Nutrient availability affects the response of the calcifying chlorophyte Halimeda opuntia (L.) J.V. Lamouroux to low pH

Atmospheric carbon dioxide emissions cause a decrease in the pH and aragonite saturation state of surface ocean water. As a result, calcifying organisms are expected to suffer under future ocean conditions, but their physiological responses may depend on their nutrient status. Because many coral ree...

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Bibliographic Details
Published in:	Planta Vol. 239; no. 1; pp. 231 - 242
Main Authors:	Hofmann, Laurie C., Heiden, Jasmin, Bischof, Kai, Teichberg, Mirta
Format:	Journal Article
Language:	English
Published:	Berlin/Heidelberg Springer-Verlag 01-01-2014 Springer Berlin Heidelberg Springer Nature B.V
Subjects:	Accretion Acidification Agriculture Algae Biological Availability Biomedical and Life Sciences Carbon Carbon - pharmacokinetics Carbon Dioxide Carbon dioxide emissions Carbonic Anhydrases - metabolism Chlorophyta - growth & development Chlorophyta - physiology Coral Reefs Ecology Forestry Halimeda opuntia Hydrogen-Ion Concentration Inorganic carbon Life Sciences Nitrate Reductase - metabolism Nitrates Nitrogen Nitrogen - pharmacokinetics Nutrient availability Nutrient balance Nutrient loading Nutrient status Nutrients Ocean acidification Opuntia Organic carbon Organic phosphorus Original Article Phosphates Phosphorus Phosphorus - pharmacokinetics Physiological responses Plant Sciences Sea water Seawater - chemistry Calcification Carbonic anhydrase Ocean acidification Photosynthesis Nitrate reductase Eutrophication
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