Figures
Abstract
Background
The lava mouse, Malpaisomys insularis, was endemic to the Eastern Canary islands and became extinct at the beginning of the 14th century when the Europeans reached the archipelago. Studies to determine Malpaisomys' phylogenetic affinities, based on morphological characters, remained inconclusive because morphological changes experienced by this insular rodent make phylogenetic investigations a real challenge. Over 20 years since its first description, Malpaisomys' phylogenetic position remains enigmatic.
Methodology/Principal Findings
In this study, we resolved this issue using molecular characters. Mitochondrial and nuclear markers were successfully amplified from subfossils of three lava mouse samples. Molecular phylogenetic reconstructions revealed, without any ambiguity, unsuspected relationships between Malpaisomys and extant mice (genus Mus, Murinae). Moreover, through molecular dating we estimated the origin of the Malpaisomys/mouse clade at 6.9 Ma, corresponding to the maximal age at which the archipelago was colonised by the Malpaisomys ancestor via natural rafting.
Citation: Pagès M, Chevret P, Gros-Balthazard M, Hughes S, Alcover JA, Hutterer R, et al. (2012) Paleogenetic Analyses Reveal Unsuspected Phylogenetic Affinities between Mice and the Extinct Malpaisomys insularis, an Endemic Rodent of the Canaries. PLoS ONE 7(2): e31123. https://doi.org/10.1371/journal.pone.0031123
Editor: Samuel T. Turvey, Zoological Society of London, United Kingdom
Received: August 31, 2011; Accepted: January 3, 2012; Published: February 21, 2012
Copyright: © 2012 Pagès et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: MP held financial support from the Foundation ARC and is currently funded by a F.R.S.-FNRS fellowship (Belgian Fund for Scientific Research). The present study is part of the Spanish program N CGL2007-62047/BTE. The work benefited from the financial support of the Dirección General de Investigación (MEC), Cabildo Insular de Fuerteventura, French National Center for Scientific Research, University Lyon 1 and ENS de LYON. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Introduction
The Canary Islands comprise seven main volcanic islands that appeared successively between 20.6 and 1.12 million years ago (Ma) ([1]; Figure 1). Located ca. 95 km offshore of the Moroccan coast, these islands have been completely isolated from the mainland since their formation. The minimum water depth between them and the continent averages 1,500 m and no connection with the mainland occurred even during the major Pleistocene sea regressions. Current and past biodiversity of the Canaries is thus the result of over-water dispersal events rather than the product of vicariant evolution.
The eastern islands where fossils of Malpaisomys have been reported are indicated in red. The K-Ar age of subaerial volcanism is indicated for each island [1]. The maps use the General Bathymetric Chart of the Oceans and were drawn with PanMap [83].
Among the vertebrate endemics, the Canarian shrew, Crocidura canariensis is the only living non-flying terrestrial mammal of the archipelago. Three endemic rodents have also been documented since the Quaternary epoch but are nowadays extinct: two giant rats, Canariomys bravoi from Tenerife and Canariomys tamarani from Gran Canaria [2], plus the lava mouse, Malpaisomys insularis, from Fuerteventura, Lanzarote and adjacent islets [3] (Figure 1). The extinction of the genus Canariomys seems to be related to the arrival of the aboriginals [4] some time between 756 cal BC and 313 cal AD [5]. M. insularis survived until the 14th century [6] and probably became extinct due to the introduction of alien mammals by the Europeans [6], [7]. This study focuses on this latter species.
Until now, using morphological data to determine the phylogenetic affinities of this endemic rodent had not resolved the riddle of its relationship to extant Murinae. M. insularis belongs undoubtedly to the subfamily Murinae (Old World Rats and Mice) but its relationships to extant Murinae remained unresolved. There is no fossil evidence to document its morphological evolution from a continental ancestor. Indeed, the earliest remains are evidence of a derived species with uncommon dental and skeletal features [8]. They are consequently difficult to affiliate with certainty to any lineage of Murinae. The first phylogenetic analysis of M. insularis was based on twenty dental traits [3]. It included several extinct and extant Murinae from western Europe and Africa: several genera of Arvicanthini, the black rat (Rattus rattus), the house mouse (Mus musculus), representatives of two genera now shifted from Murinae to Deomyinae, Acomys and Uranomys [9] and the two other Canarian species (Canariomys bravoi and C. tamarani). No clear-cut results were obtained except that Malpaisomys was grouped with Acomys and Uranomys. However, this first phylogeny seemed to be flawed by convergent evolution and did not reflect the currently well-established phylogenetic relationships among the Murinae (e.g. all the representatives of the tribe Arvicanthini sensu Lecompte et al. [10] did not cluster together). A few years later, immunological comparisons of albumin proteins extracted from bones of Malpaisomys and four other extant rodents (Mus, Cavia, Acomys and Uranomys) indicated that Malpaisomys clustered with Mus and was more distant from Acomys and Uranomys [11]. Although technically innovative, the author only tested the position of Malpaisomys within the Murinae (only one murine representative was incorporated into the taxon sampling). The last comparative studies of cranial and dental morphologies included extinct rodents from the late Neogene of western Europe and North Africa to elucidate Malpaisomys' relationships [12], [13]. However no conclusion was settled about its systematics. On the basis of these limited data, Malpaisomys insularis is currently interpreted as a member of the African tribe Arvicanthini [9].
The collection in 2006 and 2007 of geologically young Malpaisomys insularis remains in Fuerteventura [5], [6] combined with ancient DNA studies to tackle new questions on extinct species, gave us the opportunity to clarify the phylogenetic relationships of Malpaisomys independently of morphological data. We provide here the first mitochondrial and nuclear DNA sequences for M. insularis and perform phylogenetic reconstructions that reveal unsuspected affinities to extant rodents. In return, these new results allow us to re-examine the distinctive morphological features of M. insularis in a new evolutionary context.
Materials and Methods
Sampling
The native fauna on Fuerteventura and Lanzarote includes two species: the extinct lava mouse, Malpaisomys insularis and the extant shrew, Crocidura canariensis. Humans introduced alien species, such as the house mouse, Mus musculus and the black rat, Rattus rattus. Materials excavated from cracks in the volcanic sediments or from sediments filling lava tubes were without ambiguity identified as Malpaisomys insularis remains. Their size was higher than expected for shrews or house mice (e.g. the femur length is ca 19 mm and 15 mm for M. insularis, for M. musculus respectively) but smaller than expected for black rats. Moreover, tooth size and molar morphology were unequivocal. The upper and the lower molars were too wide and too stout to belong to Mus and on the contrary, too small to be those of Rattus rattus. The number of their roots was also too limited and their outlines too wide to correspond to black rat molars. Six fossils of Malpaisomys insularis, corresponding to at least four individuals, were analysed in this study (Table 1). To increase the quantity of material used for DNA extraction, 3 half-mandibles were pooled together and were considered further as a single sample (CH475) leading to a total dataset of four samples. Fossils were collected in two different sites from Fuerteventura: Cueva del Llano (in 2006) and Montaña de la Arena (in 2007). The material was obtained through field work within the Research Projects “Cronología y causas de las extinciones de vertebrados autóctonos en Canarias y Baleares: un análisis comparativo. I & II”, both funded by the Dirección General de Investigación of the Spanish Ministerio de Educación y Ciencia, and with the agreement and support of the Consejería de Cultura, Patrimonio Histórico, Educación y Juventud of the Cabildo Insular de Fuerteventura.
