Response of Betula glandulosa seedlings to simulated increases in nutrient availability, temperature and precipitation in a lichen woodland at the forest–tundra ecotone

Plant Ecology ◽  
2014 ◽  
Vol 215 (3) ◽  
pp. 305-314 ◽  
Author(s):  
Mélissa Paradis ◽  
Caroline Mercier ◽  
Stéphane Boudreau
Polar Biology ◽  
2017 ◽  
Vol 40 (11) ◽  
pp. 2265-2278 ◽  
Author(s):  
Isabel C. Barrio ◽  
Elin Lindén ◽  
Mariska Te Beest ◽  
Johan Olofsson ◽  
Adrian Rocha ◽  
...  

1991 ◽  
Vol 28 (4) ◽  
pp. 643-648 ◽  
Author(s):  
K. Gajewski

Modern pollen spectra from a series of lakes in northwestern Quebec reflect the major vegetation zones of the forest–tundra transition from latitude 55°N to 59°N. Shrub tundra samples are dominated by Betula and herb pollen, whereas Picea percentages are between 10 and 20%. Lichen woodland samples can contain over 60% Picea, with Betula and Alnus crispa each less than 20%. Pollen assemblages from the shrub subzone of the forest–tundra resemble those of the shrub tundra, while those from the forest subzone resemble lichen woodland samples. Maximum percentages of Alnus crispa are found in the forest–tundra. Classification of the samples using cluster analysis and an ordination by principal coordinates analysis suggest that densely and sparsely forested regions can be discriminated.


Polar Biology ◽  
2018 ◽  
Vol 41 (8) ◽  
pp. 1653-1654
Author(s):  
Isabel C. Barrio ◽  
Elin Lindén ◽  
Mariska Te Beest ◽  
Johan Olofsson ◽  
Adrian Rocha ◽  
...  

1993 ◽  
Vol 71 (2) ◽  
pp. 193-210 ◽  
Author(s):  
George A. King

The relationship between the vegetation and modern pollen assemblages in eastern Canada is summarized and analyzed using isopoll maps, ordination, and cluster analysis. The major vegetation zones are shrub tundra, forest tundra (divided into shrub and forest subzones), lichen woodland, closed black spruce forest, mixed boreal forest, and coastal barrens. The pollen assemblages of these zones are distinguished by differences in the relative abundance of a few important pollen types rather than by floristic differences. Northern zones have relatively high Cyperaceae and low Picea pollen percentages, and southern zones have high Picea and Abies pollen percentages. Surface samples from each vegetation zone generally form distinctive groups in the ordination analysis. However, samples from the shrub subzone of the forest tundra cluster with shrub tundra samples, and lichen woodland samples cluster with samples from the closed black spruce forest and the forest subzone of the forest tundra. Cluster analysis separates the samples into geographically distinct groups. However, these groups generally contain samples from several vegetation zones. The surface sample data set analyzed here will prove useful in reconstructing the vegetation history of the region. Key words: pollen surface samples, modern vegetation, eastern Canada.


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