| Literature DB >> 34273213 |
Andrew P Weitz1,2, Marinela Dukic1, Leo Zeitler1,3, Kirsten Bomblies1.
Abstract
Meiosis, the cell division by which eukaryotes produce haploid gametes, is essential for fertility in sexually reproducing species. This process is sensitive to temperature, and can fail outright at temperature extremes. At less extreme values, temperature affects the genome-wide rate of homologous recombination, which has important implications for evolution and population genetics. Numerous studies in laboratory conditions have shown that recombination rate plasticity is common, perhaps nearly universal, among eukaryotes. These studies have also shown that variation in the length or timing of stresses can strongly affect results, raising the important question whether these findings translate to more variable field conditions. Moreover, lower or higher recombination rate could cause certain kinds of meiotic aberrations, especially in polyploid species-raising the additional question whether temperature fluctuations in field conditions cause problems. Here, we tested whether (1) recombination rate varies across a season in the wild in two natural populations of autotetraploid Arabidopsis arenosa, (2) whether recombination rate correlates with temperature fluctuations in nature, and (3) whether natural temperature fluctuations might cause meiotic aberrations. We found that plants in two genetically distinct populations showed a similar plastic response with recombination rate increases correlated with both high and low temperatures. In addition, increased recombination rate correlated with increased multivalent formation, especially at lower temperature, hinting that polyploids in particular may suffer meiotic problems in conditions they encounter in nature. Our results show that studies of recombination rate plasticity done in laboratory settings inform our understanding of what happens in nature.Entities:
Keywords: evolution; meiosis; plasticity; polyploid; recombination
Mesh:
Year: 2021 PMID: 34273213 PMCID: PMC9292783 DOI: 10.1111/mec.16084
Source DB: PubMed Journal: Mol Ecol ISSN: 0962-1083 Impact factor: 6.622
FIGURE 1Sampling sites and genetic relatedness of populations. (a) Sampling site locations in Switzerland, with site photos. See methods for GPS coordinates. (b) Principal component analysis (PCA) of Moutier (MOU) and Göschenen (GOS) in a broader sample of Arabidopsis arenosa tetraploids from (Monnahan et al., 2019). GOS is part of a ruderal lineage of A. arenosa, which grows primarily on railways and roadsides, clustering with populations from as far away as Sweden (DFS) and Poland (KOW), while MOU clusters with the Hercynian A. arenosa from similar limestone forested rock outcrop habitats in southern Germany and the Czech Republic
FIGURE 2Hourly sampling of temperatures in summer 2019. (a) Hourly measurements of temperature (single points) at each plant from Göschenen are shown in blue and Moutier in orange. Smoothed lines show average trends for each site, with grey shading indicating the 95% confidence interval. Sampling timepoints at each site are shown with vertical dotted lines with dates and “campaign” numbers given in parentheses. (b) Average crossover rate per plant plotted against the temperature that that plant experienced averaged over the time window of 10–30 h before sampling. For correlations with temperature at individual timepoints, see Figure S1. Best fit polynomial curves are shown, with grey shading indicating the 95% confidence interval. Points and lines for GOS in blue and MOU in orange. (c) Box plots of average CO rates per plant for each population across the three sampling campaigns at each site with GOS in blue, and MOU in orange. Note that timepoint 3 in GOS has a small sample size
Sample collection attributes within each study site, including the dates and durations of collection periods for each collection campaign, the range of temperatures during sample collection for each campaign, and resulting sample sizes after cytology for analysis
| Site | Campaign | Date/time | °C |
|
| % Cells w/UV | % Cells w/MV |
|---|---|---|---|---|---|---|---|
| Göschenen | 1 | 22.05.2019 11:10–12:55 | 7.8−10.8 | 110 | 8 | 17.27 | 24.55 |
| Göschenen | 2 | 14.06.2019 11:29–12:20 | 21.3 | 110 | 4 | 16.36 | 17.27 |
| Göschenen | 3 | 30.06.2019 12:36–13:40 | 31.5–32.3 | 8 | 2 | 12.5 | 12.5 |
| Moutier | 1 | 13.05.2019 11:43–15:05 | 10.5–13 | 24 | 3 | 0 | 45.83 |
| Moutier | 2 | 03.06.2019 11:55–13:41 | 23.5–28 | 33 | 4 | 18.18 | 27.27 |
| Moutier | 3 | 24.06.2019 10:35–12:00 | 18.5–24 | 39 | 3 | 25.64 | 35.9 |
Campaign corresponds to sample collection date for each site, and date/time gives the collection date and time. °C is the temperature range during collection. “n Cells” gives the number of meiocytes scored, and “n Ind.” the number of individual plants sampled. “% cells w/UV” is the percentage of cells that contain univalents and “% cells w/MV” is the percentage of cells that contain multivalents.