In Cueva del Llano, white specimens were chosen because of their colour that may indicate a possible younger age than brown coloured specimens. They had been collected directly from the youngest layer, and the dates published for the cave stratigraphy can be extrapolated to these specimens [5], [6]. An age of ca. 800 calibrated years BC can be assigned for Cueva del Llano specimens [5]. The bones from Montaña de la Arena are probably younger than 1300 calibrated years BC [6].
Ancient DNA analysis
Paleogenetic work was carried out at PALGENE, the French National Platform of Paleogenetics (CNRS, ENS Lyon, France), following strict ancient DNA procedures [14], [15]. DNA was extracted from bone samples following the phenol–chloroform–isoamylalcohol method (described in [14], [16]) or the silica based-protocol detailed by [17]. Samples from non-relative species such as Ursus spelaeus (cave bear), Canis familiaris (dog) and Crocuta spelaea (cave hyena) were extracted at the same time to evidence any putative carrier-effect of the ancient DNA extracts [15], [16], [18].
15 short overlapping fragments (97–219 bp including primers) were targeted to obtain the nearly whole cytochrome b gene (cytb). 4 fragments were defined to cover 271 bp of the first exon of the gene encoding the Interphotoreceptor Retinoid Binding Protein (IRBP) (Figure 2). Primer sets (Table 2) were designed based on the alignment of extant murid species sequences available in GenBank. Generally, at least two independent PCR amplifications by fragment were performed in 25 µL reaction volumes containing 2.5 units of Perkin Elmer Gold Taq polymerase (Applied Biosystems), 1 mg/mL BSA (Roche, 20 mg/mL), 2 mM MgCl2, 250 µM of each dNTP, 0.5 µM of primers. For each independent PCR attempt, a range of dilutions was performed to find the best compromise between the inhibitor's concentration and the targeted DNA molecule concentration [19]. DNA was amplified with a 5 min activation step at 95°C followed by 55 to 60 cycles of denaturation (94°C, 30 s), annealing (see Table 2 for temperature, 30 s) and elongation (72°C, 45 s). Four independent blanks were carried out for each PCR attempt: i) an extraction blank to monitor exogenous contamination during extraction, ii) a PCR blank to control PCR products, iii) a PCR blank that remained opened during PCR to monitor aerosols during PCR preparation, and iv) a cross-contamination blank to control a putative carrier-effect of the ancient DNA extracts [15], [16]. Amplification products were systematically cloned using Topo TA Cloning for sequencing kit (Invitrogen) to check out artefactual substitutions due to post-mortem DNA decay. Clones of independent amplifications were sequenced to determine consensus sequences (Macrogen Seoul Korea; Genome Express, Grenoble; Cogenics).
IRBP primers are positioned on the reference sequence of Mus Coelomys pahari (GenBank accession number EU349864). For each mt fragment, samples that yielded successful amplifications are mentioned into boxes. ** indicates PCR attempt where numts were occasionally co-amplified.
Phylogenetic analyses
Malpaisomys sequences were added to a larger dataset including sequences of extant species representing 3 subfamilies of Muridae: Murinae (36 genera, 60 species), Deomyinae (4 species) and Gerbillinae (3 species). Gerbillinae were included since they were closely related to Deomyinae and Murinae [20], the two putative subfamilies to which Malpaisomys might belong [3], [11]. Species were selected in order to represent each tribe of Murinae sensu Lecompte et al., 2008 [10] and depending on their availability in GenBank (Table S1). Cytb and IRBP sequences were aligned by eye and translated into peptide sequences to ensure sequence orthology. Congruence between mitochondrial (mt) and nuclear phylogenetic information was first assessed via phylogenetic reconstruction based on each independent gene. The two nucleotide datasets were then combined into a single one using SEAVIEW [21]. Thus, a total of 2,376 bp were considered in the subsequent phylogenetic analyses (992 bp of the cytb and 271 bp of the IRBP gene were obtained for Malpaisomys, the remaining part of the sequences was thus treated as missing data for this taxa). To be sure that missing data could not bias our results, phylogenetic reconstructions were re-run on the same datasets (cytb, IRBP and concatenated dataset) but limited to the data available for Malpaisomys.
Phylogenetic trees were reconstructed using two probabilistic approaches: maximum likelihood (ML) and Bayesian inferences (BI). The appropriate model of evolution was first determined for each gene and each codon position using corrected Akaike information criterion (AICc) and the Modeltest software [22]. The general time-reversible GTR+I+Γ model was selected for both cytb and IRBP partitions. Partitioned ML analysis was performed using RAxML 7.0.3 [23]. The GTR+Γ+I model (option –m GTRGAMMAI) was selected for the six partitions (option –q multipleModelFileName). Individual α-shape parameters, GTR-rates, proportion of invariable sites and base frequencies were estimated and optimized for each partition. Robustness of the tree was assessed using the default bootstrap procedure with 1,000 replications (option -# numberOfRuns) using the ML tree estimated with RAxML tree as starting tree (option –t) [24]. Bayesian analyses were performed using MrBayes v3.1 [25]. Four independent runs of 10,000,000 generations sampled every 100th generation were performed applying independent GTR+I+Γ model of evolution to each partition (partitioning by gene and by codon position). A burn-in period of 2,500 trees (250,000 generations) was determined graphically using Tracer1.2 [26].
Assessing the confidence of the tree selection
Likelihood-based tests of alternative topologies were achieved using Bayes factors (i.e. the ratio of marginal likelihoods of two competitive models, here two competitive topologies) following methods described in [27]. MrBayes [25] was used to compare the optimal topology (i.e. the MrBayes tree) to topologies constrained to contain alternative monophyletic group including Malpaisomys (e.g. Malpaisomys embraced in a monophyletic Arvicanthini group). The harmonic mean of the likelihood values sampled from the posterior distribution of the MrBayes analysis was considered as a rough estimate of the marginal likelihood of the hypothesis [28]. Harmonic mean of the log-likelihoods were calculated using the sump command in MrBayes, based on the pooled likelihood scores of the post–burn-in trees (burn-in = 2,500) from the replicate searches for each topology (two independent runs of 10,000,000 generations sampled every 100th generation, applying independent GTR+I+Γ model of evolution to each partitions). When value of (2lnBF) was higher than 10, it was considered to be very strong evidence favouring one hypothesis (i.e. the topology with the highest likelihood score) over the other [29].
Shimodaira-Hasagawa (SH-) tests and Approximately Unbiased (AU-) tests were also performed to compare the best RAxML tree to alternative topologies. For a SH-test be accurate, the set of the compared topologies should necessarily contain every topology that can be possibly entertained as the true topology [30]. As the a priori selection of the topologies could be thorny, we decided to achieve AU-tests that relax this assumption. The site-wise lo-likelihoods of each tree was estimated from the concatenated dataset using PAUP [31] (Lscores command, options sitelikes, scorefile and SHtest = FullOpt) and applying a GTR+I+Γ model. Log-likelihoods of site-pattern trees were then used to calculate the p-values for the AU- and the SH- tests in CONSEL [32].
