Most species distribution models assume a close link between climatic conditions and species distributions. Yet, we know little about the link between species' geographical distributions and the sensitivity of performance to local environmental factors. We studied the performance of three bryophyte species transplanted at south- and north-facing slopes in a boreal forest landscape in Sweden. At the same sites, we measured both air and ground temperature. We hypothesized that the two southerly distributed species Eurhynchium angustirete and Herzogiella seligeri perform better on south-facing slopes and in warm conditions, and that the northerly distributed species Barbilophozia lycopodioides perform better on north-facing slopes and in relatively cool conditions. The northern, but not the two southern species, showed the predicted relationship with slope aspect. However, the performance of one of the two southern species was still enhanced by warm temperatures. An important reason for the inconsistent results can be that microclimatic gradients across landscapes are complex and influenced by many climate-forcing factors. Therefore, comparing only north- and south-facing slopes might not capture the complexity of microclimatic gradients. Population growth rates and potential distributions are the integrated results of all vital rates. Still, the study of selected vital rates constitutes an important first step to understand the relationship between population growth rates and geographical distributions and is essential to better predict how climate change influences species distributions.
Citation: Dahlberg CJ, Ehrlén J, Hylander K (2014) Performance of Forest Bryophytes with Different Geographical Distributions Transplanted across a Topographically Heterogeneous Landscape. PLoS ONE 9(11): e112943. https://doi.org/10.1371/journal.pone.0112943
Editor: Daniel Ballhorn, Portland State University, United States of America
Received: June 27, 2014; Accepted: October 14, 2014; Published: November 11, 2014
Copyright: © 2014 Dahlberg et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Data Availability: The authors confirm that all data underlying the findings are fully available without restriction. Data available from the Dryad Digital Repository: http://doi.org/10.5061/dryad.37104.
Funding: This work was supported by Strategic Research Programme EkoKlim (http://www.zoologi.su.se/ekoklim). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
The niche of a species can be thought of as the environmental conditions where population growth rate is positive –. Population growth rate is determined by the vital rates (survival, growth and reproduction) of individuals, which in turn are influenced by the environmental conditions –. The potential geographic distribution of a species will thus be determined by the environmental conditions that influence vital rates, i.e. the performance of individuals. Among the environmental variables that have rendered most focus in recent work on species distributions are various climatic conditions. Most species distribution models are based on the presence or absence of species and use coarse scale climatic variables , . However, we still know little about how population growth rates and the performance of individuals depend on local climatic conditions –. Yet an improved understanding of individual and population responses to local climatic conditions across species ranges should enhance our ability to predict the response of species to future climate change.
The density of many species is lower towards its range margins due to an overall lower quality in habitat or more sparse distribution of suitable habitat patches , . This implies that populations towards their range margins might become more restricted to habitat patches with locally favorable microclimate , . According to this reasoning, differences in performance that relate to variation in local climate should be more accentuated towards the range margins. In fact, the presence of species at favorable microclimatic sites far away from their main distributions is one of the strongest cases for climate as a regulating factor for species distributions . Climate has been assumed to directly influence species distributions, especially towards cold or dry conditions. In such situations, the asymmetric abiotic stress limitation (AASL) hypothesis predicts the occurrence of a species to be limited by its physiological tolerance due to stressful abiotic factors . This hypothesis is based on the assumption that the physiological tolerance of individuals influence their fitness, and thus the distribution of species , . Consequently, studies of the relationship between individual performance and climate variables at species range margins are essential to understand how climate regulates distribution patterns, and how climate change will lead to future range shifts.
There is often a relatively weak correlation between the local climate, which organisms experience, and the regional climate . Large altitudinal variation and complex terrain can lead to considerable variation in microclimate across a landscape , , . One factor leading to microclimatic variation is aspect; mountain slopes facing the equator receive more incoming solar radiation than slopes facing the poles –. Therefore, equator-ward slopes are often both warmer and drier and have larger temperature fluctuations than pole-ward slopes –. As a consequence, north- and south-facing slopes are potentially good candidates for studies on microclimatic gradients and have also shown to influence species composition . However, the interactions of many climate-forcing factors (e.g. distance to sea, canopy cover) can lead to complex microclimatic patterns and obscure the climate regulating role of aspect , . Thus, to understand the role of climate for individual performance, we need to address the local scale where microclimatic conditions correspond to the limits of a species realized niche.
The aim with this study was to explore how performance of individuals in three bryophyte species with different geographical distributions is influenced by local variation in microclimate across a topographic heterogeneous landscape. Bryophytes are particularly suitable for studies of performance and distribution patterns in relation to microclimatic gradients for several reasons. First, they closely depend on the microclimate of their immediate surroundings due to their small size and poikilohydric state; the latter resulting in that tissue water content is similar to the surrounding environment –. Secondly, bryophytes are common and occur in a broad range of habitats worldwide, often dominating the ground cover in boreal and boreonemoral forests –. Finally, many bryophyte species are easy to transplant, making them an ideal experimental system , . Despite these advantages, bryophytes remain relatively underrepresented in ecological studies.
