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Journal articles on the topic 'Tethyan relationship'

Author: Grafiati

Published: 4 June 2025

Last updated: 1 August 2025

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1

Tiwari, R. S., and Vijaya. "Reflection on relationship of Tethyan palynoflora." Journal of Palaeosciences 36 (December 31, 1987): 339–53. http://dx.doi.org/10.54991/jop.1987.1592.

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The Early Carboniferous palynoassemblage from Spiti in Tethyan Himalaya has a restricted comparability with that of Cathaysia, more pronounced relationship with that of Australia and Middle-East while apparent form similarity with the western Tethyan region. During the Permian, few elements are definitely common between Himalaya Tethys zone and the Angara-Cathaysia assemblages but there are strong indications of an influence of Indian palynoflora on Himalayan Tethys belt. Towards western Tethys wedge, the resemblance decreases gradually and new palynotaxa are observed indicating the European a

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2

Du, Bin, Zian Yang, Lifei Yang, et al. "Zircon Hf-Isotopic Mapping Applied to the Metal Exploration of the Sanjiang Tethyan Orogenic Belt, Southwestern China." Applied Sciences 12, no. 8 (2022): 4081. http://dx.doi.org/10.3390/app12084081.

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Zircon Hf-isotopic mapping can be regarded as a useful tool for evaluating the coupling relationship between lithospheric structure and metallic mineralization. Hence, this method shows important significance for mineral prediction. To explore this potential, the published granite zircon Hf isotope data from the Sanjiang Tethyan Orogen were systematically compiled. This study uses the Kriging weighted interpolation in the Mapgis software system to contour Hf isotopes, revealing a relation between the crustal structure and metallogenesis. The mapping results suggest that the Changning–Menglian

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3

Murray, Alison M., Thodoris Argyriou, and Todd D. Cook. "Palaeobiogeographic relationships and palaeoenvironmental implications of an earliest Oligocene Tethyan ichthyofauna from Egypt." Canadian Journal of Earth Sciences 51, no. 10 (2014): 909–18. http://dx.doi.org/10.1139/cjes-2014-0097.

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The Fayum Depression of Egypt has produced a great diversity of fossil material, including marine and freshwater fishes. In contrast to the Eocene formations of the Fayum, the Oligocene Jbel Qatrani Formation has been more or less consistently considered to be deposited in a freshwater environment; however, the ichthyofauna indicates a more complex picture. Cenozoic fishes have been convincingly used to interpret the palaeoenvironment in which sediments were deposited. Based on the elasmobranch and osteichthyan faunas of the Jbel Qatrani Formation, we interpret that this formation was not depo

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4

SPAHIĆ, Darko, and Tivadar GAUDENYI. "The role of the pre-Alpine polycrystalline basement in the paleogeographic configuration of multiple Neotethyan oceanic basins." Geologija 64, no. 2 (2021): 143–58. http://dx.doi.org/10.5474/geologija.2021.008.

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The study provides a deeper understanding of the early Mesozoic paleogeogeographic spatial-temporal relationship by studying the two Adria-Europe intervening basement blocks. The Drina-Ivanjica and Pelagonian crustal fragments play important role in the internal early Alpine oceanic constitution further controlling the late Jurassic emplacement of Tethyan Dinaric-Hellenic ophiolites. The proposed paleogeographic reassessment is driven by the new paleocontinental inheritance data associated with the Variscan – pre-Variscan basement terranes. The recently published data suggest an Avalonian-type

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5

Hua-Zhang, Pan, and Shen Shu-Zhong. "Late Permian (Lopingian) gastropods from the Qubuerga Formation at the Qubu section in the Mt. Everest (Qomolangma) Region, Southern Tibet (Xizang), China." Journal of Paleontology 82, no. 5 (2008): 1038–42. http://dx.doi.org/10.1666/06-089.1.

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Late Permian gastropod fauna in the Mt. Everest (Qomolangma) region, southern Tibet (Xizang), China is poorly known. This paper describes a small gastropod fauna collected by one of the authors (SSZ) from the upper part of the Qubuerga Formation at the Qubu section. The section is located at about 30 km north of Mt. Everest (Fig. 1). Although a limited number of specimens is available, the fauna is more diverse than all previously reported gastropod faunas (e.g., Yu, 1975) from southern Tibet. Description of the gastropod fauna in the Mt. Everest region adds significant data for understanding

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6

Wang, Yaning, Wei Huang, Tao Cheng, Xuan Chen, Qinqin Cong, and Jianhao Liang. "Facies-Controlled Sedimentary Distribution and Hydrocarbon Control of Lower Cretaceous Source Rocks in the Northern Persian Gulf." Journal of Marine Science and Engineering 13, no. 3 (2025): 576. https://doi.org/10.3390/jmse13030576.