Estimating dates of divergences
Divergence dates were estimated using the relaxed molecular clock approaches accounting for change in evolutionary rate over times, implemented in Multidivtime [33] and in BEAST version 1.6.1 [34], [35]. Fossil calibrations (FC) of node were set as hard bounds in Multidivtime, as soft bounds in BEAST (lognormal distribution with the median value equal to the mean of fossil calibration). We selected the three following fossil calibrations:
FC1: Following Steppan [36], we considered the detailed and well-calibrated fossil record from the Siwalik succession in Pakistan as an accurate depiction of murine history and Progonomys as either the Most Recent Common Ancestor (MRCA) of extant murines or a predecessor (12.3–8.1 Ma, [37]). Antemus which does not present the fully developed modern murine configuration (i.e. the synapomorphic triserial cusp arrangement of modern murines first seen in Progonomys but not in Antemus) predates the MRCA of murines [37]. Consequently we assigned the oldest record of Progonomys at 12.3 Ma [37] to the split between the tribe Phloemyini and the other tribes of Murinae. The conservative interval of 10.3–14.3 Ma was used in Multidivtime analysis.
FC2: Fossils of Apodemus jeanteti (7 Ma) and Apodemus dominans (7 Ma) were considered to be affiliated to A. mystacinus and A. sylvaticus respectively [38]. Consequently, we assigned a minimum age of 7 Ma to the split between A. mystacinus and A. sylvaticus.
FC3: We assigned a minimum age of 5.7 Ma to the split of Otomyini/Arvicanthi as the earliest record of the African Arvicanthini representative is dated between 5.7–5.9 Ma [39].
Even if soft bounds were set in BEAST, if there is no significant signal in the data, then the posteriors will be entirely affected by the priors. Consequently, the analyses were first performed omitting each of the calibration points in turn to assess whether the molecular dates are the result of the fossil constraints (i.e. if the same or similar divergence dates are always recovered) with BEAST and Multidivtime.
In Multidivtime, divergence times were estimated from the partitioned dataset (cytb and IRBP) for the RAxML topology following the documentation files written by Rutschmann [40] and using parameter estimates derived with PAML [41] as described by Yoder and Yang [42]. In BEAST, an uncorrelated lognormal model of evolution rate variation, a Yule speciation model for branching rates (species-level phylogeny), and a GTR+I+Γ nucleotide substitution model were implemented on the partitioned dataset (cytb and IRBP). Substitution and clock models were unlinked among partitions. The starting topology was the RaxML tree as in Multidivtime analysis. The analysis was run for 80 million generations and sampled every 1,000 generations. Convergence of the run as well as the effective sample size of each parameter trace was assessed using Tracer1.2 [26]. Posterior estimates and 95% Highest Posterior Density (HPD) limits of node heights of trees produced by BEAST were summarized using TreeAnnotator (burnin = 20,000), distributed in BEAST package.
Results and Discussion
Ancient DNA retrieval and sequence authentication
Sequences obtained in this study were deposited in EMBL with the following accession numbers JN418213-JN418217. For mt DNA, 992 bp of the cytb gene were determined for two samples (i.e. CH475 and CH559) using 12 to 15 overlapping fragments (Figure 2 and Table 3). Only two mt fragments (C1 and C6) were amplified for CH476 and none were obtained for CH560 (Table 3). Because mt DNA is present in higher copy number than nuclear DNA per cell, it is usually more difficult to obtain nuclear fragments than mt ones [43]. Indeed, only one sample, CH559, allowed the amplification of 4 overlapping fragments of the IRBP gene, i.e. 271 bp (Table 3). In summary, we were able to detect preserved DNA in 3 out of 4 samples analysed. Similar DNA preservation rates are reported in the literature for Canarian fossil specimens (e.g. cytb sequences obtained from four out of five specimens of the extinct seabird, Puffinus olsoni; no successful amplifications for four fossils of the dune shearwater, Puffinus holeae [44]). These moderate success rates are probably due to the warm climatic conditions that prevail in the Canary archipelago, known to be unfavourable for long-term DNA preservation.
When targeting mt DNA, numt amplifications are common and largely documented for rodents (e.g. in Apodemus [45]; Calomys [46]). If not detected, numts can lead to an incorrect interpretation of the data and to an inaccurate phylogenetic position of the analysed species [47]. In our study, overlapping fragments yielded an almost complete cytb sequence (992 bp) considered as the genuine mt copy. We also detected occasional amplifications of divergent sequences showing 5.4 to 20.9% of differences with this genuine sequence: a 97 pb fragment (including primers) for CH476 and 5 fragments of 153 to 189 bp for CH559 for a total length of 402 bp were concerned (Figure 2). At first sight, these sequences were considered as numts since they were obtained at a very low frequency compared to the “genuine” ones [43]. This observation is consistent with the fact that the number of mt genuine copies per cell is higher than the number of nuclear numt copies. However, we did not detect any stop codon or nucleotide insertion into these putative numts when translated into amino acids. The third position base composition of both kinds of fragments was also typical of the mammal cytb (i.e. A 39%, C 36%, G 3% and T 21%; [48]). Patterns of mutation rates at the codon positions (expected to be higher at the third positions, followed by first and then second positions for the genuine copy/expected to be less contrasted for the non-coding numt) were identical for all fragments considered. Both genuine and numt sequences, although different, gave similar percentages of identity when compared by BLAST tool to sequences available in GenBank (83% to 94% according to fragment considered). Because of the slower mutation rate in nuclear DNA, numts may exhibit much shorter branch lengths when included in phylogenetic reconstructions and may be placed at a basal position in the tree [43]. However, phylogenetic analyses performed either on what we thought to be the genuine mt sequence or the numt sequences didn't change the phylogenetic position of Malpaisomys insularis among rodents (data not shown). All previous observations seem to indicate that numt sequences amplified are Malpaisomys insularis - specific. In order to confirm our first conclusion about the “genuine” mt copy, we focused on the results obtained for the nuclear marker IRBP. For this nuclear gene, it was impossible to obtain a nuclear fragment longer than 123 bp for CH475 and CH476 specimens (no amplification out of the 22 attempts for the IRBP fragments whose length was comprised between 123 and 152 bp for CH475; no amplification out the 18 attempts for the same fragments for both CH476 and CH560). Consequently, nuclear fragments higher than 123 bp (corresponding to the smallest nuclear fragment we attempted here) don't seem to be preserved for these samples. The mt fragments obtained for them that are longer than 123 bp are thus likely to correspond to the genuine mt copy rather than to a numt copy. To reinforce this statement, CH475 and CH476 mt amplicons longer than 123 bp were indeed always homogeneous (i.e. only one type of sequence was retrieved). Using this rational, the longest cytb fragments obtained for CH475 and CH476 were used to distinguish between numt and true cytb copies in all mt amplicons. By this mean, we were able to definitively confirm our first identification of the genuine mt and the numt copies. Only the genuine cytb copy was considered in the further analyses.
