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  • 1995-1999  (2)
  • 1970-1974
  • 1965-1969  (1)
  • 1915-1919
  • 1910-1914
  • wetlands  (2)
  • Cell & Developmental Biology  (1)
  • 1
    ISSN: 1573-1480
    Keywords: wetlands ; forested catchments ; dissolved organic carbon ; carbon cycling
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Most Precambrian Shield forested catchments have some wetland component. Even small riparian wetlands are important modifiers of stream chemistry. Dissolved organic matter (DOM) is one of the most important products exported by wetlands in streams. Stratigraphic control of hydraulic conductivity generally leads to decreasing conductivity with depth. Thus important flowpaths occur in the uppermost organic rich layers and are reflected in chemical profiles of dissolved organic carbon (DOC). Accumulation of DOC in peat porewaters is the net effect of production, consumption and transport. DOC profiles vary with degree of interaction with the surrounding upland catchment and distance from the edge of the wetland as well as internal processes within the wetland. In wetlands, DOM production is offset by flushing resulting in decreasing DOC concentrations with increasing flows. Despite old carbon (2,000 to 3,000 years) at relatively shallow depths, 14C activity in DOC exported from wetlands is mostly modern (recent carbon), consistent with shallow flowpaths and export of DOM from shallow organic rich horizons. In contrast, the source area for DOM in upland catchments with developed B horizon soils increases with antecedent soil moisture conditions resulting in increasing DOC concentrations with higher stream flows. Activity of 14C in stream DOC from upland catchments span a range from low activities (older carbon) similar to B horizon soil water during dry moisture conditions to values slightly less than modern (more recent carbon) during high moisture conditions. The more modern carbon activities reflect the increased contribution of the organic rich litter and A horizon soil layers in the area immediately bordering the stream under wet antecedent moisture conditions. Reduced hydrologic export or loss of wetlands under drier climatic conditions may result in in larger fluctuations in stream DOC concentrations and reduced DOM loads to lakes.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1573-1480
    Keywords: wetlands ; artificial reservoirs ; peat islands ; flooding
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Flooding of a small boreal forest wetland (979) in northwestern Ontario, caused the formation of peat islands, which resulted in an approximate 10 °C increase in peat temperatures at a depth of 50 cm. Peat collected from the flooded wetland and a natural unflooded wetland was incubated anaerobically at temperatures of 4 °C, 15 °C, and 20 to 25 °C. Flooding of the wetland greatly increased CH4 production rates by increasing the ratio of CH4:CO2 produced from 979 peat (40% : 60%) compared to 632 peat (20% : 80%), at both preflood and postflood temperatures, likely due to the altered hydrological and geochemical conditions within the peat mats due to flooding. CH4 and CO2 production rates approximately tripled for every 10 °C temperature increase and may have been linked to to the metabolic rate of the methanogens or the fermentors independent of the substrate quality. Methane production rates from deep peat deposits within the islands were also significant and responded well to temperature increases despite peat 14C ages of 1000 years. Due to the large quantity of carbon stored within natural wetlands, artificial reservoirs may act as a significant and long term source of CH4 to the atmosphere.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 0021-9541
    Keywords: Life and Medical Sciences ; Cell & Developmental Biology
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Biology , Medicine
    Notes: Since Euglena gracilis Klebs var. bacillaris Pringsheim contains a species of DNA unique to the chloroplast, an important question concerns the extent to which light unblocks the reading of the organelle's template to provide the informational RNA's necessary to construct the plastid proteins. Experiments with 32Pi labeling of chloroplast and nonchloroplast RNA's during light-induced chloroplast development show that both the RNA of the chloroplast and of the rest of the cell become labeled during this process, with the chloroplast RNA's displaying the higher specific activity. The fact that chloroplast RNA is not uniquely labeled indicates that process other than a simple reading of the chloroplast DNA are involved. If we are to preserve the concept of a reasonable degree of chloroplast informational autonomy, we may assume, from this and other data, that the light induction of chloroplast development involves not only the unblocking of chloroplast DNA to make information available, but also a concomitant unblocking of other sites of informational RNA synthesis (e.g., nuclear and mitochondrial DNA's). Such sites external to the developing chloroplast may be concerned with making available the building blocks and energy necessary for the synthesis of chloroplast constituents coded for by the chloroplast DNA. This model leads to the prediction that photosynthesis could be gratuitous for chloroplast development if these nonchloroplast sites were providing most of the building blocks and energy. Experiments are reported which show that chloroplast formation and the acquisition of photosynthetic competence can be achieved under conditions where photosynthesis is completely inhibited for the entire span of development by using the highly selective inhibitor 3, (3,4-dichlorophenyl) 1, 1-dimethyl urea (DCMU), in agreement with the proposed model. The fact that more than just the chloroplast responds to the inducing signals for chloroplast differentiation raises the problem of experimental measurement of interaction among cellular organelles. Since chloroplast development is usually carried out in resting cells to avoid complications due to cell division, we discuss the limitations imposed by turnover in such nondividing systems and present evidence that most of the RNA labeling observed, although actinomycin-D-sensitive, is due to turnover and/or the utilization of preexisting pools. Evidence obtained with mutants of Euglena that form only partial chloroplasts or that lack plastid DNA and plastid-related structures is reported. Such evidence indicates that the functional proplastid restrains overall RNA labeling in the uninduced cells and suggests that the proplastid might be the source of regulatory metabolic signals in the normal plastid-containing cells.
    Additional Material: 16 Ill.
    Type of Medium: Electronic Resource
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