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The two-phase source rocks deposited during the Lower Cretaceous in the Persian Gulf Basin play a pivotal role in the regional hydrocarbon system. However, previous studies have lacked a macroscopic perspective constrained by the Tethyan Ocean context, which has limited a deeper understanding of their developmental patterns and hydrocarbon control mechanisms. To address this issue, this study aims to clarify the spatiotemporal evolution of the two-phase source rocks and their hydrocarbon control effects, with a particular emphasis on the critical impact of terrestrial input on the quality impr

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7

Vargas, Sergio, Michael Eitel, Odalisca Breedy, and Bernd Schierwater. "Molecules match morphology: mitochondrial DNA supports Bayer's Lytreia - Bebryce - Heterogorgia (Alcyonacea : Octocorallia) clade hypothesis." Invertebrate Systematics 24, no. 1 (2010): 23. http://dx.doi.org/10.1071/is09033.

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Several studies attempting to clarify the taxonomy and systematics of Octocorallia have highlighted the important role of molecular characters in corroborating or rejecting previous hypotheses based on morphological variation. One such hypothesis is that of a close phylogenetic relationship between the genera Lytreia, Bebryce and Heterogorgia proposed by Bayer based on morphological studies of the genera. Herein, we tested Bayer’s hypothesis using the mitochondrial marker mshI. We deduced a molecular phylogeny including members of the families Gorgoniidae and ‘Paramuriceidae’ that corroborated

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8

Vega, Francisco J., Timothy Cosma, Marco A. Coutiño, et al. "New middle Eocene decapods (Crustacea) from Chiapas, México." Journal of Paleontology 75, no. 5 (2001): 929–46. http://dx.doi.org/10.1017/s002233600003986x.

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Decapod crustacean specimens from the middle Eocene San Juan Formation in central Chiapas represent the first record of Eocene decapods in southern México. New taxa include: Dardanus mexicanus new species (Diogenidae), Lophoranina cristaspina new species, Notopus minutus new species (Raninidae); Verrucoides stenohedra new genus and new species (Xanthidae); Stoaplax nandachare new genus and new species (Goneplacidae); and Viapinnixa alvarezi new species (Pinnotheridae). Verrucoides verrucoides new genus and new combination from the Paleocene of Greenland represents a new combination. In additio

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9

KARANOVIC, IVANA. "A new Candonopsini (Ostracoda) genus from subterranean waters of New South Wales (Australia)." Zootaxa 4379, no. 2 (2018): 247. http://dx.doi.org/10.11646/zootaxa.4379.2.6.

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The Australian Candonidae ostracod fauna has few surface water representatives, despite Australia being one of the principal centers of Candonidae biodiversity. The majority of Australian species live in subterranean waters, with most genera and one tribe being endemic to the continent. Species in Australia show Tethyan and Gondwana connections, with relatives living in European and Central/South American subterranean waters. I describe Hancockcandonopsis gen. nov. from boreholes in the alluvial aquifers of the Peel River and Hunter Valley, which at present contains five species, of which thre

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10

Yoshida, Masaru, Sant M. Rai, Ananta P. Gajurel, Tara N. Bhattarai, and Bishal N. Upreti. "Relationship between the Higher Himalayan Crystalline and Tethyan Sediments in the Kali Gandaki area, western Central Nepal: South Tibetan Detachment revisited." Himalayan Journal of Sciences 2, no. 4 (2008): 285. http://dx.doi.org/10.3126/hjs.v2i4.954.

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11

XueXiang, QI, SHENG Hui, WEI Cheng, et al. "Longlin-Ruili subduction-accretionary complex belt in the southeastern Gaoligong orogen, and its relationship with the evolution of the Meso-Tethyan Ocean." Acta Petrologica Sinica 37, no. 10 (2021): 3067–94. http://dx.doi.org/10.18654/1000-0569/2021.10.07.

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12

Liu, Liang, Rui-Zhong Hu, Hong Zhong, et al. "Petrogenesis of multistage S-type granites from the Malay Peninsula in the Southeast Asian tin belt and their relationship to Tethyan evolution." Gondwana Research 84 (August 2020): 20–37. http://dx.doi.org/10.1016/j.gr.2020.02.013.

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13

Yan, Songtao, Ailing Ding, Jie Wang, et al. "Structural and Kinematic Analysis of the Xipu Dome in the Tingri Area, Southern Tibet, and New Exploration Discoveries." Minerals 14, no. 12 (2024): 1188. http://dx.doi.org/10.3390/min14121188.

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The newly delineated Xipu Dome, located in the central North Himalayan Gneiss Dome (NHGD), exhibits a significant spatiotemporal relationship with Himalayan polymetallic mineralization. Based on field geological surveys and geochronological analyses, this study provides a comprehensive assessment of the lithological assemblage, tectonic deformation, and metallogenic processes of the Xipu Dome. The findings reveal a three-tiered structure: the core consists of early Paleozoic granitic gneiss (523 Ma) and Miocene leucogranite (13.5 Ma), overlain by a cover of low-grade metamorphic or unmetamorph

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14

Moyne, Sébastien, Pascal Neige, Didier Marchandet, and Jacques Thierry. "World distribution of middle Jurassic ammonites (Upper Aalenian to Middle Bathonian): relationships between biodiversity and palaeogeography." Bulletin de la Société Géologique de France 175, no. 5 (2004): 513–23. http://dx.doi.org/10.2113/175.5.513.