To remove the artefactual mutations due to post-mortem DNA degradations, we cloned and sequenced at least two different amplicons for each PCR fragment and whenever possible two independent ones (i.e. PCRs performed at different days, Table 3). Fragment C1 was obtained only once for CH476 but was totally identical to the consensus sequence obtained for CH559 and CH475. Fragments I2 and I3 were also amplified once for CH559. But as they are largely overlapping (Figure 2), these two amplicons were considered as valid independent replicates. Ambiguities due to ancient DNA decay were alleviated in all consensus sequences performed for each sample, except three positions in the cytb fragment C11 of CH559 (R938, R941, R1000). The 2 independent positive amplifications yielded different residues at 3 positions: 1/A938/A941/A1000 and 2/G938/G941/G1000. These uncertainties are likely to correspond to G residues (see Data S1 for justification). Consensus sequence of Malpaisomys used in the subsequent phylogenetic analyses corresponds to the combination of the consensus sequences obtained for the 3 samples. To be conservative, we decided to keep the 3 positions unresolved for CH559 cytb consensus as undetermined positions (i.e. R) in the final consensus sequence. For the same reasons, two positions (36 and 44) in the IRBP fragment I4 obtained for CH559 were coded as undetermined (Y36 and Y44).
We argue that these cytb and IRBP sequences are authentic Malpaisomys sequences for the following reasons: (i) rodent samples were never introduced in the ancient DNA facilities before this analysis, (ii) the errors induced by DNA damages are perfectly congruent with the pattern generally observed for ancient DNA sequences (strong bias toward type 2 transition caused by cytosine deamination, see Table 3) [49], [50], (iii) extraction, PCR and aerosol controls performed during the same PCR sessions were negative, (iv) no PCR product was obtained when using Malpaisomys primers on bear and hyena co-extracted or co-amplified with rodent samples CH559, CH475 and CH476, suggesting that no carrier effect and thus no contamination occurred during the amplification process, (v) the sequences we obtained were identified as close to murid ones using a BLAST program but were never identical to any known murid sequences available in GenBank, (vi) independent analyses carried out on distinct samples by different manipulators, yielded the same sequences. All in all these points satisfy criteria of authentication for the ancient DNA work [51], [52].
Phylogenetic position of Malpaisomys insularis based on molecular evidences
Analyses of the combined dataset (2,376 bp, 68 taxa) yielded the best ML topology presented in Figure 3. BI and ML trees were congruent except concerning the position of the Ryukyu Island endemic genus, Tokudaia, and some relationships among the tribes Arvicanthini and Murini. In the ML tree, Tokudaia appears as the sister taxon of the genus Apodemus with moderate support (70% BP) while it is grouped in sistership with the Malacomyini in the BI tree with low PP (0.54). This discrepancy is not surprising since the phylogenetic position of Tokudaia is known to have been problematic for decades: if a close relationship between Apodemus and Tokudaia was suggested on dental morphology, e.g. [53], molecular supporting data were only recently obtained [54], [55], [56]. Incongruence among the Murini and Arvicanthini tribes concerns only low support value branching patterns and are just inconclusive regarding these positions. The topology we obtained in this study for the Muridae is congruent with the topology obtained by Lecompte et al. [10] using a larger dataset but encompassing the same genes. The sub-families of Gerbillinae, Deomyinae, and Murinae appear as monophyletic groups with maximal supports (BP≥99.9%, PP = 1.00) and tribes recognized among the Murinae subfamily are well supported (BP≥88% except the Millardini tribe, 69% BP and the Apodemini tribe, 70% BP; PP≥0.99 for all the tribes except the Apodemini grouping that is not supported in the BI tree).
ML and BI analyses of the dataset gave a similar topology. Numbers above the branches reflect support obtained from the analysis of the dataset following the two different reconstructions (BP RAxML/PP MrBayes. The symbol “–” indicates that phylogenetic relationships are not supported by one of the two analyses. Tribal arrangement following [10] is indicated on the right of the tree.
In this tree, Malpaisomys insularis is placed without ambiguity among the Murini tribe (monophyly of this clade being supported with high supports, 99.8% BP and 1.00 PP). Phylogenetic reconstructions based on each independent gene gave exactly the same result with BP = 92 and PP = 1.00 for the cytb gene and BP = 98 and PP = 1.00 for the IRBP gene (Figures S1 and S2). Phylogenetic relationships among the Murini, i.e. between the four subgenera of Mus (Nannomys, Coelomys, Pyromys and Mus), and Malpaisomys, are poorly resolved based on the combined dataset (Figure 3). The lava mouse was placed as the sister taxon of Mus pahari and Mus crociduroides in the best ML tree and the bootstrap analysis supports an association with Mus platythrix but with weak support (BP: 31%). Bayesian tree grouped Malpaisomys with Mus platythrix but with very low PP (0.42). Even if the amount of missing data was demonstrated to have a limited effect on the final topologies and their associated measures of support [57], we re-analyzed the total or gene-by-gene datasets, limiting the analyses to regions that include lava mouse data (992 bp, 452 informative characters, 68 taxa for the cytb; 274 bp, 95 informative characters, 65 taxa for the IRBP; 1266 bp, 543 informative characters, 68 taxa for the combined dataset), to test whether a similar placement within Murini is recovered. These additional analyses without missing data grouped Malpaisomys with the genus Mus with moderate to strong support (BP = 67, PP = 1.00 for the IRBP; BP = 81, PP = 1.00 for the cytb; BP = 98, PP = 1.00 for the combined dataset, Figure S3). In any cases, the relationships among the Murini, are once again poorly supported. Resolving the relationships among the tribe Murini is known to represent a real challenge and similar inconclusive results have been reported in previous studies (e.g. [58], [59], [60]).
Whatever its position inside the mouse clade, tests of alternative topologies indicate without any ambiguity that Malpaisomys belongs to the Murini tribe (Figure 4). Indeed, alternative hypotheses where Malpaisomys does not belong to the monophyletic group of the Murini (i.e. Arvicanthini, Deomyinae and Praomyini hypotheses) are strongly rejected whatever the methods or the statistics (p value<5% (SH-test) and 1<‰ (AU-test)/BF>66). On the contrary, alternative branching patterns of Malpaisomys among the Murini do not appear as significantly different considering SH-, AU-tests and BF (BF RAxML tree versus MrBayes tree = 4.16<10). However, BF gave positive evidence in favour of trees where Malpaisomys is placed at the base of the Murini, as currently defined, when the Bayesian tree or the RAxML tree represent the null hypothesis (BF = 15.68 and 11.52, respectively).
The best topology is indicated in bold. BF values higher than 10 were considered as a very strong evidence favouring one hypothesis (i.e. the topology with the highest likelihood score) over the other [29]. *** indicates BF factors where the BI tree topology (LnL0 = −36,296.42) is significantly better than the tested alternative topology.
A re-examination of morphological characters in the light of molecular findings
A close phylogenetic affinity between mice (i.e. the members of the genus Mus) and Malpaisomys has never been envisaged by studies based on morphological characters ([3], [12], [13] and see [9]). How to interpret morphological characters and singularities of the lava mouse under the light of molecular conclusions?