We investigated the relationships between individual performance of three transplanted bryophyte species, in terms of growth, vitality and capsule maturation, and environmental conditions, in terms of local temperature and slope aspect. We hypothesized that the performance of transplants would reflect the general distribution pattern of each species. Two southerly distributed species (Eurhynchium angustirete and Herzogiella seligeri) were therefore hypothesized to perform better at south-facing slopes and in warm conditions, whereas a northerly distributed species (Barbilophozia lycopodioides) was hypothesized to perform better at north-facing slopes and in relatively cool microclimatic positions.
Materials and Methods
The study area is located in central Sweden adjacent to the Bothnian sea in the county of Ångermanland (Figure 1; between the latitudes 62°50′ and 63°12′N). It extends 73 km from east to west and 42 km from north to south.
Circles indicate north-facing slopes and stars indicate south-facing slopes. Background overview maps: © Lantmäteriet Gävle 2012 (Permit i2012/899).
The area is characterized by hills reaching heights of about 100 to 200 meters above the valley bottoms. The altitude reaches 150–300 m a.s.l. by the coast and increases to 350–470 m a.s.l. further inland. The soil material is sandy/loamy/silty tills forming mainly podzolic soils on top of bedrock of mostly gneiss. The mean temperature for July is 15.6°C and the annual mean precipitation 671 mm by the city of Kramfors (mean values from 1961–1990; ). The area belongs phytogeographically mainly to the middle boreal subzone, and by the coast to the southern boreal subzone , . In these subzones, many species have their northern range margin and are found at sites with locally favorable conditions, e.g. on south-facing mountain slopes , .
Study design and data collection
The sites were selected with the help of local floras , , aerial photos, topographic maps and field visits. We selected 15 south-facing and 18 north-facing slopes (in total 33 slopes), stratified according to distance to the sea. Each slope should possess forest of at least 50 years of age (often much more), dominated or co-dominated by Norway spruce (Picea abies), with more or less closed canopy cover and positioned on mesic soil. In such forests, we selected a 4×4 meter site on each slope. Sites were stratified for variation in altitude, and selected to be situated at a minimum of 10 meters from younger forest stands, open ground and streams that could influence the microclimate. For the same reason, near vicinity to rocky outcrops was avoided. Most of the sites were situated in forests solely dominated by P. abies, but at some sites birch (Betula spp.) or Scots pine (Pinus sylvestris) co-dominated the tree layer together with P. abies.
We transplanted three species to all selected sites. The two mosses Herzogiella seligeri and Eurhynchium angustirete possess a southern distribution in Sweden and are both common south of the river Dalälven, but H. seligeri also occur along the coast northward into the focal study landscape. The foliose liverwort Barbilophozia lycopodioides is common north of the river Dalälven and thus occupies a more northern distribution in Sweden, but it also has scattered occurrences in southern Sweden , . We collected the transplant material in April 2011 from localities within the main ranges of the species. Material of H. seligeri and E. angustirete was gathered in the hemiboreal subzone ,  330 km south of the transplantation experiment (Uppland, Erken, Lat 59°50′6.30″; Long 18°30′15.03″). The growing season is on average 20 days longer at this collection site compared to the study area, while the precipitation is similar (, ). Eurhynchium angustirete grew on mesic soil in a flat spruce forest with vegetation dominated by low herbs, whereas H. seligeri grew on decaying logs of spruce in the same forest. Material of B. lycopodioides was collected in a spruce forest on a north-facing slope within the same landscape as the experiment (Ångermanland, Latberget; Lat 62°56′4.96″; Long 17°42′19.74″). When gathered, both E. angustirete and B. lycopodioides were carefully removed from the soil while for H. seligeri pieces of wood were retained for all transplants. Before transplanting, the material was stored in carpets on moist forest floor in the study area, sheltered from direct sunlight.
At the start of the experiment in April to May 2011, we removed the vegetation down to the topsoil and planted a total of nine transplants (three transplants per species) at each site. We placed the transplants directly on the ground and attached them using thin wooden sticks at ground with relatively small slope angles, and avoided placing them near large boulders or hollows. Transplants were separated by a distance of about 20 cm. They were about 10 cm in diameter for E. angustirete, 5 cm in diameter for B. lycopodiodes and 3 cm for H.seligeri. Differences in transplant size between species were mainly due to differences in the availability of planting material.
To measure air and ground temperature, we installed two temperature loggers (ibuttons, DS1922) at each site. One logger was placed at the ground level underneath a moss-patch inside two plastic zip-bags and the other one was attached to the top of a wooden pole covered by a plastic cup, one meter above the ground. The temperature was recorded every half hour during the experimental period.
We extracted twelve different microclimatic variables from the temperature data for the period 29th of May until 28th of September 2011 (Table S1). Mean temperature and the mean diurnal temperature range were calculated for both air and ground temperature. Additionally, we derived the 5th and 95th percentiles of the minimum and maximum air and ground temperatures . The 5th percentile of the minimum temperatures and the 95th percentile of the maximum temperatures were used to represent extreme cold and extreme warm conditions, respectively. The 95th percentile of the minimum temperatures and the 5th percentile of the maximum temperatures represent mild minimum and mild maximum temperatures, respectively. A high mild minimum temperature indicates that most nights of a site generally remain relatively warm, whereas a high mild maximum temperature indicates that most of the days remain relatively warm .