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Abstract The break up of the Pangea takes place in the Jurassic; the palaeoceanographic consequences are the opening of seaways, particularly at the place of the future Atlantic and Indian oceanic areas. During the Toarcian, and from the late Aalenian to the middle Bathonian, the so-called “Hispanic corridor” (or “Atlantic seaway”) exists between the “western Tethys” and the “American Pacific border”, through the “Caribbean Tethys”. Two additional seaways which play as by-passes of the Pangea are proposed, one along the northern border of Laurasia (Boreal sea), and a second along the southern

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15

Krobicki (ed.), Michał. "Field trip - Outer Flysch Carpathians, Pieniny Klippen Belt (PKB), and Tatra Mountains." Geotourism/Geoturystyka, no. 1-2(76-77) (June 18, 2024): 5–77. https://doi.org/10.7494/geotour.2024.1-2(76-77).5.

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The 36th HKT Workshop (Himalaya-Karakorum- Tibet) is organised by the AGH University of Krakow, Poland. Kraków is situated at the front of the Carpathian orogenic system of the ancient Tethys Ocean and is perfect place for meeting between European-Asian Alpine-Himalayan orogenic belt with long history of the Western and Eastern Tethyan Ocean Realms. The 36th HKT Workshop concerns mainly on this first area and the meeting will be focused on Himalaya-Karakorum-Tibet regions but will be also concentrated (especially during field trip) on comparison between Asian (eastern) and European (western) p

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16

Squires, Richard L., and David M. Advocate. "New Early Eocene mollusks from the Orocopia Mountains, southern California." Journal of Paleontology 60, no. 4 (1986): 851–64. http://dx.doi.org/10.1017/s0022336000042992.

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Five new species of mollusks are described from the early Eocene Maniobra Formation, northeastern Orocopia Mountains, southern California. The new species are from the basal part of the formation, and the fauna is indicative of the West Coast provincial molluscan early Eocene “Capay Stage.” The mollusks are shallow-marine forms that were transported a short distance into slope/upper submarine-canyon deposits.Chedevillia saltonensis n. sp. and Eocypraea? maniobraensis n. sp. resemble Eocene species from Paris Basin, France. Phalium (Semicassis) louella n. sp. is the earliest North American spec

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17

Krobicki (ed.), Michał. "Field trip – Outer Flysch Carpathians and Pieniny Klippen Belt (PKB)." Geotourism/Geoturystyka, no. 3-4(74-75) (October 3, 2023): 5–70. http://dx.doi.org/10.7494/geotour.2023.3-4(74-75).5.

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We are glad that we can meet personally during the 2nd Symposium of the IGCP 710 Project, after the pandemic time, which disrupted our idea of regular, annual meetings. After the 1st virtual meeting during the autumn of 2021, we have now the chance to discuss face to face and go to the field together to touch „Tethyan” rocks for a better understanding of what happened hundreds/decades of millions years ago in our lovely ancient ocean. As you know, through your knowledge and experience, the Tethyan Ocean history, both in its western and eastern parts, is fascinating, but enigmatic from time to

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18

Senowbari-Daryan, Baba, and George D. Stanley. "Triassic sponges (Sphinctozoa) from Hells Canyon, Oregon." Journal of Paleontology 62, no. 03 (1988): 419–23. http://dx.doi.org/10.1017/s0022336000018333.

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Two Upper Triassic sphinctozoan sponges of the family Sebargasiidae were recovered from silicified residues collected in Hells Canyon, Oregon. These sponges areAmblysiphonellacf.A. steinmanni(Haas), known from the Tethys region, andColospongia whalenin. sp., an endemic species. The latter sponge was placed in the superfamily Porata by Seilacher (1962). The presence of well-preserved cribrate plates in this sponge, in addition to pores of the chamber walls, is a unique condition never before reported in any porate sphinctozoans. Aporate counterparts known primarily from the Triassic Alps have s

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19

Senowbari-Daryan, Baba, and George D. Stanley. "Triassic sponges (Sphinctozoa) from Hells Canyon, Oregon." Journal of Paleontology 62, no. 3 (1988): 419–23. http://dx.doi.org/10.1017/s0022336000059187.

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Two Upper Triassic sphinctozoan sponges of the family Sebargasiidae were recovered from silicified residues collected in Hells Canyon, Oregon. These sponges are Amblysiphonella cf. A. steinmanni (Haas), known from the Tethys region, and Colospongia whaleni n. sp., an endemic species. The latter sponge was placed in the superfamily Porata by Seilacher (1962). The presence of well-preserved cribrate plates in this sponge, in addition to pores of the chamber walls, is a unique condition never before reported in any porate sphinctozoans. Aporate counterparts known primarily from the Triassic Alps

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20

Hulva, Pavel, Ivan Horáček, and Petr Benda. "Molecules, morphometrics and new fossils provide an integrated view of the evolutionary history of Rhinopomatidae (Mammalia: Chiroptera)." BMC Evolutionary Biology 7, no. 1 (2007): 165. https://doi.org/10.5281/zenodo.13417822.

