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Organic matter production

Trace metal dry weight organisms matter production g/ha/yr... [Pg.133]

These reactions require energy to proceed. Sunlight is the energy source for some, but not all, of these carbon fixation pathways. The sunlight-fueled fixation of carbon, i.e., photosynthesis, is responsible for most of the organic matter production on Earth. [Pg.188]

Seasonal Fluctuations in Organic Matter Production and Export... [Pg.621]

B. Pathways for Algal Dissolved Organic Matter Production... [Pg.6]

Hama, T., and N. Handa. 1987. Pattern of organic matter production by natural phytoplankton population in a eutrophic lake. 2. Extracellular products. Archiv fur Hydrobiologie 109 227-243. [Pg.21]

Kennicutt II, M.C., and Comet, P.A. (1992) research of sediment hydrocarbon sources multiparameter approaches. In Organic Matter Productivity, Accumulation, and Preservation in Recent and Ancient Sediments (Whelan, J.K., and Farrington, I.K., eds.), pp. 308-338, Columbia University Press, New York. [Pg.609]

Production of roots on top of the mineral soil has been explained as a consequence of the low nutrient availability in Amazon forests (Herrera et al. 1978, Cuevas and Medina 1983, Medina and Cuevas 1989). Vertical root distribution results from differential nutrient availability in the soil profile (Berish 1982, Berish and Ewel 1988). Shallow rooted systems may be a result of litter and soil organic matter production and decomposition rates in systems where nutrient input from litter exceeds that of nutrient release by soil weathering, as is the case of Ca, Mg, and P in terra firme forests (Medina and Cuevas 1989). In the Middle Caqueta region of Colombia, for example, Ca and Mg concentrations in the L and F layers are between 15 and 20 times higher than in the mineral soil (Duivenvoorden and Lips 1995). [Pg.61]

Paerl, H. W., Bebout, B. M., Joye, S. B., and Marais, D. J. (1993). Microscale characterization of dissolved organic matter production and uptake in marine microbial mat communities. Limnol. Oceanogr. 38, 1150-1191. [Pg.377]

Arthur M. A., Schlanger S. O., and Jenkyns H. C. (1987) The Cenomanian-Turonian Oceanic Anoxic Event II. In Paleoceanographic Controls on Organic-matter Production and Preservation, Geological Society of London Special Publication 26 (eds. J. Brooks and A. J. Fleet), pp. 401-420. [Pg.1819]

MICROBIAL ORGANIC MATTER PRODUCTION AND PROCESSING NEW INSIGHTS... [Pg.2996]

Microbial Organic Matter Production and Processing New Insights... [Pg.3022]

Arthur M. A. and Dean W. E. (1998) Organic-matter production and preservation and evolution of anoxia in the Holocene Black Sea. Paleoceanography 13, 395-411. [Pg.3613]

Paleoceaonographic controls on organic matter production and preservation. Geol. Soc. London Spec. Publ. 26, 401-420. [Pg.3827]


See other pages where Organic matter production is mentioned: [Pg.39]    [Pg.392]    [Pg.407]    [Pg.437]    [Pg.469]    [Pg.48]    [Pg.207]    [Pg.208]    [Pg.210]    [Pg.212]    [Pg.214]    [Pg.216]    [Pg.218]    [Pg.256]    [Pg.652]    [Pg.712]    [Pg.760]    [Pg.39]    [Pg.383]    [Pg.392]    [Pg.462]    [Pg.176]    [Pg.568]    [Pg.23]    [Pg.331]    [Pg.711]    [Pg.727]    [Pg.741]    [Pg.747]    [Pg.841]    [Pg.1446]    [Pg.3021]   


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