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Flora, distribution

As it leaves the still, distilled water is flee fixm microorganisms, and contamination occurs as a result of a fault in the cooling system, the storage vessel or the distribution system. The flora of contaminated distilled water is usually Gram-negative bacteria and since it is introduced after a sterilizahon process, it is often a pure culture. A level of organism up to 10 mH has been recorded. [Pg.344]

The liver plays a decisive role in the cholesterol metabolism. The liver accounts for 90% of the overall endogenic cholesterol and its esters the liver is also impli-cated in the biliary secretion of cholesterol and in the distribution of cholesterol among other organs, since the liver is responsible for the synthesis of apoproteins for pre-p-lipoproteins, a-lipoproteins, and P-lipoproteins which transport the secreted cholesterol in the blood. In part, cholesterol is decomposed by intestinal micro-flora however, its major part is reduced to coprostanol and cholestanol which, together with a small amount of nonconverted cholesterol, are excreted in the feces. [Pg.209]

There is also a segmental distribution of the types of bacteria. Strict anaerobic species are normally confined to the oral cavity and the colon, habitats they densely colonize and predominate [1-5] (fig. 1). Bacteria indigenous to the upper respiratory tract (URT flora) and anaerobic bacteria of oral origin are swallowed with saliva and recovered from the upper gut at densities below 105 CFU/ ml. Under physiological conditions, they are considered transitory rather than indigenous to the upper gut. Facultative anaerobic bacteria are usually confined to the distal small bowel and colon, but transient species entering the gut with nutrients are occasionally recovered from the healthy upper gut at low counts. [Pg.2]

Change in biodiversity Measures of impacts on flora and fauna, e.g. compatibility with native biomass, alteration of production and growth period and geographic distribution of populations and alterations in reproduction cycles of species... [Pg.117]

The absorption of vitamins K2, which are found mainly in cheese, curd cheese, and natto, is much higher and may be almost complete. Thus the nutritional importance of menaquinones is often underestimated. The vitamin K activity is related to the activation of specific proteins involved in blood clotting and bone metabolism. Clinical vitamin deficiency due to dietary inadequacy is rare or nonexistent in healthy adults, thanks to the widespread distribution of the vitamin K in foodstuffs and the microbiological flora of the gut, which synthesizes menaquinones. Only infants up to 6 months are at risk of bleeding due to a vitamin K deficiency. No data on negative effects of an overdose of vitamin K are found [417]. [Pg.613]

Differences in clinical effectiveness are partly due to differences in absorption, distribution and excretion of the individual drugs. In general tetracyclines are absorbed irregularly from the gastrointestinal tract and part of the dose remains in the gut and is excreted in the faeces. However this part is able to modify the intestinal flora. Absorption of the more lipophilic tetracyclines, doxycycline and minocycline is higher and can reach 90-100%. The absorption is located in the upper small intestine and is better in the absence of food. Absorption is impaired by chelation with divalent cations. In blood 40-80% of tetracyclines is protein bound. Minocycline reaches very high concentrations in tears and saliva. Tetracyclines are excreted unchanged, in both the urine by passive filtration and in the feces. Tetracyclines are concentrated in the bile via an active... [Pg.410]

Fossil floras provide one of the most useful sources for obtaining data that can be used to estimate paleoelevation. The distribution of modern forests is clearly delineated largely in accordance with climate, which varies with both altitude and latitude. The correlation of modern vegetation with mean temperature parameters provides the basis for comparing Cenozoic fossil floras with the thermal distribution of these modern forest types to infer paleotemperatures. Such information is a valuable source for inferring climate fluctuations through time, and in combination with thermodynamic properties of the atmosphere, it also can be used to estimate paleoelevation. [Pg.155]

Estimates of paleotemperature from fossil floras provide the primary data on which paleoelevation estimates are based. Two fundamentally different approaches have been used in paleobotany to acquire these data. The first is based on the climatic distribution of nearest living relatives (the NLR method, also sometimes referred to as the floristic method), and the second has its basis in the correlation of plant physiognomic characters with climate. [Pg.156]

Temperature parameters besides MAT, such as WMT and CMT, have been used to plot the distribution of modern vegetation types on various climagraphs, and these have also proven useful for determining the seasonality for fossil floras. Although MAT is the value that is most widely used for paleoaltimetry, WMT and CMT are often the ones that determine particular vegetation boundaries (Fig. 5 Wolfe 1979), and an understanding of the lapse rates for these seasonal temperatures is therefore also an important consideration in paleoelevation studies. For example, Meyer (1992) calculated WMT and CMT local lapse rates as well as... [Pg.162]

Figure 5. The distribution of forests in eastern Asia can be illustrated on a climagraph showing the relation of MAT, CMT, and WMT to vegetation boundaries. Diagram from Meyer (1992), based on Wolfe (1978). [Reprinted from Palaeogeography, Palaeoclimatology, Palaeoecology, v. 99, Meyer, H.W., Lapse rates and other variables applied to estimating paleoaltitudes from fossil floras, p. 71-99, 1992 Elsevier Science Publishers B.V., with permission from Elsevier.]... Figure 5. The distribution of forests in eastern Asia can be illustrated on a climagraph showing the relation of MAT, CMT, and WMT to vegetation boundaries. Diagram from Meyer (1992), based on Wolfe (1978). [Reprinted from Palaeogeography, Palaeoclimatology, Palaeoecology, v. 99, Meyer, H.W., Lapse rates and other variables applied to estimating paleoaltitudes from fossil floras, p. 71-99, 1992 Elsevier Science Publishers B.V., with permission from Elsevier.]...
The pH of a system determines the reactions that define the concentration of many dissolved chemical species in water containing salts and minerals, supplied by weathering reactions, rain, runoff, and lixiviating processes. The pH is a key parameter for biological growth and for the sustainment of life for the different aquatic flora and fauna species. As discussed in Chapter 2 the contribution of the different species will affect the final pH and vice versa (i.e., the pH on its own often determines the form of the species present). That is why the distribution diagrams of chemical species are frequently defined as functions of pH (Section 2.1.2). In summary, the main environmental processes that affect the pH and the alkalinity of natural waters include ... [Pg.117]

Gross clinical deficiency of vitamin Be is extremely rare. The vitamin is widely distributed in foods (although a significant proportion in plant foods may be biologically unavailable Section 9.1), and intestinal flora synthesize relatively large amounts, at least some of which may be absorbed and hence available. [Pg.246]

Dietary deficiency of biotin sufficient to cause clinical signs is extremely rare in human beings, although it may be a problem in intensively reared poultry. However, there is increasing evidence that suboptimal biotin status may be relatively common, despite the fact that the vitamin is widely distributed in many foods, is synthesized by intestinal flora, and there is an efficient mechanism for conserving biotin after the catabolism of biotin-containing enzymes. [Pg.324]


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See also in sourсe #XX -- [ Pg.37 , Pg.71 ]




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