2003
DOI: 10.1016/s0304-3770(03)00035-4
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Carbon acquisition mechanisms in Chara tomentosa

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Cited by 39 publications
(27 citation statements)
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“…Because of the long incubation time necessary to test the effect of this substance, pH-drift experiments are among the few experimental methods suitable (Choo et al 2002;Ray et al 2003). The major inhibition suggests that a P-type H + -ATPase (proton pump) was involved in carbon uptake in desmids.…”
Section: Discussionmentioning
confidence: 99%
“…Because of the long incubation time necessary to test the effect of this substance, pH-drift experiments are among the few experimental methods suitable (Choo et al 2002;Ray et al 2003). The major inhibition suggests that a P-type H + -ATPase (proton pump) was involved in carbon uptake in desmids.…”
Section: Discussionmentioning
confidence: 99%
“…For calcareous Chara thaii, plant calcification competed for DIC with photosynthesis in mild-alkaline water (e.g. McConnaughey and Falk, 1991;Ray et al, 2003). So the increase of DIC utilization by photosynthesis would result in the decrease of available DIC for calcification.…”
Section: The Single Effects Of Two Factors On Calcification Of Plantsmentioning
confidence: 99%
“…McConnaughey and Whelan, 1997;Siong, 2006;Siong and Asaeda, 2009b) and hyper-accumulator of heavy metals (McConnaughey, 1991;Siong and Asaeda, 2009a). In mildly alkaline water, DIC decreased by two means, either was taken up by the photosynthesis of the algae or became incorporated in the cell wall of Chara by calcification (Ray et al, 2003). However, lots of experiments studying bicarbonate utilization of Chara spp.…”
Section: Introductionmentioning
confidence: 99%
“…Thus, the C source utilized is species specific and appears to be inseparably related to the growth form of each species. Additional detailed field investigations of a range of species representing different growth forms and a range of conditions above, within and beneath a charophyte stand as well as laboratory testing the exact CO 2 acquisition for photosynthesis and membrane transport mechanisms (e.g., Ray et al, 2003;Beilby & Casanova, 2014), and respiration effects would explicitly verify our assumption. This is particularly important in the context of the aforementioned use of d 13 C values in palaeoecological studies as an indication of the source of matter in sediment deposits.…”
Section: Discussionmentioning
confidence: 69%