We retrieved sixteen additional environmental variables: altitude, basal area, broadleaved trees, canopy cover, distance to open ground, distance to the sea, ground vegetation, pH litter, pH soil, productivity (assessed using vegetation types, see below), relative elevation, shrubs, slope, solar radiation, tree age and tree height. Solar radiation (direct radiation plus diffuse radiation in kWh/m2) between the 29th of May and the 28th of September of 2011 was calculated for each site by the points solar radiation tool (spatial analyst extension), using default values (the uniform sky model, transmittivity = 0.5, proportion of diffuse radiation = 0.3) in ArcGIS Desktop 10.0. The input for the calculations was a digital elevation model (DEM) with a grid of 50×50 meter cells provided by Lantmäteriet (the Swedish mapping, cadastral and land registration authority, www.lantmateriet.se). Distance to the sea and distance to open ground was estimated by the shortest distance from the site midpoints to the coast (Figure 1) and to open ground respectively, using topographic maps and aerial photos in ArcGIS Desktop 10.0. As an estimate of productivity, we classified the vegetation within each site into one of six categories representing an increasing gradient in productivity (corresponding to the standard method of Hägglund & Lundmark ): (1) dwarf-shrubs Calluna vulgaris and Empetrum nigrum; (2) dwarf-shrub Vaccinium vitis-idaea; (3) dwarf-shrub V. myrtillus; (4) low herbs and dwarf-shrubs (V. myrtillus); (5) low herbs or (6) tall herbs. Nomenclature follows Mossberg and Stenberg  for vascular plants, Hill et al.  for mosses and Damsholt  for liverworts. See Table S1 and Text S1 for definitions and data collection methods on the remaining environmental variables, since they were only used to characterize north- and south-facing slopes and not included in the performance analyses (see below).
We calculated growth as the change in transplant size over the study for B. lycopodioides and E. angustirete. Transplant size was estimated from photographs taken at the start (30th of April until 28th of May 2011) and end of the experimental period (29th of September until 7th of October 2011), and placing a ruler along each transplant. We used the program GIMP 2.6.11 to delimit polygons of the living parts in each transplant photograph. We did not study growth of H. seligeri because it was restricted to grow on available pieces of wood. For all species we estimated the transplant vitality of the living parts (of the gametophyte) at the end of the experimental period according to the following scale: (1) <50% of the transplant was freshly green (vigorous); (2) 50–<95% of the transplant was freshly green; (3) ≥95% of the transplant was freshly green. The remaining parts of the transplants were brownish/pale and therefore not judged as vital. These categories were assumed to reflect the overall condition of each transplant, and to relate to vital rates such as growth and survival . As a measurement of reproduction, we recorded the number of immature capsules at the first occasion and the capsules that had matured at the second occasion in the monoicous H. seligeri. We did not record more than a handful sporophytes on the two dioicous species B. lycopodioides and E. angustirete.
All necessary permits were obtained for the described field studies. Permissions were granted from the County administrative board of Västernorrland and from the landowners (Kramfors and Sollefteå municipalities, SCA, the Church of Sweden and private landowners). The field studies did not involve endangered or protected species.
We examined among-site variation in six performance- variables: 1–2) mean growth and vitality of B. lycopodioides, 3–4) mean growth and vitality of E. angustirete, and 5–6) mean vitality and capsule maturation (proportion of capsules that matured) of H. seligeri. Growth and vitality of E. angustirete and vitality of H. seligeri were log-transformed before statistical analyses in order to improve model performance.
We tested if the six performance variables differed between north- and south facing slopes. Growth and vitality of E. angustirete and vitality of H. seligeri were normally distributed and t-tests were used. For B. lycopodioides vitality and H. seligeri capsule maturation, we used Wilcoxon rank-sum test because the compared groups did not conform to the assumption about normality. The Wilcoxon test of H. seligeri capsule maturation was performed with the proportions of the pooled number of capsules that matured per site. We used Bonferroni-adjusted p-values for the two tests on each species. Moreover, we compared environmental variables between north- and south-facing slopes. First, we performed a comparison of all measured environmental variables between the slope aspects by using a MANOVA with Pillai's trace test. Since we found an overall difference among aspect groups in environmental variables, we continued to explore differences among individual variables. For distance to open ground, distance to the sea, pH soil, productivity, tree age, slope, broadleaved trees, ground vegetation and shrubs we performed Wilcoxon rank-sum tests because the compared groups were not normally distributed. For the other environmental variables, we used Welch's t-tests. Canopy cover was arcsine-transformed before tests. Additionally, the relationships among the environmental variables were visualized through a PCA analysis using the package vegan (Figure S1). The variables were centered and scaled to unit variance. Otherwise, default settings were used.