Molar characters used to recognize mice are: i) the asymmetry of the anterior part (prelobe) of the upper first molar consecutive to the distal position of the lingual cusp t1, ii) the relative elongation of the first upper molar and the reduction of the third upper one measured by the ratio of their length on the length of the second molar (LM1/LM2 and LM3/LM2) [53], and iii) the length of the first upper molar being greater than half of the tooth row [61] (Figure 5). One of the earliest representatives of the genus Mus such as the Mio-Pliocene species Mus ique described from Morocco [62] already has these characters. Another Mus of the Late Miocene, Mus auctor from the Siwaliks already exhibits the asymmetric outline of the anterior part of the first upper molar [63]. Tooth variability is known to be important between species of mice and up to date is still not explicitly described despite the fact that the lab mouse is one of the most studied mammals. But even if we consider the latter argument, the lava mouse clearly does not fit with mice characters. In Malpaisomys, the ratio of upper M1 length on half the total tooth row length approximates 1 (while it is higher than 1 for mice), and ratios LM1/LM2 and LM3/LM2 are respectively ca 1.4 and 0.7, while in Mus ique for example, values are 1.8 and 0.6 (Figure 5).
(A) Mus, (B) holotype of Malpaisomys insularis (Fig. 3 in [3]). In caption, scale is given by the horizontal bar (1 mm).
Moreover, the size of Malpaisomys was estimated to be comparable with the Broad-toothed Field Mouse, Apodemus mystacinus (i.e. about 110 mm head and body length based on reconstruction of the skeleton) and its body weight at about 40 g [64]. This weight represents more than twice the weight of a house mouse. However, if mice are rather small [65], insular species are expected to be large compared to their continental relatives. This was indeed the case for the extinct species of mouse found in Crete, Mus minotaurus [66], [67]. However, other characters of this species are those of mice, as for example, the ratio of M1 length on half the total tooth row length higher than 1 (Figure 5).
In order to reconcile molecular and morphological data, one hypothesis would be to consider Malpaisomys as a giant mouse according to the rather high frequency of the trend towards a larger size that affects small mammals that settled on islands [68], [69]. Size increase has been reported for the house mouse which settled on the Canary Islands very recently [5], [70]. If Malpaisomys was an insular lineage of mouse, its evolution was characterized by a widening of the molars that introduced a strong change in first upper molar outline. This change could be related to a shift in diet [71]. In correlation with this widening, cusps became more voluminous, and small accessory structures appeared in relation with cusps t1, t3 that are part of the prelobe, and cusp t5 of the first upper molar, or in the anterior side of the lower first molar (Figure 5). Changes also affected the skull of Malpaisomys: its skull is narrow at the level of the interorbital breadth [12], a character unknown in Mus. Such a character is related to a peculiar position of the eyes that may be adaptive as it allows a better protection from predatory birds, the eastern Canary Islands being characterized by open environments and great expanses of recent lava fields (“malpaíses”) covered by scarce vegetation [54].
Presently, molecular data indicate that the lineage of Malpaisomys split at a similar time as the genus Mus radiation but the exact order of lineage origins remains impossible to ascertain. This raises the following question: did the lineage of Malpaisomys split before the typical genus Mus dental pattern differentiated or not?
Molecular dating
The chronograms derived from the BEAST and Multidivtime analyses are presented in Figure 6. Estimated ages and 95% credibility intervals (95% CI) of notable nodes are detailed in Table 4. Two independent runs of Multidivtime gave the same results. On the whole, the estimations of Multidivtime are slightly older that the ones obtained from the BEAST analysis, but in most cases, 95% CI are extensively overlapping and are of the same order (Figure 6). The estimations are particularly congruent among the Murini including Malpaisomys and for the deepest nodes of the tree while the most important discrepancies between the two methods are found among the Rattini (Figure 6). Different clock methods are known to lead to disparate results due to their inherent handling of the rate heterogeneity across lineages (i.e. random or autocorrelated lineage rates) [72]. When the lineage rate assumption is violated, relaxed-clock methods were proven to produce biased estimated credibility intervals [72]. This would explain that a specific evolutionary rate could characterize the Rattini tribe and account for the slight disparities between the two dating methods. Nonetheless, estimations and the 95% CI for the three calibration points are congruent with the paleontological evidence (Table 4). We re-ran the analyses, omitting each of the calibration points in turn to assess whether the molecular dates are the result of the fossil constraints and we obtained similar estimates (slightly older without FC1, younger without FC2 and FC3) (Table S2).
The chronograms were obtained under a Bayesian non-autocorrelated rates relaxed clock model using BEAST (in blue) and an autocorrelated model using Multidivtime (in orange) and applied to the combined cytb/IRBP dataset. 95% credibility intervals are drawn on nodes. The three fossil calibration points are indicated by a star. Variation of sea level is indicated below [84].
The split of the main lineages of Murinae took place between 12.3 and 9.8 Ma (BEAST)/12.7 and 10.8 Ma (Multidivtime). These estimates are similar to the ones obtained by Lecompte et al. [10], slightly older than the ones reported by Rowe et al. [54], and much younger than the ones found in Jansa et al. [73]. The main difference between our study and the one undertaken by Rowe et al. [74] corresponds to the addition of a third calibration interval (i.e. the Apodemus mystacinus-A. sylvaticus divergence). When this constraint is removed from the Multidivtime analysis, our estimates converged to the divergence-dates obtained by Rowe et al. [74] (Table S2). With respect to the study of Jansa et al. [70], the differences are probably not only due to sampling different taxa but also to the use of calibration points based on much older splits in the mammal lineage (overestimation of the shallowest nodes in the tree because of too ancient calibration points compared to these nodes [72]). Our molecular estimate of the age at which occurred the split of the main lineages of Murinae fits completely with the paleontological evidence, which indicates that the different modern lineages probably arose around 11 Ma. At that time, the first Progonomys and Karnimata are reported outside the Siwalik region, in Eurasia and Africa [75], [76], [77] and the modern lineages such as the Apodemus lineage arose in Europe [38].
The tribe Murini diverged from the Praomyini at 9.85 Ma (BEAST)/10.84 Ma (Multidivtime) with an overlapping CI interval of 12.46 to 8.64 Ma. The divergence of the different Murini subgenera including Malpaisomys took place at 6.94 (BEAST)/6.93 (Multidivdime) (CI = 8.3 −5.9 Ma (BEAST)/8.6 −5.4 Ma (Multidivtime)). We are confident in these estimates because they are highly congruent between the two approaches but also with previous molecular studies [58], [59] and with the oldest Murini representatives found in the fossil record of the Siwalik: Mus auctor (6.4 My) and Mus sp. (7.3 Ma) [37]. Consequently, the colonization of the Canary Islands could have occurred anytime after 6.9 Ma. However, since there is no paleontological evidence for the presence of Malpaisomys or its predecessor on the Canary Islands or on the continent previous to the Pleistocene, it is difficult to propose a date of arrival and a place for the origin of the lava mouse (Spain or Morocco). As the oldest Malpaisomys fossils are ca. 30,000 years old [8], its first occurrence predates the first human settlement (between 2,500 and 2,000 years ago, [6], [78], [79]). Thus, the hypothesis that a North African ancestor reached the eastern Canary Islands after 6.9 Ma ago during a major sea level regression via natural rafts is likely. Further phylogenetic investigations are now needed to corroborate this hypothesis and to determine whether the colonization of the Canary archipelago by terrestrial mammals corresponded to a single event or not. Investigating the phylogeny of the two other endemic extinct rodents, Canariomys, could also shed new light on this question.
