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- W2158596574 abstract "Blanket bog—characterized by an almost complete landscape covering of undecayed organic peat—is a highly distinctive biome restricted to regions that experience hyperoceanic climatic conditions. Bioclimatic modelling suggests there will be a dramatic shrinkage of the available climatic space for blanket bogs with only a few, restricted areas of persistence. Blanket bog is a highly distinctive biome restricted to disjunct hyperoceanic regions. It is characterized by a landscape covering of peat broken only by the steepest slopes1. Plant and microbial life are adapted to anoxia, low pH and low nutrient availability. Plant productivity exceeds soil organic matter decomposition, so carbon is sequestered over time. Unique climatic requirements, including high year-round rainfall and low summer temperatures2, make this biome amenable to bioclimatic modelling. However, projections of the fate of peatlands in general, and blanket bogs in particular, under climate change have been contradictory3,4,5,6,7. Here we use a simple, well-founded global bioclimatic model8, with climate-change projections from seven climate models, to indicate this biome’s fate. We show marked shrinkage of its present bioclimatic space with only a few, restricted areas of persistence. Many blanket bog regions are thus at risk of progressive peat erosion and vegetation changes as a direct consequence of climate change. New areas suitable for blanket bog are also projected, but these are often disjunct from present areas and their location is inconsistently predicted by different climate models." @default.
- W2158596574 created "2016-06-24" @default.
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- W2158596574 date "2012-09-02" @default.
- W2158596574 modified "2023-10-07" @default.
- W2158596574 title "Blanket peat biome endangered by climate change" @default.
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- W2158596574 doi "https://doi.org/10.1038/nclimate1672" @default.
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