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(Uploaded by Plazi for the Bat Literature Project) Background: The Rhinopomatidae, traditionally considered to be one of the most ancient chiropteran clades, remains one of the least known groups of Rhinolophoidea. No relevant fossil record is available for this family. Whereas there have been extensive radiations in related families Rhinolophidae and Hipposideridae, there are only a few species in the Rhinopomatidae and their phylogenetic relationship and status are not fully understood. Results: Here we present (a) a phylogenetic analysis based on a partial cytochrome b sequence, (b) new fos

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21

Hulva, Pavel, Ivan Horáček, and Petr Benda. "Molecules, morphometrics and new fossils provide an integrated view of the evolutionary history of Rhinopomatidae (Mammalia: Chiroptera)." BMC Evolutionary Biology 7, no. 1 (2007): 165. https://doi.org/10.5281/zenodo.13417822.

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(Uploaded by Plazi for the Bat Literature Project) Background: The Rhinopomatidae, traditionally considered to be one of the most ancient chiropteran clades, remains one of the least known groups of Rhinolophoidea. No relevant fossil record is available for this family. Whereas there have been extensive radiations in related families Rhinolophidae and Hipposideridae, there are only a few species in the Rhinopomatidae and their phylogenetic relationship and status are not fully understood. Results: Here we present (a) a phylogenetic analysis based on a partial cytochrome b sequence, (b) new fos

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22

Hulva, Pavel, Ivan Horáček, and Petr Benda. "Molecules, morphometrics and new fossils provide an integrated view of the evolutionary history of Rhinopomatidae (Mammalia: Chiroptera)." BMC Evolutionary Biology 7, no. 1 (2007): 165. https://doi.org/10.5281/zenodo.13417822.

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(Uploaded by Plazi for the Bat Literature Project) Background: The Rhinopomatidae, traditionally considered to be one of the most ancient chiropteran clades, remains one of the least known groups of Rhinolophoidea. No relevant fossil record is available for this family. Whereas there have been extensive radiations in related families Rhinolophidae and Hipposideridae, there are only a few species in the Rhinopomatidae and their phylogenetic relationship and status are not fully understood. Results: Here we present (a) a phylogenetic analysis based on a partial cytochrome b sequence, (b) new fos

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23

Hulva, Pavel, Ivan Horáček, and Petr Benda. "Molecules, morphometrics and new fossils provide an integrated view of the evolutionary history of Rhinopomatidae (Mammalia: Chiroptera)." BMC Evolutionary Biology 7, no. 1 (2007): 165. https://doi.org/10.5281/zenodo.13417822.

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(Uploaded by Plazi for the Bat Literature Project) Background: The Rhinopomatidae, traditionally considered to be one of the most ancient chiropteran clades, remains one of the least known groups of Rhinolophoidea. No relevant fossil record is available for this family. Whereas there have been extensive radiations in related families Rhinolophidae and Hipposideridae, there are only a few species in the Rhinopomatidae and their phylogenetic relationship and status are not fully understood. Results: Here we present (a) a phylogenetic analysis based on a partial cytochrome b sequence, (b) new fos

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24

Hulva, Pavel, Ivan Horáček, and Petr Benda. "Molecules, morphometrics and new fossils provide an integrated view of the evolutionary history of Rhinopomatidae (Mammalia: Chiroptera)." BMC Evolutionary Biology 7, no. 1 (2007): 165. https://doi.org/10.5281/zenodo.13417822.

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(Uploaded by Plazi for the Bat Literature Project) Background: The Rhinopomatidae, traditionally considered to be one of the most ancient chiropteran clades, remains one of the least known groups of Rhinolophoidea. No relevant fossil record is available for this family. Whereas there have been extensive radiations in related families Rhinolophidae and Hipposideridae, there are only a few species in the Rhinopomatidae and their phylogenetic relationship and status are not fully understood. Results: Here we present (a) a phylogenetic analysis based on a partial cytochrome b sequence, (b) new fos

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25

Hulva, Pavel, Ivan Horáček, and Petr Benda. "Molecules, morphometrics and new fossils provide an integrated view of the evolutionary history of Rhinopomatidae (Mammalia: Chiroptera)." BMC Evolutionary Biology 7, no. 1 (2007): 165. https://doi.org/10.5281/zenodo.13417822.

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(Uploaded by Plazi for the Bat Literature Project) Background: The Rhinopomatidae, traditionally considered to be one of the most ancient chiropteran clades, remains one of the least known groups of Rhinolophoidea. No relevant fossil record is available for this family. Whereas there have been extensive radiations in related families Rhinolophidae and Hipposideridae, there are only a few species in the Rhinopomatidae and their phylogenetic relationship and status are not fully understood. Results: Here we present (a) a phylogenetic analysis based on a partial cytochrome b sequence, (b) new fos

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26

Afzal, Jawad, Mark Williams, and Richard J. Aldridge. "Revised stratigraphy of the lower Cenozoic succession of the Greater Indus Basin in Pakistan." Journal of Micropalaeontology 28, no. 1 (2009): 7–23. http://dx.doi.org/10.1144/jm.28.1.7.