To select microclimatic variables for models of bryophyte performance, we examined covariance patterns using Pearson's product-moment correlations. Many of the microclimatic variables were inter-correlated (Table S3). To keep problems associated with collinearity low while providing a reasonable representation of microclimatic variation, we chose the group of four variables with the lowest maximum correlation coefficient. The microclimatic variables selected according to these criteria were 1) extreme cold air temperature, 2) mild maximum air temperature, 3) extreme warm air temperature, and 4) diurnal ground temperature range. In addition to the microclimatic variables we included four variables that were assumed to influence individual performance: distance to the sea, distance to open ground, solar radiation and productivity. Distance to sea and distance to open ground were both log-transformed, since we might suspect that their influence on climatic conditions increases exponentially with decreasing distance , . Among the eight environmental variables included in the analyses, the highest correlation coefficient was 0.65 (Pearson's product-moment correlation; Table S4).
To examine how the six performance variables did depend on these eight environmental variables, we used lasso regression (‘least absolute shrinkage and selection operator’; glmnet package in R). We performed lasso regression with gaussian error terms for the growth and vitality variables, whereas lasso regression with binomial error term was used for capsule maturation. For the latter regression, we used count data (number of capsules that matured out of total per site) instead of proportions. Lasso regression method works through shrinkage of the regression coefficients by using a cap on the sum of the absolute value of all the coefficients. In lasso, these coefficients are often shrunk exactly to zero, which is equal to removal of explanatory variables from a regression model. The glmnet package uses the penalty λΣj|βj| to residual sum of square instead of, but equivalent to, constraining the sum of coefficients , . Cross-validation with number of folds equal to sample size was performed to find the λ-value that minimized the residual sum of squares. Regression shrinkage methods such as lasso and ridge selection have been shown to perform better than subset selection using BIC when there are few observations per predictor –. Also considering the similarity between subset selection and stepwise regression, regression shrinkage methods should therefore be considered when there are few observations per predictor . The residuals of the lasso-models were examined through plotting the corresponding linear regression models, in which they showed no particularly heteroscedasticity or skewness. Lastly, we checked for spatial autocorrelation among the performance variables through Mantel tests. We applied Bonferroni correction on the p-values for the two tests on each species and used proportions for capsule maturation. No spatial autocorrelation was found. From all analyses, samples with missing values were excluded. The analyses were done in R 3.0.2 .
North- vs. south-facing slopes
There was an overall difference in the measured environmental variables between slope aspects (MANOVA, p = 0.015). Not all microclimatic variables did differ between the slopes, despite south-facing slopes receiving more incoming solar radiation than north-facing (Table 1). Largest differences were found for the extreme warm air temperature, the diurnal air temperature, the mild minimum ground temperature and the extreme cold ground temperature. South- and north-facing slopes differed more with regards to ground temperature variables than to air temperature (Figure 2; Table S2). Besides differences in several temperature variables, the south-facing slopes had on average taller trees and higher soil and litter pH than the north-facing slopes (Table S2).
p-values were derived through Welch's t-tests.
The PCA showed that many of the environmental variables were sorted along the north-south gradient. However, many other variables such as distance to the sea and the two minimum air temperatures were orthogonal to the north-south axis (Figure S1).
Performance of the transplants
The northerly distributed liverwort B. lycopodioides increased significantly more in size and had higher vitality at north-facing than at south-facing slopes (Figure 3; Table 2). The optimal lasso regression models of B. lycopodioides included negative effects of solar-radiation on both growth and vitality, while higher productivity resulted in higher vitality (Table 3).
Significant differences (at p<0.05) between the two groups for each species are indicated with the symbols a–b.
In the southern moss E. angustirete, there were no significant differences in growth or vitality between north and south-facing slopes (Figure 3; Table 2). The optimal lasso regression model for growth of E. angustirete included a positive effect of increasing mild maximum air temperature (Table 3), but did not identify any environmental variable related to variation in vitality.
There were no significant differences between north and south-facing slopes in vitality or capsule maturation of the southern moss H. seligeri (Table 2). The optimal lasso regression model identified a positive effect of distance to the sea on vitality of H. seligeri (Table 3). Variation in capsule maturation was not related to any environmental variable.
This study showed that aspect and microclimate were important in explaining the growth of two transplanted bryophyte species. However, the pattern was more complex than simply northern species performing better on northern slopes and in cold sites and southern species performing better on south facing slopes and in warm sites. This complexity may be explained by that not all microclimatic variables differed between aspects (cf. Figure 2; Table S2). Thus, even if the performance of a species is directly regulated by climatic variables it is not necessarily true that it will show different performance at north- vs. south-facing slopes.
Transplant performance of the northern liverwort B. lycopodioides was, as hypothesized, better at north-facing slopes. This is in agreement with this species' distribution pattern, since it has been found to be more abundant at north-facing than at south-facing slopes in the study area . Poor individual growth might be a part of the explanation for low abundance of a species at its range limits, and has been found to coincide with low reproduction of trees at their range margins, and with either low reproduction or low survival of herbs transplanted beyond their altitudinal range limits –. Moreover, increased growth of individuals often leads to both higher survival and increased population growth rate , , .