Conclusion
For the first time ancient DNA sequences show that Malpaisomys was more closely related to the genus Mus than to any other Murinae, a hypothesis that has never been investigated with morphological data. Further investigations are now needed to solve the inter-specific relationships among the Malpaisomys/mouse species clade. Such results will help to clarify whether Malpaisomys is embedded among the genus Mus and will have taxonomic implications for the whole group. Indeed, they will help to decipher if the mouse subgenera as currently defined (i.e. Mus, Ceolomys, Nannomys and Pyromys) [9] should be elevated to the rank of genus as already suggested [80], [81], [82]. They will also help to refine the timing of the colonization of the Canaries by the Malpaisomys ancestor and to elucidate the route taken to reach the archipelago.
Supporting Information
Figure S1.
RAxML tree depicting the relationships of Malpaisomys within Muridae based on the analysis of the cytb gene. Numbers above the branches reflect supports obtained from the analysis of the dataset following the two different reconstructions (BP RAxML/PP MrBayes.) The symbol “–” indicates that phylogenetic relationships are not supported by one of the two analyses. Numbers highlighted in bold and in grey indicate nodes which are respectively congruent and incongruent with the tree obtained based on the complete dataset (Figure 1).
https://doi.org/10.1371/journal.pone.0031123.s001
(TIF)
Figure S2.
RAxML tree depicting the relationships of Malpaisomys within Muridae based on the analysis of the IRBP gene. Numbers above the branches reflect support obtained from the analysis of the dataset following the two different reconstructions (BP RAxML/PP MrBayes.) The symbol “–” indicates that phylogenetic relationships are not supported by one of the two analyses. Numbers highlighted in bold and in grey indicate nodes which are respectively congruent and incongruent with the tree obtained based on the complete dataset (Figure 1).
https://doi.org/10.1371/journal.pone.0031123.s002
(TIF)
Figure S3.
RAxML tree depicting the relationships of Malpaisomys within Muridae based on the analysis of the combined cytb and IRBP genes without the sites missing for Malpaisomys. Numbers above the branches reflect support obtained from the analysis of the dataset following the two different reconstructions (BP RAxML/PP MrBayes.) The symbol “–” indicates that phylogenetic relationships are not supported by one of the two analyses. Numbers highlighted in bold and in grey indicate nodes which are respectively congruent and incongruent with the tree obtained based on the complete dataset (Figure 1).
https://doi.org/10.1371/journal.pone.0031123.s003
(TIFF)
Table S1.
Sequence dataset extracted from GenBank and used in this study. The tribal arrangement follows Lecompte's nomenclature [10].
https://doi.org/10.1371/journal.pone.0031123.s004
(DOC)
Table S2.
Age estimates (Ma) using BEAST and Multidivtime softwares and omitting one of the three calibration points in turn. HPD for Highest Posterior Density, CI for Credibility Interval, NA for Not Available.
https://doi.org/10.1371/journal.pone.0031123.s005
(DOC)
Data S1.
Ancient DNA degradation for CH559 sample.
https://doi.org/10.1371/journal.pone.0031123.s006
(DOC)
Acknowledgments
We thank F. García-Talavera and M. Trias for their efficient and constant help. We would like to thank all the Paleogenetics team at the IGFL in Lyon, B. Gillet from PALGENE (the French National Plateform for Paleogenetics, CNRS, ENS de Lyon) and S. Renaud for helpful discussions. We also thank Joanne Burden (IGFL, CNRS/ENS de Lyon) who proofread the English. This is publication ISE-M (UMR 5554) n° 2012 - 002.
Author Contributions
Conceived and designed the experiments: CH PC SH. Performed the experiments: MP MGB PC. Analyzed the data: MP PC. Contributed reagents/materials/analysis tools: JAA RH JCR JM CH. Wrote the paper: MP JM PC. Contributed to the writing of the manuscript: JAA RH JCR SH CH.
References
- 1. Carracedo JC, Day S, Guillou H, Rodriguez Badiola E, Canas JA, et al. (1998) Hotspot volcanism close to a passive continental margin: the Canary Island. Geol Mag 135: 119–131.
- 2. López-Martínez N, López-Jurado L (1987) Un nuevo múrido gigante del Cuaternario de Gran Canaria. Canariomys tamarani nov. sp. (Rodentia, Mammalia). Doñana Acta Vertebr 2: 1–66.
- 3. Hutterer R, Lopez-Martinez N, Michaux J (1988) A new rodent from Quaternary deposits of the Canary Islands and its relationships with neogene and recent murids of Europe and Africa. Paleovertebrata 18: 241–262.
- 4. Bocherens H, Michaux J, Garcia Talavera F, Van der Plicht J (2006) Extinction of endemic vertebrates on islands: The case of the giant rat Canariomys bravoi (Mammalia, Rodentia) on Tenerife (Canary Islands, Spain). CR Palevol 5: 885–891.
- 5. Alcover JA, Rando JC, Garcia-Talavera F, Hutterer R, Michaux J, et al. (2009) A reappraisal of the stratigraphy of Cueva des Llano (Fuerteventura) and the chronology of the introduction of the house mouse (Mus musculus) into the Canary Islands. Paleogeogr Palaeoclimatol Paleoecol 277: 184–190.
- 6. Rando JC, Alcover JA, Navarro JF, Garcia-Talavera F, Hutterer R, et al. (2008) Chronology and causes of the extinction of the Lava Mouse, Malpaisomys insularis (Rodentia: Muridae) from the Canary Islands. Quaternary Res 70: 141–148.
- 7. Rando JC, Alcover JA (2008) Evidence for a second western Palaearctic seabird extinction during the last Millennium: the Lava Shearwater Puffinus olsoni. Ibis 150: 188–192.
- 8. Michaux J, Hutterer R, Lopez-Martinez N (1991) New fossil faunas from Fuerteventura, Canary Islands: Evidence for Pleistocene age of endemic rodents and shrews. CR Acad Sci Paris, Série II: 801–806.
- 9.
Musser G, Carleton M (2005) Superfamily Muroidea. In: Wilson DE, Reeder DM, editors. Mammal species of the world A taxonomic and geographic reference Volume 2. 3rd edition. Baltimore: Johns Hopkins University. pp. 894–1531.
- 10. Lecompte E, Aplin K, Denys C, Catzeflis F, Chades M, et al. (2008) Phylogeny and biogeography of African Murinae based on mitochondrial and nuclear gene sequences, with a new tribal classification of the subfamily. BMC Evol Biol 8: 199.
- 11. Montgelard C (1992) Albumin preservation in fossil bones and systematics of Malpaisomys insularis (Muridae, Rodentia), an extinct rodent of the Canary Islands. Hist Biol 6: 293–302.
- 12. Lopez-Martinez N, Michaux J, Hutterer R (1998) The skull of Stephanomys and a review of Malpaisomys Relationships (Rodentia: Muridae): Taxonomic Ingongruence in Murids. J Mamm Evol 5: 185–215.
- 13. Renaud S, Michaux J (2004) Parallel evolution in molar outline of murine rodents: the case of the extinct Malpaisomys insularis (Eastern Canary Islands). Zool J Linn Soc 142: 555–572.
- 14. Calvignac S, Hughes S, Tougard C, Michaux J, Thevenot M, et al. (2008) Ancient DNA evidence for the loss of a highly divergent brown bear clade during historical times. Mol Ecol 17: 1962–1970.
