Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons, supplement to: Bray, Laura; Pancucci-Papadopulou, M A; Hall-Spencer, Jason M (2014): Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons. Mediterranean Marine Science, 15(3), 510-519
Ocean acidification caused by an increase in pCO2 is expected to drastically affect marine ecosystem composition, yet there is much uncertainty about the mechanisms through which ecosystems may be affected. Here we studied sea urchins that are common and important grazers in the Mediterranean (Parac...
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PANGAEA - Data Publisher for Earth & Environmental Science
2014
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Online Access: | https://dx.doi.org/10.1594/pangaea.834210 https://doi.pangaea.de/10.1594/PANGAEA.834210 |
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ftdatacite:10.1594/pangaea.834210 2023-05-15T17:50:01+02:00 Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons, supplement to: Bray, Laura; Pancucci-Papadopulou, M A; Hall-Spencer, Jason M (2014): Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons. Mediterranean Marine Science, 15(3), 510-519 Bray, Laura Pancucci-Papadopulou, M A Hall-Spencer, Jason M 2014 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.834210 https://doi.pangaea.de/10.1594/PANGAEA.834210 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://cran.r-project.org/package=seacarb https://dx.doi.org/10.12681/mms.579 https://cran.r-project.org/package=seacarb Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Animalia Arbacia lixula Benthic animals Benthos Biomass/Abundance/Elemental composition CO2 vent Echinodermata Field observation Mediterranean Sea Paracentrotus lividus Single species Temperate Site LATITUDE LONGITUDE Date Species Individuals Arsenic Bromine Cerium Chromium Copper Hafnium Manganese Molybdenum Nickel Rubidium Tin Strontium Tellurium Thorium Yttrium Zinc Calcium oxide Iron oxide Iron oxide, Fe2O3 pH pH, standard error Temperature, water Temperature, water, standard error Salinity Salinity, standard error Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide water at sea surface temperature wet air, standard error Alkalinity, total Alkalinity, total, standard error Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Carbon, inorganic, dissolved Aragonite saturation state Calcite saturation state Potentiometric Calculated using CO2SYS Potentiometric titration Calculated using seacarb after Nisumaa et al. 2010 Mediterranean Sea Acidification in a Changing Climate MedSeA Ocean Acidification International Coordination Centre OA-ICC Supplementary Dataset dataset Dataset 2014 ftdatacite https://doi.org/10.1594/pangaea.834210 https://doi.org/10.12681/mms.579 2022-02-08T16:24:46Z Ocean acidification caused by an increase in pCO2 is expected to drastically affect marine ecosystem composition, yet there is much uncertainty about the mechanisms through which ecosystems may be affected. Here we studied sea urchins that are common and important grazers in the Mediterranean (Paracentrotus lividus and Arbacia lixula). Our study included a natural CO2 seep plus reference sites in the Aegean Sea off Greece. The distribution of A. lixula was unaffected by the low pH environment, whereas densities of P. lividus were much reduced. There was skeletal degradation in both species living in acidified waters compared to reference sites and remarkable increases in skeletal manganese levels (P. lividus had a 541% increase, A. lixula a 243% increase), presumably due to changes in mineral crystalline structure. Levels of strontium and zinc were also altered. It is not yet known whether such dramatic changes in skeletal chemistry will affect coastal systems but our study reveals a mechanism that may alter inter-species interactions. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne et al, 2014) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation is 2014-07-22. Dataset Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) Bray ENVELOPE(-114.067,-114.067,-74.833,-74.833) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Animalia Arbacia lixula Benthic animals Benthos Biomass/Abundance/Elemental composition CO2 vent Echinodermata Field observation Mediterranean Sea Paracentrotus lividus Single species Temperate Site LATITUDE LONGITUDE Date Species Individuals Arsenic Bromine Cerium Chromium Copper Hafnium Manganese Molybdenum Nickel Rubidium Tin Strontium Tellurium Thorium Yttrium Zinc Calcium oxide Iron oxide Iron oxide, Fe2O3 pH pH, standard error Temperature, water Temperature, water, standard error Salinity Salinity, standard error Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide water at sea surface temperature wet air, standard error Alkalinity, total Alkalinity, total, standard error Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Carbon, inorganic, dissolved Aragonite saturation state Calcite saturation state Potentiometric Calculated using CO2SYS Potentiometric titration Calculated using seacarb after Nisumaa et al. 2010 Mediterranean Sea Acidification in a Changing Climate MedSeA Ocean Acidification International Coordination Centre OA-ICC |
spellingShingle |
