- Geological and Geochemical Analysis
- Paleontology and Stratigraphy of Fossils
- Geochemistry and Geologic Mapping
- earthquake and tectonic studies
- Geological and Geophysical Studies Worldwide
- Geochemistry and Elemental Analysis
- High-pressure geophysics and materials
- Geology and Paleoclimatology Research
- Geological Studies and Exploration
- Geological formations and processes
- Geological Formations and Processes Exploration
- Geological and Geophysical Studies
- Archaeological and Geological Studies
- Geological Modeling and Analysis
- Hydrocarbon exploration and reservoir analysis
- Radioactive element chemistry and processing
- Marine Biology and Ecology Research
- Evolution and Paleontology Studies
- Mineralogy and Gemology Studies
- Methane Hydrates and Related Phenomena
- Geographic Information Systems Studies
- Geomagnetism and Paleomagnetism Studies
- Paleontology and Evolutionary Biology
- Marine and environmental studies
- Mining and Gasification Technologies
Senckenberg Natural History Collections Dresden
2016-2025
Novelis (Canada)
2023
Diagnostics for the Real World (United Kingdom)
2022
Institute of Geochemistry
2021
University of Lisbon
2020
Institute of Mineralogy
2017
Abstract The replacement of the late Precambrian Ediacaran biota by morphologically disparate animals at beginning Phanerozoic was a key event in history life on Earth, mechanisms and time‐scales which are not entirely understood. A composite section Namibia providing biostratigraphic chemostratigraphic data bracketed radiometric dating constrains Ediacaran–Cambrian boundary to 538.6–538.8 Ma, more than 2 Ma younger previously assumed. U–Pb‐ CA ‐ ID TIMS zircon ages demonstrate an ultrashort...
Research Article| October 31, 2017 New U-Pb dates show a Paleogene origin for the modern Asian biodiversity hot spots U. Linnemann; Linnemann * 1Senckenberg Museum of Mineralogy and Geology, Natural History Collections Dresden, Königsbrücker Landstrasse 159, 01109 Germany *E-mail: Ulf.Linnemann@senckenberg.de Search other works by this author on: GSW Google Scholar T. Su; Su 2Key Laboratory Tropical Forest Ecology, Xishuangbanna Botanical Garden, Chinese Academy Sciences, Menglun, Yunnan...
Orogens with multiple (ultra)high‐pressure ((U)HP) and (ultra)high‐temperature ((U)HT) metamorphic events provide a complex but telling record of oceanic continental interaction. The Early Paleozoic history the “Heart China,” Qinling orogenic collage, offers snapshots at least three (U)HP two (U)HT events. preservation remnants both domains together ≥110 Myr magmatism allows reconstruction processes that resulted in this disparate metamorphism. Herein, we first illuminate...
The Qinling‐Dabie orogenic collage, central China, constitutes the geographic, geologic, and cultural heart of China; it plays a key role in understanding amalgamation breakup Rodinia supercontinent subduction exhumation continental crust under ultrahigh‐pressure conditions. Herein, we investigate Proterozoic evolution collage surrounding segments bounding South China craton (SCC) North (NCC), employing published new U/Th–Pb geochronology. Kongling, Hong'an‐Dabie, Douling‐Foping complexes...