Experimental evidence for disturbance as key to the conservation of dune grassland
Introduction
Humans have been attracted to coastal areas for millennia, exploiting different resources (e.g., fishery, fuel wood, construction material, shipping) as well as settling in the areas, cultivating them and more recently using them for recreation, tourism and military training (Everard et al., 2010, UNEP, 2006). Still, coastal landscapes are often controlled by natural processes (e.g., Kumler, 1993) and have high conservation value compared to many inland ecosystems. Therefore, national and international conservation legislation initiatives have been proposed to protect near-natural coastal ecosystems against further anthropogenic pressures (UNEP, 2006).
Dunes comprise an important part of coastal ecosystems and the mosaic-like vegetation structure is maintained primarily by strong, natural processes such as strong winds, sand deposition and coastal erosion (Maun, 2009, Warming, 1909). The outcome is a directional successional gradient from bare sand over species-poor pioneer communities to species-rich herb communities and finally towards leached and stabilized dunes with species-poor dwarf-shrub heath (Maun, 2009). From an evolutionary perspective dune vegetation is adapted to recurrent disturbances (Brunbjerg et al., 2012a) and without these shrubs and trees will eventually invade with loss of typical dune species (Aptroot et al., 2007).
Over longer time scales, coastal dune formation and persistence is related to climatic variability as well as exploitation causing a sparser and less resistant vegetation cover. Cold periods have caused more severe storms and this in turn has renewed the coastal dune habitats because of increasing sand mobilization (Clarke and Rendell, 2011, Provoost et al., 2011). Throughout European history, utilization of dune plants for building materials, utensils etc. as well as livestock grazing intensified the disturbance regime in coastal dunes (Jensen, 1994, Plassmann et al., 2010; reviewed in Provoost et al., 2011). During the last century these disturbances have diminished or ended. Furthermore, initiatives to prevent sand drift (e.g., establishment of dune plantations, planting of Ammophila arenaria L. Link) to protect agricultural areas, infrastructure and habitations within the last 100–200 years have led to dune stabilization (Gilbertson et al., 1999, Jensen, 1994, Provoost et al., 2011).
Over the past 70 years nitrogen (N) deposition caused by burning of fossil fuels, increasing density of livestock and use of manure may also have had an effect on dune vegetation (Bobbink et al., 2011). Critical N loads for dune grassland have been estimated to be 8–15 kg N ha−1 year−1 (Bobbink et al., 2011) and despite recent decreases in N loads (EMEP, 2010), current N-deposition in most western European countries is within or above this range. N-deposition has been found to increase biomass and decrease species richness in fixed coastal dunes and grasslands (e.g., Jones et al., 2004, Stevens et al., 2004). Furthermore, N-deposition potentially changes community composition as eutrophication and acidification may cause selective local extinction of sensitive species (Greven, 1992, McClean et al., 2011).
The interaction of disturbance and productivity has been shown to play a key role in community assembly and the maintenance of species diversity in local plant communities (Ejrnæs et al., 2006, Huston, 1994). It is argued that disturbances such as grazing and sand drift may mitigate the negative effects of N-deposition by limiting vigorous plant growth and creating gaps for re-colonization of subordinate species (Bakker and Olff, 2003, Jutila and Grace, 2002). Disturbance may affect not only species composition, but also phylogenetic community structure. Thus, disturbance has been found to cause phylogenetic clustering in ploughed fields as compared to abandoned fields (Dinnage, 2009), i.e. species in disturbed areas are more closely related than expected by chance due to shared phylogenetically conserved traits contributing to disturbance tolerance. Furthermore, clustering has been found to be the most pronounced phylogenetic signal in coastal dunes in Denmark and linked to anthropogenic disturbances (Brunbjerg et al., 2012a). We therefore expect that disturbance will change species composition and increase richness as well as the relatedness of species in the community.
In this study we examined the effect of N-addition and disturbance on species diversity, composition and productivity in a controlled field experiment along a natural ecological gradient in dry dune grassland Denmark. The study habitat is a priority habitat of the European Habitats Directive (European Commission, 2007) and knowledge about its vegetation responses to changes in nutrient availability and disturbance is paramount to its conservation. We hypothesized that the three types of disturbances (simulated grazing, trampling and blowouts) would cause an increase in species richness and reduce plant biomass while N-addition would cause a decline in species richness and an increase in plant biomass. Furthermore, species composition was expected to change in response to treatments.
Section snippets
Study site
Our study site was the near-natural, species-rich dune system “Tornby Klit” in Northern Jutland, Denmark (57°32′N, 9°54′E, Fig. 1). The study area is dominated by dry dune grassland on moderately calcareous sand with interspersed shrubs of Salix spp., Hippophäe rhamnoides L. and Rosa spp. Dominant plant species are Poa pratensis L., Festucaarenaria L., Galium verum L., Plantago lanceolata L., A. arenaria L. Link, Hypnum cupressiforme Hedw. and Camptothecium lutescens Hedw. Physical disturbance
Environmental variation
Mean temperature in May 2010 ranged from 9.4 °C to 13.0 °C across sites, while mean soil water sensor readings ranged from −0.03 to 0.06 which is equivalent to 0.00–0.06 volumetric water content (m3 m−3) (Onset Computer Corporation, 2003). Colonization started soon after the disturbance treatment in blowouts and newly arrived species could already be recognized two months after the initial treatment (Appendix E). The most frequent early colonizers were P. lanceolata (most likely new seedlings),
Succession and dynamics
Despite the restriction of our study to only encompass relatively stable dune grassland we found a clear successional gradient. Lower pH values indicated increasingly leached soils characteristic of older dunes having lost initial base cations from the deposited sand (Warming, 1909). Decreasing pH corresponded with increasing soil organic matter. In contrast to dune succession on acidic sand with poor pH-buffering capacity, where leaching and acidification leads to infertile dune heathlands (
Acknowledgements
We thank Roar Poulsen, Bettina Nygaard and Bjarke Huus for valuable help on selecting the research area; Ako Mirza, Jakob Thyrring, Jens Brunbjerg, Lars Dalby, Ditte Barild, Dagmar Andersen, Mette Odgaard, Wolf Eiserhardt, Anders Juel, Peder Bøcher, Sara Andersen, Marie Thomsen, Kamonnate Srithi and Jantrararuk Tovaranonte for assistance on field work; Roar Poulsen and Mats Gustafsson for help with lichen and bryophyte identification. The European Research Council (ERC-2012-StG-310886-HISTFUNC
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