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  • English  (4)
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  • 1
    Call number: S 90.0081(440)
    In: Reports of the Department of Geodetic Science and Surveying
    Type of Medium: Series available for loan
    Pages: IX, 61 S.
    Series Statement: Report / Department of Geodetic Science and Surveying, the Ohio State University 440
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
    Publication Date: 2023-03-24
    Description: Over the last years, perennial ice deposits located within caves have awakened interest as places to study microbial communities since they represent unique cryospheric archives of climate change. Since the beginning of the twentieth century, the temperature has gradually increased, and it is estimated that by the end of this century the increase in average temperature could be around 4.0°C. In this context of global warming the ice deposits of the Pyrenean caves are undergoing a significant regression. Among this type of caves, that on the Cotiella Massif in the Southern Pyrenees is one of the southernmost studied in Europe. These types of caves house microbial communities which have so far been barely explored, and therefore their study is necessary. In this work, the microbial communities of the Pyrenean ice cave A294 were identified using metabarcoding techniques. In addition, research work was carried out to analyze how the age and composition of the ice affect the composition of the bacterial and microeukaryotic populations. Finally, the in vivo effect of climate change on the cellular machinery that allow microorganisms to live with increasing temperatures has been studied using proteomic techniques.
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 3
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-06-19
    Description: The San Rafael waterfall sinkhole on the Coca River in February 2020 caused by soil erosion raises the question of the stability of the knickpoint structure. The main objective of this research is to obtain tomographic images to interpret the seismic stratigraphic profile around the San Rafael knickpoint using seismic tomography. We use data from fourteen seismic stations of the permanent Ecuadorian seismic network in the region. The tomography results for the vertical cross-section P-wave velocity model show the geological formations and their transition to volcanic deposits. It also shows a structure with a high P-wave velocity value directly below the knickpoint. In contrast, the horizontal cross-section shows the structure of the extension of the volcanic deposits. The relative P-wave velocity shows a volumetric structure below the last pyroclastic deposits generated by the Reventador. The dimensions and characteristic velocity of the anomaly allow us to relate it to an igneous intrusion similar to the granodioritic intrusions known to the east of the volcano cone. Therefore, the presence of this pluton should condition the stability of the Coca riverbed, its slopes, and cliffs. The volcanic deposits in direct contact with the intrusion are suspected to be poorly consolidated. The P-wave velocity model shows that these volcanic deposits have an extension of 40 km. Greater stability is expected upstream of the San Rafael pluton. The relocation obtained by tomography also allows for defining the possible magmatic feeding system of the Reventador volcano.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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  • 4
    Publication Date: 2024-02-05
    Description: Glaciers constitute a polyextremophilic environment characterized by low temperatures, high solar radiation, a lack of nutrients, and low water availability. However, glaciers located in volcanic regions have special characteristics, since the volcanic foci provide them with heat and nutrients that allow the growth of microbial communities highly adapted to this environment. Most of the studies on these glacial ecosystems have been carried out in volcanic environments in the northern hemisphere, including Iceland and the Pacific Northwest. To better know, the microbial diversity of the underexplored glacial ecosystems and to check what their specific characteristics were, we studied the structure of bacterial communities living in volcanic glaciers in Deception Island, Antarctica, and in the Kamchatka peninsula. In addition to geographic coordinates, many other glacier environmental factors (like volcanic activity, altitude, temperature, pH, or ice chemical composition) that can influence the diversity and distribution of microbial communities were considered in this study. Finally, using their taxonomic assignments, an attempt was made to compare how different or similar are the biogeochemical cycles in which these microbiomes are involved.
    Language: English
    Type: info:eu-repo/semantics/article
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