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Molecular phylogeny of the Notostraca.

TitreMolecular phylogeny of the Notostraca.
Type de publicationJournal Article
Year of Publication2013
AuteursKorn, M, Rabet, N, Ghate, HV, Marrone, F, Hundsdoerfer, AK
JournalMol Phylogenet Evol
Volume69
Ticket3
Pagination1159-71
Date Published2013 Dec
ISSN1095-9513
Mots-clésAnimals, Bayes Theorem, Biological Evolution, Cell Nucleus, Crustacea, DNA, Mitochondrial, Fossils, Likelihood Functions, Models, Genetic, Phylogeny, Sequence Alignment, Sequence Analysis, DNA
Résumé

We used a combined analysis of one nuclear (28S rDNA) and three mitochondrial markers (COI, 12S rDNA, 16S rDNA) to infer the molecular phylogeny of the Notostraca, represented by samples from the six continents that are inhabited by this group of branchiopod crustaceans. Our results confirm the monophyly of both extant notostracan genera Triops and Lepidurus with good support in model based and maximum parsimony analyses. We used branchiopod fossils as a calibration to infer divergence times among notostracan lineages and accounted for rate heterogeneity among lineages by applying relaxed-clock models. Our divergence date estimates indicate an initial diversification into the genera Triops and Lepidurus in the Mesozoic, most likely at a minimum age of 152.3-233.5 Ma, i.e., in the Triassic or Jurassic. Implications for the interpretation of fossils and the evolution of notostracan morphology are discussed. We further use the divergence date estimates to formulate a biogeographic hypothesis that explains distributions of extant lineages predominantly by overland dispersal routes. We identified an additional hitherto unrecognised highly diverged lineage within Lepidurus apus lubbocki and three additional previously unknown major lineages within Triops. Within T. granarius we found deep differentiation, with representatives distributed among three major phylogenetic lineages. One of these major lineages comprises T. cancriformis, the T. mauritanicus species group and two hitherto unrecognised T. granarius lineages. Samples that were morphologically identified as T. granarius diverged from the most basal nodes within this major lineage, and divergence dates suggested an approximate age of 23.7-49.6 Ma for T. cancriformis, indicating the need for a taxonomic revision of Triassic and Permian fossils that are currently attributed to the extant T. cancriformis. We thus elevate T. cancriformis minor to full species status as Triops minorTrusheim, 1938 and include in this species the additional Upper Triassic samples that were attributed to T. cancriformis. We further elevate T. cancriformis permiensis to full species status as Triops permiensisGand et al., 1997.

DOI10.1016/j.ympev.2013.08.006
Alternate JournalMol. Phylogenet. Evol.
Identifiant (ID) PubMed23973879