Since effects of interspecific competition were not important in this study, the poor transplant performance of B. lycopodioides at south-facing slopes indicates that the species occurrences might be limited by abiotic factors, and that south-facing slopes are outside the species fundamental niche. The Lasso-model did not identify any effects of temperature variables on the growth or vitality of B. lycopodioides (Table 3), which imply that other abiotic factors could be important for its distribution pattern in the study area. It is probable that the south-facing slopes also in our study area are drier compared to north-facing, because they have larger temperature fluctuations (Figure 2), which implies less stable moisture conditions . Therefore, it is possible that B. lycopodioides is more limited by drought than by high temperatures per se in this landscape. Also other studies of terrestrial plants in temperate Europe have revealed that climate, in particularly drought, frequently limit species ranges towards the equator , , . Moreover, liverworts are generally considered more drought sensitive compared to mosses , , and consequently favored under moist conditions. Future studies should thus take into account variations in both ground and air humidity which may have as strong or stronger impact than temperatures per se.
One way of testing if a species is in equilibrium with current climatic conditions, and thereby if climatic conditions are range limiting, is to transplant individuals outside its range margins , . For E. angustirete transplanted outside its range, the good performance suggests that most study sites lies within its climatic niche. This would imply that the species distribution is in disequilibrium with current climatic conditions and that microclimatic conditions are not the main limiting factors at the northern range margin of E. angustirete. This would thus represent a different pattern compared to that of several bryophytes in central Europe, which range margins towards colder regions are related to winter isotherms . However, extreme climatic events often have been shown to increase mortality or physiological stress at range margins of different species , . Long-term studies might therefore be necessary to conclude if species ranges are limited by rare climatic conditions, or if other factors, such as dispersal, are limiting. Transplant experiments in which individuals have been placed outside their range margins and performed well, have been carried out also for other species, e.g., forest herbs , . In these studies, the species have been suggested to be dispersal limited and therefore in disequilibrium with climate. However, bryophytes have rather small spores which potentially can be wind-dispersed over long distances . Therefore, dispersal is not likely to be a main limiting factor for bryophytes that often produce spore capsules. It is probable that at least some individual shoots in the often large populations of E. angustirete produce capsules over a growing-season, which would make dispersal limitation less important. Still, a species could be limited by interspecific competition, possibly also in combination with unfavorable environmental conditions such as low temperature or ground pH, thereby limiting its range , , .
Growth and survival of early life-stages in margin populations have been suggested to be important in determining range edges , , . A study in which butterflies were transplanted outside their range margins showed that cool temperatures hampered the development of early life-stages. Therefore, unfavorable climatic conditions were suggested to directly limit the range margins of this species . Further on, although transplanted adults of a crab species survived beyond their range margin, lab experiments suggested that low temperature were still limiting ranges through negative effects on larval development . Analogously, climatic equilibrium could prevail in E. angustirete if climate limit the species range through its impact on early life-stages in spite of that adult transplants grew well.
Even if transplant performance of E. angustirete was relatively good, transplants were growing better at sites with high mild maximum air temperatures, which is in agreement with its geographical distribution towards warmer regions. Although the mild maximum air temperature was higher at south facing slopes, the performance did not significantly differ between north- and south-facing slopes. This could be explained by that also other climate-forcing factors such as altitude are important for the mild maximum air temperature. Furthermore, other temperature variables could influence transplant performance, but not all of them did differ between north- and south-facing slopes (Figure 2). Additionally, water availability could possibly be important for the transplant performance of E. angustirete. The transplants might have been water-saturated and active, and subsequently growing for longer periods at north-facing slopes due to longer lasting moisture. At south facing slopes, they might have been growing faster due to higher daytime temperatures that were closer to their temperature optimum. At the same time, their growth periods were probably shorter at south-facing slopes due to longer drought periods with water deficit. After such drought periods, the transplants should have been able to start growing quickly since E. angustirete is a rather desiccation-tolerant species . This could have contributed to the roughly equal performance at both aspects, and its desiccation-tolerance might explain the relatively high vitality at both aspects in spite of the potentially drier environment at south-facing slopes.
The results for vitality and capsule maturation in H. seligeri suggest that the performance might not be related to its distribution, since also this species performed well on north-facing slopes and had higher vitality further inland which does not coincide with its realized niche. Furthermore, no microclimatic influence on capsule maturation was found.
This study provided equivocal support for that the species geographic distribution patterns reflected their individual performance in relation to microclimatic gradients. The results for B. lycopodioides was consistent with that species with more northern distribution perform better at north-facing slopes. However, both the southern species performed well outside their range and only E. angustirete was significantly affected by microclimate. By understanding climatic influence on all vital rates and, thus, population growth rate at range margins, we should be able to predict the influence of a warming climate on species potential distributions. The complex microclimatic gradients across the landscape make it difficult to rely only on aspect as an explanatory variable for performance. This is particularly important in topographically complex landscapes where larger differences between ground and air temperatures might be suspected. It is important to bear in mind that our study tests hypotheses for the three different species and does not allow any broader inferences regarding differences between northern vs. southern species, or mosses vs. liverworts. Still, well-replicated studies on three different species provide important evidence of that relationships between distributions and environmental factors might be much more complex than often anticipated.
