Respiration rate, carbon dioxide; Salinity; Single species; Species; Temperate; Temperature; Temperature, water; Temperature, water, standard deviation; Time in minutes; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 9400 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-03-15
    Description: Only about half of all the CO_2 that has been produced by the burning of fossil fuels now remains in the atmosphere. The CO_2 "missing" from the atmosphere is the subject of an important debate. It was thought that the great majority of the missing CO_2 has invaded the ocean, for this system naturally acts as a giant chemical regulator of the atmosphere. Although it is clear that ocean processes have a major role in the regulation of the carbon dioxide content of the atmosphere through air-sea exchange processes, recent studies of the oceanic carbon cycle and air-sea interaction indicate that oceanic carbon is in a quasi-steady state via the system of biological and physical processes in the ocean interior. It is difficult to determine whether the ocean has the capacity to take up the increasing air-born CO_2 released by human activities over the past five or six decades. To understand this enigma, we need a better understanding of the natural variability of the oceanic carbon cycle.
    Keywords: Alkalinity, total; Aragonite saturation state; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate of calcium carbonate; Calcite saturation state; Calculated; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbon dioxide; Coast and continental shelf; DATE/TIME; DEPTH, water; Entire community; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Experimental treatment; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Measured; OCE; Oceanography; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Radiation, photosynthetically active; Rocky-shore community; Salinity; Suzuki_95; Temperate; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 340 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-03-15
    Description: Production (abundance and biomass) and net calcification rates of the coccolithophorid Pleurochrysis carterae under different partial pressures of CO2 (pCO2) were examined using short (15, 24 and 39 h), long (7 d) and dark (7 d) incubation experiments. Short incubations were conducted at ambient, 500 and 820 ppm pCO2 levels in natural seawater that was enriched with nutrients and inoculated with P. carterae. Long incubations were conducted at ambient and 1200 ppm pCO2 levels in natural seawater (0.2 µm filtered as well as unfiltered) that was enriched with nutrients and inoculated with P. carterae. Dark incubations were conducted at ambient and 1200 ppm pCO2 in unfiltered seawater that was inoculated with P. carterae. The abundance and biomass of coccolithophorids increased with pCO2 and time. The abundance and biomass of most noncalcifying phytoplankton also increased, and were hardly affected by CO2 inputs. Net calcification rates were negative in short incubations during the pre-bloom phase regardless of pCO2 levels, indicating dissolution of calcium carbonate. Further, the negative values of net calcification in short incubations became less negative with time. Net calcification rates were positive in long incubations during blooms regardless of pCO2 level, and the rate of calcification increased with pCO2. Our results show that P. carterae may adapt to increased (~1200 ppm) pCO2 level with time, and such increase has little effect on the ecology of noncalcifying groups and hence in ecosystem dynamics. In dark incubations, net calcification rates were negative, with the magnitude being dependent on pCO2 levels.
