Representation of Tundra Vegetation by Pollen in Lake Sediments of Northern Alaska W
Journal of Biogeography, 30, 521–535 Representation of tundra vegetation by pollen in lake sediments of northern Alaska W. Wyatt Oswald1,2*, Patricia M. Anderson2, Linda B. Brubaker1, Feng Sheng Hu3 and Daniel R. Engstrom41College of Forest Resources, 2Quaternary Research Center, Box 351360, University of Washington, Seattle, WA 98195, USA, 3Departments of Biology and Geology, University of Illinois, Urbana, IL, USA and 4St Croix Watershed Research Station, Science Museum of Minnesota, St Croix, MN, USA Abstract Aim To understand better the representation of arctic tundra vegetation by pollen data, we analysed pollen assemblages and pollen accumulation rates (PARs) in the surface sediments of lakes. Location Modern sediment samples were collected from seventy-eight lakes located in the Arctic Foothills and Arctic Coastal Plain regions of northern Alaska. Methods For seventy of the lakes, we analysed pollen and spores in the upper 2 cm of the sediment and calculated the relative abundance of each taxon (pollen percentages). For eleven of the lakes, we used 210Pb analysis to determine sediment accumulation rates, and analysed pollen in the upper 10–15 cm of the sediment to estimate modern PARs. Using a detailed land-cover map of northern Alaska, we assigned each study site to one of five tundra types: moist dwarf-shrub tussock-graminoid tundra (DST), moist graminoid prostrate-shrub tundra (PST) (coastal and inland types), low-shrub tundra (LST) and wet graminoid tundra (WGT). Results Mapped pollen percentages and multivariate comparison of the pollen data using discriminant analysis show that pollen assemblages vary along the main north– south vegetational and climatic gradients.
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