PCA analysis of the environmental variables related to sites. Light-grey points represents north-facing slopes, dark-grey triangles represents south-facing slopes. Black arrows marks environmental variables as follows: A = Altitude (m), Ag = Tree age (years), B = Broadleaved trees (%), Ba = Basal area (m3), C = Canopy cover (%), G = Ground vegetation (cm), H = Tree height (m), N = North-facing slopes, O = Distance to open ground (log(m)), Phl = pH litter, Phs = pH soil, Re = Relative elevation (m), S = South-facing slopes, Se = Distance to the sea (log(km)), Sh = Shrubs (%), Sl = Slope (°), T5maa = Mild maximum air temperature (°C), T5mag = Mild maximum ground temperature (°C), T5mia = Extreme cold air temperature (°C), T5mig = Extreme cold ground temperature (°C), T95maa = Extreme warm air temperature (°C), T95mag = Extreme warm ground temperature (°C), T95mig = Mild minimum air temperature (°C), T95mig = Mild minimum ground temperature (°C), Tma = Mean air temperature (°C), Tmg = Mean ground temperature (°C), Tra = Diurnal air temperature range (°C), Trg = Diurnal ground temperature range (°C), P = productivity.
Environmental variables not included in the performance analyses and microclimatic variables. These are compared between south- and north-facing slopes, for which mean, minimum and maximum values are presented.
Pearson product-moment correlation analyses between the microclimatic variables.
Pearson product-moment correlation analyses between the environmental variables used in lasso regression.
We would like to thank Nikki Vercauteren for assistance in the field and discussions on climatic patterns, and Johannes Forsberg, Samuel Olausson, and Liselott Wilin for assistance in the field. Thanks also to Johan Dahlgren for help with statistical issues. Thanks to many private landowners, Kramfors and Sollefteå municipalities, SCA and the Church of Sweden, for letting us perform this experiment on their properties. Thanks to the County administration board of Västernorrland that provided permission for studies at Omneberget nature reserve.
Conceived and designed the experiments: CJD JE KH. Performed the experiments: CJD. Analyzed the data: CJD. Wrote the paper: CJD JE KH.
- 1. Maguire B (1973) Niche response structure and analytical potentials of its relationship. Am Nat 107: 213–246.
- 2. Hutchinson GE (1978) An introduction to population ecology. New Haven, Connecticut, USA: Yale University Press. 271 p.
- 3. Sibly RM, Hone J (2002) Population growth rate and its determinants: an overview. Philos Trans R Soc Lond B Biol Sci 357: 1153–1170.
- 4. Lomolino MV, Riddle BR, Brown JH (2006) Biogeography. 3rd ed. Sunderland, Massachusetts: Sinauer Associates, Incorporated. 845 p.
- 5. Gaston KJ (2009) Geographic range limits: achieving synthesis. Proc R Soc B-Biol Sci 276: 1395–1406.
- 6. Violle C, Navas M-L, Vile D, Kazakou E, Fortunel C, et al. (2007) Let the concept of trait be functional!. Oikos 116: 882–892.
- 7. Pearce JL, Boyce MS (2006) Modelling distribution and abundance with presence-only data. J Appl Ecol 43: 405–412.
- 8. Austin MP, Van Niel KP (2011) Improving species distribution models for climate change studies: variable selection and scale. J Biogeogr 38: 1–8.
- 9. Guisan A, Zimmermann NE (2000) Predictive habitat distribution models in ecology. Ecol Model 135: 147–186.
- 10. Gilman SE (2006) Life at the edge: an experimental study of a poleward range boundary. Oecologia 148: 270–279.
- 11. Brown JH (1984) On the relationship between abundance and distribution of species. Am Nat 124: 255–279.
- 12. Gaston KJ (2003) The structure and dynamics of geographic ranges. Oxford: Oxford University Press. 266 p.
- 13. Hampe A, Jump AS (2011) Climate relicts: past, present, future. Annu Rev Ecol Evol Syst 42: 313–333.
- 14. Dobrowski SZ (2011) A climatic basis for microrefugia: the influence of terrain on climate. Glob Change Biol 17: 1022–1035.
- 15. Normand S, Treier UA, Randin C, Vittoz P, Guisan A, et al. (2009) Importance of abiotic stress as a range-limit determinant for European plants: insights from species responses to climatic gradients. Glob Ecol Biogeogr 18: 437–449.
- 16. Arnold SJ (1983) Morphology, performance and fitness. Am Zool 23: 347–361.
- 17. Fridley JD (2009) Downscaling climate over complex terrain: high finescale (<1000 m) spatial variation of near-ground temperatures in a montane forested landscape (Great Smoky Mountains). J Appl Meteorol Climatol 48: 1033–1049.
- 18. Ashcroft MB, Gollan JR (2012) Fine-resolution (25 m) topoclimatic grids of near-surface (5 cm) extreme temperatures and humidities across various habitats in a large (200×300 km) and diverse region. Int J Climatol 32: 2134–2148.
- 19. Fu PD, Rich PM (2002) A geometric solar radiation model with applications in agriculture and forestry. Comput Electron Agric 37: 25–35.
