Photosynthesis and calcification in the calcifying algae Halimeda discoidea studied with microsensors
By D. de Beer, A. Larkum. 2001
154 citations recorded by the source corpus.
Subfields: Atomic and Molecular Physics, and Optics, Cellular and Molecular Neuroscience, Ecology, Evolution, Behavior and Systematics
View Paper: https://www.semanticscholar.org/paper/c169e0c53964811a148c5601d1bd7063835d1ad3
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In Atomic and Molecular Physics, and Optics
In Cellular and Molecular Neuroscience
In Ecology, Evolution, Behavior and Systematics
Citations in the corpus
- Response of photosynthesis to ocean acidification (2015, background): “…coccolithophores growing at elevated CO2 have a tendency to produce degraded or aberrant coccoliths (Figure 2E; Riebesell et al., 2000; Langer et al., 2006; Feng et al., 2008; Iglesias-Rodriguez et al., 2008; De Bodt et al., 2010; Müller et al., 2010, 2012; Ramos et al., 2010; Langer, 2011).”
- Ocean acidification effects on calcifying macroalgae (2014, background): “Some Halimeda spp. are able to uptake HCO3− directly (Borowitzka & Larkum 1976b) and do not rely on external CA (de Beer & Larkum 2001).”
- Concentration boundary layers around complex assemblages of macroalgae: Implications for the effects of ocean acidification on understory coralline algae (2013, background): “…surface of corals (De Beer et al. 2000), phytoplankton (Rink et al. 1998), benthic diatoms (Roberts et al. 2007), and other macroalgae (De Beer and Larkum 2001; Larkum et al. 2003), with pH rising to between 8.2–9.6 in the light due to photosynthesis and decreasing to 8.1–7.0 in darkness due to…”
- Combined effects of ocean acidification and solar UV radiation on photosynthesis, growth, pigmentation and calcification of the coralline alga Corallina sessilis (Rhodophyta) (2009, background): “Calcification of coralline algae requires energy input from photosynthesis (Borowitzka & Larkum, 1976) and depends on pH (de Beer & Larkum, 2001).”
- Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels (2012, background): “The mechanism of calciWcation in Halimeda spp. has been heavily studied (Borowitzka and Larkum 1976a, b, c; De Beer and Larkum 2001) and is reported to occur as the deposition of aragonite crystals in the intercellular spaces of the alga.”
- Climate change and ocean acidification effects on seagrasses and marine macroalgae (2013, methodology): “For example, a light-induced putative H+ pump at the cell surface of Halimeda is triggered at low light (~12 lmol m 2 s 1; de Beer & Larkum, 2001), perhaps as a mechanism to prime photosynthesis by lowering pH and elevating CO2 availability through the dehydration of HCO3 , part of a proton…”
- Species-specific consequences of ocean acidification for the calcareous tropical green algae Halimeda (2011, background): “However, Halimeda regulate carbonate chemistry in the semi-isolated inter-utricle space by passive diffusion of ions across the siphons (De Beer & Larkum 2001, Lee & Carpenter 2001).”
- Skeletal mineralogy in a high-CO2 world (2011, background): “Calcifying bryopsidalean algae, such as Halimeda (Borowitzka and Larkum, 1976; De Beer and Larkum,2001; Ries, 2009), are thought toprecipitate their aragonite needles from a discrete calcifying fluid as well, although without the control afforded by organic crystal nucleation templates.”