A circumpolar comparison of terricolous lichens in East Asian boreal vegetation and flora
Teuvo T. AHTI
Finnish Museum of Natural History, Helsinki, Finland
Terricolous, fruticose lichens are dominant members in the ground layer of xeric,
open woodlands in extensive areas of continental sectors of the boreal zone in
East Asia. Certain species are also common in the bryophyte-dominated mesic
and submesic community types. In addition, lichens are often dominant on thin soil
over open rock outcrops, in boulder fields, on sand-dunes, and on hummocks or
even wet surfaces of peatlands. Their remarkable ecological role tends to increase
towards the polar or alpine timberlines and in various forest successions on welldrained
soil, but also on peatlands after forest fires or logging, then binding humus
and parent soil against erosion, and forming lichen-rich, seral communities. The
major lichen species in East Asian vegetation are largely circumpolar (e.g., Cladonia
stellaris), occupying similar sites and subzones elsewhere in the circumboreal
zone. Another element is present in all four boreal coastal regions (e.g., Cladonia
maxima). The East Asian element is small, including Cladonia cineracea and
some coastal species. The Amphiberingian element includes Cladonia alaskana,
C. alinii, C. jacutica, C. kanewskii, C. nipponica, C. pseudoevansii,
C. scotteri, and
Flavocetraria minuscula. Cetraria laevigata and Cladonia wainioi occupy similar
ecological niches extending to eastern North America. The arid boreal sectors (as
in the Sakha Republic) include areas where calcicolous, primarily arctic or steppe
lichens may form soil crusts with numerous tiny crustose species.
© 2012 Organizing Committee
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