Lateglacial vegetation and palaeoenvironment in W Norway, with new pollen data from the Sunnmøre region
| العنوان: | Lateglacial vegetation and palaeoenvironment in W Norway, with new pollen data from the Sunnmøre region |
|---|---|
| المؤلفون: | Anne E. Bjune, Linn Cecilie Krüger, John Inge Svendsen, Aage Paus |
| المصدر: | Boreas. 40:616-635 |
| بيانات النشر: | Wiley, 2011. |
| سنة النشر: | 2011 |
| مصطلحات موضوعية: | Archeology, Empetrum, biology, Ecology, Geology, Ecotone, Older Dryas, biology.organism_classification, Artemisia norvegica, Dominance (ecology), Physical geography, Younger Dryas, Stadial, Ecology, Evolution, Behavior and Systematics, Holocene |
| الوصف: | Kruger, L. C., Paus, A., Svendsen, J. I. & Bjune, A. E. 2011: Lateglacial vegetation and palaeoenvironment in W Norway, with new pollen data from the Sunnmore region. Boreas, 10.1111/j.1502-3885.2011.00213.x. ISSN 0300-9483. Two sediment sequences from Sunnmore, northern W Norway, were pollen-analytically studied to reconstruct the Lateglacial vegetation history and climate. The coastal Dimnamyra was deglaciated around 15.3 ka BP, whereas Lokjingsmyra, further inland, became ice-free around 14 ka BP. The pioneer vegetation dominated by snow-bed communities was gradually replaced by grassland and sparse heath vegetation. A pronounced peak in Poaceae around 12.9 ka BP may reflect warmer and/or drier conditions. The Younger Dryas (YD) cooling phase shows increasing snow-bed vegetation and the local establishment of Artemisia norvegica. A subsequent vegetation closure from grassland to heath signals the Holocene warming. Birch forests were established 500–600 years after the YD–Holocene transition. This development follows the pattern of the Sunnmore region, which is clearly different from the Empetrum dominance in the Lateglacial interstadial further south in W Norway. The Lateglacial oscillations GI-1d (Older Dryas) and GI-1b (Gerzensee) are hardly traceable in the north, in contrast to southern W Norway. The southern vegetation was probably closer to an ecotone and more susceptible to climate changes. |
| تدمد: | 0300-9483 1502-3885 |
| DOI: | 10.1111/j.1502-3885.2011.00213.x |
| URL الوصول: | https://explore.openaire.eu/search/publication?articleId=doi_________::b3c46348b7054fa1f59201c22ecd88cf https://doi.org/10.1111/j.1502-3885.2011.00213.x |
| Rights: | OPEN |
| رقم الانضمام: | edsair.doi...........b3c46348b7054fa1f59201c22ecd88cf |
| قاعدة البيانات: | OpenAIRE |
| تدمد: | 03009483 15023885 |
|---|---|
| DOI: | 10.1111/j.1502-3885.2011.00213.x |