Sea surface temperature and the growth of the West Atlantic reef-building coral Montastraea annularis

By J. Carricart-Ganivet. 2004

174 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/8e7f55da1585126b061a5e1a36d69f210f43ae50

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In Ecology

In Global and Planetary Change

In Nature and Landscape Conservation

Citations in the corpus

Species-specific physiological response by the cold-water corals Lophelia pertusa and Madrepora oculata to variations within their natural temperature range (2014, background): “Thermal acclimation of key physiological processes, such as respiration and calcification, is well established for a number of temperate and tropical scleractinian coral species (Jacques et al., 1983; Lough and Barnes, 1997, 2000; Howe and Marshall, 2001; Carricart-Ganivet, 2004; Nakamura et al., 20”
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).”
Densitometry from digitized images of X-radiographs: Methodology for measurement of coral skeletal density (2007, background): “It is important to remove such an artificial trend because the strong link between calcification rate and seawater temperature (Lough and Barnes, 2000; Carricart-Ganivet, 2004) provides, perhaps, the most important environmental parameter that is presently recovered from coral skeletal density bandi”
Decline in skeletal growth of the coral Porites lutea from the Andaman Sea, South Thailand between 1984 and 2005 (2009, background): “Positive relationships between temperature and calcification were also noted in studies that examined coral growth rates over latitudinal scales (Lough and Barnes 2000; Carricart-Ganivet 2004).”
Summary for Policymakers (2022, unknown): “More importantly, perhaps, a greater amount of symbiont-produced photosynthates may provide more fuel for the active transport processes involved in coral calcification (Chalker and Taylor, 1975), as well as more raw materials for the synthesis of the coral organic matrix (Wainwright, 1963; Muscatin”