| Literature DB >> 23467191 |
Brian Oney1, Björn Reineking, Gregory O'Neill, Juergen Kreyling.
Abstract
Species distribution modeling (SDM) is an important tool to assess the impact of global environmental change. Many species exhibit ecologically relevant intraspecific variation, and few studies have analyzed its relevance for SDM. Here, we compared three SDM techniques for the highly variable species Pinus contorta. First, applying a conventional SDM approach, we used MaxEnt to model the subject as a single species (species model), based on presence-absence observations. Second, we used MaxEnt to model each of the three most prevalent subspecies independently and combined their projected distributions (subspecies model). Finally, we used a universal growth transfer function (UTF), an approach to incorporate intraspecific variation utilizing provenance trial tree growth data. Different model approaches performed similarly when predicting current distributions. MaxEnt model discrimination was greater (AUC - species model: 0.94, subspecies model: 0.95, UTF: 0.89), but the UTF was better calibrated (slope and bias - species model: 1.31 and -0.58, subspecies model: 1.44 and -0.43, UTF: 1.01 and 0.04, respectively). Contrastingly, for future climatic conditions, projections of lodgepole pine habitat suitability diverged. In particular, when the species' intraspecific variability was acknowledged, the species was projected to better tolerate climatic change as related to suitable habitat without migration (subspecies model: 26% habitat loss or UTF: 24% habitat loss vs. species model: 60% habitat loss), and given unlimited migration may increase amount of suitable habitat (subspecies model: 8% habitat gain or UTF: 12% habitat gain vs. species model: 51% habitat loss) in the climatic period 2070-2100 (SRES A2 scenario, HADCM3). We conclude that models derived from within-species data produce different and better projections, and coincide with ecological theory. Furthermore, we conclude that intraspecific variation may buffer against adverse effects of climate change. A key future research challenge lies in assessing the extent to which species can utilize intraspecific variation under rapid environmental change.Entities:
Keywords: Intraspecific diversity; North America; lodgepole pine; niche modeling; range shift; within-species variability
Year: 2013 PMID: 23467191 PMCID: PMC3586652 DOI: 10.1002/ece3.426
Source DB: PubMed Journal: Ecol Evol ISSN: 2045-7758 Impact factor: 2.912
Climate variables investigated across the ranges of Pinus contorta and subspecies
| Climate variables | Unit | Source |
|---|---|---|
| Annual Heat/Moisture Index | Wang et al. ( | |
| Summer Heat/Moisture Index | Wang et al. ( | |
| Mean Annual Temp. | Wang et al. ( | |
| Mean Warm Monthly Temp. | Wang et al. ( | |
| Mean Cold Monthly Temp. | Wang et al. ( | |
| Temp. Difference/Annual Range | Wang et al. ( | |
| Mean Annual Precip. | mm | Wang et al. ( |
| Mean Summer Precip. | mm | Wang et al. ( |
| Isothermality | Hijmans et al. ( | |
| Mean Diurnal Range | Hijmans et al. ( | |
| Temp. Seasonality | Hijmans et al. ( | |
| Mean Temp. of Wettest Quarter | Hijmans et al. ( | |
| Mean Temp. of Driest Quarter | Hijmans et al. ( | |
| Mean Temp. of Warmest Quarter | Hijmans et al. ( | |
| Mean Temp. of Coldest Quarter | Hijmans et al. ( | |
| Precip. of Wettest Month | mm | Hijmans et al. ( |
| Precip. of Driest Month | mm | Hijmans et al. ( |
| Precip. Seasonality | mm | Hijmans et al. ( |
| Precip. of Wettest Quarter | mm | Hijmans et al. ( |
| Precip. of Driest Quarter | mm | Hijmans et al. ( |
| Precip. of Coldest Quarter | mm | Hijmans et al. ( |
| Precip. of Warmest Quarter | mm | Hijmans et al. ( |
| Mean Max. Temp. of Driest Quarter | This study |
Figure 1Pinus contorta subspecies distributions across its natural range. The number of observations documented to subspecies was low; therefore the nearest observation that was classified to subspecies was assigned that observations' subspecies classification. The dashed line outlines the model building buffer area i.e. model training and evaluation (see Supporting Information). Occurrence data were obtained mainly from the British Columbia Ministry of Forests and US Forest Service Forest Inventory and Analysis; the observational data cover most of the natural range. Within the modeling range, each raster cell was assigned either a presence or absence.
The summarizing dimensions of the climate niche for each modeling subject using MaxEnt
| Subject | Variable | I.(%) | Range | Curve |
|---|---|---|---|---|
| Subsp. | Mean diurnal range | 44.7 | 4–13 | Unimodal, pos. |
| Maximum temperature of dry quarter | 29.8 | −7–30 | Unimodal, pos. | |
| Mean temperature of wet quarter | 25.5 | −7–19 | Unimodal, pos. | |
| Subsp. | Precipitation of warm quarter | 40.3 | 1–232 | Sigmoidal, neg. |
| Precipitation of cold quarter | 25.3 | 11–581 | Sigmoidal, neg. | |
| Maximum temperature of dry quarter | 14.9 | −7–21 | Unimodal, pos. | |
| Precipitation seasonality | 9.8 | 19–110 | Unimodal, pos. | |
| Precipitation of wet quarter | 9.7 | 152–760 | Sigmoidal, neg. | |
| Subsp. | Mean annual temperature | 72.8 | −12–14 | Unimodal, pos. |
| Precipitation of dry quarter | 14.7 | 0–262 | Unimodal, pos. | |
| Precipitation seasonality | 12.5 | 6–70 | Sigmoidal, neg. | |
| Species model | Mean temperature of warm quarter | 72.8 | 0–22 | Unimodal, pos. |
| Precipitation of dry quarter | 19.8 | 2–470 | Unimodal, pos. | |
| Precipitation seasonality | 7.4 | 20–75 | Sigmoidal, neg. |
A set of variables was found to be less correlated (ρ < 0.7) and important to explain the distributions of each subspecies. The ranges of variables (units are in Table 1), in which each subspecies responds to climatic conditions, and the shape of their response curve highlight the different characteristics of each subspecies, and provide an informative contrast to the conventional method (species model). Furthermore, the importance (I. (%)) of each variable, measured by the relative change in AUC when singularly randomizing, hints at the dominant climate factors depicted by each model.
Figure 2Occurrence probability distributions were modeled in the current climatic period (1950–2000) and the three models (a) species model (b) subspecies model and (c) universal transfer function (UTF) were projected onto North American climate data (Hijmans et al. 2005). The models were trained and evaluated on the modeling range (see Fig. 1) and projected to the projection range (dashed line), which corresponds to most of the North American continent. The MaxEnt models are highly discriminative, but the UTF is better calibrated.
Figure 3Projections of the three models (a) species model (b) subspecies model and (c) universal transfer function onto North American climate for the period 2070–2100 under the A2a emissions scenario from the HadCM3 global climate model.
Figure 4Predicted suitable habitat area of Pinus contorta relative to the reference climatic period 1950–2000 assuming (a) full dispersal and (b) no dispersal for each climatic period for all modeling techniques. Modeling techniques which incorporate intraspecific variability – the UTF and subspecies model, predict more optimistic outcomes for Pinus contorta.
Figure 5Relative predicted suitable habitat area of Pinus contorta subspecies assuming (a) full dispersal and (b) no dispersal for each climatic period (taken from the subspecies model).