Animalia Arbacia lixula Benthic animals Benthos Biomass/Abundance/Elemental composition CO2 vent Echinodermata Field observation Mediterranean Sea Paracentrotus lividus Single species Temperate Site LATITUDE LONGITUDE Date Species Individuals Arsenic Bromine Cerium Chromium Copper Hafnium Manganese Molybdenum Nickel Rubidium Tin Strontium Tellurium Thorium Yttrium Zinc Calcium oxide Iron oxide Iron oxide, Fe2O3 pH pH, standard error Temperature, water Temperature, water, standard error Salinity Salinity, standard error Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide water at sea surface temperature wet air, standard error Alkalinity, total Alkalinity, total, standard error Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Carbon, inorganic, dissolved Aragonite saturation state Calcite saturation state Potentiometric Calculated using CO2SYS Potentiometric titration Calculated using seacarb after Nisumaa et al. 2010 Mediterranean Sea Acidification in a Changing Climate MedSeA Ocean Acidification International Coordination Centre OA-ICC Bray, Laura Pancucci-Papadopulou, M A Hall-Spencer, Jason M Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons, supplement to: Bray, Laura; Pancucci-Papadopulou, M A; Hall-Spencer, Jason M (2014): Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons. Mediterranean Marine Science, 15(3), 510-519 |
topic_facet |
Animalia Arbacia lixula Benthic animals Benthos Biomass/Abundance/Elemental composition CO2 vent Echinodermata Field observation Mediterranean Sea Paracentrotus lividus Single species Temperate Site LATITUDE LONGITUDE Date Species Individuals Arsenic Bromine Cerium Chromium Copper Hafnium Manganese Molybdenum Nickel Rubidium Tin Strontium Tellurium Thorium Yttrium Zinc Calcium oxide Iron oxide Iron oxide, Fe2O3 pH pH, standard error Temperature, water Temperature, water, standard error Salinity Salinity, standard error Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide water at sea surface temperature wet air, standard error Alkalinity, total Alkalinity, total, standard error Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Carbon, inorganic, dissolved Aragonite saturation state Calcite saturation state Potentiometric Calculated using CO2SYS Potentiometric titration Calculated using seacarb after Nisumaa et al. 2010 Mediterranean Sea Acidification in a Changing Climate MedSeA Ocean Acidification International Coordination Centre OA-ICC |
description |
Ocean acidification caused by an increase in pCO2 is expected to drastically affect marine ecosystem composition, yet there is much uncertainty about the mechanisms through which ecosystems may be affected. Here we studied sea urchins that are common and important grazers in the Mediterranean (Paracentrotus lividus and Arbacia lixula). Our study included a natural CO2 seep plus reference sites in the Aegean Sea off Greece. The distribution of A. lixula was unaffected by the low pH environment, whereas densities of P. lividus were much reduced. There was skeletal degradation in both species living in acidified waters compared to reference sites and remarkable increases in skeletal manganese levels (P. lividus had a 541% increase, A. lixula a 243% increase), presumably due to changes in mineral crystalline structure. Levels of strontium and zinc were also altered. It is not yet known whether such dramatic changes in skeletal chemistry will affect coastal systems but our study reveals a mechanism that may alter inter-species interactions. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne et al, 2014) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation is 2014-07-22. |
format |
Dataset |
author |
Bray, Laura Pancucci-Papadopulou, M A Hall-Spencer, Jason M |
author_facet |
Bray, Laura Pancucci-Papadopulou, M A Hall-Spencer, Jason M |
author_sort |
Bray, Laura |
title |
Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons, supplement to: Bray, Laura; Pancucci-Papadopulou, M A; Hall-Spencer, Jason M (2014): Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons. Mediterranean Marine Science, 15(3), 510-519 |
title_short |
Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons, supplement to: Bray, Laura; Pancucci-Papadopulou, M A; Hall-Spencer, Jason M (2014): Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons. Mediterranean Marine Science, 15(3), 510-519 |
title_full |
Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons, supplement to: Bray, Laura; Pancucci-Papadopulou, M A; Hall-Spencer, Jason M (2014): Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons. Mediterranean Marine Science, 15(3), 510-519 |
title_fullStr |
Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons, supplement to: Bray, Laura; Pancucci-Papadopulou, M A; Hall-Spencer, Jason M (2014): Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons. Mediterranean Marine Science, 15(3), 510-519 |
title_full_unstemmed |
Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons, supplement to: Bray, Laura; Pancucci-Papadopulou, M A; Hall-Spencer, Jason M (2014): Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons. Mediterranean Marine Science, 15(3), 510-519 |
title_sort |
sea urchin response to rising pco2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons, supplement to: bray, laura; pancucci-papadopulou, m a; hall-spencer, jason m (2014): sea urchin response to rising pco2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons. mediterranean marine science, 15(3), 510-519 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2014 |
url |
https://dx.doi.org/10.1594/pangaea.834210 https://doi.pangaea.de/10.1594/PANGAEA.834210 |
long_lat |
ENVELOPE(-114.067,-114.067,-74.833,-74.833) |
geographic |
Bray |
geographic_facet |
Bray |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
https://cran.r-project.org/package=seacarb https://dx.doi.org/10.12681/mms.579 https://cran.r-project.org/package=seacarb |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.834210 https://doi.org/10.12681/mms.579 |
_version_ |
1766156580543266816 |