| Literature DB >> 32933168 |
Aleksandra Skalska1, Christoph Stritt2, Michele Wyler2, Hefin W Williams3, Martin Vickers4, Jiwan Han5, Metin Tuna6, Gulsemin Savas Tuna7, Karolina Susek8, Martin Swain3, Rafał K Wóycicki9, Saurabh Chaudhary10, Fiona Corke11, John H Doonan11, Anne C Roulin2, Robert Hasterok1, Luis A J Mur3,5.
Abstract
Brachypodium distachyon (Brachypodium) is a non-domesticated model grass species that can be used to test if variation in genetic sequence or methylation are linked to environmental differences. To assess this, we collected seeds from 12 sites within five climatically distinct regions of Turkey. Seeds from each region were grown under standardized growth conditions in the UK to preserve methylated sequence variation. At six weeks following germination, leaves were sampled and assessed for genomic and DNA methylation variation. In a follow-up experiment, phenomic approaches were used to describe plant growth and drought responses. Genome sequencing and population structure analysis suggested three ancestral clusters across the Mediterranean, two of which were geographically separated in Turkey into coastal and central subpopulations. Phenotypic analyses showed that the coastal subpopulation tended to exhibit relatively delayed flowering and the central, increased drought tolerance as indicated by reduced yellowing. Genome-wide methylation analyses in GpC, CHG and CHH contexts also showed variation which aligned with the separation into coastal and central subpopulations. The climate niche modelling of both subpopulations showed a significant influence from the "Precipitation in the Driest Quarter" on the central subpopulation and "Temperature of the Coldest Month" on the coastal subpopulation. Our work demonstrates genetic diversity and variation in DNA methylation in Turkish accessions of Brachypodium that may be associated with climate variables and the molecular basis of which will feature in ongoing analyses.Entities:
Keywords: Brachypodium; DNA methylation; drought; flowering; genome; phenomics
Year: 2020 PMID: 32933168 PMCID: PMC7556024 DOI: 10.3390/ijms21186700
Source DB: PubMed Journal: Int J Mol Sci ISSN: 1422-0067 Impact factor: 5.923
Geographical origins of Brachypodium accessions used in this study (sorted by collecting date).
| Region | Station | Collecting Date | Latitude | Longitude | Altitude (m) * |
|---|---|---|---|---|---|
| 2 | 1 | 22-May-2016 | 38.5055 | 27.31671667 | 349 |
| 2 | 5 | 23-May-2016 | 37.49243333 | 27.3395 | 67 |
| 2 | 8 | 24-May-2016 | 37.20506667 | 27.65306667 | 40 |
| 2 | 9 | 24-May-2016 | 37.31233333 | 28.03705 | 626 |
| 2 | 14 | 25-May-2016 | 36.94201667 | 30.96305 | 10 |
| 2 | 20 | 27-May-2016 | 36.95461667 | 34.7507 | 161 |
| 1c | 25 | 28-June-2016 | 39.86911667 | 32.7329 | 1042 |
| 1c | 26 | 28-June-2016 | 39.68008333 | 32.19811667 | 879 |
| 1c | 27 | 29-June-2016 | 38.40685 | 34.03873333 | 1122 |
| 1c | 28 | 30-June-2016 | 38.738 | 34.83881667 | 1063 |
| 1a | 29 | 1-July-2016 | 37.73385 | 38.53376667 | 668 |
| 1a | 30 | 1-July-2016 | 37.69656667 | 37.89476667 | 696 |
| 1a | 31 | 2-July-2016 | 37.03268333 | 37.60995 | 735 |
| 1a | 32 | 2-July-2016 | 37.23601667 | 38.87008333 | 605 |
| 1c | 34 | 3-July-2016 | 39.09433333 | 33.39311667 | 933 |
| 1c | 35 | 3-July-2016 | 40.19286667 | 32.59326667 | 1059 |
| 4 | 36 | 3-July-2016 | 40.73106667 | 31.51755 | 865 |
| 3 | 38 | 7-July-2016 | 41.12035 | 26.65313333 | 58 |
| 3 | 40 | 23-July-2016 | 40.61361667 | 26.43273333 | 63 |
| 3 | 41 | 27-July-2016 | 41.0926 | 27.22096667 | 97 |
| 3 | 42 | 8-August-2016 | 41.3691 | 27.13661667 | 50 |
| 4 | 45 | 15-August-2016 | 40.86231667 | 32.54991667 | 1242 |
| 4 | 47 | 16-July-2016 | 40.87441667 | 35.60698333 | 605 |
| 4 | 49 | 16-July-2016 | 40.59275 | 36.83505 | 283 |
| 4 | 51 | 16-July-2016 | 40.15375 | 38.14713333 | 920 |
| 4 | 52 | 19-July-2016 | 41.32165 | 36.25826667 | 128 |
| 3 | 54 | 29-July-2016 | 40.83846667 | 27.02001667 | 205 |
| 3 | 55 | 29-July-2016 | 40.5003 | 26.70376667 | 88 |
Five distinct regions (1a, 1c, 2, 3, and 4) were selected for Brachypodium sampling defined by Köppen climate classifications [25]. There were at least five sampling sites (“stations”) within each region and individual stations were sampled at least 12 times to derive individual accessions. Thus, for example, an accession designed 2_14_13 refers respectively to region, station, individual plant sample. *—meters above sea level.
