Hidden impacts of ocean acidification to live and dead coral framework
Cobertura |
LATITUDE: 56.823000 * LONGITUDE: -7.376000 * DATE/TIME START: 2011-07-01T00:00:00 * DATE/TIME END: 2011-07-30T00:00:00 |
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Data(s) |
19/05/2016
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Resumo |
Cold-water corals, such as Lophelia pertusa, are key habitat-forming organisms found throughout the world's oceans to 3000 m deep. The complex three-dimensional framework made by these vulnerable marine ecosystems support high biodiversity and commercially important species. Given their importance, a key question is how both the living and the dead framework will fare under projected climate change. Here, we demonstrate that over 12 months L. pertusa can physiologically acclimate to increased CO2, showing sustained net calcification. However, their new skeletal structure changes and exhibits decreased crystallographic and molecular-scale bonding organization. Although physiological acclimatization was evident, we also demonstrate that there is a negative correlation between increasing CO2 levels and breaking strength of exposed framework (approx. 20-30% weaker after 12 months), meaning the exposed bases of reefs will be less effective 'load-bearers', and will become more susceptible to bioerosion and mechanical damage by 2100. |
Formato |
text/tab-separated-values, 9135 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.860558 doi:10.1594/PANGAEA.860558 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
Hennige, S J; Wicks, LC; Kamenos, NA; Perna, G; Findlay, Helen S; Roberts, J Murray (2015): Hidden impacts of ocean acidification to live and dead coral framework. Proceedings of the Royal Society B-Biological Sciences, 282(1813), 20150990, doi:10.1098/rspb.2015.0990 Hennige, Sebastian; Wicks, LC; Kamenos, NA; Perna, G; Findlay, Helen S; Roberts, J Murray (2015): Physiological, biomineralisation and structural measurements of the cold-water coral (CWC) Lophelia pertusa in response to increases in CO2 and temperature. British Oceanographic Data Centre, Natural Environment Research Council, doi:10.5285/13d58735-4252-109d-e053-6c86abc0bae4 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloise (2015): seacarb: seawater carbonate chemistry with R. R package version 3.0.8. https://cran.r-project.org/package=seacarb |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #Alkalinity, total; Alkalinity, total, standard deviation; Aragonite saturation state; Aragonite saturation state, standard deviation; Area; Bicarbonate ion; Breaking load; Calcification rate of calcium carbonate; Calcite saturation state; Calculated using CO2calc; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Diameter; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Full width at half maximum; Group; Height; Height/width ratio; Identification; Incubation duration; Mingulayreef; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Peak area; Peak centre; Peak height; Percentage; pH; pH, standard deviation; Potentiometric titration; Ratio; Registration number of species; Replicate; Respiration rate, oxygen; Salinity; Salinity, standard deviation; Sample ID; Species; Temperature, water; Temperature, water, standard deviation; Thickness; Treatment; Type; Uniform resource locator/link to reference; Width |
Tipo |
Dataset |