A5045726922- Geology and Paleoclimatology Research
- Marine and environmental studies
- Geological Formations and Processes Exploration
- Geological formations and processes
- Geological and Geophysical Studies Worldwide
- Paleontology and Stratigraphy of Fossils
- Evolution and Paleontology Studies
- Geological and Geochemical Analysis
- Geomagnetism and Paleomagnetism Studies
- earthquake and tectonic studies
- Pleistocene-Era Hominins and Archaeology
- Geological and Geophysical Studies
- Geological Studies and Exploration
- Isotope Analysis in Ecology
- Geochemistry and Geologic Mapping
- Methane Hydrates and Related Phenomena
- Hydrocarbon exploration and reservoir analysis
- Archaeological and Geological Studies
- Maritime and Coastal Archaeology
- Archaeology and ancient environmental studies
- Archaeological and Historical Studies
- Astro and Planetary Science
- Ancient and Medieval Archaeology Studies
- Soil and Environmental Studies
- Paleontology and Evolutionary Biology
Utrecht University
2016-2025
Vrije Universiteit Amsterdam
2008
Planetary Science Institute
2008
University of California, Berkeley
2008
Berkeley Geochronology Center
2008
Scripps Institution of Oceanography
2004-2006
University of California, San Diego
2004
University of Cambridge
2000
Calibration of the geological time scale is achieved by independent radioisotopic and astronomical dating, but these techniques yield discrepancies approximately 1.0% or more, limiting our ability to reconstruct Earth history. To overcome this fundamental setback, we compared 40Ar/39Ar ages tephras in marine deposits Morocco calibrate age Fish Canyon sanidine, most widely used standard geochronology. This calibration results a more precise older 28.201 +/- 0.046 million years ago (Ma)...
Abstract We propose a revised age calibration of the Messinian salinity crisis onset in Mediterranean at 5.971 Ma based on recognition an extra gypsum cycle transitional interval Perales section (Sorbas basin, Spain) and revision magnetostratigraphy Monticino (Vena del Gesso Italy). This re‐calibration allows to state more accurately that: (i) encompassing MSC ‐onset is continuous, thus ruling out any erosional feature or stratigraphic hiatus related major sea‐level fall affecting...
The Pontocaspian (Black Sea - Caspian Sea) region has a very dynamic history of basin development and biotic evolution. is the remnant once vast Paratethys Sea. It contains some best Eurasian geological records tectonic, climatic paleoenvironmental change. Pliocene-Quaternary co-evolution Black Sea-Caspian dominated by major changes in water (lake sea) levels resulting pulsating system connected isolated basins. Understanding region, including drivers lake level faunal evolution, hampered...
The Xining subbasin of the Longzhong basin holds longest continuous Cenozoic stratigraphic record at margin northeastern Tibetan Plateau. Despite a rich biostratigraphic content (including Xiejia mammal fauna), tectonic evolution is largely unconstrained. In this study we present stratigraphic, biostratigraphic, and magnetostratigraphic results that provide basis for reconstructing with respect to adjacent regions Magnetostratigraphic analysis from three red bed sections in indicates...
Research Article| August 01, 2010 Age of the Badenian salinity crisis; impact Miocene climate variability on circum-Mediterranean region A. de Leeuw; Leeuw * 1Paleomagnetic Laboratory “Fort Hoofddijk,” Faculty Geosciences, Utrecht University, Budapestlaan 17, 3584 CD Utrecht, Netherlands *E-mail: adeleeuw@geo.uu.nl. Search for other works by this author on: GSW Google Scholar K. Bukowski; Bukowski 2Faculty Geology, Geophysics and Environmental Protection, AGH University Science Technology,...
Abstract The Tarim Basin in western China formed the easternmost margin of a shallow epicontinental sea that extended across Eurasia and was well connected to Tethys during Paleogene. Climate modelling studies suggest westward retreat this from Central Asia may have been as important Tibetan Plateau uplift forcing aridification monsoon intensification Asian continental interior due redistribution land‐sea thermal contrast. However, testing hypothesis is hindered by poor constraints on timing...