4.7 Article

Compositional shifts of alpine plant communities across the high Andes

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GLOBAL ECOLOGY AND BIOGEOGRAPHY
卷 -, 期 -, 页码 -

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WILEY
DOI: 10.1111/geb.13721

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climate change; community thermal scores; latitude; mountains; species richness; thermophilization; vegetation dynamics

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The study focuses on vegetation changes in the High Andes region in response to climate change. It reveals a decrease in vegetation cover, an increase in species richness, and a shift towards species with wider thermal niches. The findings highlight the importance of considering large-scale patterns of vegetation changes in the Andes when predicting the effects of global warming.
Aim: Climate change is transforming mountain summit plant communities worldwide, but we know little about such changes in the High Andes. Understanding large-scale patterns of vegetation changes across the Andes, and the factors driving these changes, is fundamental to predicting the effects of global warming. We assessed trends in vegetation cover, species richness (SR) and community-level thermal niches (CTN) and tested whether they are explained by summits' climatic conditions and soil temperature trends.Location: High Andes.Time period: Between 2011/2012 and 2017/2019.Major taxa studied: Vascular plants.Methods: Using permanent vegetation plots placed on 45 mountain summits and soil temperature loggers situated along a similar to 6800 km N-S gradient, we measured species and their relative percentage cover and estimated CTN in two surveys (intervals between 5 and 8 years). We then estimated the annual rate of changes for the three variables and used generalized linear models to assess their relationship with annual precipitation, the minimum air temperatures of each summit and rates of change in the locally recorded soil temperatures.Results: Over time, there was an average loss of vegetation cover (mean = -0.26%/yr), and a gain in SR across summits (mean = 0.38 species m(2)/yr), but most summits had significant increases in SR and vegetation cover. Changes in SR were positively related to minimum air temperature and soil temperature rate of change. Most plant communities experienced shifts in their composition by including greater abundances of species with broader thermal niches and higher optima. However, the measured changes in soil temperature did not explain the observed changes in CTN.Main conclusions: High Andean vegetation is changing in cover and SR and is shifting towards species with wider thermal niche breadths. The weak relationship with soil temperature trends could have resulted from the short study period that only marginally captures changes in vegetation through time.

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