Influence of coral mucus on nutrient fluxes in carbonate sands

By C. Wild, Holger Woyt, M. Huettel. 2005

165 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/af334d09fbc362ad7f12b5091c3789c8697dcadb

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

1. Michael Lesser
2. Mark E. Warner
3. M. Naumann
4. C. Wild
5. O. Hoegh‐Guldberg
6. A. Haas
7. A. Grottoli
8. V. Schoepf

In Global and Planetary Change

1. M. Naumann
2. Michael Lesser
3. Mark E. Warner
4. V. Schoepf
5. J. Bauer
6. Justin H. Baumann
7. Matthew D. Aschaffenburg
8. Stephen J. Levas

In Oceanography

1. Michael Lesser
2. Mark E. Warner
3. M. Naumann
4. A. Haas
5. C. Wild
6. O. Hoegh‐Guldberg
7. V. Schoepf
8. J. Bauer

Citations in the corpus

• Coral surface area quantification–evaluation of established techniques by comparison with computer tomography (2008, methodology): “In coral reef studies, the surface area of corals serves as an important reference parameter, for example, regarding the standardisation of metabolic processes such as photosynthesis, respiration and the release of coral-derived organic material to the environment (Wild et al. 2005).”
• Nitrogen fixation by symbiotic cyanobacteria provides a source of nitrogen for the scleractinian coral Montastraea cavernosa (2007, background): “…corals release large quantities of dissolved organic material containing high concentrations of both organic and inorganic sources of nitrogen (Wild et al. 2005), which has implications for the biogeochemical fluxes of nitrogen in carbonate sands and pore waters, and therefore nitrogen…”
• Organic matter release by Red Sea coral reef organisms-Potential effects on microbial activity and in situ O2 availability (2010, background): “…showed that scleractinian corals, through the release of both dissolved and particulate organic matter (DOM and POM), can affect biogeochemical cycles and establish fauna–microbe interactions in warm- (Wild et al. 2005a) and cold-water (Wild et al. 2008, Wild et al. 2009a) coral-reef ecosystems.”
• Can heterotrophic uptake of dissolved organic carbon and zooplankton mitigate carbon budget deficits in annually bleached corals? (2016, result): “4f, i), consistent with findings from most previous studies of healthy nonbleached coral DOC fluxes (Crossland 1987; Wild et al. 2004, 2005, 2008, 2010a, b; Tanaka et al. 2008, 2009; Haas et al. 2010; Naumann et al. 2010; Levas et al. 2015).”
• Organic matter release by dominant hermatypic corals of the Northern Red Sea (2010, methodology): “To allow comparisons with previous studies (Herndl and Velimirov 1986; Wild et al. 2005b) and to rule out the influence of water currents on organic matter release, beaker contents were not stirred during incubations.”