Observations of the tissue-skeleton interface in the scleractinian coral Stylophora pistillata
By É. Tambutté, Denis Allemand, D. Zoccola, A. Meibom, Séverine Lotto, N. Caminiti, S. Tambutté. Coral reefs, 2007
140 citations recorded by the source corpus.
Subfields: Biomaterials, Ecology, Ecology, Evolution, Behavior and Systematics
View Paper: https://www.semanticscholar.org/paper/5b2981dce46de8db3250a2b37b40b7b2ef47aa01
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In Biomaterials
In Ecology
In Ecology, Evolution, Behavior and Systematics
Citations in the corpus
- The reef coral two compartment proton flux model: A new approach relating tissue-level physiological processes to gross corallum morphology (2011, background): “Tambutté et al. (2007) conducted a detailed histological study of reef corals and concluded that tissues which calcify at the highest rates, or which initiate calcification, do not possess zooxanthellae.”
- Cell Biology of Cnidarian-Dinoflagellate Symbiosis (2012, background): “, not in the immediate vicinity of the calicodermis, where symbionts are absent [355]) and then transferred to the calicoblastic cells via the aboral gastrodermal cells.”
- Possible effects of ocean acidification on coral reef biogeochemistry: topics for research (2008, background): “For example, Tambutté et al. (2007) report that some tissues calcifying at the highest rates in Stylophora pistillata consist only of ectodermal cell-layers separated by mesoglea.”
- A physicochemical framework for interpreting the biological calcification response to CO 2 -induced ocean acidification (2011, methodology): “This model is supported by direct observations of the tissue-skeleton interface (e.g., Clode and Marshall, 2002; Cuif and Dauphin, 2005; Tambutté et al., 2007), by the existence of desmocytes in the calicoblastic epithelium of corals (e.”
- Hot‐spring Systems Geobiology: abiotic and biotic influences on travertine formation at Mammoth Hot Springs, Yellowstone National Park, USA (2011, methodology): “seasonal changes in sea surface temperature and, thus, fossil banding is commonly used for palaeothermometry, palaeoclimatology and palaeoecology reconstructions (Moses et al., 2006; Lough & Barnes, 1997; Barnes & Lough, 1993; Tambutte et al., 2007; Helman et al., 2008; Vago, 2008).”