The influence of tree‐scale and ecosystem‐scale factors on epiphytic lichen communities across a long‐term retrogressive chronosequence

• Published in: Journal of Vegetation Science
• Main Authors: Asplund, Johan, Sandling, Aron, Kardol, Paul, Wardle, David A.
• Other Authors: Halvorsen, Rune, Swedish Research Council, Wallenberg Scholars award
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2013
• Subjects: Plant Science; Ecology; Northern Sweden
• Online Access: http://dx.doi.org/10.1111/jvs.12149; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fjvs.12149; https://onlinelibrary.wiley.com/doi/pdf/10.1111/jvs.12149

Abstract Questions We tested the relationship between total cover, species richness and composition of epiphytic lichens on trunks of Betula pubescens and ecosystem retrogression (i.e. prolonged absence of major disturbance). We then investigated how the relationships changed when also accounting for tree‐scale factors (aspect, height and bark characteristics) and ecosystem‐scale factors (e.g. light transmission, tree species diversity and soil fertility). Location Thirty forested islands in northern Sweden differing in fire history, which collectively represent a retrogressive chronosequence spanning ca. 5000 yr. Results Total lichen cover responded negatively to long‐term absence of major disturbance, but only at exposed positions on the tree trunk, indicating that lichen cover on substrates with more favourable microclimates is less susceptible to environmental change at the ecosystem scale. Further, although there was no overall effect of island size on lichen species richness, we did find a significant interactive effect between island size and height on trunk on species richness. This emerged because species richness decreased with retrogression for lichen communities at breast height, but showed a hump‐shaped response to retrogression at the trunk base. Shifts in ecosystem properties with retrogression explained some of the variation in lichen community composition, but most of the variation could be explained by tree‐scale factors, notably height on the trunk. Conclusions While it has frequently been shown that lichens increase in abundance and richness during the first two or three centuries of succession, our results highlight that over a much longer time scale, encompassing soil aging and declining soil fertility, the lichen flora can be negatively affected. However, these effects are heavily mediated by tree‐scale factors. These changes in the lichen community may be of potential importance for ecosystem processes and higher trophic level interactions driven by lichen communities.