- 20. Geiger R, Aron RH, Todhunter P (2003) The climate near the ground. 6th ed. Lanham, Maryland: Rowman and Littlefield Publishers. 584 p.
- 21. Huang SL, Rich PM, Crabtree RL, Potter CS, Fu PD (2008) Modeling monthly near-surface air temperature from solar radiation and lapse rate: Application over complex terrain in Yellowstone National Park. Phys Geogr 29: 158–178.
- 22. Radcliffe JE, Lefever KR (1981) Aspect influences on pasture microclimate at coopers creek, North-Canterbury. N Z J Agric Res 24: 55–66.
- 23. Rorison IH, Sutton F, Hunt R (1986) Local climate, topography and plant-growth in Lathkill-dale NNR. 1. A 12-year summary of solar-radiation and temperature. Plant Cell Environ 9: 49–56.
- 24. Bennie J, Hill MO, Baxter R, Huntley B (2006) Influence of slope and aspect on long-term vegetation change in British chalk grasslands. J Ecol 94: 355–368.
- 25. Åström M, Dynesius M, Hylander K, Nilsson C (2007) Slope aspect modifies community responses to clear-cutting in Boreal forests. Ecology 88: 749–758.
- 26. Vercauteren N, Destouni G, Dahlberg CJ, Hylander K (2013) Fine-resolved, near-coastal spatiotemporal variation of temperature in response to insolation. J Appl Meteorol Climatol 52: 1208–1220.
- 27. Proctor MCF (2009) Physiological ecology. In: Goffinet B, Shaw J, editors. Bryophyte biology. New York: Cambridge University Press. pp. 237–268.
- 28. Proctor MCF (2011) Climatic responses and limits of bryophytes: comparisons and contrasts with vascular plants. In: Tuba Z, Slack NG, Stark LR, editors. Bryophyte ecology and climate change. New York: Cambridge University Press. pp. 35–54.
- 29. Crandall-Stotler B, Stotler RE, Long DG (2009) Morphology and classification of the Marchantiophyta. In: Goffinet B, Shaw J, editors. Bryophyte biology. New York: Cambridge University Press. pp. 1–54.
- 30. Goffinet B, Buck WR, Shaw J (2009) Morphology, anatomy, and classification of the Bryophyta. In: Goffinet B, Shaw J, editors. Bryophyte biology. New York: Cambridge University Press. pp. 55–138.
- 31. Vanderpoorten A, Goffinet B (2009) Introduction to bryophytes. Cambridge: Cambridge University Press. 328 p.
- 32. Esseen P-A, Ehnström B, Ericson L, Sjöberg K (1997) Boreal forests. Ecol Bull 16–47.
- 33. Slack NG (2011) The ecological value of bryophytes as indicators of climate change. In: Tuba Z, Slack NG, Stark LR, editors. Bryophyte ecology and climate change. New York: Cambridge University Press. pp. 3–12.
- 34. Hylander K (2005) Aspect modifies the magnitude of edge effects on bryophyte growth in boreal forests. J Appl Ecol 42: 518–525.
- 35. Schmalholz M, Hylander K (2011) Microtopography creates small-scale refugia for boreal forest floor bryophytes during clear-cut logging. Ecography 34: 637–648.
- 36. Swedish Meteorological and Hydrological Institute (2013) Klimatdata. Database: Dataserier med normalvärden för perioden 1961–1990. Available: http://www.smhi.se/klimatdata/meteorologi/temperatur/dataserier-med-normalvärden-1.7354. Accessed 15 September 2014.
- 37. Ahti T, Hämet-Ahti L, Jalas J (1968) Vegetation zones and their sections in north-western Europe. Ann Bot Fenn 5: 169–211.
- 38. Andersson G, Selin B (1912) Den norrländska florans geografiska fördelning och invandringshistoria med särskild hänsyn till dess sydskandinaviska arter. Uppsala: Almqvist & Wiksell. 416 p.
- 39. Mascher JW (1990) Ångermanlands flora. Lund: SBT-redaktionen. 720 p.
- 40. Artdatabanken SLU (2011) Artportalen, rapportsystem för växter, djur och svampar. Database: Artportalen. Available: http://www.artportalen.se/ViewSighting/SearchSighting. Accessed 15 April 2011.
- 41. Söderström L (1981) Distribution of bryophytes in spruce forests on hill slopes in central Sweden. Wahlenbergia 7: 141–153.
- 42. Tuhkanen S (1980) Climatic parameters and indices in plant geography. Acta Phytogeogr Suec 67: 1–110.
- 43. Hägglund B, Lundmark J-E (1982) Handledning i bonitering med Skogshögskolans boniteringssystem. Del 3, Markvegetationstyper-skogsmarksflora. Jönköping: Skogsstyrelsen. 128 p.
- 44. Mossberg B, Stenberg L (2012) Den nya nordiska floran. Hung Hing: Bonnier Fakta. 928 p.
- 45. Hill MO, Bell N, Bruggeman-Nannenga MA, Brugués M, Cano MJ, et al. (1996) An annotated checklist of the mosses of Europe and Macaronesia. J Bryol 28: 198–267.
