| Literature DB >> 22675485 |
Richard I Bailey1, Clara I Saldamando-Benjumea, Haruki Tatsuta, Roger K Butlin.
Abstract
Understanding why some hybrid zones are bimodal and others unimodal can aid in identifying barriers to gene exchange following secondary contact. The hybrid zone between the grasshoppers Chorthippus brunneus and C. jacobsi contains a mix of allopatric parental populations and inter-mingled bimodal and unimodal sympatric populations, and provides an ideal system to examine the roles of local selection and gene flow between populations in maintaining bimodality. However, it is first necessary to confirm, over a larger spatial scale, previously identified associations between population composition and season and habitat. Here we use cline-fitting of one morphological and one song trait along two valley transects, and intervening mountains, to confirm previously identified habitat associations (mountain versus valley) and seasonal changes in population composition. As expected from previous findings of studies on a smaller spatial scale, C. jacobsi dominated mountain habitats and mixed populations dominated valleys, and C. brunneus became more prevalent in August. Controlling for habitat and incorporating into the analysis seasonal changes in cline parameters and the standard errors of parental trait values revealed wider clines than previous studies (best estimates of 6.4 to 24.5 km in our study versus 2.8 to 4.7 km in previous studies) and increased percentage of trait variance explained (52.7% and 61.5% for transects 1 and 2 respectively, versus 17.6%). Revealing such strong and consistent patterns within a complex hybrid zone will allow more focused examination of the causes of variation in bimodality in mixed populations, in particular the roles of local selection versus habitat heterogeneity and gene flow between differentiated populations.Entities:
Mesh:
Year: 2012 PMID: 22675485 PMCID: PMC3366992 DOI: 10.1371/journal.pone.0037684
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Figure 1Sampling locations in Spain.
Map of northern Spain indicating cline centres (open diamonds) and widths (unbroken lines) along transects 1 (the LE232, to the west) and 2 (the C615 to the east) in season 3 (the season most closely matching collecting periods by Bridle and colleagues). Collecting sites at the northern and southern ends of each transect are indicated by open circles and the four mountain sites (M1 to M4 moving from north to south) by grey-filled circles. Black circles indicate major towns and cities close to the study area. The existing fitted two-dimensional cline centre for stridulatory peg number [28] is indicated by a dashed line, and the square indicates the study area in which strong seasonality and habitat associations were previously identified [27].
List of tested models for each of stridulatory peg number and echeme length, in order of AIC (best-fitting model first).
| Peg number | Echeme length | ||||||
| Model | Likelihood | Parameters | AIC | Model | Likelihood | Parameters | AIC |
| 3w2c2b | −2746.97 | 18 | 5529.94 | 3w2c2b | −843.07 | 18 | 1722.14 |
| 2w3c2b | −2747.33 | 18 | 5530.65 | 3w2c3b | −841.14 | 20 | 1722.28 |
| 3w2c3b | −2746.16 | 20 | 5532.32 | 3w3c3b | −840.71 | 22 | 1725.42 |
| 3w3c2b | −2746.75 | 20 | 5533.5 | 3w3c2b | −843 | 20 | 1726 |
| 2w2c2b | −2751.13 | 16 | 5534.26 | 2w2c2b | −847.19 | 16 | 1726.37 |
| 2w3c3b | −2747.28 | 20 | 5534.57 | 2w3c2b | −845.19 | 18 | 1726.38 |
| 2w2c3b | −2750.81 | 18 | 5537.63 | 2w2c1b | −849.84 | 14 | 1727.68 |
| 3w3c3b | −2747.39 | 22 | 5538.79 | 2w1c1b | −852.73 | 12 | 1729.46 |
| 1w2c2b | −2757.75 | 14 | 5543.49 | 2w3c3b | −845.14 | 20 | 1730.27 |
| 2w1c2b | −2768.04 | 14 | 5564.08 | 2w2c3b | −847.29 | 18 | 1730.58 |
| 1w2c1b | −2774.61 | 12 | 5573.22 | 2w1c2b | −851.67 | 14 | 1731.33 |
| 2w2c1b | −2772.68 | 14 | 5573.35 | 1w2c1b | −854.11 | 12 | 1732.22 |
| 1w1c2b | −2788.5 | 12 | 5601 | 1w1c2b | −854.28 | 12 | 1732.56 |
| 2w1c1b | −2788.64 | 12 | 5601.28 | 1w2c2b | −852.54 | 14 | 1733.08 |
| 1w1c1b | −2816.17 | 10 | 5652.35 | 1w1c1b | −868 | 10 | 1756 |
w = cline width, c = cline centre relative to distances listed in Table S1, b = elevation in trait variance at the zone centre.
