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Link to original content: http://pubmed.ncbi.nlm.nih.gov/23144757/
Major radiations in the evolution of Caviid rodents: reconciling fossils, ghost lineages, and relaxed molecular clocks - PubMed Skip to main page content
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. 2012;7(10):e48380.
doi: 10.1371/journal.pone.0048380. Epub 2012 Oct 29.

Major radiations in the evolution of Caviid rodents: reconciling fossils, ghost lineages, and relaxed molecular clocks

Affiliations

Major radiations in the evolution of Caviid rodents: reconciling fossils, ghost lineages, and relaxed molecular clocks

María Encarnación Pérez et al. PLoS One. 2012.

Abstract

Background: Caviidae is a diverse group of caviomorph rodents that is broadly distributed in South America and is divided into three highly divergent extant lineages: Caviinae (cavies), Dolichotinae (maras), and Hydrochoerinae (capybaras). The fossil record of Caviidae is only abundant and diverse since the late Miocene. Caviids belongs to Cavioidea sensu stricto (Cavioidea s.s.) that also includes a diverse assemblage of extinct taxa recorded from the late Oligocene to the middle Miocene of South America ("eocardiids").

Results: A phylogenetic analysis combining morphological and molecular data is presented here, evaluating the time of diversification of selected nodes based on the calibration of phylogenetic trees with fossil taxa and the use of relaxed molecular clocks. This analysis reveals three major phases of diversification in the evolutionary history of Cavioidea s.s. The first two phases involve two successive radiations of extinct lineages that occurred during the late Oligocene and the early Miocene. The third phase consists of the diversification of Caviidae. The initial split of caviids is dated as middle Miocene by the fossil record. This date falls within the 95% higher probability distribution estimated by the relaxed Bayesian molecular clock, although the mean age estimate ages are 3.5 to 7 Myr older. The initial split of caviids is followed by an obscure period of poor fossil record (referred here as the Mayoan gap) and then by the appearance of highly differentiated modern lineages of caviids, which evidentially occurred at the late Miocene as indicated by both the fossil record and molecular clock estimates.

Conclusions: The integrated approach used here allowed us identifying the agreements and discrepancies of the fossil record and molecular clock estimates on the timing of the major events in cavioid evolution, revealing evolutionary patterns that would not have been possible to gather using only molecular or paleontological data alone.

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Conflict of interest statement

Competing Interests: The authors have declared that no competing interests exist.

Figures

Figure 1
Figure 1. Reduced strict consensus of the parsimony combined phylogenetic analysis of morphological and molecular dataset using TNT.
Small yellow circles show the multiple alternative positions in the most parsimonious trees of the late Miocene caviid Allocavia (pruned from the reduced consensus tree). Numbered nodes on the tree indicate the calibration constraints used in the molecular clock estimates (see Calibrated Nodes). The phylogenetic tree is calibrated against geological time based on the first occurrence of fossil taxa in the fossil record. The most relevant South American Land Mammal Ages are highlighted in color.
Figure 2
Figure 2. Nodal support values of the parsimony combined phylogenetic analysis of morphological and molecular dataset using TNT.
Three values are indicated for each node, the first of them is the Bremer support value, the second is the absolute frequency of each node in the bootstrap replicates and the third is the absolute frequency in the jackknife replicates (see Document S1 for further details).
Figure 3
Figure 3. Phylogenetic relationships of extant-only taxa of Cavioidea with support values.
This topology was retrieved for both the combined parsimony analysis and the Bayesian analysis of the molecular partition. For each node we indicate the posterior probability of the Bayesian analysis, the absolute bootstrap frequency of the parsimony analysis, and the absolute jackknife frequency of the parsimony analysis.
Figure 4
Figure 4. Phylogenetic hypothesis retrieved from the molecular dataset of extant cavioids obtained in BEAST.
The time of divergence of each clade plotted in the tree is based on the mean estimates of the relaxed molecular clock using four calibration points. Colored bars in the tree represents the 95%HPD for the ages of Caviidae (blue), Dolichotinae (yellow), and the caviine Galea (red). Numbers on the tree indicate the calibration constraints used (see Calibrated Nodes). Dots on the left of the graphic indicate the mean age estimates for Caviidae (blue), Dolichotinae (yellow), and the caviine Galea (red) obtained with all possible combinations of one, two, three, and four calibrated nodes (using both normal and gamma prior distributions for calibrated nodes). Dotted blue lines represent the maximum breadth of the 95%HPD obtained for the age of Caviidae with different number of calibration constraints.
Figure 5
Figure 5. 95%HPD of age estimates for the time of diversification of Caviidae as estimated for each of the 30 different Bayesian relaxed molecular clock analyses conducted in this study.
Figure 6
Figure 6. Diversification plot of cumulative number of cavioid lineages (leading to both extinct and extant species) against geological time.
The red curve represents the number of lineages based on the simultaneous analysis of morphological and molecular data of both extinct and extant taxa (as shown in Fig. 4). The uncertainty in the geological age of each fossil creates a maximum and minimum times of divergence and is represented by the breadth of the diversification events on the red curve. The blue line represents the timing of diversification events of crown caviid lineages based on mean age estimates of the molecular clock estimates. The most relevant SALMAs are highlighted and the numbers 1, 2, 3a, and 3b represents the Deseadan radiation (1), the Santacrucian radiation (2), the initial diversification of Caviidae (3a), and the diversification of modern and morphologically well differentiated lineages of caviids during the Chasicoan (3b). The black arrow marks the discrepancy between the timing of the initial diversification of Caviidae based on the paleontological record (red curve) and the molecular clock estimates (blue curve).
Figure 7
Figure 7. Species diversity map of fossil rodents in all known Oligocene-Pleistocene fossiliferous localities across South America.
The number of valid species known for each region has been compiled and color coded. Blue colored regions represent the absence of rodent remains and warmer colors represent increasing number of species (taxonomic diversity) of fossil rodents. The red colored region highlights the highest species diversity of fossil rodents recorded in the “Pinturan”/Santacrucian fossiliferous localities of southern South America (Patagonia). Grey arrow indicates the rodent record of Laventan age in Colombia, where the oldest Caviidae (P. pridiana) is recorded.

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Grants and funding

Research for this contribution was supported by ANPCyT PICT 2613 (to MEP) and the CONICET program for stays abroad for postdoctoral fellows (to MEP). Additional support that allowed the study of relevant specimens was provided to MEP by the American Museum of Natural History (AMNH) Collection Study Grant and the Yale Peabody Museum (YPM) Ostrom Fund. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

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