| Literature DB >> 23133560 |
David Sánchez-Fernández1, Pedro Aragón, David T Bilton, Jorge M Lobo.
Abstract
A basic aim of ecology is to understand the determinants of organismal distribution, the niche concept and species distribution models providing key frameworks to approach the problem. As temperature is one of the most important factors affecting species distribution, the estimation of thermal limits is crucially important for inferring range constraints. It is expectable that thermal physiology data derived from laboratory experiments and species' occurrences may express different aspects of the species' niche. However, there is no study systematically testing this prediction in a given taxonomic group while controlling by potential phylogenetic inertia. We estimate the thermal niches of twelve Palaearctic diving beetles species using physiological data derived from experimental analyses in order to examine the extent to which these coincided with those estimated from distribution models based on observed occurrences. We found that thermal niche estimates derived from both approaches lack general congruence, and these results were similar before and after controlling by phylogeny. The congruence between potential distributions obtained from the two different procedures was also explored, and we found again that the percentage of agreement were not very high (~60%). We confirm that both thermal niche estimates derived from geographical and physiological data are likely to misrepresent the true range of climatic variation that these diving beetles are able to tolerate, and so these procedures could be considered as incomplete but complementary estimations of an inaccessible reality.Entities:
Mesh:
Year: 2012 PMID: 23133560 PMCID: PMC3485027 DOI: 10.1371/journal.pone.0048163
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Values of thermal tolerance, size of potential distribution, geographical range and dispersal capacity for the considered species.
| Species | MaxTWM | MinTCM | TRO | UTL | LTL | TRPH | DTR | PDO | PDPH | CPD | APD | DC | S Lim | N Lim | LRE |
|
| 29.1 | 5.3 | 23.8 | 45.68 | −3.4 | 49.08 | 25.28 | 340 | 13824 | 13824 | 2.46 | 1.16 | 36 | 36.5 | 0.5 |
|
| 25.5 | −4.2 | 29.7 | 43.62 | −7.68 | 51.3 | 21.60 | 6248 | 13728 | 13728 | 45.51 | 1.00 | 42 | 43.5 | 1.5 |
|
| 29.0 | −8.8 | 37.8 | 44.06 | −8.34 | 52.4 | 14.60 | 17339 | 16791 | 18598 | 83.51 | 1.12 | 44 | 48.0 | 4.0 |
|
| 34.5 | −4.2 | 38.7 | 44.47 | −9.43 | 53.9 | 15.20 | 13672 | 26719 | 26719 | 51.17 | 1.15 | 40 | 43.0 | 3.0 |
|
| 32.7 | −7.6 | 40.3 | 45.2 | −7.69 | 52.89 | 12.59 | 17892 | 19269 | 19269 | 92.85 | 1.11 | 37 | 38.0 | 1.0 |
|
| 39.9 | −5.9 | 45.8 | 45.74 | −7.39 | 53.13 | 7.33 | 31879 | 44739 | 44739 | 71.26 | 1.30 | 31 | 47.5 | 16.5 |
|
| 33.4 | −7.6 | 41 | 45.57 | −5.15 | 50.72 | 9.72 | 21768 | 18802 | 24722 | 64.10 | 1.20 | 36 | 44.5 | 8.5 |
|
| 28.4 | −19.7 | 48.1 | 46.91 | −9.96 | 56.87 | 8.77 | 35746 | 21222 | 37203 | 53.13 | 1.01 | 41 | 69.0 | 28.0 |
|
| 33.3 | −7.4 | 40.7 | 44.7 | −6.09 | 50.79 | 10.09 | 11579 | 9423 | 11595 | 81.13 | 1.25 | 40 | 42.0 | 2.0 |
|
| 36.0 | −5.8 | 41.8 | 45.63 | −6.46 | 52.09 | 10.29 | 18614 | 21793 | 21793 | 85.41 | 1.21 | 36 | 45.5 | 9.5 |
|
| 29.6 | −6.5 | 36.1 | 42.63 | −9.06 | 51.69 | 15.59 | 13188 | 19224 | 19224 | 68.60 | 1.08 | 42.5 | 45.5 | 3.0 |
|
| 32.5 | −3.6 | 36.1 | 42.83 | −9.08 | 51.91 | 15.81 | 5049 | 11999 | 11999 | 42.08 | 1.07 | 40 | 41.0 | 1.0 |
Highest value of the maximum temperature of the warmest month (MaxTWM), lowest value of the minimum temperature of the coldest month (MinTCM) and thermal range (TRO) from occurrence data (°C); Upper Thermal Limit (UTL), Lower Thermal Limit (LTL) and thermal range (TRPH) from physiological experiments (°C); difference between both thermal ranges (DTR = TRPH – TRO); Number of pixels (0.2degrees) of the potential distribution using climatic data derived from occurrences (PDO) and physiological thermal limits (PDPH ); Combined potential distribution map using both methods (CPD) and percentage of agreement between these two approaches for estimating potential distributions (APD) (see methods for details); Dispersal Capacity (DC); and Southern (S Lim) and northern (N Lim) range limits (degrees), and latitudinal range extents (LRE) for the Deronectes species studied.
Figure 1Tolerance to cold, heat and thermal range.
Relationships between the tolerance to cold (A), heat (B) and thermal range (C), obtained from environmental data based on site occupancy (vertical axis) and from physiological experiments (horizontal axis). A) Highest value of the Maximum temperature of the warmest month (MaxTWM) from occurrence data, Upper Thermal Limit (UTL) from physiological experiments; B) lowest value of the minimum temperature of the coldest month (MinTCM) from occurrence data, Lower Thermal Limit (LTL) from physiological experiments; and C) thermal range (TRO) from occurrence data and thermal range (TRPH) from physiological experiments. Continuous line represents the regression line; dotted line is equality. Species names are abbreviated.
Figure 2Potential distribution maps.
Grey surface represents the area that is predicted as potential distribution only using climatic data from occurrences; light green surface represents the area that is predicted as potential distribution only using physiological tolerance; dark green surface represents the potential area shared by the two procedures (i.e. areas where both methods overlap). For each species, the combined potential distribution (CPD) using both methods is represented as the sum of the three colours. Red points indicate occupied localities. A: D. algibensis; B: D. angusi; C: D. aubei aubei; D: D. bicostatus; E: D. depresicollis; F: D. fairmairei; G: D. hispanicus; H: D. latus; I: D. mazzoldi; J: D. opatrinus; K: D. semirufus; L: D. wewalkai.