- 46. Damsholt K (2002) Illustrated flora of the nordic liverworts and hornworts. Lund: Nordic Bryological Society. 838 p.
- 47. Økland RH (1995) Population biology of the clonal moss Hylocomium splendens in norwegian boreal spruce forests. I. Demography. J Ecol 83: 697–712.
- 48. Frank IE, Friedman JH (1993) A statistical view of some chemometrics regression tools. Technometrics 35: 109–135.
- 49. Tibshirani R (1996) Regression shrinkage and selection via the Lasso. J R Stat Soc Ser B-Methodol 58: 267–288.
- 50. Ribbing J, Nyberg J, Caster O, Jonsson EN (2007) The lasso - a novel method for predictive covariate model building in nonlinear mixed effects models. J Pharmacokinet Pharmacodyn 34: 485–517.
- 51. Dahlgren JP (2010) Alternative regression methods are not considered in Murtaugh (2009) or by ecologists in general. Ecol Lett 13: 7–9.
- 52. R Core Team (2013) R: A language and environment for statistical computing. Vienna: R Foundation for Statistical Computing. Available: http://www.R-project.org/.
- 53. Hiesey WM, Nobs MA, Björkman O (1971) Experimental studies on the nature of species. V. Biosystematics, genetics, and physiological ecology of the Erythranthe section of Mimulus. Washington, DC: Carnegie Institute of Washington. 213 p.
- 54. Despland E, Houle G (1997) Climate influences on growth and reproduction of Pinus banksiana (Pinaceae) at the limit of the species distribution in eastern North America. Am J Bot 84: 928–937.
- 55. Angert AL, Schemske DW (2005) The evolution of species' distributions: Reciprocal transplants across the elevation ranges of Mimulus cardinalis and M. lewisii. Evolution 59: 1671–1684.
- 56. Nault A, Gagnon D (1993) Ramet demography of Allium Tricoccum, a spring ephemeral, Perennial Forest Herb. J Ecol 81: 101–119.
- 57. Eriksson O (1988) Ramet behaviour and population growth in the clonal herb Potentilla anserina. J Ecol 76: 522–536.
- 58. Breckle S-W (2002) Walter's vegetation of the earth: the ecological systems of the geo-biosphere. 7th ed. Berlin: Springer-Verlag. 527 p.
- 59. Hampe A (2005) Fecundity limits in Frangula alnus (Rhamnaceae) relict populations at the species' southern range margin. Oecologia 143: 377–386.
- 60. Kurschner H (1999) Life strategies of epiphytic bryophytes in Mediterranean Pinus woodlands and Platanus orientalis alluvial forests of Turkey. Cryptogam Bryol 20: 17–33.
- 61. Hylander K, Dynesius M, Jonsson BG, Nilsson C (2005) Substrate form determines the fate of bryophytes in riparian buffer strips. Ecol Appl 15: 674–688.
- 62. Svenning J-C, Sandel B (2013) Disequilibrium vegetation dynamics under future climate change. Am J Bot 100: 1266–1286.
- 63. Frahm J-P, Klaus D (2001) Bryophytes as indicators of recent climate fluctuations in Central Europe. Lindbergia 26: 97–104.
- 64. Zimmermann NE, Yoccoz NG, Edwards TC, Meier ES, Thuiller W, et al. (2009) Climatic extremes improve predictions of spatial patterns of tree species. Proc Natl Acad Sci U S A 106: 19723–19728.
- 65. Van der Veken S, Rogister J, Verheyen K, Hermy M, Nathan R (2007) Over the (range) edge: a 45-year transplant experiment with the perennial forest herb Hyacinthoides non-scripta. J Ecol 95: 343–351.
- 66. Van der Veken S, De Frenne P, Baeten L, Van Beek E, Verheyen K, et al. (2012) Experimental assessment of the survival and performance of forest herbs transplanted beyond their range limit. Basic Appl Ecol 13: 10–19.
- 67. Lönnell N, Jonsson BG, Hylander K (2014) Production of diaspores at the landscape level regulates local colonization: an experiment with a spore-dispersed moss. Ecography 37: 591–598.
- 68. Davison AW (1977) The ecology of Hordeum Murinum L.: III. Some effects of adverse climate. J Ecol 65: 523–530.
- 69. Skov F, Svenning JC (2004) Potential impact of climatic change on the distribution of forest herbs in Europe. Ecography 27: 366–380.
- 70. Gimenez-Benavides L, Escudero A, Iriondo JM (2008) What shapes the altitudinal range of a high mountain Mediterranean plant? Recruitment probabilities from ovule to seedling stage. Ecography 31: 731–740.
- 71. Crozier LG (2004) Field transplants reveal summer constraints on a butterfly range expansion. Oecologia 141: 148–157.
- 72. Sanford E, Holzman SB, Haney RA, Rand DM, Bertness MD (2006) Larval tolerance, gene flow, and the northern geographic range limit of fiddler crabs. Ecology 87: 2882–2894.
- 73. Wood AJ (2007) The nature and distribution of vegetative desiccation-tolerance in hornworts, liverworts and mosses. The Bryologist 110: 163–177.