The relative importance of nitrogen deposition and climate change in driving plant diversity decline in roadside grasslands

Nitrogen deposition and climate change have been identified as major threats to the biodiversity of semi-natural grasslands. Their relative contribution to recent biodiversity loss is however not fully understood, and may depend on local site conditions such as soil type, which hampers efforts to prevent further decline. We used data from >900 permanent plots in semi-natural grasslands in Dutch roadsides to investigate whether trends in plant diversity and community composition (2004-2020) could be explained by: (1) nitrogen deposition (NH<sub>x</sub> and NO<sub>y</sub>) and climate change (winter degree days and summer drought), (2) the interactive effect of nitrogen deposition and climate change, and (3) the interactive effect of nitrogen deposition and climate change with soil type. Overall we observed a decline in plant diversity and an increased dominance of tall species and grasses. These changes were linked to winter warming, but not to changes in summer drought and nitrogen deposition. The effect of winter warming was more pronounced in areas with higher NO<sub>y</sub> deposition, but was consistent across different soil types. Our results suggest that winter warming will become an important driver of plant diversity loss by altering competitive interactions, which could have major repercussions for other trophic levels and ecosystem services. Future conservation and restoration of grassland biodiversity therefore requires management regimes that are adapted to winter warming.

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Publication Details

Journal
The Science of The Total Environment
Published
2024-10-16
DOI
https://doi.org/10.1016/j.scitotenv.2024.176962
Citations
3
Primary Topic
Plant responses to elevated CO2
Type
article
Field-Weighted Citation Impact
1.80

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article

The relative importance of nitrogen deposition and climate change in driving plant diversity decline in roadside grasslands

W.A. Ozinga, Jeroen Scheper, Wiene Bakker, Toine Morel et al.
3 citations
The Science of The Total Environment
Plant responses to elevated CO2
1.80
article

The relative importance of nitrogen deposition and climate change in driving plant diversity decline in roadside grasslands

W.A. Ozinga, Jeroen Scheper, Wiene Bakker, Toine Morel, Philippine Vergeer
article en
3 citations

Abstract

Nitrogen deposition and climate change have been identified as major threats to the biodiversity of semi-natural grasslands. Their relative contribution to recent biodiversity loss is however not fully understood, and may depend on local site conditions such as soil type, which hampers efforts to prevent further decline. We used data from >900 permanent plots in semi-natural grasslands in Dutch roadsides to investigate whether trends in plant diversity and community composition (2004-2020) could be explained by: (1) nitrogen deposition (NH<sub>x</sub> and NO<sub>y</sub>) and climate change (winter degree days and summer drought), (2) the interactive effect of nitrogen deposition and climate change, and (3) the interactive effect of nitrogen deposition and climate change with soil type. Overall we observed a decline in plant diversity and an increased dominance of tall species and grasses. These changes were linked to winter warming, but not to changes in summer drought and nitrogen deposition. The effect of winter warming was more pronounced in areas with higher NO<sub>y</sub> deposition, but was consistent across different soil types. Our results suggest that winter warming will become an important driver of plant diversity loss by altering competitive interactions, which could have major repercussions for other trophic levels and ecosystem services. Future conservation and restoration of grassland biodiversity therefore requires management regimes that are adapted to winter warming.

The Science of The Total EnvironmentVol. 955
Rijksmuseum (NL), Wageningen University & Research (NL)
Rijkswaterstaat
Climate action
Openalex Percentile: Top 13%
Plant responses to elevated CO2
1.80
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