Spatial and temporal pattern in seagrass community composition and productivity in south Florida
By J. Fourqurean, A. Willsie, C. Rose, L. Rutten. 2001
204 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/667160a140eaf2340eb76c25e8e58c9b1e265293
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In Ecology
- O. Pedersen
- J. Fourqurean
- L. Rutten
- J. Borum
- D. Krause‐Jensen
- T. M. Greve
- Gérard Pergent
- Carlos M. Duarte
In Oceanography
- O. Pedersen
- J. Fourqurean
- L. Rutten
- J. Borum
- D. Krause‐Jensen
- T. M. Greve
- Gérard Pergent
- Carlos M. Duarte
Citations in the corpus
- The potential role of plant oxygen and sulphide dynamics in die‐off events of the tropical seagrass, Thalassia testudinum (2005, background): “J. C. ZIEMAN‡, J. W. FOURQUREAN§ and C. J. MADDEN¶ Freshwater Biological Laboratory, University of Copenhagen, Helsingørsgade 51, DK-3400 Hillerød, Denmark, † Department of Marine Ecology, National Environmental Research Institute, Vejlsøvej 25, DK-8600 Silkeborg, Denmark, ‡ Department of Environmen”
- The Impact of Hurricane Georges on Soft-Bottom, Back Reef Communitites: Site- and Species-Specific Effects in South Florida Seagrass Beds (2004, methodology): “1, see Fourqurean et al., 2001; Fourqurean and Rutten, 2003 for a description of the monitoring program).”
- Seagrass Conservation Biology: An Interdisciplinary Science for Protection of the Seagrass Biome (2007, background): “, 2000) and in the United States in the Florida Keys National Marine Sanctuary (Fourqurean et al., 2001).”
- Interspecific variation in the elemental and stable isotope content of seagrasses in South Florida (2009, background): “Within each year, a network of 30 permanent monitoring stations was sampled 4 3 times (see Fourqurean et al. 2001 for further description).”
- Dynamics of Seagrass Stability and Change (2007, background): “24◦ N) abundance and growth of Thalassia testudinum in summer and winter, respectively, are 30% higher than and 30% lower than the mean even at this relatively low latitude, but the seasonal variability decreases toward the equator and increases toward more northern latitudes (Fourqurean et al., 200”