Background: was described as an emydine turtle based on a well-preserved skull retrieved from late Miocene deposits exposed on Piram Island, India. The description and figures provided in the original publication are vague and do not support assignment to Emydinae. This taxon has mostly been ignored by subsequent authors.
Material And Methods: We reexamine the holotype specimen, provide an extensive description and diagnosis for , and include this taxon in a global character-taxon matrix for Pleurodira.
Results: The presence of a processus trochlearis pterygoidei conclusively shows pleurodiran affinities for . Inclusion of this taxon in a phylogenetic analysis retrieves it within Stereogenyini closely related to the Asian taxa and .
Discussion: Our reexamination of the holotype of confidently rejects the original assessment of this taxon as an emydine testudinoid and conclusively shows affinities with the pleurodiran clade Stereogenyini instead. Even though most taxa from this lineage are thought to be coastal turtles, all Asian stereogenyines were collected from continental deposits, suggesting a more diverse paleoecology for the group.
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http://dx.doi.org/10.7717/peerj.5938 | DOI Listing |
Proc Natl Acad Sci U S A
January 2025
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China.
Subducted plates often stagnate in the mantle transition zone (MTZ), and the fate of the stagnant slabs is still debatable. They may sink into the lower mantle, or remain partially trapped in the MTZ, but it is uncertain whether they can return to the upper mantle. We report geochemical evidence of late-Miocene (~6 Ma) basalts from, and upper mantle seismic evidence beneath Shuangyashan, an area above the slab tear of the stagnant Pacific plate in eastern Asia, to show how the slab returns to the upper mantle from the MTZ.
View Article and Find Full Text PDFProc Biol Sci
January 2025
Department of Biology, Saint Louis University, St Louis, MO 63103, USA.
Jawless vertebrates once dominated Palaeozoic waters, but just two lineages have persisted to the present day: lampreys and hagfishes. Living lampreys are a relatively small clade, with just over 50 species described, but knowledge of their evolutionary relationships has always been based on either a few mitochondrial genes or a small number of taxa. Biogeographers have noted the disjunct antitropical distribution of living lamprey families.
View Article and Find Full Text PDFBiology (Basel)
December 2024
Liaoning Key Laboratory of Development and Utilization for Natural Products Active Molecules, Anshan Normal University, Anshan 114000, China.
Climate change and human activities are expected to have a profound impact on the distribution of species, especially for narrowly distributed species. is endemically distributed in China, and all species are listed under Chinese protected wild species. Here, we reconstructed the phylogeny and estimated the divergence time of based on whole plastomes, conducted the niche evolution, and predicted the potential habitat area of from the LGM to the future.
View Article and Find Full Text PDFBiology (Basel)
December 2024
Department of Earth Sciences, NOVA School of Science and Technology, GEOBIOTEC, Campus de Caparica, 2829-516 Caparica, Portugal.
On the African continent, Picrodendraceae are represented by four genera. Their intracontinental paleophytogeographic histories and paleoecological aspects are obscured by the lack of pre-Miocene fossils. For this study, late Eocene sediments from Kenya were investigated.
View Article and Find Full Text PDFSci Rep
December 2024
College of Mining Engineering, Guizhou University of Engineering Science, Bijie, 551700, China.
The Laurani high-sulfidation epithermal deposit, located in the northeastern Altiplano of Bolivia, is a representative gold-polymetallic deposit linked to the late Miocene volcanic rocks that were formed approximately at about 7.5 Ma. At Laurani, four mineralization stages are defined.
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