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Abstract. A refined stratigraphy for the lower Cenozoic succession of the Greater Indus Basin in Pakistan is presented. This region preserves an important East Tethyan marine succession through the Paleocene–Eocene, but its interpretation in terms of regional (tectonic) and global (climatic) effects has been inhibited by poor stratigraphy. Established dinoflagellate, nannofossil, planktonic foraminiferal and shallow benthonic foraminiferal biostratigraphical data for the Greater Indus Basin in Pakistan are collated, reinterpreted (where necessary) and correlated with the global standard chrono

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27

Rieppel, Olivier, Li Jinling, and Liu Jun. "Lariosaurus xingyiensis (Reptilia: Sauropterygia) from the Triassic of China." Canadian Journal of Earth Sciences 40, no. 4 (2003): 621–34. http://dx.doi.org/10.1139/e02-067.

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The anatomy of a specimen of Lariosaurus xingyiensis (IVPP V 11866) from the Middle Triassic of southern China is described in detail. The specimen ranks among the best preserved of its genus. Specimen IVPP V 11866 is the first unequivocal record of the occurrence of Lariosaurus in the Triassic of southern China, indeed the first record of this genus outside the western Tethyan province. A cladistic analysis using parsimony found IVPP V 11866 to represent the sister taxon of Lariosaurus calcagnii from the Middle Triassic of the southern Alps. This result reinforces the signal for western Tethy

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28

Guerrera, Francesco, and Manuel Martín-Martín. "Geodynamic events reconstructed in the Betic, Maghrebian, and Apennine chains (central-western Tethys)." Bulletin de la Société Géologique de France 185, no. 5 (2014): 329–41. http://dx.doi.org/10.2113/gssgfbull.185.5.329.

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Abstract A synthetic study has been made to identify main tectono-sedimentary and geodynamic events in central-western Tethys. For this, an interdisciplinary analysis has been performed on successions belonging to tectonic units derived from Betic-Maghrebian-southern Apennine “Flysch basin” domain. The stratigraphic records of the internal, external, and mixed successions deposited in lateral basins of different chains show very similar characters, especially regarding: (a) lithostratigraphy and ages; (b) kind and provenance of supplies (immature and supermature petrofacies from internal and e

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Scott, Robert W., Xiaqiao Wan, Jingeng Sha, and Shi-Xuan Wen. "Rudists of Tibet and the Tarim Basin, China: Significance to Requieniidae phylogeny." Journal of Paleontology 84, no. 3 (2010): 444–65. http://dx.doi.org/10.1666/09-137.1.

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Rudists are a principal biotic component of Cretaceous carbonates in Tibet and in the Western Tarim Basin. Barremian to Maastrichtian carbonate units are widespread on the northern margin of the Indian Plate and in Tethyan tectonic slices that were welded onto Eurasia in successive stages during the Late Cretaceous and Paleogene. In far northwestern Tibet, Barremian-Cenomanian endemic rudists and cosmopolitan orbitolinid foraminifera occupied isolated carbonate platforms in the eastern Tethys. Rudists, corals, and stromatoporoids composed bioherms up to 10 m thick and several kilometers in lat

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Zhang, Ji’en, Wenjiao Xiao, John Wakabayashi, Fulong Cai, and Kyaing Sein. "Detrital Zircon Dating, Deformation Stages, and Tectonics of the Pane Chaung Formation and Surrounding Units in the Western Indo-Burma Range, Southeast Asia." Minerals 14, no. 12 (2024): 1290. https://doi.org/10.3390/min14121290.

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The Indo-Burma Range (IBR), as one of the youngest accreted units in the Eastern Neotethys, plays a crucial role in understanding the interactive relationships between the Gondwana supercontinent and its rifted microcontinents in SE Asia. However, its basement nature and tectonic evolution remain debated. Here, we conducted a comprehensive structural analysis across six sections within the IBR and correlated Late Triassic flysch units between the Western IBR (Pane Chaung Formation) and the Tethyan Himalaya. Within the Mindat section, the eastern segment of the Pane Chaung Formation unit displa

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Broquet, Paul. "Sicily in its Mediterranean geological frame." Boletín Geológico y Minero 127, no. 2-3 (2016): 547–62. http://dx.doi.org/10.21701/bolgeomin.127.2-3.017.

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The Island of Sicily is generally considered to be the geological link between the North African Fold Belt and the Appennines, in Italy. This comes from a cylindristic meaning and is only partly exact. As a matter of fact, Sicily is essentially Greek; Ionian. Up to Middle Cretaceous time, the Sicilian area was a submerged shoal in the sea or the Panormide area, bordering the Ionian Ocean. This shoal lay between the future North African Fold Belt and the Appennines, forming an intermediate link between the Appenninic, Apulian, Panormian and Tunisian platforms. It was only during the Middle to U

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32

Müller, Johannes. "The anatomy of Askeptosaurus italicus from the Middle Triassic of Monte San Giorgio and the interrelationships of thalattosaurs (Reptilia, Diapsida)." Canadian Journal of Earth Sciences 42, no. 7 (2005): 1347–67. http://dx.doi.org/10.1139/e05-030.

