Cold-water coral growth in relation to the hydrography of the Celtic and Nordic European continental margin

By W. Dullo, S. Flögel, A. Rüggeberg. 2008

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Cold-water corals in a changing ocean (2014, background): “65 kg m (3)) perhaps because larvae disperse laterally along this horizon [9].”
Species-specific physiological response by the cold-water corals Lophelia pertusa and Madrepora oculata to variations within their natural temperature range (2014, background): “Occurrence and local abundance of CWC appear dependent on principal environmental factors, such as availability of settling substrate, current velocity, food supply, aragonite saturation state, but also gradients of seawater density, as a function of seawater temperature and salinity (Guinotte et al”
When the species is also a habitat: Comparing the predictively modelled distributions of Lophelia pertusa and the reef habitat it forms (2011, background): “Reef habitat forms in areas of enhanced turbidity, within a narrow density envelope, with high current velocities that prevent local sedimentation but provide enhanced encounter-rates with food particles (Thiem et al., 2006; Mienis et al., 2007; Dullo et al., 2008).”