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Celtic Sea

Poremba, K., and H.-G. Hoppe. 1995. Spatial variation of benthic microbial production and hydrolytic enzymatic activity down the continental slope of the Celtic Sea. Marine Ecology Progress Series 118 237-245. [Pg.341]

Beaugrand G, Ibanez F, Reid PC (2000) Spatial, seasonal and long-term fluctuations of plankton in relation to hydrodynamic features in the English Channel, Celtic Sea and Bay of Biscay. Mar Ecol Progr Ser 200 93-102... [Pg.58]

Celtic Sea Shelf Edge American Shelf, Belgium... [Pg.315]

Rees, A. P., Joint, I., and Donald, K. M. (1999b). Early spring bloom phytoplankton-nutrient dynamics at the Celtic Sea Shelf Break. Deep Sea Res. 146, 483—510. [Pg.379]

Zubkov, M. V., Fuchs, B. M., Burkill, P. H., and Amann, R. (2001). Comparison of cellular and biomass specific activities of dominant bacterioplankton groups in stratified waters of the Celtic Sea. Appl. Environ. Microbiol. 61, 5210—5218. [Pg.384]

Williams, R., and Poulet, S. A. (1986). Relationship between the zooplankton, phytoplankton, particulate matter and dissolved free amino acids in the Celtic Sea. I. Unstratified water conditions. Mar. Biol 90, 279-284. [Pg.1196]

Figure 2b. Computer-plotted undulation profile (2.5-68 m) for a UOR Mark 2 tow at 5.5 m/s with 200-m, 6-mm outside diameter (OD) cable outboard of 200-m, 8-mm OD cable (about 300 m of cable in water). Taken from F.R.V. Cirolana, Celtic Sea, May 1981. Figure 2b. Computer-plotted undulation profile (2.5-68 m) for a UOR Mark 2 tow at 5.5 m/s with 200-m, 6-mm outside diameter (OD) cable outboard of 200-m, 8-mm OD cable (about 300 m of cable in water). Taken from F.R.V. Cirolana, Celtic Sea, May 1981.
Figure 7. Vertical sections of temperature (0.2 °C intervals) and chlorophyll (1.0-mg/m intervals) and abundance of Stage 1 mackerel eggs (number per square meter) from UOR tows along two transects in the Celtic Sea in May 1981 (F.R.V. Cirolana). The inset shows the cruise track. Figure 7. Vertical sections of temperature (0.2 °C intervals) and chlorophyll (1.0-mg/m intervals) and abundance of Stage 1 mackerel eggs (number per square meter) from UOR tows along two transects in the Celtic Sea in May 1981 (F.R.V. Cirolana). The inset shows the cruise track.
Figure 8. Vertical sections of temperature (0.5 °C intervals) (a) and chlorophyll concentration (1-, 2.5-, and 5-mg/m contours, shaded > 2.5 mg/m ) (b) for a UOR Mark 2 tow in the Celtic Sea, July 7, 1982, RRS Frederick Russell. The inset shows the cruise area. Figure 8. Vertical sections of temperature (0.5 °C intervals) (a) and chlorophyll concentration (1-, 2.5-, and 5-mg/m contours, shaded > 2.5 mg/m ) (b) for a UOR Mark 2 tow in the Celtic Sea, July 7, 1982, RRS Frederick Russell. The inset shows the cruise area.
From this series of measurements, two conclusions can be drawn. First, the vertical distribution of temperature and chlorophyll is homogeneous spatially throughout this area of the Celtic Sea second, a close relationship exists between the vertical structure of temperature and chlorophyll for all the seasons, although the exact relationship may differ for the... [Pg.328]

Figure 9a, Microcomputer-generated vertical profiles from near surface to 54 m (in 3-m depth averages) of temperature (°C) (left) and chlorophyll concentration (mg/m ) (right) from a single undulation of a UOR tow in the Celtic Sea. Key a, June 12,1982 b, July 7,1982 and c, September 22,1982, Cruise area is shown in the inset of Figure 8,... Figure 9a, Microcomputer-generated vertical profiles from near surface to 54 m (in 3-m depth averages) of temperature (°C) (left) and chlorophyll concentration (mg/m ) (right) from a single undulation of a UOR tow in the Celtic Sea. Key a, June 12,1982 b, July 7,1982 and c, September 22,1982, Cruise area is shown in the inset of Figure 8,...
A simple, quantitative, steady-state diffusion model (36) demonstrates the importance of physical processes in shaping the vertical distribution of phytoplankton. This model uses values of the eddy diffusion coefficient K from the theoretical model of James (35), which reproduces accurately the annual cycle of vertical temperature structure for this area of the Celtic Sea. The submodels for photosynthetic production, light, and grazing can be varied to any of the established models nutrient luxury or nutrient limitation of growth can be included. The model reproduces the main features of the UOR observations in the Celtic Sea and English Channel. [Pg.330]

Table salt, the most commonly used type of salt, is acid-forming. I recommend that you switch to Celtic sea salt or Himalayan salt, which are alkalizing to the body. Celtic sea salt and similar unrefined sea salts look gray and a bit moist. Himalayan salt has a naturally occurring orange color. Both types of salt contain a healthier, alkalizing form of sodium and are packed with many other minerals, including potassium and calcium. [Pg.79]

Vi tsp Celtic sea salt or Himalayan salt Pinch cayenne pepper... [Pg.151]

Vi tsp Celtic sea salt or Himalayan salt Pinch cayenne pepper Small handful fresh cilantro, finely chopped 2 green onions, finely chopped... [Pg.155]

Herbs and Spices Celtic sea salt Himalayan salt Fresh and dried herbs basil, cilantro, oregano, parsley, rosemary, sage, thyme, etc. Cayenne pepper Curry powder Nutmeg Table salt Vanilla ... [Pg.177]


See other pages where Celtic Sea is mentioned: [Pg.77]    [Pg.91]    [Pg.93]    [Pg.326]    [Pg.327]    [Pg.80]    [Pg.97]    [Pg.140]    [Pg.140]    [Pg.146]    [Pg.147]    [Pg.148]    [Pg.149]    [Pg.149]    [Pg.150]    [Pg.152]    [Pg.153]    [Pg.155]    [Pg.159]    [Pg.160]    [Pg.163]    [Pg.164]    [Pg.165]    [Pg.165]    [Pg.166]    [Pg.167]    [Pg.172]   


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