- 15. Hughes S, Hayden TJ, Douady CJ, Tougard C, Germonpre M, et al. (2006) Molecular phylogeny of the extinct giant deer, Megaloceros giganteus. Mol Phylogenet Evol 40: 285–291.
- 16. Calvignac S, Terme JM, Hensley SM, Jalinot P, Greenwood AD, et al. (2008) Ancient DNA identification of early 20th century simian T-cell leukemia virus type 1. Mol Biol Evol 25: 1093–1098.
- 17. Rohland N, Hofreiter M (2007) Ancient DNA extraction from bones and teeth. Nat Protoc 2: 1756–1762.
- 18.
Cooper A (1994) Dried samples : soft tissues, DNA from museum specimens. In: Hermann BH, Hummel S, editors. Ancient DNA, Recovery and analysis of genetic material from paleontological, archeological, museum, medical, and forensic samples. Springer-Verlag. pp. 149–165.
- 19. Hänni C, Brousseau T, Laudet V, Stehelin D (1995) Isopropanol precipitation removes PCR inhibitors from ancient bone extracts. Nucleic Acids Res 23: 881–882.
- 20. Michaux J, Reyes A, Catzeflis F (2001) Evolutionary history of the most speciose mammals: molecular phylogeny of muroid rodents. Mol Biol Evol 18: 2017–2031.
- 21. Galtier N, Gouy M, Gautier C (1996) SEAVIEW and PHYLO_WIN: two graphic tools for sequence alignment and molecular phylogeny. Comput Appl Biosci 12: 543–548.
- 22. Posada D, Crandall KA (1998) MODELTEST: testing the model of DNA substitution. Bioinformatics 14: 817–818.
- 23. Stamatakis A (2006) RAxML-VI-HPC: maximum likelihood-based phylogenetic analyses with thousands of taxa and mixed models. Bioinformatics 22: 2688–2690.
- 24. Stamatakis A, Hoover P, Rougemont J (2008) A rapid bootstrap algorithm for the RAxML Web servers. Syst Biol 57: 758–771.
- 25. Ronquist F, Huelsenbeck JP (2003) MrBayes 3: Bayesian phylogenetic inference under mixed models. Bioinformatics 19: 1572–1574.
- 26.
Rambaut A, Drummond A (2007) Tracer v1.4, Available: http://tree.bio.ed.ac.uk/software/tracer/. Accessed 2012 January 5.
- 27. Nylander JAA, Ronquist F, Huelsenbeck JP, Nieves-Aldrey LJ (2004) Bayesian phylogenetic analysis of combined data. Syst Biol 53: 47–67.
- 28. Newton MA, Raftery AE (1994) Approximate Bayesian inference by the weighted likelihood bootstrap (with Discussion). J R Stat Soc, series B 56: 3–48.
- 29. Kass RE, Raftery AE (1995) Bayes factors. J Am Stat Assoc 90: 773–795.
- 30. Goldman N, Anderson JP, Rodrigo AG (2000) Likelihood-based tests of topologies in phylogenetics. Syst Biol 49: 652–670.
- 31.
Swofford DL (1998) PAUP*. Phylogenetic Analysis using Parsimony (*and other methods). Version 4. Sinauer Associates, Sunderland, Massachusetts.
- 32. Shimodaira H, Hasegawa M (2001) CONSEL: for assessing the confidence of phylogenetic tree selection. Bioinformatics 17: 1246–1247.
- 33. Thorne JL, Kishino H (2002) Divergence time and evolutionary rate estimation with multilocus data. Syst Biol 51: 689–702.
- 34. Drummond AJ, Ho SY, Phillips MJ, Rambaut A (2006) Relaxed phylogenetics and dating with confidence. PLoS Biol 4: e88.
- 35. Drummond AJ, Rambaut A (2007) BEAST: Bayesian evolutionary analysis by sampling trees. BMC Evol Biol 7: 214.
- 36. Steppan S, Adkins R, Anderson J (2004) Phylogeny and divergence-date estimates of rapid radiations in muroid rodents based on multiple nuclear genes. Syst Biol 53: 533–553.
- 37.
Jacobs LL, Flynn LJ (2005) Of mice… again: the Siwalik rodent record, murine distribution, and molecular clocks. In: Lieberman D, Smith R, Kelley J, editors. Interpreting the past: essays on human, primate and mammal evolution. Leiden: Brill Academic Publisher. pp. 63–80.
- 38. Michaux J, Aguilar J, Montuire S, Wolff A, Legendre S (1997) Les Murinae (Rodentia, Mammalia) néogènes du Sud de la France: Evolution et Paléoenvironnement. Geobios 20: 379–385.
- 39. Winkler AJ (2002) Neogene paleobiogeography and East African paleoenvironments: contributions from the Tugen Hills rodents and lagomorphs. J Hum Evol 42: 237–256.
- 40.
Rutschmann F (2005) Bayesian molecular dating using PAML/MULTIDIVTIME. A step-by-step manual, v. 1.4. Available: http://statgen.ncsu.edu/thorne/multidivtime.html. Accessed 2012 January 5.
- 41. Yang Z (1997) PAML: a program package for phylogenetic analysis by maximum likelihood. Comput Appl Biosci 13: 555–556.
- 42. Yoder AD, Yang Z (2004) Divergence dates for Malagasy lemurs estimated from multiple gene loci: geological and evolutionary context. Mol Ecol 13: 757–773.
- 43. den Tex RJ, Maldonado JE, Thorington R, Leonard JA (2010) Nuclear copies of mitochondrial genes: another problem for ancient DNA. Genetica 138: 979–984.
- 44. Ramirez O, Illera JC, Rando JC, Gonzalez-Solis J, Alcover JA, et al. (2010) Ancient DNA of the extinct lava shearwater (Puffinus olsoni) from the Canary Islands reveals incipient differentiation within the P. puffinus complex. PLoS One 5: e16072.
- 45. Dubey S, Michaux J, Brünner H, Hutterer R, Vogel P (2009) False phylogenies on wood mice due to cryptic cytochrome b pseudogene. Mol Phylogenet Evol 50: 633–641.
- 46. González-Ittig R, Gardenal C (2007) Co-amplification of mitochondrial pseudogenes in Calomys musculinus (Rodentia, Cricetidae): a source of error in phylogeographic studies. Genome Biol 51: 73–78.
- 47. Orlando L, Leonard JA, Thenot A, Laudet V, Guerin C, et al. (2003) Ancient DNA analysis reveals woolly rhino evolutionary relationships. Mol Phylogenet Evol 28: 485–499.
- 48. Johns GC, Avise JC (1998) A comparative summary of genetic distances in the vertebrates from the mitochondrial cytochrome b gene. Mol Biol Evol 15: 1481–1490.
- 49. Hofreiter M, Jaenicke V, Serre D, Haeseler Av A, Paabo S (2001) DNA sequences from multiple amplifications reveal artifacts induced by cytosine deamination in ancient DNA. Nucleic Acids Res 29: 4793–4799.
- 50. Gilbert MT, Hansen AJ, Willerslev E, Rudbeck L, Barnes I, et al. (2003) Characterization of genetic miscoding lesions caused by postmortem damage. Am J Hum Genet 72: 48–61.
