The sensitivity of middle Miocene paleoenvironments to changing marine gateways in Central Europe
@article{Simon2018TheSO, title={The sensitivity of middle Miocene paleoenvironments to changing marine gateways in Central Europe}, author={Dirk Simon and Dan Valentin Palcu and Paul Th. Meijer and Wout Krijgsman}, journal={Geology}, year={2018} }
15 Citations
Marine facies differentiation along complex paleotopography: an example from the Middle Miocene (Serravallian) of Lower Austria
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In the area of Bad Deutsch-Altenburg (Hainburg Mountains, Lower Austria) a Middle Miocene transgression over Mesozoic basement was explored in the course of the Danube power plant project “Hainburg”.…
Hypersalinity drives convergent bone mass increases in Miocene marine mammals from the Paratethys
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Target-free calibration of flat refractive imaging systems using two-view geometry
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Sedimentary response to current and nutrient regime
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29 During the early and middle Miocene, the Mediterranean had become a restricted marginal marine sea 30 with diminishing and ultimate loss of connectivity to the Indian Ocean. This dramatically…
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- Geography, Environmental Science
- 2021
Hydrological Changes in Restricted Basins: Insights From Strontium Isotopes on Late Miocene‐Pliocene Connectivity of the Eastern Paratethys (Dacian Basin, Romania)
- Geography, Environmental ScienceGeochemistry, Geophysics, Geosystems
- 2021
The Dacian Basin was uniquely situated to record late Miocene hydrological changes that influenced depositional environments and faunal dispersal patterns in Central Eurasia's mega‐lake Paratethys.…
The Temperature of Halite Crystallization in the Badenian Saline Basins, in the Context of Paleoclimate Reconstruction of the Carpathian Area
- Geology, Environmental ScienceMinerals
- 2021
Currently, fluid inclusions in halite have been frequently studied for the purpose of paleoclimate reconstruction. For example, to determine the air temperature in the Middle Miocene (Badenian), we…
The Miocene: The Future of the Past
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The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative to today. Continental configurations and mountain topography transitioned toward modern conditions, and many flora and…
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