    Keywords: 13C tracer technique according to Hama et al. (1993); Alkalinity, total; Alkalinity, total, standard deviation; Alkalinity anomaly technique (Smith and Key, 1975); Aragonite saturation state; Bacteria, biomass; Bacteria, biomass as carbon, standard deviation; Bicarbonate ion; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcification rate, standard deviation; Calcification rate of calcium carbonate; Calcite saturation state; Calculated; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, particulate; Carbon, organic, particulate; Carbon, organic, particulate/Nitrogen, organic, particulate ratio; Carbon, total; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chromista; Coccolithophoridae, biomass as carbon; Coccolithophoridae, biomass as carbon, standard deviation; Cyanobacteria, biomass as carbon; Cyanobacteria, biomass as carbon, standard deviation; Entire community; Experimental treatment; Experiment day; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Haptophyta; Laboratory experiment; Laboratory strains; Mass spectrometer Thermo Finnigan DELTA plus Advantage; Measured; Microscopy; Microzooplankton, biomass as carbon; Microzooplankton, biomass as carbon, standard deviation; Nitrate; Nitrogen, organic, particulate; Not applicable; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate inorganic carbon/particulate organic carbon ratio; Particulate inorganic carbon/particulate organic carbon ratio, standard deviation; Pelagos; pH; pH, standard deviation; pH meter (Orion); Phosphate; Phytoplankton; Phytoplankton, other, noncalcifying, biomass as carbon; Phytoplankton, other, noncalcifying, biomass as carbon, standard deviation; Pico-/Nanoplankton heterotrophic eukaryotic, biomass; Pico-/Nanoplankton heterotrophic eukaryotic, biomass, standard deviation; Pleurochrysis carterae; Potentiometric titration (Radiometer TIM850); Primary production/Photosynthesis; Primary production of carbon; Salinity; Single species; Temperature, water; Time in hours
    Type: Dataset
    Format: text/tab-separated-values, 760 data points
    Location Call Number Limitation Availability
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  • 5
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    PANGAEA
    In:  Supplement to: Sultana, Rumana; Casareto, Beatriz E; Sohrin, Rumi; Suzuki, Toshiyuki; Alam, Md Shafiul; Fujimura, Hiroyuki; Suzuki, Yoshimi (2016): Response of Subtropical Coastal Sediment Systems of Okinawa, Japan, to Experimental Warming and High pCO2. Frontiers in Marine Science, 3, https://doi.org/10.3389/fmars.2016.00100
    Publication Date: 2024-03-15
    Description: Increasing seawater temperatures and CO2 levels associated with climate change affect the shallow marine ecosystem function. In this study, the effects of elevated seawater temperature and partial pressure of CO2 (pCO2) on subtropical sediment systems of mangrove, seagrass, and coral reef lagoon habitats of Okinawa, Japan, were examined. Sediment and seawater from each habitat were exposed to four pCO2-temperature treatments, including ambient pCO2- ambient temperature, ambient pCO2-high temperature (ambient temperature + 4°C), high pCO2 (936 ppm)-ambient temperature, and high pCO2-high temperature. Parameters including primary production, nutrient flux, pigment content, photosynthetic community composition, and bacterial abundance were examined. Neither high temperature nor high pCO2 alone impacted mangrove and seagrass sediment primary production significantly (Tukey's test, P 〉 0.05). However, the combined stress significantly (Tukey's test, P 〈 0.01) increased primary production in these two habitats. In sediments from the coral reef lagoon, single and combined stress treatments induced a shift from heterotrophy to autotrophy. Significant increases in net primary production (Tukey's test, P 〈 0.01), and gross primary production (Tukey's test, P 〈 0.05) under the combined stress suggested that benthic microalgae in mangrove and seagrass sediments were more responsive to high temperature and pCO2 conditions than those in coral reef lagoon sediments. Additionally, combined stress significantly increased the sediment chlorophyll a content (Tukey's test, P 〈 0.05) in all habitats. These increases were associated with increased net primary production, indicating that combined stress stimulates primary production activity by the photosynthetic benthic microalgae in all habitats. Diatom activity increased, as silicate uptake increased in all habitats. Microbial abundance significantly increased under the combined stress treatment (Tukey's test, P 〈 0.01), but did not exceed autotrophic activity. Respiration did not change significantly in any of the three habitats (Tukey's test, P 〉 0.05) under the combined stress, suggesting that heterotrophic processes were less affected by the combined stress than autotrophic processes. In summary, mangrove and seagrass sediments minimize the negative impacts of elevated temperature and pCO2 via increased primary production and carbon storage. Lagoonal sediments also act as a carbon sink under temperature and ocean acidification stress.