Figure 2Stridulatory peg numbers and fitted clines.
Stridulatory peg numbers (grey diamonds) along (a) transect 1 and (b) transect 2 for each temporally separated collection; and fitted clines (solid lines) from the best-fitting model with combined width and centre estimates for song and pegs ± fitted standard deviation (SD) in peg number (thin dashed lines). Thick vertical dashed lines indicate fitted cline centres.
Parameter estimates for parental means and variances for stridulatory peg number and log(echeme length) and for cline centre, width and variance elevation for each season.
| Stridulatory peg number | |||
|
|
|
|
|
| 73.04 | 101.65 | 115.65 | 114.72 |
| Log(Echeme length) (sec) | |||
|
|
|
|
|
| −1.726 | 0.044 | −0.667 | 0.023 |
| Transect 1 | |||
| Centre (1, 2) | Width (1, 2, 3) (km) |
|
|
| 5.81, 13.6 | 19.89, 24.47, 17.76 | −1763.14, −99.95 | −0.899, −0.113 |
| Transect 2 | |||
| Centre (1, 2) | Width (1, 2, 3) (km) |
|
|
| 8.02, 8.15 | 6.82, 13.29, 21.77 | −1852.88, −81.97 | −0.536, −0.092 |
Numbers in brackets after parameter names indicate season. Estimates are from the model with 2 centres, 3 widths and 2 elevations in variance in which cline centre and width were constrained to be identical for peg number and echeme length. Higher negative values for b indicate a greater elevation in trait variance in the zone centre; zero would indicate no elevation in variance. The first parameter of the quadratic (not shown) = (C. jacobsi variance – C. brunneus variance) – b.
Comparison between mountain site mean stridulatory peg number and the mean and variance predicted from interpolation between the two valley transects.
| Site | Season | Distance | Mean | Variance | Likelihood | Predicted mean | Predicted variance | Likelihood | P |
| M1 | 1 | −5.32 | 80.24 | 357.74 | |||||
| M1 | 2 | −9.83 | 101.6 | 271.38 | −32.52 | 77.76 | 112.06 | −59.85 | <0.001*** |
| M1 | 3 | −9.83 | 115.91 | 158.89 | −32.88 | 78.17 | 112.85 | −102.4 | <0.001*** |
| M2 | 1 | −1.7 | 89.04 | 530.57 | |||||
| M2 | 2 | −7.6 | 118.9 | 186.1 | −30.63 | 80.13 | 116.45 | −95.52 | <0.001*** |
| M2 | 3 | −7.6 | 115.5 | 56.28 | −24.65 | 80.57 | 117.2 | −78.03 | <0.001*** |
| M3 | 1 | 3.8 | 119.2 | 65.36 | −13.99 | 105.31 | 443.82 | −16.87 | 0.05<P<0.1 |
| M3 | 2 | −0.88 | 118.14 | 38.48 | −15.78 | 92.36 | 130.12 | −35.81 | <0.001*** |
| M3 | 3 | −0.88 | 110.5 | 286.06 | −32.78 | 92.45 | 130.17 | −46.75 | <0.001*** |
| M4 | 1 | 5.68 | 119.29 | 41.24 | −16.02 | 109.08 | 348.62 | −21.89 | <0.005** |
| M4 | 2 | 1.63 | 118 | 184.67 | −30.59 | 97.98 | 131.38 | −45.97 | <0.001*** |
| M4 | 3 | 1.63 | 115.4 | 87.82 | −26.88 | 97.82 | 131.39 | −39.16 | <0.001*** |
Distance = distance in km directly south from the predicted cline centre.