Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons


Autoria(s): Bray, Laura; Pancucci-Papadopulou, M A; Hall-Spencer, Jason M
Cobertura

MEDIAN LATITUDE: 37.644325 * MEDIAN LONGITUDE: 23.637834 * SOUTH-BOUND LATITUDE: 37.637850 * WEST-BOUND LONGITUDE: 23.357911 * NORTH-BOUND LATITUDE: 37.653088 * EAST-BOUND LONGITUDE: 24.023764 * DATE/TIME START: 2012-05-01T00:00:00 * DATE/TIME END: 2012-09-30T00:00:00

Data(s)

22/07/2014

Resumo

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.

Formato

text/tab-separated-values, 3851 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.834210

doi:10.1594/PANGAEA.834210

Idioma(s)

en

Publicador

PANGAEA

Relação

Lavigne, Héloise; Epitalon, Jean-Marie; Gattuso, Jean-Pierre (2014): seacarb: seawater carbonate chemistry with R. R package version 3.0. https://cran.r-project.org/package=seacarb

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Fonte

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, doi:10.12681/mms.579

Palavras-Chave #abundance; Alkalinity, total; Alkalinity, total, standard error; Aragonite saturation state; Arsenic; Bicarbonate ion; Bromine; Calcite saturation state; Calcium oxide; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cerium; Chromium; Copper; Date; echinoderms; EXP; Experiment; field; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Hafnium; Hellenic_Volcanic_Arc; Individuals; Iron oxide; Iron oxide, Fe2O3; LATITUDE; LONGITUDE; Manganese; Mediterranean; Mediterranean Sea Acidification in a Changing Climate; MedSeA; Molybdenum; morphology; Nickel; OA-ICC; Ocean Acidification International Coordination Centre; other process; 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; pH; pH, standard error; Potentiometric; Potentiometric titration; Rubidium; Salinity; Salinity, standard error; Site; Species; Strontium; Tellurium; Temperature, water; Temperature, water, standard error; Thorium; Tin; Yttrium; Zinc
Tipo

Dataset