| Literature DB >> 32324877 |
Yudong Cai1, Weiwei Fu1, Dawei Cai2, Rasmus Heller3, Zhuqing Zheng1, Jia Wen1, Hui Li1,4, Xiaolong Wang1, Akil Alshawi5,6, Zhouyong Sun7, Siqi Zhu2, Juan Wang8, Miaomiao Yang7, Songmei Hu7, Yan Li1, Zhirui Yang1, Mian Gong1, Yunan Hou1, Tianming Lan9,10, Kui Wu11,12, Yulin Chen1, Yu Jiang1, Xihong Wang1.
Abstract
Goats are one of the most widespread farmed animals across the world; however, their migration route to East Asia and local evolutionary history remain poorly understood. Here, we sequenced 27 ancient Chinese goat genomes dating from the Late Neolithic period to the Iron Age. We found close genetic affinities between ancient and modern Chinese goats, demonstrating their genetic continuity. We found that Chinese goats originated from the eastern regions around the Fertile Crescent, and we estimated that the ancestors of Chinese goats diverged from this population in the Chalcolithic period. Modern Chinese goats were divided into a northern and a southern group, coinciding with the most prominent climatic division in China, and two genes related to hair follicle development, FGF5 and EDA2R, were highly divergent between these populations. We identified a likely causal de novo deletion near FGF5 in northern Chinese goats that increased to high frequency over time, whereas EDA2R harbored standing variation dating to the Neolithic. Our findings add to our understanding of the genetic composition and local evolutionary process of Chinese goats.Entities:
Keywords: zzm321990 EDA2Rzzm321990 ; zzm321990 FGF5zzm321990 ; Chinese goats; adaptation; ancient DNA; population genomics
Mesh:
Substances:
Year: 2020 PMID: 32324877 PMCID: PMC7306693 DOI: 10.1093/molbev/msaa103
Source DB: PubMed Journal: Mol Biol Evol ISSN: 0737-4038 Impact factor: 16.240
Sample Information of All Ancient Chinese Goats
| ID | Site | Date (YBP) | Sex | Mt Hap | Cov. Auto | Cov. Mt |
|---|---|---|---|---|---|---|
| SMG04 | Shimao | ∼3,900 | M | A | 0.013 | 2.788 |
| SMG05 | Shimao | ∼3,900 | F | A | 0.007 | 2.342 |
| SMG07* | Shimao | ∼3,900 | M | B | 0.036 | 8.208 |
| SMG10 | Shimao | ∼3,900 | M | A | 0.097 | 4.067 |
| SMG11* | Shimao | ∼3,900 | M | C | 0.020 | 9.730 |
| MZG20 | Muzhuzhuliang |
| F | A | 1.051 | 41.872 |
| MZG28 | Muzhuzhuliang | ∼2,700 | F | A | 0.024 | 3.344 |
| MZG29 | Muzhuzhuliang | ∼2,700 | F | A | 0.181 | 15.586 |
| MZG34 | Muzhuzhuliang | ∼2,700 | F | A | 0.092 | 5.273 |
| MZG38 | Muzhuzhuliang | ∼2,700 | F | A | 0.105 | 8.602 |
| BG1 | Xinzhouyaozi | ∼2,500 | F | B | 0.067 | 45.689 |
| BG2 | Xinzhouyaozi | ∼2,500 | F | A | 0.204 | 78.515 |
| BG3 | Xinzhouyaozi | ∼2,500 | M | A | 0.118 | 72.911 |
| BG4 | Xinzhouyaozi | ∼2,500 | F | D | 0.059 | 34.689 |
| LSM11 | Xiaoshuanggucheng | ∼2,500 | F | A | 0.366 | 91.485 |
| WDH03 | Wangdahu | ∼2,500 | F | A | 0.732 | 62.431 |
| WDH05 | Wangdahu | ∼2,500 | F | A | 0.575 | 108.729 |
| WDH06* | Wangdahu | ∼2,500 | F | A | 8.106 | 567.882 |
| WDH08 | Wangdahu | ∼2,500 | M | A | 0.038 | 2.824 |
| JLS05 | Jiulongshan | ∼2,500 | F | C | 0.047 | 2.606 |
| JLS06 | Jiulongshan | ∼2,500 | F | D | 0.354 | 29.336 |
| ZZ01 | Zhongzhuang | ∼2,500 | F | B | 0.135 | 4.226 |
| YJL01 | Yanjialiang | ∼650 | F | A | 7.350 | 661.325 |
| YJL02* | Yanjialiang |
| M | A | 13.439 | 455.267 |
| GTM01 | Tianxi |
| F | B | 0.051 | 3.439 |
| GTM02 | Tianxi |
| F | B | 0.099 | 13.702 |
| GTM03 | Tianxi |
| F | A | 1.524 | 285.982 |
| GTM04 | Tianxi | ∼450 | F | B | 0.020 | 3.629 |
| GTM06 | Tianxi | ∼450 | M | B | 0.202 | 107.890 |
| GTM08 | Tianxi | ∼450 | F | B | 0.181 | 57.152 |
| GTM11 | Tianxi | ∼450 | F | B | 0.189 | 57.842 |
