Calcification rate and the effect of temperature in a zooxanthellate and an azooxanthellate scleractinian reef coral

By Alan T. Marshall, Peta L. Clode. Coral reefs, 2004

215 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Nature and Landscape Conservation

View Paper: https://www.semanticscholar.org/paper/79ba53c5668d059c1ec4405c480a56524aad9f46

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Citations in the corpus

Effects of temperature, light and heterotrophy on the growth rate and budding of the temperate coral Cladocora caespitosa (2008, background): “Enzyme activity is maximal at the optimal temperature of the organism and decreases at high ( Marshall and Clode 2004; Al-Horani 2005) and low temperatures (Jacques et al. 1983).”
Possible effects of ocean acidification on coral reef biogeochemistry: topics for research (2008, background): “…other parameters Hermatypic coral calcification is a strong function of light (Gladfelter 1984, Allemand et al. 2004), shows temperature optima (Marshall & Clode 2004), and is affected by nutrients (Tanaka et al. 2007) and particulate feeding (Houlbrèque et al. 2003), yet there are no studies…”
ENVIRONMENTAL AND BIOLOGICAL CONTROLS ON THE INITIATION AND GROWTH OF A MIDDLE TRIASSIC (ANISIAN) REEF COMPLEX ON THE GREAT BANK OF GUIZHOU, GUIZHOU PROVINCE, CHINA (2006, background): “A detrimental effect of high temperature—independent of PCO2—is suggested by experiments and field observations (e.g., Reynaud et al., 2003; Carricart-Ganivet, 2004; Marshall and Clode, 2004).”
Decline in skeletal growth of the coral Porites lutea from the Andaman Sea, South Thailand between 1984 and 2005 (2009, result): “This result is consistent with other experimental studies, where the optimum temperature for calcification was *27 C (Clausen and Roth 1975; Highsmith 1979; Marshall and Clode 2004; Al-Horani 2005).”
Species-specific physiological response by the cold-water corals Lophelia pertusa and Madrepora oculata to variations within their natural temperature range (2014, background): “A positive correlation of ambient temperature and skeletal growth is indeed well-established for various tropical symbiotic scleractinians (Crossland, 1984; Lough and Barnes, 2000; Marshall and Clode, 2004), as well as for non-symbiotic and symbiotic temperate coral taxa (Jacques et al.”
Coral calcification from skeletal records revisited (2008, background): “…(Kleypas et al. 1999), and the third possibility is a non-linear response of coral calcification rates to rising water temperatures with calcification reaching a plateau and then declining at higher temperatures (Jokiel & Coles 1977, Marshall & Clode 2004, Kleypas et al. 2005, Cooper et al. 2008).”
Metabolic tolerance of the cold-water coral Lophelia pertusa (Scleractinia) to temperature and dissolved oxygen change (2007, background): “Growth rates of tropical and temperate corals increase with temperature within their natural temperature range, but will decline with further increases (Coles and Jokiel, 1978; Marshall and Clode, 2004; Edmunds, 2005; Rodolfo-Metalpa et al., 2006), but to date no studies have investigated this for L”
Calcification and organic production on a Hawaiian coral reef (2011, unknown): “However, light data were not available for all deployments and these trends do not agree with many studies showing that NEC is positively correlated with temperature and light (Barnes, 1982; Langdon and Atkinson, 2005; Marshall and Clode, 2004; Marubini et al., 2001).”