Polynomial regression model outputs of the relationship between average crossover rate and each temperature period
| Crossover rate model | Model equation |
|
|
|
|---|---|---|---|---|
| Temperature during collection | lm(Average Crossover Rate ~ poly(Collection Temperature, degree = 2, raw = T)):Site | .54 | 5.58 (4,19) | . |
| Temperature 30 h before collection | lm(Average Crossover Rate ~ poly(Temperature 30 h before collection, degree = 2, raw = T)):Site | .28 | 1.83 (4,19) | .16 |
| Temperature 20 h before collection | lm(Average Crossover Rate ~ poly(Temperature 20 h before collection, degree = 2, raw = T)):Site | .47 | 4.25 (4,19) | . |
| Temperature 10 h before collection | lm(Average Crossover Rate ~ poly(Temperature 10 h before collection, degree = 2, raw = T)):Site | .42 | 3.37 (4,19) | . |
| Temperature 10–30 h before collection | lm(Average Crossover Rate ~ poly(Temperature 10–30 h before collection, degree = 2, raw = T)):Site | .53 | 5.33 (4,19) | . |
Crossover Rate model gives the model used. Model Equation gives the equation. R2 gives the R2 value from the polynomial regression fit. F(df) gives the F‐value and in parentheses the degrees of freedom. The bold values indicate statistical significance (p < 0.05).
Linear regression model outputs of univalent rate and multivalent rate as a function of crossover rate
| Model | Model equation |
|
|
|
|---|---|---|---|---|
| Univalent rate | lm(Crossover Rate ~ Univalent Rate):Site | .1531 | 29.01 (2,321) | <.001 |
| Multivalent rate | lm(Crossover Rate ~ Multivalent Rate):Site | .08953 | 15.78 (2,321) | <.001 |
FIGURE 3Univalent and multivalent formation. (a) Univalent (left) and multivalent (right) incidence per cell plotted against crossover rate measured for the same cell. Best fit linear regression fits are shown with grey shading indicating the 95% confidence interval. (b) Average univalent (left) and multivalent (right) rate per individual plotted against the temperature experienced by that individual averaged across the 10–30 h before sampling. There was no significant linear or polynomial trend for univalent rate, while multivalents showed a polynomial trend for MOU and a linear fit for GOS (grey shading indicating the 95% confidence interval). (c) Average univalent (left) and multivalent (right) rate per individual across the three campaigns. In all panels, Blue = GOS, orange = MOU
Polynomial regression model outputs of the relationship between average multivalent rates and each temperature period
| Multivalent rate model | Model equation |
|
|
|
|---|---|---|---|---|
| Temperature during collection | lm(Average Multivalent Rate ~ poly(Collection Temperature, degree = 2, raw = T):Site | .45 | 3.89 (4,19) | .018 |
| Temperature 30 h before collection | lm(Average Multivalent Rate ~ poly(Temperature 30 h before collection, degree = 2, raw = T):Site | .49 | 4.59 (4, 19) | .0092 |
| Temperature 20 h before collection | lm(Average Multivalent Rate ~ poly(Temperature 20 h before collection, degree = 2, raw = T):Site | .59 | 6.80 (4,19) | .0014 |
| Temperature 10 h before collection | lm(Average Multivalent Rate ~ poly(Temperature 10 h before collection, degree = 2, raw = T):Site | 0.55 | 5.78 (4,19) | .0032 |
| Temperature 10–30 h before collection | lm(Average Multivalent Rate ~ poly(Temperature 10–30 h before collection, degree = 2, raw = T):Site | 0.53 | 5.33 (4,19) | .0048 |