| Literature DB >> 30177868 |
Ardern Hulme-Beaman1,2, Thomas Cucchi3, Allowen Evin4, Jeremy B Searle5, Keith Dobney1,6.
Abstract
Taxonomic uncertainties in the Rattus genus persist due to among-species morphological conservatism coupled with within-species environmental variation in morphology. As a result, this genus contains a number of possible cryptic species. One important example can be found in R. praetor, where morphological studies indicate it is a possible species complex. Genetic studies of R. praetor (limited to analysis of mitochondrial DNA) have been inconclusive, but do indicate such subdivision. Here we use geometric morphometrics to explore this possible species complex by analysing the dental traits of 48 specimens from New Guinea and neighbouring regions. We find separate molar morphologies for Bougainsville Island, central New Guinea and west New Guinea which cannot be easily explained by different environmental factors (climate, precipitation and altitude), strongly suggesting the existence of a number of evolutionarily distinct taxa within what is currently called R. praetor thus supporting previous suggestions that R. praetor is a species complex. Our findings demonstrate the potential of advanced morphological analyses in identifying separate species, contrary to the claims of morphological conservatism. Future analyses should combine geometric morphometrics with genetic analyses over the species range and include sub-fossil specimens from the Bismarck archipelago and Solomon Islands to resolve the evolutionary history of R. praetor.Entities:
Keywords: Cryptic species; Geometric morphometrics; Phylogeography; Rat; Sahul
Year: 2018 PMID: 30177868 PMCID: PMC6067089 DOI: 10.1016/j.mambio.2018.04.002
Source DB: PubMed Journal: Mamm Biol ISSN: 1616-5047 Impact factor: 1.863
Fig. 1(A) Map of New Guinea and neighbouring islands indicating approximated distribution of Rattus praetor (cross hatching) (Taylor et al., 1982). All insular populations east and north of New Guinea belong to the subspecies R. p. praetor and all mainland New Guinea populations belong to R. p. coenorum. Approximate sea levels of 50 m (dark grey) and 100 m (light grey) below modern mean sea level are indicated and represent the likely sea levels at 12 and 21 Ka BP respectively (Sathiamurthy and Voris, 2006; Voris, 2000). Points reflect location of specimens used in this study and colours indicate group classification identified using clustering analyses. (B) PCA of island (solid line) versus mainland (dashed line) tooth shape for R. praetor, with colours matching the results found from the morphological cluster analyses. The mean tooth shape of each group with additional landmarks to capture the curves of the cusps is plotted on the PCA in its group’s corresponding colour (see SI 1 and SI Fig. 1 for mean tooth shapes of analysed landmark configurations).
Sample information table. This table includes the unique locations from museum labelling, the approximate area that location represents and the number of specimens from that location in this study.
| Landmass | Location | Approximate location area (km2) | Sample size |
|---|---|---|---|
| New Guinea | Bokondini | 1000 | 4 |
| New Guinea | Bulung River, Huongulf | 1000 | 2 |
| New Guinea | Prauwenbivak | 10 | 1 |
| New Guinea | Sibil Valley | 2000 | 2 |
| New Guinea | Teluk Etna | 1400 | 11 |
| New Guinea | West Sepik, Brugnowi | 20 | 4 |
| New Guinea | West Sepik, May River | 40 | 2 |
| Bougainville Island | Cape Torokina | 30 | 9 |
| Bougainville Island | Pokapa, SW of Tinputz | 100 | 3 |
| Bougainville Island | Tinputz | 10 | 3 |
| Bougainville Island | Mt. Karaea, Wakonvasike | unknown | 1 |
| Bougainville Island | Mutahi, SW of Tinputz | 20 | 3 |
| Bougainville Island | Mt. Balbi | 20 | 3 |
Fig. 2Schematic of a Rattus first left mandibular molar showing landmark protocol.