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The anatomy of the thalattosauriform reptile Askeptosaurus italicus from the Middle Triassic of Monte San Giorgio is redescribed. Important anatomical features are the plesiomorphic braincase, the unique fronto-lacrimal contact, the absence of a previously described thyroid fenestra, and significant intraspecific variation in the carpus. An analysis of thalattosaur ingroup relationships reveals that Endennasaurus and the monophyletic Askeptosaurus and Anshunsaurus are the sister group to all other thalattosaurs, whereas the Monte San Giorgio taxa Clarazia and Hescheleria form the sister clade

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33

Saghatelyan, A. A. "Phytogeographical relationships and analysis of the flora of South Texas Plains." Journal of the Botanical Research Institute of Texas 11, no. 2 (2017): 527–61. http://dx.doi.org/10.17348/jbrit.v11.i2.1090.

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The southernmost tip of Texas is a part of the Tamaulipan Province of northeastern Mexico which some authors consider in the Madrean Subkingdom of the Holarctic Kingdom, while others the “Xerofitica Mexicana” of the Neotropical Kingdom. To shed more light on this question, a natural flora of fourteen counties in the S TX Plains ecoregion, South Texas Plains flora (S TX), was compiled, studied from a biogeographical perspective, and analyzed in this work. The analysis was based primarily on the species and genera distribution outlines. Phylogenetic literature was searched to find relationships,

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Ridgway, S. A., D. G. Reid, J. D. Taylor, G. M. Branch, and A. N. Hodgson. "A cladistic phylogeny of the family Patellidae (Mollusca: Gastropoda)." Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 353, no. 1375 (1998): 1645–71. http://dx.doi.org/10.1098/rstb.1998.0316.

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A phylogenetic hypothesis for the patellid limpets is reconstructed by cladistic analysis of morphological characters from 37 species, representing all but one of the living members of the family. Characters included in the analysis are derived from shell shape and microstructure, headfoot and pallial complex, radula and sperm. The species fall into four clades, providing the basis for a new phylogenetic classification into four monophyletic genera: Helcion (four species; southern Africa), Cymbula (eight species; southern Africa, eastern Atlantic, southern Indian Ocean), Scutellastra (17 speci

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Crasquin-Soleau, Sylvie, and Aymon Baud. "New Permian ostracods from Greece (Hydra Island)." Journal of Micropalaeontology 17, no. 2 (1998): 131–52. http://dx.doi.org/10.1144/jm.17.2.131.

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Abstract. A new Permian (Late Asselian–Dorashamian) ostracod fauna (66 species belonging to 35 genera) from Hydra Island (Greece) is described. Twelve new species are described: Hollinella (P.) hydraensis Crasquin-Soleau n.sp, Bairdia episkopiensis Crasquin-Soleau n.sp., Bairdia rigasensis Crasquin-Soleau n.sp., Bairdia thikiaensis Crasquin-Soleau n.sp., Chamishaella marmariensis Crasquin-Soleau n.sp., Cypridina gussevaae Crasquin-Soleau n.sp., Cyathus barmariensis Crasquin-Soleau n.sp., Cyathus klimakiensis Crasquin-Soleau n.sp., Bairdiacypris bistiensis Crasquin-Soleau n.sp., Shishaella hell

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Anan, Haidar Salim. "PALEONTOLOGY AND PALEOGEOGRAPHY OF FORTY DIAGNOSTIC SOUTHERN TETHYAN CRETACEOUS-PALEOGENE GLOBIGERINID PLANKTIC FORAMINIFERA." Acta Scientifica Malaysia 8, no. 2 (2024): 93–98. https://doi.org/10.26480/asm.02.2024.93.98.

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Forty planktic foraminiferal species were erected from ten localities in the Southern Tethys: Tunisia, Egypt, Angola, Tanzania, Iraq, Kuwait, UAE, Iran, Pakistan, and India. Sixteen of the identified species were erected from Egypt, while 4 from each of Kuwait and India, 3 from UAE, 2 from each of Tunisia, Angola, and Pakistan. Some of the recorded species were recorded also from many countries in the Northern and Southern Tethys: i.e., Austria, Denmark, Spain, Australia, New Zealand, and USA. Three out of the identified species are believed here to be new: *Morozovella arabica*, *Morozovella

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Heim, Isabel, Michael Nickel, and Franz Brümmer. "Phylogeny of the genus Tethya (Tethyidae: Hadromerida: Porifera): molecular and morphological aspects." Journal of the Marine Biological Association of the United Kingdom 87, no. 6 (2007): 1615–27. http://dx.doi.org/10.1017/s0025315407058419.

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The genus Tethya represents a large cosmopolitan group of 81 recognized and a significant number of additional, still undescribed sponge species. The phylogenetic relationships within this old taxon are almost unknown. This is represented by the fact that several species are regarded as cosmopolitan. However, some of them might represent groups of closely related but distinct species. Using molecular and morphological characters, we aimed at a fundamental phylogenetic study for the genus Tethya, evaluating an existing morphological matrix and the cytochrome oxidase subunit I (COI) as a molecul

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Kim, Chi-fai, Simon K. Y. Lee, Jackie Price, Ralph W. Jack, Geoffrey Turner та Richard Y. C. Kong. "Cloning and Expression Analysis of the pcbAB-pcbC β-Lactam Genes in the Marine Fungus Kallichroma tethys". Applied and Environmental Microbiology 69, № 2 (2003): 1308–14. http://dx.doi.org/10.1128/aem.69.2.1308-1314.2003.