Figure 1(A) Genetic diversity of Brachypodium germplasm from different environmental regions of Turkey as indicated using hierarchical clustering. (B) Ancestry coefficients were estimated with TESS3 two ancestral groups amongst Brachypodium accessions (listed in Supplementary Materials Table S1) and (C) mapped to Turkey by purple and yellow colors. The yellow and purple horizontal regions indicate accessions corresponding to the ancestral groups and geographically distinguishable as coastal and central subpopulations, respectively. The correspondence between the coastal and central subpopulations and the previously defined Extremely Delayed Flowering (EDF+) and Turkish (T+) populations [10], respectively, is indicated.
Figure 2Hierarchical clustering analysis showing variation in whole genome (A) CpG, (B) CHG and (C) CHH methylation patterns based on the similarity of the accession’s methylation profiles. Accessions from particular regions are color-coded (1a—orange, 1c—light green, 2—dark green, 3—light blue, 4—dark blue). Bd21 (from Iraq) is indicated in black. The yellow and purple horizontal bars indicate accessions broadly classified as central and coastal subpopulations, respectively. Region 1c accessions (1c_25_14, 1c_25_15, 1c_35_1, 1c_35_7) with an Extremely Delayed Flowering (EDF+) [10] genotype are also located with the coastal subpopulation clade and are given that classification. Although classified as part of the coastal subpopulation the S+ genotype accessions 2_14_15, 2_14_20, 2_20_16, were found in distinct clades in each methylation context; especially in CHH (C).
Figure 3Phenotypic variation in the Turkish collection of Brachypodium. Brachypodium accessions (n = 8 plants) were vernalized for six weeks at 4 °C before being transferred to 22 °C and either maintained with full watering (n = 4 plants, white bars) or at 15% soil water content (n = 4 plants, black bars). At 12 d the plants were imaged at the National Plant Phenomics Centre, Aberystwyth, UK, where (A) height and (B) side area were derived. Data are grouped based on regional origins (1a, 1c, 2, 3, 4); (C) yellow pixels were extracted from the images of plants. Pixel data are presented as % of the total pixel count for the whole plant. The purple and yellow horizontal bars on (A–C) indicate data from accessions sampled from central (1a, 1c) and coastal (2, 3, 4) subpopulations, respectively; (D) after a further eight weeks the percentage of control plants originating from the coastal and central subpopulations which had flowered was measured.
Figure 4Bioclim modelling of environmental variables. These indicated the climate suitability of Brachypodium subpopulations in Turkey. (A) Color-coded, Maxent model climate suitability for the central subpopulation. Black squares represent sampling sites for the central subpopulation; (B) Maxent model climate suitability for the coastal subpopulation. Black circles represent sampling sites for the coastal subpopulation; (C) Maxent model response curve for the relationship between the probability of presence of the coastal subpopulation and the Minimum Temperature of the Coldest Month (°C); (D) Maxent model response curve for the relationship between the probability of presence of the coastal subpopulation and the Precipitation of the Driest Quarter (mm); (E) Maxent model response curve for the relationship between the probability of presence of the central subpopulation and the Precipitation of the Driest Quarter (mm).