The morphological response of Emiliania huxleyi to seawater carbonate chemistry changes: an inter-strain comparison
Cobertura |
MEDIAN LATITUDE: 5.162500 * MEDIAN LONGITUDE: 76.658333 * SOUTH-BOUND LATITUDE: -42.300000 * WEST-BOUND LONGITUDE: -20.333330 * NORTH-BOUND LATITUDE: 63.400000 * EAST-BOUND LONGITUDE: 169.833330 * DATE/TIME START: 1998-09-01T00:00:00 * DATE/TIME END: 2005-11-30T00:00:00 |
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Data(s) |
21/01/2011
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Resumo |
Four strains of the coccolithophore Emiliania huxleyi (RCC1212, RCC1216, RCC1238, RCC1256) were grown in dilute batch culture at four CO2 levels ranging from ~200 µatm to ~1200 µatm. Coccolith morphology was analyzed based on scanning electron micrographs. Three of the four strains did not exhibit a change in morphology over the CO2 range tested. One strain (RCC1256) displayed an increase in the percentage of malformed coccoliths with increasing CO2 concentration. We conclude that the sensitivity of the coccolith-shaping machinery to carbonate chemistry changes is strain-specific. Although it has been shown before that carbonate chemistry related changes in growth- and calcification rate are strain-specific, there seems to be no consistent correlation between coccolith morphology and growth or calcification rate. We did not observe an increase in the percentage of incomplete coccoliths in RCC1256, indicating that the coccolith-shaping machinery per se is affected by acidification and not the signalling pathway that produces the stop-signal for coccolith growth. |
Formato |
text/tab-separated-values, 496 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.826456 doi:10.1594/PANGAEA.826456 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
Lavigne, Héloise; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4. https://cran.r-project.org/package=seacarb |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Fonte |
Supplement to: Langer, Gerald; Probert, Ian; Nehrke, Gernot; Ziveri, Patrizia (2011): The morphological response of Emiliania huxleyi to seawater carbonate chemistry changes: an inter-strain comparison. Journal of Nannoplankton Research, 32(1), 29-34, hdl:10013/epic.37875.d001 |
Palavras-Chave | #Alkalinity, total; Aragonite saturation state; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; 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; Coccoliths, incomplete; Coccoliths, incomplete, standard deviation; Coccoliths, malformed and incomplete; Coccoliths, malformed and incomplete, standard deviation; Coccoliths, normal; Coccoliths, normal, standard deviation; EPOCA; European Project on Ocean Acidification; Event label; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); laboratory; Malformation rate; Malformation rate, standard deviation; Mediterranean Sea Acidification in a Changing Climate; MedSeA; molecular biology; morphology; Nitrate; North_Atlantic_OA; North_Pacific_OA; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Phosphate; phytoplankton; Potentiometric titration; Replicates; Salinity; South_Atlantic_OA; Species; Strain; Tasman_Sea_OA; Temperature, water |
Tipo |
Dataset |