| Literature DB >> 26848385 |
Mariano Soley-Guardia1, Eliécer E Gutiérrez2, Darla M Thomas3, José Ochoa-G4, Marisol Aguilera5, Robert P Anderson6.
Abstract
Correlative ecological niche models (ENMs) estimate species niches using occurrence records and environmental data. These tools are valuable to the field of biogeography, where they are commonly used to infer potential connectivity among populations. However, a recent study showed that when locally relevant environmental data are not available, records from patches of suitable habitat protruding into otherwise unsuitable regions (e.g., gallery forests within dry areas) can lead to overestimations of species niches and their potential distributions. Here, we test whether this issue obfuscates detection of an obvious environmental barrier existing in northern Venezuela - that of the hot and xeric lowlands separating the Península de Paraguaná from mainland South America. These conditions most likely promote isolation between mainland and peninsular populations of three rodent lineages occurring in mesic habitat in this region. For each lineage, we calibrated optimally parameterized ENMs using mainland records only, and leveraged existing habitat descriptions to assess whether those assigned low suitability values corresponded to instances where the species was collected within locally mesic conditions amidst otherwise hot dry areas. When this was the case, we built an additional model excluding these records. We projected both models onto the peninsula and assessed whether they differed in their ability to detect the environmental barrier. For the two lineages in which we detected such problematic records, only the models built excluding them detected the barrier, while providing additional insights regarding peninsular populations. Overall, the study reveals how a simple procedure like the one applied here can deal with records problematic for ENMs, leading to better predictions regarding the potential effects of the environment on lineage divergence.Entities:
Keywords: Gallery forests; Paraguaná; habitat connectivity; niche conservatism; small mammals; soft allopatry
Year: 2016 PMID: 26848385 PMCID: PMC4730904 DOI: 10.1002/ece3.1900
Source DB: PubMed Journal: Ecol Evol ISSN: 2045-7758 Impact factor: 2.912
Figure 1Study system. (A) Digital elevation map showing a close‐up of the Península de Paraguaná in northern South America. Light gray indicates elevations 200–500 m; dark gray 500–1000 m; and black >1000 m. Peninsular sites known to harbor populations of at least one of the study species are shown in bold; CSA: Cerro Santa Ana; FMC: Fila de Monte Cano; YQ: Yabuquiva. (B) Habitat present at, or surrounding, the peninsular sites shown in (A). Mesic habitat on the peninsula is scarce, mostly restricted to Cerro Santa Ana (approximately 850 m in elevation). A few patches of mesic habitat also exist at lower elevations due to local topographic and atmospheric factors. The rest of the peninsula is characterized by xerophytic thorn forests and desert scrub that also extend throughout the narrow isthmus (Istmo de los Médanos; partly exhibiting sand dunes) and adjacent lowlands on the mainland (Markezich et al. 1997; Anderson 2003a; IGVSB 2004; Gutiérrez and Molinari 2008; Anderson et al. 2012). Top pictures: abrupt transition from mesic forests at middle‐to‐high elevations on Cerro Santa Ana, to the xerophytic vegetation predominating in the lowlands (e.g., thorn scrub). Bottom pictures: patches of mesic habitat occurring within the otherwise hot and xeric peninsular lowlands (i.e., protruding spatially marginal localities). Elevation from Shuttle Radar Topography Mission (SRTM), with 3 arc‐second resolution (~90 m), obtained through WeoGeo (http://www.weogeo.com). Photographic credits: CSA top and FMC taken by MSG; CSA base by RPA; YQ by JOG.
