Mats Rundgren
Senior lecturer
Rapid Holocene climate changes in the North Atlantic: evidence from lake sediments from the Faroe Islands
Author
Summary, in English
Holocene records from two lakes on the Faroe Islands were investigated to determine regional climatic variability: the fairly wind-exposed Lake Starvatn on Streymoy and the more sheltered Lake Lykkjuvotn on Sandoy. Sediment cores were analysed for content of biogenic silica, organic carbon and clastic material, and magnetic susceptibility. In addition, a new qualitative proxy for past lake ice cover and wind activity was developed using the flux of clastic grains that are larger than 255 mu m. Both long-term and short-term climatic developments were similar between the two lakes, suggesting a response to a regional climate signal. The long-term climate development is characterized by early Holocene rapid warming followed by Holocene climatic optimum conditions ending around 8300 cal. yr BP. A more open landscape as evidenced from increased sand grain influx in the period 8300-7200 cal. yr BP could reflect the aftermath of the 8200 cal. yr BP event, although the event itself is not recognized in either of the two lake records. From around 7200 cal. yr BP the mid-Holocene climate deterioration is observed and from 4200 cal. yr BP the climate deteriorated further with increased amplitude of centennial cooling episodes.
Department/s
- Quaternary Sciences
Publishing year
2006
Language
English
Pages
23-34
Publication/Series
Boreas
Volume
35
Issue
1
Document type
Journal article
Publisher
John Wiley & Sons Inc.
Topic
- Geology
Status
Published
ISBN/ISSN/Other
- ISSN: 1502-3885