A5058707160- Geology and Paleoclimatology Research
- Isotope Analysis in Ecology
- Marine and environmental studies
- Marine and coastal ecosystems
- Marine Biology and Ecology Research
- Methane Hydrates and Related Phenomena
- Geological formations and processes
- Scientific Research and Discoveries
- Geological Studies and Exploration
- Hydrocarbon exploration and reservoir analysis
- Archaeology and ancient environmental studies
- Oceanographic and Atmospheric Processes
- Microbial Community Ecology and Physiology
- Marine Bivalve and Aquaculture Studies
- Diatoms and Algae Research
- Groundwater and Isotope Geochemistry
- Historical and Archaeological Studies
- Ocean Acidification Effects and Responses
- Toxic Organic Pollutants Impact
- Pleistocene-Era Hominins and Archaeology
- Arctic and Antarctic ice dynamics
- Environmental DNA in Biodiversity Studies
- Climate change and permafrost
- Digital Imaging for Blood Diseases
- Tree-ring climate responses
University of Gothenburg
2010-2024
Stockholm University
2009
Lund University
2009
Åbo Akademi University
2009
University of Helsinki
2009
Chalmers University of Technology
1987-1988
Viable diatom and dinoflagellate resting stages were recovered from sediments in Koljö Fjord on the west coast of Sweden. To determine maximum survival time buried stages, samples sediment depths down to 50 cm incubated at temperatures 3, 10 18 °C. Sediment cores dated by 210Pb age containing viable was determined using constant rate supply model. Dilution cultures surface allowed semiquantitative estimates potential seed bank. Dinoflagellate cysts species such as Diplopsalis sp.,...
Abstract A synthesis is presented of the envronmental and climatic variations that are inferred to have occurred in southern Sweden (up latitude 59°N) Denmark during Weichselian Late‐glacial (14‐9 ka BP). The chronology characteristics main phases deglaciation, sea‐level change, periglacial activity, soil development, vegetation cover climate change summarised. curve representing changes temperature, including quantitative estimates based upon beetle data using ‘mutual range’ method, presented.
In the Kattegat, between Sweden and Denmark, a large number of cores containing Holocene seafloor deposits were investigated stratigraphically. Sedimentological, biostratigraphical, chronostratigraphical variables especially emphasized. Palynological foraminiferal analyses indicate several changes in oceanographic circulation system Skagerrak‐Kattegat during Holocene. Radiocarbon datings pollen suggest that these occurred at 8000, 4000, 2000, 1000 500, 300 years B.P. Compilation...
From stratigraphic investigations of 38 piston and vibro cores, four fine‐grained Late Weichselian sediment units can be defined in the southern Kattegat. A continuous record sediments cannot established from single cores due to uneven distribution units, but by compilation relative stratigraphies a composite determined for deposited between approximately 13,500 10,000 BP. The contain both lithological biostratigraphical evidence that Baltic Ice Lake was suddenly drained through Öresund...