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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    European journal of neuroscience 12 (2000), S. 0 
    ISSN: 1460-9568
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: The second messenger Ca2+ is known to act in a broad spectrum of fundamental cell processes, including modifications of cell shape and motility, through the intermediary of intracellular calcium-binding proteins. The possible impact of the lack of the intracellular soluble Ca2+-binding proteins parvalbumin (PV) and calbindin D-28 k (CB) was tested on spine morphology and topology in Purkinje cell dendrites of genetically modified mice. Three different genotypes were studied, i.e. PV or CB single knock-out (PV–/–, CB–/–) and PV and CB double knock-out mice (PV–/–CB–/–). Purkinje cells were microinjected with Lucifer Yellow and terminal dendrites scanned at high resolution with a confocal laser microscope followed by three-dimensional (3-D) reconstruction. The absence of PV had no significant effect on spine morphology, whereas the absence of CB resulted in a slight increase of various spine parameters, most notably spine length. In double knock-out mice, the absence of both PV and CB entailed a doubling of spine length, an increase in spine volume and spine surface, a higher spine density along the dendrites, as well as a more clustered spine distribution. In all three genotypes, a reduction in the number of stubby spines was observed compared with wild-type animals. These results suggest a morphological compensation for the lack of the soluble calcium buffers in the cytoplasm of Purkinje cell dendritic spines. The increase in various spine parameters, particularly volume, may counteract the lack of the calcium buffers, such as to adjust Ca2+-transients at the transitional zone between spines and dendrites.
    Type of Medium: Electronic Resource
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  • 2
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    Geological Society of America (GSA)
    Publication Date: 2011-05-01
    Description: Ancient speleothems were recovered from caves that today are situated in a high-alpine cirque landscape at 2500 m altitude at the northern rim of the European Alps. U-Pb ages date speleothem deposition to the early Quaternary (between 2.16 and 2.12 Ma and ca. 2.00 Ma), i.e., well before the onset of major alpine and Northern Hemisphere glaciations. Using a stable isotope-based modeling approach, we quantitatively estimate the paleoelevation of both the caves and their former catchment area, which in turn allows us to calculate rates of rock and surface uplift (and hence erosion) since 2 Ma. We show that for the frontal part of the Alps, rates of rock uplift and erosion were [~]0.75 and [~]0.5 mm/yr, respectively, and further suggest that isostatic uplift of mountain peaks of as much as [~]500 m in response to enhanced glacial erosion occurred during the Quaternary. This study highlights the potential of U-Pb-dated speleothems for reconstructing paleoaltimetry, particularly in calcareous mountain ranges, where a standard thermochronologic assessment of exhumation and erosion is generally not feasible.
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
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