Figure 2Projections of maxent models onto the Península de Paraguaná in northern South America, showing categorical estimates of suitability for each lineage. Predictions correspond to either models built with all records, or to composite predictions – the latter made by overlaying the categorical estimates of suitability obtained from the models built without records from protruding spatially marginal (PSM) localities, on top of the binary estimates of suitability obtained from the models built with all records. Gray: unsuitable areas; pale colors: areas of low suitability (suitable only at the lenient threshold); dark colors: areas of higher suitability (suitable at both the lenient and the species‐specific stricter thresholds; details in text). In the composite predictions, the tan color indicates areas suitable only in the models built with all records and at the lenient threshold (denoting areas where the species might occur if locally mesic conditions exist). (A) Suitability draped over an elevation surface (the latter exaggerated for clarity). Shading according to elevation is provided for visual purposes and does not constitute a color gradient. Note differences in the potential for geographic connectivity among mainland and peninsular populations according to the different models. (B) Close‐up of the projections shown in (A) – within the center of the peninsula. Each pixel measures ~1 km2. Symbols indicate known peninsular records of the studied species, with triangles marking those occurring within PSM localities. Dashed lines indicate approximate contours of areas of higher elevation (ca. 150 m) within the peninsula. CSA: Cerro Santa Ana; FMC: Fila de Monte Cano; YQ: Yabuquiva. Note qualitative differences in suitability assigned to PSM localities (and areas between them) by the different models. Projections were made in arcscene ® 9.2 (ESRI, Redlands, CA, USA). Elevation from Shuttle Radar Topography Mission (SRTM), with 3 arc‐second resolution (~90 m), obtained through WeoGeo (http://www.weogeo.com).
Environmental values (means and ranges) for different sets of occurrence records of each of the three lineages studied. The two variables included herein correspond to those with high “percent contribution” during internal iterations of the generation of each MaxEnt model. Because of possible differences in environmental signals between occurrence datasets, as well as the machine‐learning approach used by MaxEnt, the identity of the two variables with the highest importance differed for each specific model (i.e., calibrated with vs. without records from protruding spatially marginal (PSM) localities). For presentation, we chose variables that had a high “percent contribution” in both models (percentages shown in parentheses), and which were also included in each respective final model (i.e., present with nonzero weights in the “lambdas” file). Conveniently, these corresponded to both temperature (°C) and precipitation (mm) variables for each lineage. For Heteromys anomalus, the “mainland regular localities” consist mostly of extensive forests; however, that dataset also includes four PSM localities that received higher rankings, and seven localities for which no habitat descriptions were found (Soley‐Guardia et al. 2014). n: Sample size for each successive column from left to right; NA: not applicable (i.e., no PSM localities were found). Although no statistical tests are conducted here, note that for Rhipidomys venezuelae and the Heteromys lineage, PSM localities unambiguously showed substantially higher means for temperature and markedly lower means for precipitation (for both mainland and peninsular comparisons)
| Lineage | Variables: % contribution (All records/ Excluding PSM localities) | Mainland PSM localities (vegetation mosaics) | Mainland regular localities (extensive forests) | Mainland rest of localities (highest suitability values; not inspected) | Peninsular PSM localities (vegetation mosaics) | Peninsular regular localities (extensive forests) |
|---|---|---|---|---|---|---|
|
| Temperature annual range (16%/NA) | NA | 13 (11–14) | 13 (9–16) | NA | 12 (12–12) |
| Precipitation of driest quarter (23%/NA) | NA | 37 (25–51) | 86 (16–253) | NA | 73 (59–76) | |
|
| Maximum temperature of warmest month (76/63%) | 35 (34–36) | 32 (31–32) | 26 (21–31) | 33 (32–34) | 30 (30–30) |
| Precipitation of driest quarter (5/2%) | 37 (13–61) | 125 (60–200) | 87 (32–141) | 44 (31–56) | 76 (75–76) | |
|
| Maximum temperature of warmest month (44/41%) | 34 (31–36) | 32 (22–36) | 29 (20–34) | 33 (32–33) | 30 (30–30) |
| Precipitation of driest quarter (9/15%) | 38 (7–152) | 92 (12–276) | 144 (35–322) | 51 (46–56) | 76 (75–76) |