2002
DOI: 10.1071/pp01187
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Freshwater angiosperm carbon concentrating mechanisms: processes and patterns

Abstract: Aquatic angiosperms are derived from terrestrial ancestors and appear to have re-invaded water on many occasions. While removing problems of water supply and reducing the need for supporting tissue, freshwaters have a potentially low and fluctuating supply of CO2 for photosynthesis, as well as generally low light. This paper reviews the structural, morphological, physiological, and biochemical features of freshwater macrophytes in the context of maximising net carbon uptake underwater, and discusses how inorga… Show more

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Cited by 205 publications
(163 citation statements)
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“…Higher concentrations of CO 2 in bottom sediments (as a result of microbial activity) are also exploited by some macrophytes (e.g., Isoetes) whereby CO 2 in the interstitial sediment water diffuses into the roots and then through gas-filled lacunae to the leaves (Raven et al, 1988). In addition to morphological changes, physiological strategies such as utilization of bicarbonate (in addition to CO 2 ) as an inorganic carbon source and additional biochemical carboxylation pathways (including crassulacean acid metabolism, found, for example, in Isoetes, Crassula, Littorella, Sagittaria and Vallisneria, and C4-like metabolism found in Hydrilla verticillata and Egeria densa) have evolved to cope with reduced availability of CO 2 and the prevalence of HCO 3 -as the dominant form of inorganic carbon in higher-pH waters (Maberly & Madsen, 2002). The limited availability of oxygen in aquatic systems has also resulted in development of aerenchyma-tissue containing enlarged gas spaces-for transport of oxygen from shoot to roots and venting of gases (carbon dioxide, ethylene, methane) from the root and soil (Sculthorpe, 1967).…”
Section: Species and Generic Diversitymentioning
confidence: 99%
“…Higher concentrations of CO 2 in bottom sediments (as a result of microbial activity) are also exploited by some macrophytes (e.g., Isoetes) whereby CO 2 in the interstitial sediment water diffuses into the roots and then through gas-filled lacunae to the leaves (Raven et al, 1988). In addition to morphological changes, physiological strategies such as utilization of bicarbonate (in addition to CO 2 ) as an inorganic carbon source and additional biochemical carboxylation pathways (including crassulacean acid metabolism, found, for example, in Isoetes, Crassula, Littorella, Sagittaria and Vallisneria, and C4-like metabolism found in Hydrilla verticillata and Egeria densa) have evolved to cope with reduced availability of CO 2 and the prevalence of HCO 3 -as the dominant form of inorganic carbon in higher-pH waters (Maberly & Madsen, 2002). The limited availability of oxygen in aquatic systems has also resulted in development of aerenchyma-tissue containing enlarged gas spaces-for transport of oxygen from shoot to roots and venting of gases (carbon dioxide, ethylene, methane) from the root and soil (Sculthorpe, 1967).…”
Section: Species and Generic Diversitymentioning
confidence: 99%
“…Compared with terrestrial plants, aquatic macrophytes experience approximately 10 4 slower diffusion and a much lower solubility of gases in water than in air [1,2]. The efficient exchange of nutrients and gases is further exacerbated by the diffusive boundary layer (DBL) surrounding all submersed surfaces [3].…”
Section: Introductionmentioning
confidence: 99%
“…Even though there is no evidence for PEPC-activity resp. C 4 photosynthesis within Myriophyllum species (Maberly & Madsen, 2002), the HCO À 3 use mechanisms were induced by environmental conditions in our study. Olesen & Madsen (2000) reported a generally better performance of submerged species like E. canadensis in HC compared to LC environments, even though the species are known for their HCO À 3 usage.…”
Section: Discussionmentioning
confidence: 99%