The relationship between plant species richness and soil pH vanishes with increasing aridity across Eurasian dry grasslands : научное издание

Описание

Тип публикации: статья из журнала

Год издания: 2017

Идентификатор DOI: 10.1111/geb.12549

Ключевые слова: Alpha diversity, diversity–environment relationship, dry grassland, macroecology, plant species richness, precipitation, semi-arid ecosystem, soil chemistry, soil pH, steppe

Аннотация: Aim: Soil pH is considered an important driver of fine-scale plant species richness in terrestrial ecosystems. However, it is unclear to what extent this relationship is influenced by precipitation, which often directly affects both soil pH and species richness. We asked: (1) what is the relationship between fine-scale vascular plaПоказать полностьюnt species richness and soil pH in regions with different levels of precipitation and (2) what are the relative effects of soil pH and precipitation on species richness?. Location: Dry grasslands in eight regions of northern Eurasia. Methods: Species richness and soil pH were measured in 1055 10 m × 10 m plots and precipitation values were derived from global datasets. Relationships between variables were explored using general linear models, mixed-effect models and partial regressions. Variation partitioning was used to assess the relative effect of each predictor on species richness. Results: In wetter regions, soil pH range was broader, mean species richness was higher and the richness–pH relationship was unimodal. In drier regions, mean soil pH was higher and its range narrower, species richness was on average lower and less variable, and the richness–pH relationship was negative or absent. The richness–pH relationship persisted after controlling for the effect of precipitation, but precipitation, uniquely or together with soil pH, explained more variation in species richness in most regions than did pH alone. Main conclusions: The relationship between plant species richness and soil pH in dry grasslands changes from unimodal, through negative, to none with decreasing regional precipitation in Eurasia. However, it seems that the species richness–soil pH relationship in dry grasslands over broad areas is substantially influenced and confounded by precipitation either indirectly, by shortening and shifting the pH gradient, or directly, by decreasing the negative effects of drought stress on richness. © 2016 John Wiley & Sons Ltd

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Издание

Журнал: Global Ecology and Biogeography

Выпуск журнала: Vol. 26, Is. 4

Номера страниц: 425-434

ISSN журнала: 1466822X

Издатель: Blackwell Publishing Ltd

Персоны

  • Palpurina S. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic)
  • Wagner V. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic)
  • von Wehrden H. (Institute of Ecology, Faculty of Sustainability and Centre of Methods, Leuphana University Lüneburg, Scharnhorststrasse 1, Lüneburg, Germany)
  • Hájek M. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic)
  • Horsák M. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic)
  • Brinkert A. (Institute of Landscape Ecology, University of Münster, Heisenbergstrasse 2, Münster, Germany)
  • Hölzel N. (Institute of Landscape Ecology, University of Münster, Heisenbergstrasse 2, Münster, Germany)
  • Wesche K. (Senckenberg Museum of Natural History Görlitz, Görlitz, Germany, German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Deutscher Platz 5e, Leipzig, Germany)
  • Kamp J. (Institute of Landscape Ecology, University of Münster, Heisenbergstrasse 2, Münster, Germany)
  • Hájková P. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic, Department of Vegetation Ecology, Institute of Botany, The Czech Academy of Sciences, Lidická 25/27, Brno, Czech Republic)
  • Danihelka J. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic, Department of Vegetation Ecology, Institute of Botany, The Czech Academy of Sciences, Lidická 25/27, Brno, Czech Republic)
  • Lustyk P. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic)
  • Merunková K. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic)
  • Preislerová Z. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic)
  • Kočí M. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic)
  • Kubešová S. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic, Department of Botany, Moravian Museum, Hviezdoslavova 29a, Brno, Czech Republic)
  • Cherosov M. (Institute for Biological Problems of Cryolithozone, Siberian Branch of the Russian Academy of Sciences, Lenin Ave 41, Yakutsk, Russian Federation, Institute of Natural Sciences, North-Eastern Federal University Named After M.K. Ammosov, Kulakovsky Str 48, Yakutsk, Russian Federation)
  • Ermakov N. (Central Siberian Botanical Garden, Russian Academy of Sciences, Zolotodolinskaya 101, Novosibirsk, Russian Federation)
  • German D. (Department of Biodiversity and Plant Systematics, Centre for Organismal Studies (COS) Heidelberg, Heidelberg University, Im Neuenheimer Feld 345, Heidelberg, Germany, South-Siberian Botanical Garden, Altai State University, Lenin Str. 61, Barnaul, Russian Federation)
  • Gogoleva P. (Institute of Natural Sciences, North-Eastern Federal University Named After M.K. Ammosov, Kulakovsky Str 48, Yakutsk, Russian Federation)
  • Lashchinsky N. (Central Siberian Botanical Garden, Russian Academy of Sciences, Zolotodolinskaya 101, Novosibirsk, Russian Federation)
  • Martynenko V. (Institute of Biology, Ufa Scientific Center, Russian Academy of Sciences, Prosp. Oktyabrya 69, Ufa, Bashkortostan, Russian Federation)
  • Chytrý M. (Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, Czech Republic)

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