- Geology and Paleoclimatology Research
- Methane Hydrates and Related Phenomena
- Paleontology and Stratigraphy of Fossils
- Coral and Marine Ecosystems Studies
- Geological and Geophysical Studies
- Geological formations and processes
- Marine Biology and Ecology Research
- Seismic Imaging and Inversion Techniques
- Marine and coastal plant biology
- Ocean Acidification Effects and Responses
- Hydrocarbon exploration and reservoir analysis
- Geophysics and Gravity Measurements
- Marine Bivalve and Aquaculture Studies
- Isotope Analysis in Ecology
- Geological Modeling and Analysis
- Marine and fisheries research
- Geological and Geophysical Studies Worldwide
- Coastal and Marine Dynamics
- Marine Sponges and Natural Products
- Coastal wetland ecosystem dynamics
- Calcium Carbonate Crystallization and Inhibition
- Reservoir Engineering and Simulation Methods
- Pacific and Southeast Asian Studies
- Maritime and Coastal Archaeology
- earthquake and tectonic studies
Leibniz Centre for Tropical Marine Research
2015-2025
University of Bremen
2014-2024
King Abdullah University of Science and Technology
2022-2024
Fahrenheit (Germany)
2014-2021
Staats- und Universitätsbibliothek Bremen
2021
Friedrich-Alexander-Universität Erlangen-Nürnberg
2004-2005
Leibniz University Hannover
2001-2004
Institut für Geologie und Umwelt (Germany)
2004
University of Miami
2000-2002
Universitat de les Illes Balears
2002
Abstract Large benthic foraminifera are major carbonate components in tropical platforms, important producers, stratigraphic tools and powerful bioindicators (proxies) of environmental change. The application large coral reef environments has gained considerable momentum recent years. These modern ecological assessments often carried out by micropalaeontologists or ecologists with expertise the identification foraminifera. However, have been under‐represented favour macro reef‐builders, for...
ABSTRACT Comparison of ultrastructures in Pliocene periplatform carbonates from the Bahamas with Silurian limestones Gotland (Sweden) reveals that despite differences primary sediment composition and age, they reflect a similar mechanism lithification. In both sequences calcite microspar was formed as cement at an early stage marine burial diagenesis. Neither significant compression nor meteoric influence are necessary for formation microspar. A model is proposed process microsparitic...