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ABSTRACT Here we report the identification of the β-lactam biosynthesis genes pcbAB and pcbC from a cosmid genomic DNA library of the marine fungus Kallichroma tethys. A BLAST homology search showed that they share high sequence identity with the δ-(l-α-aminoadipyl)-l-cysteinyl-d-valine (ACV) synthetases and isopenicillin N synthases, respectively, of various fungal and bacterial β-lactam producers, while phylogenetic analysis indicated a close relationship with homologous genes of the cephalosporin-producing pyrenomycete Acremonium chrysogenum. Expression analysis by reverse transciption-PCR

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HUANG, ZHEN-FU, HIDEYUKI CHIBA, XIAO-HUA DENG, SI-YAO HUANG, MIN WANG, and XIAO-LING FAN. "Molecular and morphological evidence reveals that Daimio Murray, 1875 is a junior synonym of Tagiades Hübner, 1819 (Lepidoptera: Hesperiidae: Tagiadini)." Zootaxa 4731, no. 4 (2020): 595–600. http://dx.doi.org/10.11646/zootaxa.4731.4.13.

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Previous studies have shown that the genus Tagiades Hübner, 1819 is paraphyletic with regard to Daimio Murray, 1875 and/or Darpa Moore, 1866. In this study, we attempt to disentangle the relationships among these three genera based on an integrative approach including molecular data, morphological characters, and biological data from available sources. All evidence shows that Daimio and Tagiades are congeneric, isolated from Darpa. According to the rule of priority, Daimio (syn. n.) is a junior synonym of Tagiades. Therefore, we subsume tethys under Tagiades as Tagiades tethys (Ménétriés, 1875

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Budd, Ann F., and Anthony G. Coates. "Nonprogressive evolution in a clade of Cretaceous Montastraea-like corals." Paleobiology 18, no. 4 (1992): 425–46. http://dx.doi.org/10.1017/s0094837300010988.

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A phylogeny of Cretaceous Montastraea-like corals was constructed and used to evaluate the importance of differential speciation, selective extinction, and developmental constraints in the evolutionary history of the clade. Colonies assembled from localities across the central and western Tethyan region were subdivided into four stratigraphic levels: (1) Neocomian to lower Albian, (2) upper Albian to Cenomanian, (3) Turonian to Campanian, and (4) Maastrichtian. Ten corallite characters were measured on transverse thin sections of each colony, and analyzed following a three-step procedure: (1)

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Albino, Adriana, Jorge D. Carrillo-Briceño, and James M. Neenan. "An enigmatic aquatic snake from the Cenomanian of Northern South America." PeerJ 4 (May 24, 2016): e2027. http://dx.doi.org/10.7717/peerj.2027.

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We report the first record of a snake from the Cretaceous of northern South America. The remains come from the La Luna Formation (La Aguada Member, Cenomanian of Venezuela) and consist of several vertebrae, which belong to the precloacal region of the vertebral column. Comparisons to extant and extinct snakes show that the remains represent a new taxon,Lunaophis aquaticusgen. et sp nov. An aquatic mode of life is supported by the ventral position of the ribs, indicating a laterally compressed body. The systematic relationships of this new taxon are difficult to determine due to the scarcity of

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Górniak, Katarzyna. "Origin of marls from the Polish Outer Carpathians: lithological and sedimentological aspects." Mineralogia Polonica 42, no. 4 (2012): 165–297. http://dx.doi.org/10.2478/v10002-011-0012-9.

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AbstractOutcrops of marls, occurring within the sandstone-shaly flysch deposits of the Polish part of Outer Carpathians, considered to be locus typicus of these rocks, were described, measured and sampled. Lithologic features of marls, representing 15 complexes of different age and occurring in 15 complexes of various tectonic units, are presented (Fig. 1, 2). The present studies were concerning Jurassic marls from the Silesian Unit (Goleszów Marls), Upper Cretaceous marls from the Skole and Sub-Silesian Units (Siliceous-Fucoid and Węgierka Marls and Węglowka, Frydek, Jasienica and Zegocina Ma

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Budd, Ann F., Francesca R. Bosellini, and Nathan D. Smith. "Diversification of Cenozoic Reef Corals and Its Relationship to Closure of the Tethys." Paleontological Society Special Publications 13 (2014): 22. http://dx.doi.org/10.1017/s247526220001042x.

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Crasquin-Soleau, Sylvie, Denis Vaslet, and Yves-Michel Le Nindre. "Ostracods of the Permian-Triassic Khuff Formation, Saudi Arabia: palaeoecology and palaeobiogeography." GeoArabia 11, no. 1 (2006): 55–76. http://dx.doi.org/10.2113/geoarabia110155.

