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dc.contributor.authorTeptina, A.en
dc.contributor.authorPaukov, A.en
dc.contributor.authorRajakaruna, N.en
dc.date.accessioned2021-08-31T15:01:17Z-
dc.date.available2021-08-31T15:01:17Z-
dc.date.issued2018-
dc.identifier.citationTeptina A. Ultramafic vegetation and soils in the circumboreal region of the Northern Hemisphere / A. Teptina, A. Paukov, N. Rajakaruna. — DOI 10.1007/s11284-018-1577-1 // Ecological Research. — 2018. — Vol. 33. — Iss. 3. — P. 609-628.en
dc.identifier.issn9123814-
dc.identifier.otherFinal2
dc.identifier.otherAll Open Access, Green3
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85044610178&doi=10.1007%2fs11284-018-1577-1&partnerID=40&md5=a9bc323b94d4f3cfcde30bfb6d93b7af
dc.identifier.otherhttps://digitalcommons.calpoly.edu/cgi/viewcontent.cgi?article=1534&context=bio_facm
dc.identifier.urihttp://elar.urfu.ru/handle/10995/102016-
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 discussed. © 2018, The Ecological Society of Japan.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherSpringer Tokyoen
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceEcol. Res.2
dc.sourceEcological Researchen
dc.subjectEDAPHIC ENDEMISMen
dc.subjectMETAL HYPERACCUMULATIONen
dc.subjectOBLIGATE SERPENTINOPHYTESen
dc.subjectULTRAMAFIC SOILSen
dc.subjectULTRAMAFIC VEGETATIONen
dc.titleUltramafic vegetation and soils in the circumboreal region of the Northern Hemisphereen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.rsi35713089-
dc.identifier.doi10.1007/s11284-018-1577-1-
dc.identifier.scopus85044610178-
local.contributor.employeeTeptina, A., Institute of Natural Sciences and Mathematics, Ural Federal University, Lenin av., 51, Yekaterinburg, 620000, Russian Federation
local.contributor.employeePaukov, A., Institute of Natural Sciences and Mathematics, Ural Federal University, Lenin av., 51, Yekaterinburg, 620000, Russian Federation
local.contributor.employeeRajakaruna, N., Biological Sciences Department, California Polytechnic State University, San Luis Obispo, CA 93407, United States, Unit for Environmental Sciences and Management, North-West University, Private Bag X6001, Potchefstroom, 2520, South Africa
local.description.firstpage609-
local.description.lastpage628-
local.issue3-
local.volume33-
dc.identifier.wos000435608000010-
local.contributor.departmentInstitute of Natural Sciences and Mathematics, Ural Federal University, Lenin av., 51, Yekaterinburg, 620000, Russian Federation
local.contributor.departmentBiological Sciences Department, California Polytechnic State University, San Luis Obispo, CA 93407, United States
local.contributor.departmentUnit for Environmental Sciences and Management, North-West University, Private Bag X6001, Potchefstroom, 2520, South Africa
local.identifier.purebfc4f979-f138-41d4-8f71-e18df70ce859uuid
local.identifier.pure7419650-
local.identifier.eid2-s2.0-85044610178-
local.identifier.wosWOS:000435608000010-
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