Ocean acidification has no effect on thermal bleaching in the coral Seriatopora caliendrum


Autoria(s): Wall, Christopher B; Fan, Tung-Yung; Edmunds, Peter J
Cobertura

LATITUDE: 21.946650 * LONGITUDE: 120.749470 * DATE/TIME START: 2011-07-22T00:00:00 * DATE/TIME END: 2011-07-22T00:00:00

Data(s)

11/07/2014

Resumo

The objective of this study was to test whether elevated pCO2 predicted for the year 2100 (85.1 Pa) affects bleaching in the coral Seriatopora caliendrum (Ehrenberg 1834) either independently or interactively with high temperature (30.5 °C). Response variables detected the sequence of events associated with the onset of bleaching: reduction in the photosynthetic performance of symbionts as measured by maximum photochemical efficiency (F v/F m) and effective photochemical efficiency (delta F/F m') of PSII, declines in net photosynthesis (P net) and photosynthetic efficiency (alpha), and finally, reduced chlorophyll a and symbiont concentrations. S. caliendrum was collected from Nanwan Bay, Taiwan, and subjected to combinations of temperature (27.7 vs. 30.5 °C) and pCO2 (45.1 vs. 85.1 Pa) for 14 days. High temperature reduced values of all dependent variables (i.e., bleaching occurred), but high pCO2 did not affect Symbiodinium photophysiology or productivity, and did not cause bleaching. These results suggest that short-term exposure to 81.5 Pa pCO2, alone and in combination with elevated temperature, does not cause or affect coral bleaching.

Formato

text/tab-separated-values, 1801 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.833949

doi:10.1594/PANGAEA.833949

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: Wall, Christopher B; Fan, Tung-Yung; Edmunds, Peter J (2013): Ocean acidification has no effect on thermal bleaching in the coral Seriatopora caliendrum. Coral Reefs, 33(1), 119-130, doi:10.1007/s00338-013-1085-2

Palavras-Chave #Alkalinity, total; Alkalinity, total, standard error; Aragonite saturation state; Bicarbonate ion; Bicarbonate ion, standard error; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate ion, standard error; Carbonate system computation flag; Carbon dioxide; Cell density; Chlorophyll a; Chlorophyll a per cell; corals; Effective quantum yield; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Hobihu_Reef; Identification; Maximum photochemical quantum yield of photosystem II; multiple factors; Net photosynthesis rate, oxygen; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; 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; photosynthesis; Photosynthetic efficiency; Potentiometric titration; Replicate; Respiration rate, oxygen; Salinity; Species; Spectrophotometric; Surface area; temperature; Temperature, water; Temperature, water, standard error
Tipo

Dataset