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ABSTRACT Ostracods were recovered for the first time from outcrops of the Permian-Triassic Khuff Formation in central Saudi Arabia. The fauna is exceptional in that the Khuff lithofacies were not considered favourable for their development and preservation. This ostracod fauna positions the Triassic-Permian Boundary between the Lower and Upper Khartam members of the Khuff Formation. The palaeoecological analysis shows that the Saudi Arabian Permian ostracods are typical of a shallow, intertropical, warm-water setting. The evolution of the ostracods is directly linked with variations of sea lev

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WEN, W., S. X. HU, Q. Y. ZHANG, et al. "A new species of Platysiagum from the Luoping Biota (Anisian, Middle Triassic, Yunnan, South China) reveals the relationship between Platysiagidae and Neopterygii." Geological Magazine 156, no. 4 (2018): 669–82. http://dx.doi.org/10.1017/s0016756818000079.

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AbstractFour complete platysiagid fish specimens are described from the Luoping Biota, Anisian (Middle Triassic), Yunnan Province, southwest China. They are small fishes with bones and scales covered with ganoine. All characters observed, such as nasals meeting in the midline, a keystone-like dermosphenotic, absence of post-rostral bone, two infraorbitals between dermosphenotic and jugal, large antorbital, and two postcleithra, suggest that the new materials belong to a single, new Platysiagum species, P. sinensis sp. nov. Three genera are ascribed to Platysiagidae: Platysiagum, Helmolepis and

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ZHANG, CONG, THOMAS BADER, LINGMIN ZHANG, TINGTING SHEN, PENG LI, and XUPING LI. "Metamorphic evolution and age constraints of the garnet-bearing mica schist from the Xindaduo area of the Sumdo (U)HP metamorphic belt, Tibet." Geological Magazine 156, no. 07 (2018): 1175–89. http://dx.doi.org/10.1017/s001675681800033x.

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AbstractAs one of the major components of the Himalayan–Tibetan Orogeny, the Lhasa terrane plays a key role in understanding the origin and evolution of this giant orogenic belt and the opening and closure of the Tethys oceans. The eclogite-bearing Sumdo Complex in the central Lhasa terrane was recognized as the main suture of the Palaeo-Tethys Ocean between the north and south Lhasa sub-terranes. Despite the eclogite having been studied for a long time, no attempts have been applied to studying the country rocks, causing confusion in understanding the relationship between the eclogite and the

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Parenti, LR. "Ocean basins and the biogeography of freshwater fishes." Australian Systematic Botany 4, no. 1 (1991): 137. http://dx.doi.org/10.1071/sb9910137.

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Geological evolution of the Indian and Pacific Ocean basins, including the Tethys Sea, is relevant to the evolution and distribution of Indo-Pacific freshwater fishes. Area cladograms derived from phylogenetic analyses of atherinomorph fishes are compared, in part, with those for plant bugs, cicadas and bats. Geologically and biologically composite islands in the Indo-Australian archipelago such as New Guinea, Borneo and Sulawesi, are confirmed. If any lines (such as Wallace's, Weber's and so on) are to be drawn, they should pass through these complex islands, not between them, to mark the clo

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Nützel, Alexander, Maryam Mannani, Baba Senowbari-Daryan, and Mehdi Yazdi. "Gastropods from the Late Triassic Nayband Formation (Iran), their relationships to other Tethyan faunas and remarks on the Triassic gastropod body size problem." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 256, no. 2 (2010): 213–28. http://dx.doi.org/10.1127/0077-7749/2010/0049.

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Hughes, Nigel C., Peng Shanchi, and Luo Huilin. "Kunmingaspis(Trilobita) putatively from the Yunling collage, and the Cambrian history of the eastern Himalayan syntaxial region." Journal of Paleontology 76, no. 4 (2002): 709–17. http://dx.doi.org/10.1017/s0022336000041962.

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Faunal data provide critical constraints upon tectonic models, particularly in such areas of extreme structural complexity as the region adjacent to the eastern syntaxis of the Himalaya. Trilobites reported to have been collected from the Yunling collage at Yinchangou, northwestern Yunnan, are here assigned toKunmingaspis yunnanensisChang, 1964, and the concept of the genusKunmingaspisis reconsidered. Although there is debate about to the paleogeographic affinities of the Yunling collage, the apparent presence of this species supports previous arguments for faunal links between the Yangtze pla

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Liu, Hongmei, and Harald Schneider. "Evidence supporting Davallia canariensis as a Late Miocene relict endemic to Macaronesia and Atlantic Europe." Australian Systematic Botany 26, no. 5 (2013): 378. http://dx.doi.org/10.1071/sb13029.

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The present study investigated the hypothesis that several fern species occurring in Macaronesia and Atlantic Europe are relicts of the Miocene Paratethyan–Tethyan flora that survived in Macaronesia refugia. The hypothesis was tested by reconstructing the phylogenetic relationships of the derived fern Davallia canariensis, which is the only species of a mainly South-east Asian family, Davalliaceae, occurring naturally in Europe, Macaronesia and northern Africa. The dataset comprised a comprehensive taxonomic sampling of the family, with representatives of the five major lineages and ~50–60% of

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