کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
10122084 1642594 2005 23 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Deglacial vegetation succession and Holocene tree-limit dynamics in the Scandes Mountains, west-central Sweden: stratigraphic data compared to megafossil evidence
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فسیل شناسی
پیش نمایش صفحه اول مقاله
Deglacial vegetation succession and Holocene tree-limit dynamics in the Scandes Mountains, west-central Sweden: stratigraphic data compared to megafossil evidence
چکیده انگلیسی
High-resolution records of plant macrofossils, magnetic susceptibility, and total carbon content, complemented by pollen data, were obtained from a postglacial lake sediment sequence at alpine Lake Stentjärn (987 m a.s.l.), in west-central Sweden. Holocene vegetational and environmental changes were reconstructed from the data, with particular emphasis on the deglacial establishment of terrestrial vegetation and subsequent tree-limit dynamics. A short-lived pioneer flora with Geum rivale, Dryas octopetala, Empetrum nigrum, Ledum palustre, Saxifraga sp., Salix spp., and Oxyria digyna established locally following deglaciation at c. 10,500 cal year BP. The pioneer flora was out-competed by establishing Betula pubescens and grasses at c. 10,300 cal year BP. Subsequent local expansions of B. pubescens at c. 9800 cal year BP and Pinus sylvestris at c. 9200 cal year BP were followed by a temporary retraction of the birch tree-limit and a permanent retreat of pine between 8500 and 8000 cal year BP, accompanied by declining aquatic productivity and increasing catchment erosion. A gradual decrease in forest density initiated at c. 6000 cal year BP led to a retreat of the birch tree-limit from the lake catchment at c. 3500 cal year BP, followed by persistence of scattered trees until c. 2000 cal year BP. A mosaic heath vegetation dominated by Empetrum nigrum and Betula nana developed at c. 3500 cal year BP. Comparison of the stratigraphic data from Lake Stentjärn with records of radiocarbon-dated subfossil wood remains (megafossils) obtained from adjacent areas during recent decades revealed a high level of consistency of the inferred tree-limit variations for P. sylvestris, B. pubescens, and Alnus incana. Chronological control was established by radiocarbon dating of terrestrial macrofossils and geochemical identification of a tephra horizon originating from the Icelandic Askja-1875 eruption.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Review of Palaeobotany and Palynology - Volume 134, Issues 3–4, May 2005, Pages 129-151
نویسندگان
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