- 51. Gilbert MT, Bandelt HJ, Hofreiter M, Barnes I (2005) Assessing ancient DNA studies. Trends Ecol Evol 20: 541–544.
- 52. Pagès M, Desse-Berset N, Tougard C, Brosse L, Hänni C, et al. (2009) Historical presence of the sturgeon Acipenser sturio in the Rhône basin determined by the analysis of ancient DNA cytochrome b sequences. Conserv Genet 10(1): 217–224.
- 53.
Misonne X (1969) African and Indo-Australian Muridae. Evolutionary trends. Tervuuren: Ann Mus Royal Afr Centr. 219 p.
- 54. Rowe KC, Reno ML, Richmond DM, Adkins RM, Steppan SJ (2008) Pliocene colonization and adaptive radiations in Australia and New Guinea (Sahul): Multilocus systematics of the old endemic rodents (Muroidea: Murinae). Mol Phylogenet Evol 47: 84–101.
- 55. Michaux JR, Chevret P, Filippucci MG, Macholan M (2002) Phylogeny of the genus Apodemus with a special emphasis on the subgenus Sylvaemus using the nuclear IRBP gene and two mitochondrial markers: cytochrome b and 12S rRNA. Mol Phylogenet Evol 23: 123–136.
- 56. Sato J, Suzuki H (2004) Phylogenetic relationships and divergence times of the genus Tokudaia within Murinae (Muridae; Rodentia) inferred from the nucleotide sequences encoding the Cytb gene, RAG 1, and IRBP. Can J Zool 82: 1343–1351.
- 57. Fulton TL, Strobeck C (2006) Molecular phylogeny of the Arctoidea (Carnivora): effect of missing data on supertree and supermatrix analyses of multiple gene data sets. Mol Phylogenet Evol 41: 165–181.
- 58. Suzuki H, Shimada T, Terashima M, Tsuchiya K, Aplin K (2004) Temporal, spatial, and ecological modes of evolution of Eurasian Mus based on mitochondrial and nuclear gene sequences. Mol Phylogenet Evol 33: 626–646.
- 59. Chevret P, Veyrunes F, Britton-Davidian J (2005) Molecular phylogeny of the genus Mus (Rodentia: Murinae) based on mitochondrial and nuclear data. Biol J Linn Soc 84: 417–427.
- 60. Shimada T, Aplin K, Jenkins P, Suzuki H (2007) Rediscovery of Mus nitidulus Blyth (Rodentia: Muridae), an endemic murine rodent of the central basin of Myanmar. Zootaxa 1498: 45–68.
- 61.
Chaimanee Y (1998) Plio-Pleistocene Rodents of Thailand. 303 p. Thai Studies in Biodiversity, editor.
- 62. Geraads D (1998) Rongeurs du Mio-Pliocène de Lissasfa (Casablanca, Maroc). Geobios 31: 229–245.
- 63. Jacobs LL (1978) Fossil rodents (Rhizomyidae and Muridae) from Neogene Siwalik deposits, Pakistan. Mus North Arizona Press 104.
- 64. Boye P, Hutterer R, Lopez-Martinez N, Michaux J (1992) A reconstruction of the Lava mouse (Malpaisomys insularis), an extinct rodent of the Canary Islands. Z Saugetierkd 57: 29–38.
- 65.
Nowak RM (1999) Walker's Mammals of the World. Volume II. Baltimore, MD: The John Hopkins University Press. 1936 p.
- 66. Kuss SE, Misonne X (1968) Pleistocäne Muriden des Insel Kreta. N Jb Geol Paläont Abh 132: 55–69.
- 67.
Mayhew DP (1977) The endemic Pleistocene Murids of Crete I and II; Proceedings of the Koninklijke Akademie van Wetenschappen (Series B). 80. (3): pp. 182–214.
- 68. Damuth J (1993) Cope's rule, the island rule and the scaling of mammalian population density. Nature 365: 748–750.
- 69. Millien V, Damuth J (2004) Climate change and size evolution in an island rodent species: new perspectives on the island rule. Evolution 58: 1353–1360.
- 70. Michaux J, Chevret P, Renaud S (2007) Morphological diversity of Old World rats and mice (Rodentia, Muridae) mandible in relation with phylogeny and adaptation. J Zool Syst Evol Res 45: 263–279.
- 71. Firmat C, Gomes Rodrigues H, Hutterer R, Rando JC, Alcover JA, et al. (2011) Diet of the extinct Lava mouse Malpaisomys insularis from the Canary Islands: insights from dental microwear. Naturwissenschaften 98: 33–37.
- 72. Battistuzzi FU, Filipski A, Hedges SB, Kumar S (2010) Performance of relaxed-clock methods in estimating evolutionary divergence times and their credibility intervals. Mol Biol Evol 27: 1289–1300.
- 73. Jansa SA, Barker FK, Heaney LR (2006) The pattern and timing of diversification of Philippine endemic rodents: evidence from mitochondrial and nuclear gene sequences. Syst Biol 55: 73–88.
- 74. Robins JH, McLenachan PA, Phillips MJ, Craig L, Ross HA, et al. (2008) Dating of divergences within the Rattus genus phylogeny using whole mitochondrial genomes. Mol Phylogenet Evol.
- 75. Aguilar J, Michaux J (1996) The beginning of the age of Murinae (Mammalia: Rodentia) in southern France. Acta Zool Cracov 39: 35–45.
- 76. Jacobs LL (1985) The beginning of the age of Murids in Africa. Acta Zool Fenn 170: 149–151.
- 77.
Winkler AJ, Denys C, Avery DM (2010) Chapter 17: Rodentia. Cenozoic Mammals of Africa. In: Werdelin L, Sanders WJ, editors. Berkeley: University of California Press. pp. 263–305.
- 78. Navarro JF, Martín E, Rodríguez A (1990) Las primeras etapas del programa de excavaciones en las Cuevas de San Juan y su aportación a la diacronía de la Prehistoria de Canarias. Investigaciones Arqueológicas en Canarias II: 189–201.
- 79.
Atoche P, Paz JA, Ramírez MA, Ortiz ME (1995) Evidencias arqueológicas del mundo romano en Lanzarote (Islas Canarias). 149 p. Servicio de Publicaciones del Cabildo de Lanzarote: Arrecife.
- 80.
Bonhomme F (1986) Evolutionary relationships in the genus Mus. In: Potter M, Nadeau J, Cancro M, editors. Current topics in microbiology and immunology. New York: Springer Verlag. pp. 19–34.
- 81.
Bonhomme F (1992) Genetic diversity and evolution in the genus Mus. In: Goldowitz D, Wahlsten D, Wimer R, editors. Techniques for the genetic analysis of brain and behavior. Elsevier Sciences Publishers. pp. 41–56.
- 82. Chevret P, Jenkins P, Catzeflis F (2003) Evolutionary systematics of the Indian mouse Mus famulus Bonhote, 1898: molecular (DNA/DNA hybridization and 12S rRNA sequences) and morphological evidences. Zool J Linn Soc 137: 385–401.
- 83.
Diepenbroek M, Grobe H, Sieger R (2000) PanMap Available: http://www.pangaea.de/Software/PanMap. Accessed 2012 January 5.
- 84. Haq BU, Hardenbol J, Vail PR (1987) Chronology of fluctuating sea level since the Triassic. Science 235: 1156–1167.