Fast coral reef calcifiers are more sensitive to ocean acidification in short-term laboratory incubations
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- Comeau, Steeve
- 作成者
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- Edmunds, Peter J
- 作成者
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- Spindel, N B
- 作成者
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- Yang, Yan
- 寄与者
メタデータ
- 公開日
- 2014-01-01
- DOI
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- 10.1594/pangaea.832584
- 公開者
- PANGAEA
- データ作成者 (e-Rad)
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- Comeau, Steeve
- Carpenter, Robert C
- Edmunds, Peter J
- Spindel, N B
説明
To identify the properties of taxa sensitive and resistant to ocean acidification (OA), we tested the hypothesis that coral reef calcifiers differ in their sensitivity to OA as predictable outcomes of functional group alliances determined by conspicuous traits. We contrasted functional groups of eight corals and eight calcifying algae defined by morphology in corals and algae, skeletal structure in corals, spatial location of calcification in algae, and growth rate in corals and algae. The responses of calcification to OA were unrelated to morphology and skeletal structure in corals; they were, however, affected by growth rate in corals and algae (fast calcifiers were more sensitive than slow calcifiers), and by the site of calcification and morphology in algae. Species assemblages characterized by fast growth, and for algae, also cell-wall calcification, are likely to be ecological losers in the future ocean. This shift in relative success will affect the relative and absolute species abundances as well as the goods and services provided by coral reefs.
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 2014-05-16.
Supplement to: Comeau, Steeve; Edmunds, Peter J; Spindel, N B; Carpenter, Robert C (2014): Fast coral reef calcifiers are more sensitive to ocean acidification in short-term laboratory incubations. Limnology and Oceanography, 59(3), 1081-1091
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キーワード
- Ocean Acidification International Coordination Centre (OA-ICC)
- Salinity
- Lithophyllum kotschyanum
- inorganic
- Alkalinity
- total scale
- Pocillopora verrucosa
- South Pacific
- Temperature, water
- Carbon, inorganic, dissolved
- Macroalgae
- Chlorophyta
- Calculated using seacarb after Nisumaa et al 2010
- Porites sp.
- Aragonite saturation state
- Hydrolithon reinboldii
- Plantae
- Alkalinity, total
- Buoyant weighing technique according to Davies (1989)
- total
- Psammocora profundacella
- pH
- Temperature
- Calcification rate of calcium carbonate
- dissolved
- Buoyant weighing technique according to Davies 1989
- Halimeda minima
- Laboratory experiment
- Carbonate ion
- Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
- Containers and aquaria 20 1000 L or 1 m 2
- Earth System Research
- Date time start
- Containers and aquaria (20-1000 L or < 1 m**2)
- Porites rus
- Calcification/Dissolution
- Potentiometric titration
- Calcite saturation state
- Potentiometric
- water
- Porolithon onkodes
- Acropora pulchra
- Neogoniolithon frutescens
- Porites irregularis
- Amphiroa fragilissima
- Benthos
- Cnidaria
- Tropical
- Ocean Acidification International Coordination Centre OA ICC
- Lithophyllum flavescens
- Animalia
- Bicarbonate ion
- Date/time end
- Calculated using seacarb after Nisumaa et al. (2010)
- Species
- Date/time start
- Pocillopora damicornis
- Carbonate system computation flag
- Date time end
- pH, total scale
- Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
- Carbon
- Partial pressure of carbon dioxide water at sea surface temperature wet air
- Carbon dioxide
- Rhodophyta
- Single species
- Calcification Dissolution
- Fugacity of carbon dioxide water at sea surface temperature wet air
- Benthic animals
- Halimeda macroloba
- Coast and continental shelf
- Pavona cactus
- Porites sp
詳細情報 詳細情報について
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- CRID
- 1882272492427290624
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- 本文言語コード
- en
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- データソース種別
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- OpenAIRE
