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dc.contributor.authorTeptina, Anzhelika
dc.contributor.authorRajakaruna, Nishanta
dc.contributor.authorPaukov, Alexander
dc.date.accessioned2019-03-27T10:58:18Z
dc.date.available2019-03-27T10:58:18Z
dc.date.issued2018
dc.identifier.citationTeptina, A. et al. 2018. Ultramafic vegetation and soils in the circumboreal region of the Northern Hemisphere. Ecological research, 33(3):609-628. [https://doi.org/10.1007/s11284-018-1577-1]en_US
dc.identifier.issn0912-3814
dc.identifier.issn1440-1703 (Online)
dc.identifier.urihttp://hdl.handle.net/10394/32071
dc.identifier.urihttps://esj-journals.onlinelibrary.wiley.com/doi/10.1007/s11284-018-1577-1
dc.identifier.urihttps://doi.org/10.1007/s11284-018-1577-1
dc.description.abstractThe paper summarizes literature on climate, soil chemistry, vegetation and metal accumulation by plants found on ultramafic substrata in the circumboreal zone (sensu Takhtajan, Floristic regions of the world, 1986) of the Northern Hemisphere. We present a list of 50 endemic species and 18 ecotypes obligate to ultramafic soils from the circumboreal region of Holarctic, as well as 30 and 2 species of Ni and Zn hyperaccumulators, respectively. The number of both endemics and hyperaccumulators are markedly lower compared to that of the Mediterranean and tropical regions. The diversity of plant communities on ultramafics soils of the circumboral region is also described. The underlying causes for the differences of ultramafic flora between arctic, cold, cool temperate and Mediterranean and tropical regions are also discusseden_US
dc.language.isoenen_US
dc.publisherWileyen_US
dc.subjectUltramafic vegetationen_US
dc.subjectUltramafic soilsen_US
dc.subjectObligate serpentinophytesen_US
dc.subjectEdaphic endemismen_US
dc.subjectMetal hyperaccumulationen_US
dc.titleUltramafic vegetation and soils in the circumboreal region of the Northern Hemisphereen_US
dc.typeArticleen_US
dc.contributor.researchID24678104 - Rajakaruna, Nishanta


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