General Palaeontology (Palaeobiochemistry) Biomineralisation in reef-building corals: from molecular mechanisms to environmental control

By D. Allemand, C. Ferrier‐Pagès, P. Furla, F. Houlbrèque, Sandrine Puverel, S. Reynaud, É. Tambutté, S. Tambutté, D. Zoccola. 2004

384 citations recorded by the source corpus.

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Citations in the corpus

Interactive effects of ocean acidification and temperature on two scleractinian corals from Moorea, French Polynesia (2012, background): “…has revolved around the unresolved relationships among light, the Symbiodinium symbionts, photosynthesis, and the capacity to calcify rapidly (Allemand et al., 2004, 2011), as well as which DIC spe- cies (i.e., HCO3 vs. CO3 2 ) is favored for calcification (Schneider & Erez, 2006; Jury et…”
Biological mechanisms supporting adaptation to ocean acidification in coastal ecosystems (2015, unknown): “Scleractinian corals do not precipitate their aragonite calcium carbonate skeleton directly from seawater, but from an extracellular calcifying medium, located at the interface between the coral polyp’s basal cell layer and the underlying skeleton (e.g. Allemand et al., 2004).”
Observations of the tissue-skeleton interface in the scleractinian coral Stylophora pistillata (2007, background): “In S. pistillata, calicoblastic cells have been shown to be the site of organic matrix synthesis (Puverel et al. 2004) and the inhibition of organic matrix synthesis leads to the inhibition of calciWcation ( Allemand et al. 1998 ).”
The impact of seawater saturation state and bicarbonate ion concentration on calcification by new recruits of two Atlantic corals (2011, background): “, [CO3 ]) of the calcifying fluid at the site of calcification by converting aqueous CO2 and bicarbonate to carbonate ions (e.g., Cohen and McConnaughey 2003; Allemand et al. 2004), then why is the initial [CO3 ] of the external seawater so important in influencing the calcification outcome? The ans”
Calcification in bleached and unbleached Montastraea faveolata: evaluating the role of oxygen and glycerol (2010, background): “In addition, organic carbon and metabolic energy are required and can be supplied by the symbiotic algae (reviewed in Allemand et al. 2004).”
Short-term metabolic and growth responses of the cold-water coral lophelia pertusa to ocean acidification (2013, background): “The process of increasing pH at calcification sites within corals is driven by CaATPase, which pumps Ca ions into the sub-calicoblastic space in exchange for H ions (Allemand et al., 2004; Cohen and McConnaughey, 2003; Mass et al., 2012).”
Possible effects of ocean acidification on coral reef biogeochemistry: topics for research (2008, background): “In hermatypic corals, the supply of Ca2+, as well as HCO3– derived from host tissue respiration (via a carbonic anhydrase), are biologically controlled (Allemand et al. 2004).”
Vital effects in coral skeletal composition display strict three‐dimensional control (2006, background): “Knowledge of cellular pathways and molecular mechanisms involved in transport and production of the skeletal constituents, including organic molecules, is sparse [Allemand et al., 2004].”
Environmental controls on coccolithophore calcification (2012, background): “Despite the perceived problems with large Ca2+ fluxes through the cytosol, Allemand et al. (2004) suggested that diffusible Ca-binding proteins are involved in the calicoblastic layer outside the aboral endoderm adjacent to the aragonitic skeleton of scleractinian corals.”
Nutritional status and metabolism of the coral Stylophora subseriata along a eutrophication gradient in Spermonde Archipelago (Indonesia) (2011, background): “…respect to Pg. Reasons for decreased GL under high nutrient levels are found in a decoupling of symbiont and host (Dubinsky et al. 1990; Ferrier-Pagès et al. 2000; Allemand et al. 2004) or a direct inhibition of carbonate crystallization by inorganic nutrients (Simkiss 1964; Gattuso et al. 1999).”
Coral calcification responds to seawater acidification: a working hypothesis towards a physiological mechanism (2008, background): “The experimental inhibition of any of these processes has been shown to inhibit calcification (Allemand et al. 2004).”
The reef coral two compartment proton flux model: A new approach relating tissue-level physiological processes to gross corallum morphology (2011, background): “The contemporary four cell layer model of calcification (Allemand et al., 2004; Furla et al, 2000a) is shown in Fig.”
Cell Biology of Cnidarian-Dinoflagellate Symbiosis (2012, background): “For more extensive information on calcification at the organismal or ecosystem level, the reader is referred to recent reviews (5, 6, 55, 129, 357).”