Literature DB >> 24012785

Is Erica tetralix abundance on wet heathlands controlled by nitrogen deposition or soil acidification?

Christian Damgaard1, Morten Strandberg, Søren Munch Kristiansen, Knud Erik Nielsen, Jesper L Bak.   

Abstract

Erica tetralix is the key species on NW European wet heathlands, where it is often found to be the dominating plant species. Consequently, it is of considerable concern that the species has decreased significantly in cover from 28% to 18% over a six-year period. In order to understand the underlying causes, a structural equation modeling (SEM) approach was applied on ecological data from 1130 wet heathland plots. Both atmospheric N deposition and soil acidification were included in the SEM. The most important causal effect revealed by the SEM was a significant negative effect of N deposition on the cover of E. tetralix, whereas soil acidity tended to have a negative effect of relatively less importance. There was no significant effect of N deposition on soil pH, which indicates that there are no major indirect effects of N deposition on the cover of E. tetralix mediated by soil acidification.
Copyright © 2013 Elsevier Ltd. All rights reserved.

Entities:  

Keywords:  Atmospheric N deposition; Ecosystem processes; Erica tetralix; Soil acidification; Wet heathlands

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Year:  2013        PMID: 24012785     DOI: 10.1016/j.envpol.2013.07.047

Source DB:  PubMed          Journal:  Environ Pollut        ISSN: 0269-7491            Impact factor:   8.071


  1 in total

1.  Long-term and realistic global change manipulations had low impact on diversity of soil biota in temperate heathland.

Authors:  Martin Holmstrup; Christian Damgaard; Inger K Schmidt; Marie F Arndal; Claus Beier; Teis N Mikkelsen; Per Ambus; Klaus S Larsen; Kim Pilegaard; Anders Michelsen; Louise C Andresen; Merian Haugwitz; Lasse Bergmark; Anders Priemé; Andrey S Zaitsev; Slavka Georgieva; Marie Dam; Mette Vestergård; Søren Christensen
Journal:  Sci Rep       Date:  2017-01-25       Impact factor: 4.379

  1 in total

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