Note.—Samples marked with an asterisk were previously published (Zheng et al. 2020). “Mt Hap,” mitochondrial haplogroup; “Cov. Auto,” mean depth of coverage across autosomes; “Cov. Mt,” mean depth of coverage across mitochondria. Calibrated radiocarbon dates are shown in bold with 95.4% confidence interval. Dates in plain text are estimated from the archaeological context or the radiocarbon dates from the same site (Supplementary Material online). Note that the majority of Muzhuzhuliang belong to the Longshan culture, similar to the Shimao site, while a few remains are more recent. Five Muzhuzhuliang samples were collected in this study. One of them, MZG20, was radiocarbon dated to ~2700 YBP. Therefore, the other four samples in this site without radiocarbon-dated are also marked as ~2700 YBP (Supplementary Material online).
. 1.The genetic origin of Chinese goats. (a) Locations and ages of all ancient samples used in this study. All ancient Chinese goats are labeled, and the numbers of genomes reported are in parentheses. (b) Principal component analysis (PCA) with modern globally distributed goats, ancient Chinese goats, and Neolithic goats around the Fertile Crescent. (c) Allele sharing between Chinese goats and Neolithic goats around the Fertile Crescent. A negative D statistic indicates a higher level of allele sharing between Chinese goats and Neolithic East goats. (d) Allele sharing between Chinese goats and ancient goats from different time periods in the eastern Fertile Crescent. A negative D statistic indicates a higher level of allele sharing between Chinese goats and Chalcolithic Iranian goats. Standard errors are shown with bars. Statistics with a |Z score| <2 are shown with unfilled symbols.
. 2.Genetic differentiation in Chinese goats. (a) Neighbor-Joining (NJ) tree of the Chinese goat population, only modern samples and three ancient (YJL01, YJL02, and WDH06) Chinese goats with at least 3× coverage were included. (b) Principal component analysis (PCA) including all Chinese goats. The ancient samples were projected onto the axes computed using modern populations. All modern samples are represented with crosses, and ancient samples are shown with other symbols according to their age. (c) Mitochondrial haplogroup distributions in different Chinese goat groups. (d) In each test X (Y, Z), a positive D statistic indicates a higher level of allele sharing between X and Z, whereas a negative one indicates a higher level of allele sharing between X and Y. Points with a |Z score| >2 are colored in green. (e) Outgroup f3 statistics for the shared genetic history between ancient Shimao goats and modern Asian goats. Higher f3 values represent a closer genetic affinity with Shimao. The average temperature in January is also shown.
. 3.Genome-wide selection scan. (a) Manhattan plot of the genome-wide distribution of pairwise FST between SC and NC using a 50-kb window size and a 10-kb step size. The threshold of FST values is marked with a horizontal line. Windows selected in NC and SC are colored in blue and red, respectively. (b) Selection signs around FGF5. FST based on single nucleotide polymorphisms (SNPs) is plotted as a line using a nonoverlapping 10-kb sliding window. FST based on copy number variants (CNVs) is plotted as a rectangle. The conservation scores of 100 vertebrate species are shown in green, and H3K4Me1 signals are shown in brown. (c) The frequency of the 504-bp deletion (chromosome 6: 95,454,685–95,455,188 bp) in each population. (d) Sequence context of the 504-bp deletion in different species, showing deletion solely in the goat-mutant (goat-M) type. The black rectangles indicate transcription factor binding sites. (e) Dual-luciferase assay using goat fibroblasts showing that the FGF5 downstream deletion sequence enhanced the activity of luciferase. Data are shown as the mean ± standard error. The P-value was calculated using Student’s t-test.
. 4.Selective sweep region on the X chromosome. (a) Selection signals around EDA2R in X chromosome (NW_017189516.1). FST, θπ, and Tajima’s D were plotted as a line using a nonoverlapping 10-kb sliding window. (b) Haplotype network based on pairwise differences within the selective sweep region (chrX: 17,915,001–18,539,000) in EDA2R.