Abstract:Didelphidae is the largest New World radiation of marsupials, and is mostly represented by arboreal, small- to medium-sized taxa that inhabit tropical and/or subtropical forests. The group originated and remained isolated in South America for millions of years, until the formation of the Isthmus of Panama. In this study, we present the first reconstruction of the biogeographic history of Didelphidae including all major clades, based on parametric models and stratified analyses over time. We also compiled all t… Show more
“…This estimate is also broadly congruent with the molecular node-dating analysis of Jansa et al (2014) and with the total evidence tip-and-node dating analysis of Beck and Taglioretti (2020); however, it is considerably younger than estimated divergence dates suggested by several other molecular studies, which have dated the last common ancestor of living didelphimorphians as having lived in the early Oligocene or Eocene (Steiner et al, 2005;Meredith et al, 2008b;Mitchell et al, 2014;Vilela et al, 2015). Our estimated divergence date is broadly congruent with the known fossil record of didelphids (recently reviewed by Beck and Taglioretti, 2020;Castro et al, 2021): the oldest probable (crownclade) didelphids described to date are from the early Miocene (Colhuehuapian SALMA, ~21.0-20.1 Mya; Goin et al, 2007a;Dunn et al, 2012;Castro et al, 2021). However, these specimens are highly fragmentary (isolated teeth only), and their affinities are correspondingly uncertain (Goin et al, 2007a;Beck and Taglioretti, 2020;Castro et al, 2021).…”
supporting
confidence: 89%
“…Our estimated divergence date is broadly congruent with the known fossil record of didelphids (recently reviewed by Beck and Taglioretti, 2020;Castro et al, 2021): the oldest probable (crownclade) didelphids described to date are from the early Miocene (Colhuehuapian SALMA, ~21.0-20.1 Mya; Goin et al, 2007a;Dunn et al, 2012;Castro et al, 2021). However, these specimens are highly fragmentary (isolated teeth only), and their affinities are correspondingly uncertain (Goin et al, 2007a;Beck and Taglioretti, 2020;Castro et al, 2021).…”
The current literature on marsupial phylogenetics includes numerous studies based on analyses of morphological data with relatively limited sampling of Recent and fossil taxa, and many studies based on analyses of molecular data that include a dense sampling of Recent taxa, but relatively few that combine both data types. Another dichotomy in the 9 2021) belonging to seven clades that are currently ranked as orders in the Linnean hierarchy (Table 1; Aplin and Archer, 1987;Wilson and Reeder, 2005;Burgin et al., 2018;Eldridge et al., 2019): Didelphimorphia (opossums), Paucituberculata (shrew opossums), Microbiotheria (the "monito del monte" Dromiciops gliroides), Dasyuromorphia (predominantly carnivorous forms such as quolls, antechinuses, dunnarts, the Tasmanian devil, the numbat, and the recently extinct thylacine), Diprotododontia (possums, gliders, kangaroos, wallabies, rat kangaroos, wombats, koalas, etc.), Notoryctemorphia (marsupial moles), and Peramelemorphia (bandicoots and bilbies).
