Calcification in aquatic plants
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Borowitzka, M.A.
ORCID: 0000-0001-6504-4563
(1984)
Calcification in aquatic plants.
Plant, Cell and Environment, 7
(6).
pp. 457-466.
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Abstract
The CaCO3 deposits of aquatic plants may be intra‐, inter‐ and extracellular. Calcification is mainly the result of photosynthetic CO2 or HCO− 3 assimilation. This raises the local pH and CO2− 3 concentration resulting from shifts in the dissolved inorganic carbon equilibrium, due to either net CO2 depletion as in Halimeda or localized OH− efflux (or H+ influx) as in Chara. The plant cell wall may be important in CaCO3 nucleation by acting as an epitaxial substratum or template, or by creating a microenvironment enriched in Ca2+ compared to Mg2+. Hypotheses on the reason for the lack of calcification in many aquatic plants are presented.
| Item Type: | Journal Article |
|---|---|
| Murdoch Affiliation(s): | School of Environmental and Life Sciences |
| Copyright: | © 1984, Wiley Blackwell. |
| URI: | http://researchrepository.murdoch.edu.au/id/eprint/32729 |
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