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DOIhttps://doi.org/10.1594/PANGAEA.779926
Seawater carbonate chemistry and pteropod Limacina helicina antarctica shell dissolution during experiments, 2012
Bednaršek; Nina; Tarling; Geraint A; Bakker; Dorothee C E; Fielding; Sophie; Cohen; Anne L; Kuzirian; Alan; McCorkle; Daniel C; Lézé; Bertrand; Montagna; Roberto
发布日期2012-04-24
数据集类型dataset
英文关键词Animalia ; Antarctic ; Bottles or small containers/Aquaria ( 20 L) ; Calcification/Dissolution ; Laboratory experiment ; Limacina helicina antarctica ; Mollusca ; Open ocean ; Pelagos ; Single species ; Temperate ; Zooplankton
英文简介Anthropogenic ocean acidification is likely to have negative effects on marine calcifying organisms, such as shelled pteropods, by promoting dissolution of aragonite shells. Study of shell dissolution requires an accurate and sensitive method for assessing shell damage. Shell dissolution was induced through incubations in CO2 enriched seawater for between 4 and 14 days. We describe a procedure that allows the level of dissolution to be assessed and classified into three main types: Type I with partial dissolution of the prismatic layer; Type II with exposure of underlying crossed-lamellar layer, and Type III, where crossed-lamellar layer shows signs of dissolution. Levels of dissolution showed a good correspondence to the incubation conditions, with the most severe damage found in specimens held for 14 d in undersaturated condition (Ohm ~ 0.8). This methodology enables the response of small pelagic calcifiers to acidified conditions to be detected at an early stage, thus making pteropods a valuable bioindicator of future ocean acidification.
语种英语
国家国际
学科大类气候变化
学科子类气候变化
文献类型数据集
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/217678
推荐引用方式
GB/T 7714
Bednaršek,Nina,Tarling,et al. Seawater carbonate chemistry and pteropod Limacina helicina antarctica shell dissolution during experiments, 2012.2012-04-24.https://doi.org/10.1594/PANGAEA.779926.
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