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Vegetation on mesic loamy and sandy soils along a 1700-km maritime Eurasia Arctic Transect.
Walker, Donald A; Epstein, Howard E; Sibík, Jozef; Bhatt, Uma; Romanovsky, Vladimir E; Breen, Amy L; Chasníková, Silvia; Daanen, Ronald; Druckenmiller, Lisa A; Ermokhina, Ksenia; Forbes, Bruce C; Frost, Gerald V; Geml, Jozsef; Kaärlejarvi, Elina; Khitun, Olga; Khomutov, Artem; Kumpula, Timo; Kuss, Patrick; Matyshak, Georgy; Moskalenko, Natalya; Orekhov, Pavel; Peirce, Jana; Raynolds, Martha K; Timling, Ina.
Afiliación
  • Walker DA; Alaska Geobotany Center Institute of Arctic Biology & Department of Biology and Wildlife University of Alaska Fairbanks Alaska.
  • Epstein HE; Department of Environmental Sciences University of Virginia Charlottesville Virginia.
  • Sibík J; Plant Science and Biodiversity Center Slovak Academy of Sciences Institute of Botany Bratislava Slovak Republic.
  • Bhatt U; Geophysical Institute & Department of Atmospheric Science University of Alaska Fairbanks Alaska.
  • Romanovsky VE; Geophysical Institute & Department of Atmospheric Science University of Alaska Fairbanks Alaska.
  • Breen AL; International Arctic Research Center University of Alaska Fairbanks Alaska.
  • Chasníková S; Plant Science and Biodiversity Center Slovak Academy of Sciences Institute of Botany Bratislava Slovak Republic.
  • Daanen R; Division of Geological & Geophysical Surveys Fairbanks Alaska.
  • Druckenmiller LA; Alaska Geobotany Center Institute of Arctic Biology & Department of Biology and Wildlife University of Alaska Fairbanks Alaska.
  • Ermokhina K; Earth Cryosphere Institute Tyumen Scientific Center Russian Academy of Sciences, Siberian Branch Tyumen Russia.
  • Forbes BC; A.N. Severtsov Institute of Ecology and Evolution Russian Academy of Science Moscow Russia.
  • Frost GV; Arctic Center University of Lapland Rovaniemi Finland.
  • Geml J; Alaska Biological Research, Inc. Fairbanks Alaska.
  • Kaärlejarvi E; Naturalis Biodiversity Center CR Leiden The Netherlands.
  • Khitun O; Department of Ecology and Environmental Sciences Umeå University Umeå Sweden.
  • Khomutov A; Komarov Botanical Institute Russian Academy of Sciences St. Petersburg Russia.
  • Kumpula T; University of Tyumen Tyumen Russia.
  • Kuss P; University of Eastern Finland Joensuu Finland.
  • Matyshak G; Institute of Systematic and Evolutionary Botany University of Zürich Zürich Switzerland.
  • Moskalenko N; Department of Soil Science Lomonosov Moscow State University Moscow Russia.
  • Orekhov P; Earth Cryosphere Institute Tyumen Scientific Center Russian Academy of Sciences, Siberian Branch Tyumen Russia.
  • Peirce J; Earth Cryosphere Institute Tyumen Scientific Center Russian Academy of Sciences, Siberian Branch Tyumen Russia.
  • Raynolds MK; Alaska Geobotany Center Institute of Arctic Biology & Department of Biology and Wildlife University of Alaska Fairbanks Alaska.
  • Timling I; Alaska Geobotany Center Institute of Arctic Biology & Department of Biology and Wildlife University of Alaska Fairbanks Alaska.
Appl Veg Sci ; 22(1): 150-167, 2019 Jan.
Article en En | MEDLINE | ID: mdl-31130818
ABSTRACT
QUESTIONS How do plant communities on zonal loamy vs. sandy soils vary across the full maritime Arctic bioclimate gradient? How are plant communities of these areas related to existing vegetation units of the European Vegetation Classification? What are the main environmental factors controlling transitions of vegetation along the bioclimate gradient? LOCATION 1700-km Eurasia Arctic Transect (EAT), Yamal Peninsula and Franz Josef Land (FJL), Russia.

METHODS:

The Braun-Blanquet approach was used to sample mesic loamy and sandy plots on 14 total study sites at six locations, one in each of the five Arctic bioclimate subzones and the forest-tundra transition. Trends in soil factors, cover of plant growth forms (PGFs) and species diversity were examined along the summer warmth index (SWI) gradient and on loamy and sandy soils. Classification and ordination were used to group the plots and to test relationships between vegetation and environmental factors.

RESULTS:

Clear, mostly non-linear, trends occurred for soil factors, vegetation structure and species diversity along the climate gradient. Cluster analysis revealed seven groups with clear relationships to subzone and soil texture. Clusters at the ends of the bioclimate gradient (forest-tundra and polar desert) had many highly diagnostic taxa, whereas clusters from the Yamal Peninsula had only a few. Axis 1 of a DCA was strongly correlated with latitude and summer warmth; Axis 2 was strongly correlated with soil moisture, percentage sand and landscape age.

CONCLUSIONS:

Summer temperature and soil texture have clear effects on tundra canopy structure and species composition, with consequences for ecosystem properties. Each layer of the plant canopy has a distinct region of peak abundance along the bioclimate gradient. The major vegetation types are weakly aligned with described classes of the European Vegetation Checklist, indicating a continuous floristic gradient rather than distinct subzone regions. The study provides ground-based vegetation data for satellite-based interpretations of the western maritime Eurasian Arctic, and the first vegetation data from Hayes Island, Franz Josef Land, which is strongly separated geographically and floristically from the rest of the gradient and most susceptible to on-going climate change.
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Texto completo: 1 Base de datos: MEDLINE Idioma: En Revista: Appl Veg Sci Año: 2019 Tipo del documento: Article

Texto completo: 1 Base de datos: MEDLINE Idioma: En Revista: Appl Veg Sci Año: 2019 Tipo del documento: Article