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  • 1
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    PANGAEA
    In:  Supplement to: Collard, Marie; Laitat, Kim; Moulin, Laure; Catarino, Ana Isabel; Grosjean, Philippe; Dubois, Philippe (2013): Buffer capacity of the coelomic fluid in echinoderms. Comparative Biochemistry and Physiology Part A: Molecular & Integrative Physiology, 166(1), 199-206, https://doi.org/10.1016/j.cbpa.2013.06.002
    Publication Date: 2024-03-15
    Description: The increase in atmospheric CO2 due to anthropogenic activity results in an acidification of the surface waters of the oceans. The impact of these chemical changes depends on the considered organisms. In particular, it depends on the ability of the organism to control the pH of its inner fluids. Among echinoderms, this ability seems to differ significantly according to species or taxa. In the present paper, we investigated the buffer capacity of the coelomic fluid in different echinoderm taxa as well as factors modifying this capacity. Euechinoidea (sea urchins except Cidaroidea) present a very high buffer capacity of the coelomic fluid (from 0.8 to 1.8 mmol/kg SW above that of seawater), while Cidaroidea (other sea urchins), starfish and holothurians have a significantly lower one (from -0.1 to 0.4 mmol/kg SW compared to seawater). We hypothesize that this is linked to the more efficient gas exchange structures present in the three last taxa, whereas Euechinoidea evolved specific buffer systems to compensate lower gas exchange abilities. The constituents of the buffer capacity and the factors influencing it were investigated in the sea urchin Paracentrotus lividus and the starfish Asterias rubens. Buffer capacity is primarily due to the bicarbonate buffer system of seawater (representing about 63% for sea urchins and 92% for starfish). It is also partly due to coelomocytes present in the coelomic fluid (around 8% for both) and, in P. lividus only, a compound of an apparent size larger than 3 kDa is involved (about 15%). Feeding increased the buffer capacity in P. lividus (to a difference with seawater of about 2.3 mmol/kg SW compared to unfed ones who showed a difference of about 0.5 mmol/kg SW) but not in A. rubens (difference with seawater of about 0.2 for both conditions). In P. lividus, decreased seawater pH induced an increase of the buffer capacity of individuals maintained at pH 7.7 to about twice that of the control individuals and, for those at pH 7.4, about three times. This allowed a partial compensation of the coelomic fluid pH for individuals maintained at pH 7.7 but not for those at pH 7.4.
    Keywords: Acid-base regulation; Alkalinity, total; Animalia; Aragonite saturation state; Asterias rubens; Benthic animals; Benthos; Bicarbonate ion; Calcite saturation state; Calculated; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Coelomic fluid, alkalinity; Coelomic fluid, pH; Containers and aquaria (20-1000 L or 〈 1 m**2); Description; Difference; Duration, number of days; Echinaster sepositus; Echinocardium cordatum; Echinodermata; Echinometra mathaei; Eucidaris tribuloides; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Henricia oculata; Holothuria forskali; Holothuria tubulosa; Identification; Laboratory experiment; Not applicable; OA-ICC; Ocean Acidification International Coordination Centre; Other; Paracentrotus lividus; Partial pressure of carbon dioxide (water) at equilibrator temperature (wet air); Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Phyllacanthus imperialis; Potentiometric; Potentiometric titration; Remaining buffer capacity; Replicates; Salinity; Sample code/label; Single species; Species; Temperate; Temperature, water; Treatment; Tripneustes ventricosus; Tropical
    Type: Dataset
    Format: text/tab-separated-values, 6964 data points
    Location Call Number Limitation Availability
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  • 2
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    Unknown
    PANGAEA
    In:  Supplement to: Moulin, Laure; Grosjean, Philippe; Leblud, Julien; Batigny, Antoine; Dubois, Philippe (2014): Impact of elevated pCO2 on acid–base regulation of the sea urchin Echinometra mathaei and its relation to resistance to ocean acidification: A study in mesocosms. Journal of Experimental Marine Biology and Ecology, 457, 97-104, https://doi.org/10.1016/j.jembe.2014.04.007
    Publication Date: 2024-03-15
    Description: Due to their low metabolism and apparent poor ion regulation ability, sea urchins could be particularly sensitive to ocean acidification resulting from increased dissolution of atmospheric carbon dioxide. Therefore, we evaluated the acid-base regulation ability of the coral reef sea urchin Echinometra mathaei and the impact of decreased pH on its growth and respiration activity. The study was conducted in two identical artificial reef mesocosms during seven weeks. Experimental tanks were maintained respectively at mean pHT 7.7 and 8.05 (with field-like night and day variations). The major physico-chemical parameters were identical, only pCO2 and pHT differed. Results indicate that E. mathaei can regulate the pH of its coelomic fluid in the considered range of pH, allowing a sustainable growth and ensuring an unaffected respiratory metabolism, at least at short term.
    Keywords: Acid-base regulation; Alkalinity, total; Animalia; Aquarium number; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Calcite saturation state; Calculated; Calculated using seacarb; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Coelomic fluid, alkalinity; Coelomic fluid, partial pressure of carbon dioxide; Coelomic fluid, pH; Containers and aquaria (20-1000 L or 〈 1 m**2); Date; Echinodermata; Echinometra mathaei; Figure; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth; Growth/Morphology; Identification; Incubation duration; Indian Ocean; Individual code; Infrared spectrometric; Laboratory experiment; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Potentiometric; Potentiometric titration; Respiration; Respiration rate, oxygen; Salinity; Single species; Species; Temperature, water; Tropical
    Type: Dataset
    Format: text/tab-separated-values, 3152 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2022-05-25
    Description: Author Posting. © Oceanography Society, 2007. This article is posted here by permission of Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 20, 2 (2007): 172-187.
    Description: When Victor Hensen deployed the first true plankton1 net in 1887, he and his colleagues were attempting to answer three fundamental questions: What planktonic organisms are present in the ocean? How many of each type are present? How does the plankton’s composition change over time? Although answering these questions has remained a central goal of oceanographers, the sophisticated tools available to enumerate planktonic organisms today offer capabilities that Hensen probably could never have imagined.
    Description: This material is based upon work supported by the National Science Foundation under Grants OCE-0325018, OCE-0324937, OCE-0325167 and OCE-9423471, and the European Union under grants Q5CR-2002-71699, MAS3-ct98-0188, and MAS2-ct92-0015.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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