2013
DOI: 10.1016/j.aquabot.2013.04.002
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Calcium carbonate incrustation and phosphorus fractions in five charophyte species

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Cited by 51 publications
(43 citation statements)
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“…However, no statistically significant differences were found between the apical portions (new tissue) and the basal portions (old tissue) of the same individual. Clearly, coprecipitation may have contributed to maintain low soluble P concentrations, always < 0.005 mg l -1 , in the water spring (Kufel et al, 2013). The clear negative influence exerted by C. hispida on microalgal densities can also be related to infochemical interactions (Hilt and Gross, 2008).…”
Section: Resultsmentioning
confidence: 99%
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“…However, no statistically significant differences were found between the apical portions (new tissue) and the basal portions (old tissue) of the same individual. Clearly, coprecipitation may have contributed to maintain low soluble P concentrations, always < 0.005 mg l -1 , in the water spring (Kufel et al, 2013). The clear negative influence exerted by C. hispida on microalgal densities can also be related to infochemical interactions (Hilt and Gross, 2008).…”
Section: Resultsmentioning
confidence: 99%
“…Their N uptake is very efficient, and they remove this nutrient from the water column (Rodrigo and Alonso-Guillén, 2008). Charophytes are also known to affect phosphorus cycling by direct uptake and by deposition of calcium carbonate in the form of encrustations on the tissues, accompanied by coprecipitation of inorganic P (Pelechaty et al, 2013;Puckaz et al, 2013;Kufel et al, 2013). Charophytes from this water spring also precipitated large amounts of calcium carbonate, with an annual mean of 30% (± 15% SD) of the DW for C. hispida and 21± 9% for N. hyalina.…”
Section: Resultsmentioning
confidence: 99%
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“…When this calcification occurs, phosphorus from the water column is co-precipitated with the calcium, resulting in a reduction of its concentration in the water, which in turn decreases the phosphorus available for phytoplankton, thus maintaining lake transparency (Hilt et al, 2006;Kufel et al, 2013). Calcium and bonded phosphorus cannot be used by phytoplankton, and the bonded phosphorus deposited in the sediment tends to remain there, thanks to its shape, which makes its subsequent diffusion less likely (Ishii et al, 2008;Yokoyama et al, 2008).…”
Section: Introductionmentioning
confidence: 99%
“…In natural water, Ca is liable to combine with inorganic carbon and phosphorus (P), triggering co-precipitate of CaCO 3 with phosphorus that results in the P transport of water column. Calcium bound P is insensitive to redox potential and once deposited in bottom sediments, it may get long-term retention (Kufel et al 2013). Sediment is an important storage sink for metals (Mishra et al 2008;Nemati et al 2011).…”
Section: Introductionmentioning
confidence: 99%