Trophic structure of a cold-water coral mound community (Rockall Bank, NE Atlantic) in relation to the near-bottom particle supply and current regime

By G. Duineveld, M. Lavaleye, M. Bergman, H. Stigter, F. Mienis. 2007

182 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/01c59b2980d3c4637cb2802ef2d445dfab5e892c

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Citations in the corpus

Mingulay reef complex: an interdisciplinary study of cold-water coral habitat, hydrography and biodiversity (2009, background): “Such internal waves have now been recorded transporting fluorescent material to coral carbonate mounds in the southeast Rockall Trough (Duineveld et al. 2007, Mienis et al. 2007).”
The effect of flow speed and food size on the capture efficiency and feeding behaviour of the cold-water coral Lophelia pertusa (2016, background): “During most periods, near bottom currents recorded in CWC sites are lower than 15 cm s− 1 (White and Dorschel, 2010; Mienis et al., 2012; Khripounoff et al., 2014) with average flow speeds between 5 and 15 cm s− 1 (Duineveld et al., 2007; Mienis et al., 2007, 2009, 2012; Davies et al., 2010).”
Predicting global habitat suitability for stony corals on seamounts (2009, background): “A lack of evidence for the influence of salinity on habitat suitability for deep-sea stony corals may again reflect the inability of our analyses to capture the small scale at which such processes operate, but may also reflect the fact that other oceanographic processes may be important in driving f”
Acclimation to ocean acidification during long‐term CO2 exposure in the cold‐water coral Lophelia pertusa (2012, background): “Very little is known about the nutrition of L. pertusa in their natural habitat, but d15N signatures (Duineveld et al., 2004, 2007) and fatty acid composition in L. pertusa tissues (Dodds et al., 2009) indicate that it predominantely relies on food supplied directly from surface production.”
Opportunistic feeding on various organic food sources by the cold-water coral Lophelia pertusa (2013, background): “, 2011), while POM availability can vary spatially and temporally (Duineveld et al., 2007).”
Stable C and N isotopic composition of cold-water corals from the Newfoundland and Labrador continental slope: Examination of trophic, depth and spatial effects (2008, background): “Fatty acid and stable nitrogen isotope signatures suggest cold-water scleractinia may also feed on detrital particulate organic matter (POM; Duineveld et al., 2004, 2007; Kiriakoulakis et al., 2005).”
The cold‐water coral community as hotspot of carbon cycling on continental margins: A food‐web analysis from Rockall Bank (northeast Atlantic) (2009, background): “Kiriakoulakis et al. (2005) found a comparatively high proportion of monounsaturated fatty acids (MUFAs) in the living tissue of CWCs, suggesting that zooplankton contribute to the diet of CWCs. Duineveld et al. (2004) concluded from d13C and d15N data that an algal–animal mix was the most likely di”