Sökning: "Lowland Point"
Visar resultat 1 - 5 av 8 uppsatser innehållade orden Lowland Point.
1. SPECIES DELIMITATION IN GENIPA (RUBIACEAE) USING INTEGRATIVE TAXONOMY
Master-uppsats, Göteborgs universitet / Institutionen för biologi och miljövetenskapSammanfattning : The genus Genipa L. is a widespread, lowland, Neotropical lineage of trees in the coffeefamily, Rubiaceae. There is long-standing disagreement on the number of species thatshould be recognised in the genus. LÄS MER
2. Post-IR IRSL dating of K-feldspar from Loess at Lowland Point, SW England : Developing a Chronology for Past Climate Records
Kandidat-uppsats, Uppsala universitet/Institutionen för geovetenskaperSammanfattning : Loess deposits are terrestrial clastic sediments derived from aeolian deposition. Loess is transported in periglacial conditions and was mainly deposited in cold environments around glaciers during the Quaternary period. LÄS MER
3. Nature-based solutions as a climate change adaptation strategy
Kandidat-uppsats, Lunds universitet/Institutionen för kulturgeografi och ekonomisk geografiSammanfattning : Because of climate change, rising sea levels in Kristianstad Municipality is more urgent than ever. Sea levels around Scania are estimated to rise more than 2,5 meters in 80 years considering that they are currently rising with 3,2 mm per year. LÄS MER
4. Investigating the Magnetic Susceptibility of Cornish Loess as a Tool for Understanding the Palaeoclimate of SW England
Master-uppsats, Uppsala universitet/Institutionen för geovetenskaperSammanfattning : Loess is a silty material produced via glacial grinding and its deposition is usually associated with colder periods when there is a considerable increase in atmospheric dust transport. The magnetic susceptibility of loess-palaeosol sequences has been the subject of extensive research within palaeoclimatology as it has proven to be reliable climate proxy. LÄS MER
5. Identifying Quaternary Climate Change with XRF Analysis on Loess From South-Western England
Kandidat-uppsats, Uppsala universitet/Institutionen för geovetenskaperSammanfattning : Huge changes in climate occurred at the end of the last Quaternary glaciation. The end of this glaciation corresponds with the end of Pleistocene with its repeated glacial cycles and the start of the current geological epoch, the Holocene interglacial. LÄS MER