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Ammonium, flux; Ammonium, flux, standard deviation; Aragonite saturation state; Benthos; beta-Carotene, flux; beta-Carotene, flux, standard deviation; Bicarbonate ion; Bicarbonate ion, standard deviation; Biomass/Abundance/Elemental composition; Bise_seagrass; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, standard deviation; Change in bacterial abundance; Change in bacterial abundance, standard deviation; Chlorophyll a, flux; Chlorophyll a, flux, standard deviation; Chlorophyll b, flux; Chlorophyll b, flux, standard deviation; Chlorophyll c2, flux; Chlorophyll c2, flux, standard deviation; Coast and continental shelf; Entire community; Event label; EXP; Experiment; Fucoxanthin, flux; Fucoxanthin, flux, standard deviation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gross primary production, standard deviation; Gross primary production of carbon; Habitat; Laboratory experiment; Light mode; Net primary production of carbon; Net primary production of carbon, standard deviation; Nitrite and nitrate, flux; Nitrite and nitrate, flux, standard deviation; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Other metabolic rates; Oxygen, flux; Oxygen, flux, standard deviation; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; Phosphate, flux; Phosphate, flux, standard deviation; Potentiometric; Potentiometric titration; Primary production/Photosynthesis; Respiration; Respiration rate, carbon; Respiration rate, carbon dioxide, standard deviation; Salinity; Salinity, standard deviation; Sesoko_reef; Silicate, flux; Silicate, flux, standard deviation; Soft-bottom community; Temperate; Temperature; Temperature, water; Temperature, water, standard deviation; Treatment; Type; Yagachi_Island; Zeaxanthin, flux; Zeaxanthin, flux, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 3156 data points
    Location Call Number Limitation Availability
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 352 (1991), S. 612-614 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Our experiments were conducted as part of the Joint Global Ocean Flux Study (JGOFS), which had the objective of examining the 1989 spring phytoplankton bloom in the North Atlantic Ocean (47° N; 18° W) and its role in the ocean carbon cycle5. The bloom started in late April, as indicated by ...
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 32 (1976), S. 235-241 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract By using the new fluorometric method of determination of the total selenium (Σ Se), Se (IV) and Se (VI), the content of selenium in sea weter was determined in the western North Pacific. Results showed that the content ofΣ Se in surface water ranged from 0.06 to 0.12μg l−1, while in deeper layers, the content increased to 0.20μg l−1. It was found that Se (IV) showed rather uniform distribution with depth, while Se (VI) increased with depth to about three times that in the surface. The ratio of Se (IV) to theΣ Se ranged from 0.5 to 0.8 in the surface and 0.4 to 0.6 in the deep. The coexistence of the hexa- and tetravalent ions of selenium was confirmed both in surface and deep layers. Some results of observations on the content of selenium in the coastal areas of Japan were also reported.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 33 (1977), S. 23-29 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract A new method of determination of selenium and separation of Se(IV) and Se(VI) in sea water is described. The selenium is determined by fluorometric method using Se-DAN complex in cyclohexane media. Prior to the fluorometric determination, Se(IV) is separated from sea water by means of Se(IV)-DDTC complex which is adsorbed on the macroreticular resin. As to the separation of the total selenium from sea water sample, the reduction and coprecipitation method is used. Se(VI) is determined with the same method as used for the total selenium after the separation of Se(IV). The average recoveries are 92.5±1.3% for Se(IV) and 97.4±0.9% for ∑Se. The standard deviation of analytical results is below 10%.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Journal of oceanography 34 (1978), S. 93-96 
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract In order to clarify the chemical forms of minor metallic elements occurring in the ocean, a new method of separation of organic compounds of metals in sea water by using XAD-2 resin was contrived. By applying the new method of determination, it is found that, (1) More than 80 % of V, Fe, Cd and Cu dissolved in sea water are present in organic forms regardless of the depth; (2) A most part of Co and Pb are present in organic forms near the surface, but they change into inorganic forms in the deep layer up to 50 to 60%; (3) Of the total amounts of dissolved Al, Ni, Zn, Ag, Mo, and U, less than 30 % are present in organic forms in sea water anywhere in the ocean; (4) Up to 45% of Se is in organic forms.
    Type of Medium: Electronic Resource
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