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1.
PeerJ ; 9: e11805, 2021.
Artículo en Inglés | MEDLINE | ID: mdl-34430073

RESUMEN

The geoemydid turtles of the Eocoene Messel Pit Quarry of Hesse, Germany, are part of a rich Western European fossil record of testudinoids. Originally referred to as "Ocadia" kehreri and "Ocadia" messeliana, their systematic relationships remain unclear. A previous study proposed that a majority of the Western European geoemydids, including the Messel geoemydids, are closely related to the Recent European representatives of the clade Mauremys. Another study hypothesised that the Western European geoemydid fauna is more phylogenetically diverse, and that the Messel geoemydids are closely related to the East Asian turtles Orlitia and Malayemys. Here we present the first quantitative analyses to date that investigate this question. We use continuous characters in the form of ratios to estimate the placement of the Messel geoemydids in a reference tree that was estimated from molecular data. We explore the placement error obtained from that data with maximum likelihood and Bayesian methods, as well as linear parsimony in combination with discrete characters. We find good overall performance with Bayesian and parsimony analyses. Parsimony performs even better when we also incorporated discrete characters. Yet, we cannot pin down the position of the Messel geoemydids with high confidence. Depending on how intraspecific variation of the ratio characters is treated, parsimony favours a placement of the Messel fossils sister to Orlitia borneensis or sister to Geoemyda spengleri, with weak bootstrap support. The latter placement is suspect because G. spengleri is a phylogenetically problematic species with molecular and morphological data. There is even less support for placements within the Mauremys clade.

2.
PeerJ ; 7: e7476, 2019.
Artículo en Inglés | MEDLINE | ID: mdl-31497387

RESUMEN

BACKGROUND: In the last 20 years, a general picture of the evolutionary relationships between geoemydid turtles (ca. 70 species distributed over the Northern hemisphere) has emerged from the analysis of molecular data. However, there is a paucity of good traditional morphological characters that correlate with the phylogeny, which are essential for the robust integration of fossil and molecular data. Part of this problem might be due to intrinsic limitations of traditional discrete characters. Here, we explore the use of continuous data in the form of 3D coordinates of homologous landmarks on the turtle shell for phylogenetic inference and the phylogenetic placement of single species on a scaffold molecular tree. We focus on the performance yielded by sampling the carapace and/or plastral lobes and using various phylogenetic methods. METHODS: We digitised the landmark coordinates of the carapace and plastron of 42 and 46 extant geoemydid species, respectively. The configurations were superimposed and we estimated the phylogenetic tree of geoemydids with landmark analysis under parsimony, traditional Farris parsimony, unweighted squared-change parsimony, maximum likelihood with a Brownian motion model, and neighbour-joining on a matrix of pairwise Procrustes distances. We assessed the performance of those analyses by comparing the trees against a reference phylogeny obtained from seven molecular markers. For comparisons between trees we used difference measures based on quartets and splits. We used the same reference tree to evaluate phylogenetic placement performance by a leave-one-out validation procedure. RESULTS: Whatever method we used, similarity to the reference phylogeny was low. The carapace alone gave slightly better results than the plastron or the complete shell. Assessment of the potential for placement of single species on the reference tree with landmark data gave much better results, with similar accuracy and higher precision compared to the performance of discrete characters with parsimony.

3.
BMC Evol Biol ; 19(1): 117, 2019 06 10.
Artículo en Inglés | MEDLINE | ID: mdl-31182024

RESUMEN

BACKGROUND: The branchiostegal series consists of an alignment of bony elements in the posterior portion of the skull of osteichthyan vertebrates. We trace the evolution of the number of elements in a comprehensive survey that includes 440 extant and 66 extinct species. Using a newly updated actinopterygian tree in combination with phylogenetic comparative analyses, we test whether osteichthyan branchiostegals follow an evolutionary trend under 'Williston's law', which postulates that osteichthyan lineages experienced a reduction of bony elements over time. RESULTS: We detected no overall macroevolutionary trend in branchiostegal numbers, providing no support for 'Williston's law'. This result is robust to the subsampling of palaeontological data, but the estimation of the model parameters is much more ambiguous. CONCLUSIONS: We find substantial evidence for a macroevolutionary dynamic favouring an 'early burst' of trait evolution over alternative models. Our study highlights the challenges of accurately reconstructing macroevolutionary dynamics even with large amounts of data about extant and extinct taxa.


Asunto(s)
Evolución Biológica , Extinción Biológica , Fósiles , Vertebrados/anatomía & histología , Animales , Biodiversidad , Modelos Teóricos , Filogenia , Tamaño de la Muestra , Cráneo/anatomía & histología , Factores de Tiempo
4.
R Soc Open Sci ; 4(11): 170899, 2017 Nov.
Artículo en Inglés | MEDLINE | ID: mdl-29291083

RESUMEN

In a previous study, we estimated the cranial disparity of turtles (Testudinata) through time using geometric morphometric data from both terminal taxa and hypothetical ancestors to compensate for temporal gaps in the fossil record. While this method yielded reasonable results for the Mesozoic and the early Cenozoic, we found a large drop in cranial disparity for the Miocene, for which we found no correlation with known environmental changes or extinction events. Instead, we speculated that the Miocene dip was a result of poor sampling of fossils or ancestors in this time bin. To countervail this problem, we here updated our original dataset and interpolated changes of shape along the branch lengths and compared them with the previous data. We furthermore explored the impact of topological and temporal uncertainty, demonstrating that the Miocene dip, indeed, is a sampling artefact. All remaining conclusions of the previous study could be more or less supported, nevertheless, including an apparent correlation with global biogeographic events, a minor correlation between cranial disparity and global temperature, and resilience across the K/T extinction event.

5.
La Paz; 1980. 132 p. ilus.
Tesis en Español | LIBOCS, LIBOSP | ID: biblio-1311295

RESUMEN

El presente trabajo constituye un estudio para posibilitar la rehabilitacion de una empresa que se halla en esta situacion deficitaria. Por tratarsede un trabajo academico se lo ha encarado desde este punto de vista; en tal sentido incluye disgnosticos a nivel de subregion, a nivel nacional y de la propia empresa; un plan de rehabilitacion; estudio de mercado, estudio tecnico y estudio economico-financiero, sin dejar de lado la posibilidad de su aplicacion practica. Para la realizacion del trabajo se han utilizado informes, estudios y antecedentes sobre el tema, ademas de diagnosticos y datos estadisticos disponibles tanto a nivel de Camara de Industrias, Asociacion de Industriales del cuero y calzado como a nivel de Instituciones del Estado. Esta tarea ha sido complementada con la realizacion de un trabajo de campo intenso, con el objeto de tomar todos los datos y antecedentes correspondientes a la empresa, objeto del estudio. Para finalizar, el presente estudio no tiene otro proposito, que el de poder contribuir con la presentacion de un tema diferente pero de fundamental interes, tanto para empresarios, trabajadores, como para el propio gobierno.

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