Paleoenvironmental evolution of the Paratethys in the Slovenian Basin during the Late Paleogene     

Gerhard?SchmiedlEmail author  Maria?Scherbacher  Angela?A.?Bruch  Bogomir?Jelen  James?H.?Nebelsick  Christoph?Hemleben  Volker?Mosbrugger  Helena?Rifelj 《International Journal of Earth Sciences》2002,91(1):123-132

Several sections from the uppermost Eocene and Oligocene of northern Slovenia have been investigated with respect to sedimentary facies, foraminiferal assemblages, stable isotopes, carbonate microfacies, and palynology. The main objective was to reconstruct the paleoenvironmental history of the Paleogene Paratethys in this region of the eastern Alpine realm. The sediments exhibit a transgressive succession beginning with conglomerates, sandstones, and mudstones of fluvial and lacustrine origin followed by carbonates and muddy marls indicating marine conditions. The foraminiferal faunal changes from brackish to shallow marine to deeper marine assemblages and the distribution of the palynofloras corroborate the sedimentological results. Microfacies analysis of the limestones shows a wide variation of shallow water, generally mud-rich facies dominated by coralline algae, foraminifera, and corals. Microfaunas adapted to low-oxygen conditions indicate temporal sluggish bottom-water circulation which can be associated with high fresh-water fluxes. These results are discussed as reflecting both the global sea-level rise during the Early Oligocene and the regional tectonic and climatic evolution.  相似文献   

Changes in ice phenology characteristics of two Central European steppe lakes from 1926 to 2012 - influences of local weather and large scale oscillation patterns     

Anna-Maria?Soja  Károly?Kutics  Karl?Maracek  Gábor?Molnár  Gerhard?SojaEmail author 《Climatic change》2014,124(1-2):119-132

This paper investigates how the role of climate in tourist destination choice has changed over the last 15 years. To this end, a demand model for international tourism is estimated, including the main classic determinants but allowing a time-varying climatic sensitivity of tourists. Moreover, a complete database considering international tourism movement between 178 countries for the period 1995 to 2010 is used. Results show how turning point temperatures in origin and destination countries have changed over the period of analysis, evidencing a loss of competitiveness for traditional warm destinations. Additionally, using data for the projected growth of Gross Domestic Product per capita and climatic conditions within A2, B1 and B2 scenarios, an updated vision of their expected impact on international tourism flows is assessed, evaluating how climate change would imply a greater loss of attractiveness for traditional warm destinations around the world but would increase attractiveness for high latitude countries.  相似文献   

Gravity Changes and Internal Processes: Some Results Obtained from Observations at Three Volcanoes     

Gerhard?JentzschEmail author  Adelheid?Weise  Carlos?Rey  Carl?Gerstenecker 《Pure and Applied Geophysics》2004,161(7):1415-1431

Temporal gravity changes provide information about mass and/or density variations within and below the volcano edifice. Three active volcanoes have been under investigation; each of them related to a plate boundary: Mayon/Luzon/Philippines, Merapi/Java/Indonesia, and Galeras/Colombia. The observed gravity changes are smaller than previously expected but significant. For the three volcanoes under investigation, and within the observation period, mainly the increase of gravity is observed, ranging from 1,000 nm^–2 to 1,600 nms^–2. Unexpectedly, the gravity increase is confined to a rather small area with radii of 5 to 8 km around the summit. At Mayon and Merapi the parallel GPS measurements yield no significant elevation changes. This is crucial for the interpretation, as the internal pressure variations do not lead to significant deformation at the surface. Thus the classical Mogi-model for a shallow extending magma reservoir cannot apply. To confine the possible models, the attraction due to changes of groundwater level or soil moisture is estimated along the slope of Merapi exemplarily by 2-D modelling. Mass redistribution or density changes were evaluated within the vent as well as deeper fluid processes to explain the gravity variations; the results are compared to the model incorporating the additional effect of elastic deformation.  相似文献