30 research outputs found

    A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude

    Get PDF
    Early to Middle Miocene sea-level oscillations of approximately 40-60 m estimated from far-field records1-3 are interpreted to reflect the loss of virtually all East Antarctic ice during peak warmth2. This contrasts with ice-sheet model experiments suggesting most terrestrial ice in East Antarctica was retained even during the warmest intervals of the Middle Miocene4,5. Data and model outputs can be reconciled if a large West Antarctic Ice Sheet (WAIS) existed and expanded across most of the outer continental shelf during the Early Miocene, accounting for maximum ice-sheet volumes. Here we provide the earliest geological evidence proving large WAIS expansions occurred during the Early Miocene (~17.72-17.40 Ma). Geochemical and petrographic data show glacimarine sediments recovered at International Ocean Discovery Program (IODP) Site U1521 in the central Ross Sea derive from West Antarctica, requiring the presence of a WAIS covering most of the Ross Sea continental shelf. Seismic, lithological and palynological data reveal the intermittent proximity of grounded ice to Site U1521. The erosion rate calculated from this sediment package greatly exceeds the long-term mean, implying rapid erosion of West Antarctica. This interval therefore captures a key step in the genesis of a marine-based WAIS and a tipping point in Antarctic ice-sheet evolution

    Studio delle relazioni tra vegetazione, topografia, e forme del paesaggio fisico, nell'Alto Appennino Settentrionale, mediante la realizzazione di un GIS.

    No full text
    A GIS was developed to detect the relationships between vegetation types, landforms and topographic variables in the Mount Prado area (N-Apennines, Italy). Data sets were derived from detailed vegetational and geomorphological maps, whereas the DEM and some primary topographic attributes were derived from a topographic map. The distribution of vegetation types was correlated with landforms and topographic parameters. The correlations thus obtained were than critically analysed
    corecore