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Estuarine gradient

Mannino, A., and Harvey, H. R. (2000). Biochemical composition of particles and dissolved organic matter along an estuarine gradient Sources and implications for DOM reactivity. Limnol. Oceanogr. 45, 775-788. [Pg.446]

Boynton, W.R., and Kemp, W.M. (1985) Nutrient regeneration and oxygen consumption by sediments along an estuarine gradient. Mar. Ecol. Prog. Ser. 23, 45-55. [Pg.552]

O Donohue, M.J.H., and Dennison, W.C. (1997) Phytoplankton productivity response to nutrient concentrations, light availability, and temperature along an Australian estuarine gradient. Estuaries 20, 521-533. [Pg.639]

Horrigan, S. G., Montoya, J. P., Nevins, J. L., and McCarthy, J. J. (1990). Natural isotopic composition of dissolved inorganic nitrogen in the Chesapeake Bay. Estuar. Coast. Shelf Sci. 30, 393—410. Horrocks, J. L., Stewart, G. R., and Dennison, W. C. (1995). Tissue nutrient content of Gracilaria spp. (Rhodophyta) and water quality along an estuarine gradient. Mar. Freshw. Res. 46, 975—983. Howarth, R. W. (1988). Nutrient limitation of net primary production in marine ecosystems. Annu. Rev. Ecol. Syst. 19, 89-110. [Pg.941]

Hewson, L, and Puhrman, J. A. (2004). Richness and diversity of bacterioplankton species along an estuarine gradient in Moreton Bay, Australia. Appl. Environ. Microbiol. 70, 3425—3433. [Pg.1335]

Estuarine gradients Figures.pdf is a visualization of the data from Estuarine gra-dients Tables.pdf. The data are arranged to short transects stretching from the nearshore (freshwater influenced) via the offshore to the open sea stations. Also confidence intervals are given. The figures are taken from Wasmund et al. (2001). [Pg.661]

Primary production.pdf is a table of phytoplankton primary production data from the different sea areas, compiled from the literature in order to estimate a total primary production value for the Baltic Sea. The mean value of 150gC/(m year) is compared with earlier estimates inTable 15.1, which demonstrates the eutrophication during the past 2 decades. Special attention was paid to the eutrophicated coastal waters, as exemplified already in the files Estuarine gradients Tables.pdf and Estuarine gradients Figures. pdf. This is a modified table from Wasmund et al. (2001). [Pg.661]

Lauv, B., Rozhkova, M. (2007). Deripaska Territory. Vedomosti, 746(1920), 08.08.2(X)7. Lehtoranta, J., Heiskanen, A.-S., Pitkanen, H. (2(X)4). Particulate N and P characterizing the fate of nutrients along the estuarine gradient of the River Neva (Baltic Sea). Estuarine, Coastal and Shelf Science, 61.275-287. [Pg.952]


See other pages where Estuarine gradient is mentioned: [Pg.198]    [Pg.251]    [Pg.264]    [Pg.629]    [Pg.658]    [Pg.235]    [Pg.835]    [Pg.448]    [Pg.448]    [Pg.452]    [Pg.453]    [Pg.453]    [Pg.660]    [Pg.660]    [Pg.661]    [Pg.675]    [Pg.295]   
See also in sourсe #XX -- [ Pg.448 , Pg.453 ]




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