| Literature DB >> 29769358 |
Frédéric Delsuc1, Melanie Kuch2, Gillian C Gibb3,4, Jonathan Hughes2, Paul Szpak5, John Southon6, Jacob Enk2,7, Ana T Duggan2, Hendrik N Poinar8.
Abstract
Mylodon darwinii is the extinct giant ground sloth named after Charles Darwin, who first collected its remains in South America. We have successfully obtained a high-quality mitochondrial genome at 99-fold coverage using an Illumina shotgun sequencing of a 12 880-year-old bone fragment from Mylodon Cave in Chile. Low level of DNA damage showed that this sample was exceptionally well preserved for an ancient subfossil, probably the result of the dry and cold conditions prevailing within the cave. Accordingly, taxonomic assessment of our shotgun metagenomic data showed a very high percentage of endogenous DNA with 22% of the assembled metagenomic contigs assigned to Xenarthra. Additionally, we enriched over 15 kb of sequence data from seven nuclear exons, using target sequence capture designed against a wide xenarthran dataset. Phylogenetic and dating analyses of the mitogenomic dataset including all extant species of xenarthrans and the assembled nuclear supermatrix unambiguously place Mylodon darwinii as the sister-group of modern two-fingered sloths, from which it diverged around 22 million years ago. These congruent results from both the mitochondrial and nuclear data support the diphyly of the two modern sloth lineages, implying the convergent evolution of their unique suspensory behaviour as an adaption to arboreality. Our results offer promising perspectives for whole-genome sequencing of this emblematic extinct taxon.Entities:
Keywords: Mylodon darwinii; Xenarthra; ancient DNA; mitochondrial genomes; nuclear data; phylogenetics
Mesh:
Substances:
Year: 2018 PMID: 29769358 PMCID: PMC5966596 DOI: 10.1098/rspb.2018.0214
Source DB: PubMed Journal: Proc Biol Sci ISSN: 0962-8452 Impact factor: 5.349
Figure 1.(a) DNA damage profiles from the Mylodon bone sample (12 880 ± 35 14C yrpb) compared to a fossil glyptodont sample (Doedicurus sp.) dated at (12 015 ± 50 14C yrpb), a 40-year-old museum specimen of greater fairy armadillo (Calyptophractus retusus) and three modern xenarthran samples. (b) Taxonomic assignation of 223 contigs assembled from Mylodon shotgun reads represented with Krona.
Figure 2.Bayesian consensus phylograms of Pilosa obtained under the site-heterogeneous CAT-GTR+G4 mixture model for the (a) mitogenomic and (b) nuclear datasets. Values at nodes represent clade posterior probabilities under the CAT model (PPCAT), mixed model (PPPART), and maximum-likelihood bootstrap percentages under a partitioned model (BPML). Asterisks indicate maximum support from all statistical indices. The complete phylograms are available in electronic supplementary material, figures S3–S8. Graphical representation and taxon images derive from Gibb et al. [21].
Figure 3.Bayesian chronograms of Pilosa obtained using a rate-autocorrelated log-normal relaxed molecular clock model under the CAT-GTR+G4 mixture model with a birth death prior on the diversification process, and six soft calibration constraints for the (a) mitogenomic and (b) nuclear datasets. Mean divergence dates and associated 95% credibility intervals are represented as node bars. Plain black node bars indicated calibration constraints. The main geological periods follow the geological time scale of the Geological Society of America (E, early; M, middle; L, late; Palaeo., Palaeocene; Pli., Pliocene; P., Pleistocene). The complete chronograms are available in the electronic supplementary material (electronic supplementary material, figures S9 and S10). Graphical representation and taxon images derive from Gibb et al. [21].
Divergence time estimates for the main xenarthran nodes inferred using the site-heterogeneous CAT-GTR+G4 substitution model and an autocorrelated log-normal (LN) relaxed molecular clock model. Mean posterior estimates, associated standard errors and 95% credibility intervals are expressed in million years ago (mean date ± s.d. [95% CredI]). s.d., standard deviation; 95% CredI, 95% credibility interval; MRCA, most recent common ancestor.
| nodes | mitogenomes | nuclear exons |
|---|---|---|
| Xenarthraa | 67.3 ± 3.2 [59.9–71.4] | 69.3 ± 2.2 [63.5–71.8] |
| Pilosa MRCAa
| 55.6 ± 4.4 [46.4–63.2] | 61.2 ± 2.5 [55.4–65.0] |
| Folivora MRCAa (sloths) | 24.8 ± 6.2 [15.8–37.6] | 27.7 ± 4.0 [19.6–35.9] |
| Mylodontidae + Megalonychidae (two-fingered sloths) | 21.9 ± 5.7 [13.3–33.9] | 22.5 ± 3.7 [15.5–30.6] |
| Megalonychidae MRCA (two-fingered sloths) | 4.7 ± 1.5 [2.5–8.3] | 3.8 ± 1.1 [2.2–6.5] |
| Bradypodidae MRCA (three-fingered sloths) | 14.3 ± 4.1 [8.4–23.1] | 12.1 ± 2.4 [7.8–17.5] |
| 5.4 ± 1.8 [2.8–9.6] | 4.5 ± 1.1 [2.7–7.0] | |
| 4.2 ± 1.5 [2.2–7.7] | 3.9 ± 1.0 [2.3–6.2] | |
| Vermilingua MRCAa (anteaters) | 34.2 ± 5.1 [23.9–44.2] | 43.7 ± 3.2 [36.6–49.7] |
| Myrmecophaga/Tamandua | 10.7 ± 3.0 [5.6–17.6] | 11.9 ± 2.1 [8.4–16.7] |
| 0.8 ± 0.3 [0.4–1.5] | 2.0 ± 0.5 [1.2–3.2] | |
| C | 44.2 ± 3.5 [37.9–51.5] | 42.3 ± 2.4 [37.7–47.2] |
| Dasypodidae MRCA (long-nosed armadillos) | 11.5 ± 3.4 [7.2–20.4] | 8.7 ± 1.6 [6.3–12.4] |
| Chlamyphoridae MRCA | 36.6 ± 3.3 [31.2–44.1] | 33.4 ± 2.1 [29.7–38.2] |
| Euphractinae MRCA (hairy armadillos) | 10.3 ± 2.7 [6.4–16.6] | 6.1 ± 1.3 [4.0–9.2] |
| Chlamyphorinae/Tolypeutinae | 32.4 ± 3.1 [27.8–39.7] | 31.5 ± 2.0 [28.0–36.0] |
| Chlamyphorinae MRCA (fairy armadillos) | 19.7 ± 2.7 [15.5–26.3] | 14.8 ± 2.4 [10.4–19.9] |
| Tolypeutinae MRCAa | 25.8 ± 2.6 [22.5–32.5] | 23.7 ± 1.3 [21.7–27.1] |
| 22.5 ± 2.5 [19.1–28.8] | 21.1 ± 1.5 [18.6–24.6] | |
| 13.7 ± 2.0 [10.7–18.4] | 11.9 ± 1.5 [9.2–15.2] | |
| 8.4 ± 1.5 [5.9–11.9] | 6.5 ± 1.4 [4.1–9.4] |
aUsed as a priori calibration constraints.