Dromiciops gliroides (the sole extant microbiotherian) and the three genera of modern paucituberculatans (Caenolestes, Lestoros, and Rhyncholestes, all members of the family Caenolestidae) are exclusively South American in distribution (Gardner, 2008). Fossil members of both orders are known from South America (
“…This estimate is also broadly congruent with the molecular node-dating analysis of Jansa et al (2014) and with the total evidence tip-and-node dating analysis of Beck and Taglioretti (2020); however, it is considerably younger than estimated divergence dates suggested by several other molecular studies, which have dated the last common ancestor of living didelphimorphians as having lived in the early Oligocene or Eocene (Steiner et al, 2005;Meredith et al, 2008b;Mitchell et al, 2014;Vilela et al, 2015). Our estimated divergence date is broadly congruent with the known fossil record of didelphids (recently reviewed by Beck and Taglioretti, 2020;Castro et al, 2021): the oldest probable (crownclade) didelphids described to date are from the early Miocene (Colhuehuapian SALMA, ~21.0-20.1 Mya; Goin et al, 2007a;Dunn et al, 2012;Castro et al, 2021). However, these specimens are highly fragmentary (isolated teeth only), and their affinities are correspondingly uncertain (Goin et al, 2007a;Beck and Taglioretti, 2020;Castro et al, 2021).…”
supporting
confidence: 89%
“…Our estimated divergence date is broadly congruent with the known fossil record of didelphids (recently reviewed by Beck and Taglioretti, 2020;Castro et al, 2021): the oldest probable (crownclade) didelphids described to date are from the early Miocene (Colhuehuapian SALMA, ~21.0-20.1 Mya; Goin et al, 2007a;Dunn et al, 2012;Castro et al, 2021). However, these specimens are highly fragmentary (isolated teeth only), and their affinities are correspondingly uncertain (Goin et al, 2007a;Beck and Taglioretti, 2020;Castro et al, 2021).…”
The current literature on marsupial phylogenetics includes numerous studies based on analyses of morphological data with relatively limited sampling of Recent and fossil taxa, and many studies based on analyses of molecular data that include a dense sampling of Recent taxa, but relatively few that combine both data types. Another dichotomy in the 9 2021) belonging to seven clades that are currently ranked as orders in the Linnean hierarchy (Table 1; Aplin and Archer, 1987;Wilson and Reeder, 2005;Burgin et al., 2018;Eldridge et al., 2019): Didelphimorphia (opossums), Paucituberculata (shrew opossums), Microbiotheria (the "monito del monte" Dromiciops gliroides), Dasyuromorphia (predominantly carnivorous forms such as quolls, antechinuses, dunnarts, the Tasmanian devil, the numbat, and the recently extinct thylacine), Diprotododontia (possums, gliders, kangaroos, wallabies, rat kangaroos, wombats, koalas, etc.), Notoryctemorphia (marsupial moles), and Peramelemorphia (bandicoots and bilbies).
Dromiciops gliroides (the sole extant microbiotherian) and the three genera of modern paucituberculatans (Caenolestes, Lestoros, and Rhyncholestes, all members of the family Caenolestidae) are exclusively South American in distribution (Gardner, 2008). Fossil members of both orders are known from South America (
“…Recently, Castro et al (2021), when revising the fossil record of Didelphidae from South America, considered that the middle Miocene didelphids from Madre de Dios (MD-67),…”
Section: Biostratigraphical and Chronostratigraphical Implicationsmentioning
confidence: 99%
“…The Amazonian region has been regarded as a key area concerning the Neogene marsupial radiations (Goin, 1997;Antoine et al, 2017;Suárez Gómez, 2019;Castro et al, 2021). The records from La Venta, for instance, suggest that this area was both a "cradle", i.e., a high-diversification rate area, as well as a "museum", with low extinction rates (Suárez Gómez, 2019).…”
“…Reig, 1981; Simpson, 1980) to the history and dynamics of a given region (see the different chapters in Patterson & Costa, 2012) or a given taxon (e.g. Castro et al, 2021). In general, inferred biogeographic patterns have been linked to a wide range of geological and climatic events (e.g.…”
Aim
Tropical South America, in particular Amazonia, has been identified as the area of the basal diversification of several large mammal clades. Whether this scenario also holds for younger and widely distributed clades remains unclear. Here, we assessed the historical biogeography of a young but diverse and widely distributed mammal clade.
Location
The Neotropics.
Taxon
Long‐tailed mice of the genus Oligoryzomys.
Methods
We estimated a dated species tree by sampling five genes (one mitochondrial and four nuclear) from 30 of the 32 living species of the genus. We inferred the distribution of the most recent common ancestors (MRCAs) of distinct species groups, using a 13 ecoregion scheme and fitting three biogeographical models, to simulate dispersal events under the selected model.
Results
The DEC model best explained the diversification of Oligoryzomys. The MRCA of the genus had an age of ~2.64 Mya and its ancestral area was inferred as a large region encompassing Boreal and Southern Amazonia, Chaco and Tropical Andes. Subsequent vicariance events, followed by dispersal events towards the present, account for its diversification and wide distribution.
Main conclusion
The biogeographical history of Oligoryzomys is complex. It originated in the northern half of South America; and then after a series of vicariant events, a series of dispersion events allowed it to colonize southern South America, the Andes and closer to the present Central and North America. This radiation, which constitutes one of the fastest and largest Pleistocene diversifications of Neotropical mammals, involves events previously suggested for other groups (e.g. Andean diversification), others that are novel for rodents and for the most part for South American mammals (e.g. the identification of the Chaco as a centre of diversification).
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