Pub Date : 2023-12-15DOI: 10.1080/02724634.2023.2282650
Emily G. Cross, Clarence Surette, Carney Matheson
Ironstone surrounds many fossils and has a hardness that provides a significant challenge to fossil conservators globally. There are various forms of ironstone, with the carbonate forms of siderite...
{"title":"Geochemical extraction of ceratopsian remains from ironstone","authors":"Emily G. Cross, Clarence Surette, Carney Matheson","doi":"10.1080/02724634.2023.2282650","DOIUrl":"https://doi.org/10.1080/02724634.2023.2282650","url":null,"abstract":"Ironstone surrounds many fossils and has a hardness that provides a significant challenge to fossil conservators globally. There are various forms of ironstone, with the carbonate forms of siderite...","PeriodicalId":17597,"journal":{"name":"Journal of Vertebrate Paleontology","volume":null,"pages":null},"PeriodicalIF":1.4,"publicationDate":"2023-12-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138685709","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-12-12DOI: 10.1080/02724634.2023.2281490
Carlos De Gracia, Björn Berning, Jürgen Kriwet
We report the oldest fossil record of Istiophoridae from the Northern Alpine Foreland Basin (Western Paratethys) in Pucking, Austria (Lower Miocene, lower Aquitanian, ∼22.4 Ma). The studied specime...
{"title":"The origin of modern marlins (Teleostei: Istiophoridae): new fossil evidence from the Lower Miocene of Austria","authors":"Carlos De Gracia, Björn Berning, Jürgen Kriwet","doi":"10.1080/02724634.2023.2281490","DOIUrl":"https://doi.org/10.1080/02724634.2023.2281490","url":null,"abstract":"We report the oldest fossil record of Istiophoridae from the Northern Alpine Foreland Basin (Western Paratethys) in Pucking, Austria (Lower Miocene, lower Aquitanian, ∼22.4 Ma). The studied specime...","PeriodicalId":17597,"journal":{"name":"Journal of Vertebrate Paleontology","volume":null,"pages":null},"PeriodicalIF":1.4,"publicationDate":"2023-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138685714","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-12-04DOI: 10.1080/02724634.2023.2281478
Alexey V. Lopatin, Alexander O. Averianov
Bayshinoryctes shuvalovi gen. et sp. nov. is based on a fragmentary skull including right maxilla associated with right and left dentaries with partially preserved dentition from the Upper Cretaceo...
Bayshinoryctes shuvalovi gen. et sp. 11 .是基于一个碎片头骨,包括与左右牙齿相关的右上颌骨,部分保存的牙齿来自上白垩纪…
{"title":"A New Eutherian Mammal from the Upper Cretaceous Bayinshire Formation of Mongolia","authors":"Alexey V. Lopatin, Alexander O. Averianov","doi":"10.1080/02724634.2023.2281478","DOIUrl":"https://doi.org/10.1080/02724634.2023.2281478","url":null,"abstract":"Bayshinoryctes shuvalovi gen. et sp. nov. is based on a fragmentary skull including right maxilla associated with right and left dentaries with partially preserved dentition from the Upper Cretaceo...","PeriodicalId":17597,"journal":{"name":"Journal of Vertebrate Paleontology","volume":null,"pages":null},"PeriodicalIF":1.4,"publicationDate":"2023-12-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138528990","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-11-24DOI: 10.1080/02724634.2023.2279530
Yu Qiao, Ryosuke Motani, Masaya Iijima, Jun Liu
Hupehsuchia, an enigmatic group of marine reptiles from the Lower Triassic of South China, is characterized by a suite of features including polydactyly in either or both fore and hind limbs. Parti...
{"title":"A new hupehsuchian (Reptilia: Ichthyosauromorpha) from the Lower Triassic of South China with implications for the evolution of polydactyly","authors":"Yu Qiao, Ryosuke Motani, Masaya Iijima, Jun Liu","doi":"10.1080/02724634.2023.2279530","DOIUrl":"https://doi.org/10.1080/02724634.2023.2279530","url":null,"abstract":"Hupehsuchia, an enigmatic group of marine reptiles from the Lower Triassic of South China, is characterized by a suite of features including polydactyly in either or both fore and hind limbs. Parti...","PeriodicalId":17597,"journal":{"name":"Journal of Vertebrate Paleontology","volume":null,"pages":null},"PeriodicalIF":1.4,"publicationDate":"2023-11-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138528977","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-11-03DOI: 10.1080/02724634.2023.2255236
Bill D. Mueller, Adam K. Huttenlocker, Bryan J. Small, James L. Pinto, Kendra Dean-Wallace, Sankar Chatterjee
ABSTRACTA new kannemeyeriiform dicynodont is described from the Upper Triassic Tecovas Formation (Dockum Group) of west Texas, U.S.A. The taxon, Argodicynodon boreni gen. et sp. nov., is diagnosed by numerous cranial characters including: squamosal-interparietal sutural contact broad and interdigitating; tall, narrow intertemporal region formed by the parietals with long postorbitals forming the lateral face of the dorsal platform; interparietal forms knobby, bilobed exostoses that wedge between the parietals to form a W-shaped outline in dorsal view; basioccipital and exoccipital contributions to the occipital condyle are distinct, and the dorsal fossa separating the exoccipitals is deeply incised and dorsoventrally deep; caniniform process of the maxilla is dorsoventrally deep and well developed; and an elongated tab-like medial process of the articular exceeds the width of the quadrate roller. A phylogenetic analysis based on 23 continuous and 176 discrete (numeric) morphological characters and 120 taxa finds Argodicynodon conservatively to be a placeriine near the Placerias + Moghreberia group, representing the oldest placeriine in the southwestern U.S.A. and the first named dicynodont genus from the Dockum Group of Texas. A review of Euramerican dicynodont records exposes their hidden diversity and abundance in Laurasia during the Late Triassic. The records of Argodicynodon and other previously undescribed dicynodont fossils from nearby localities underscores the diversity of non-Placerias dicynodonts in the North American Upper Triassic.http://zoobank.org/urn:lsid:zoobank.org:pub:AB9B7ABC-6C84-4B04-909F-F1DA114030AB ACKNOWLEDGMENTSThis study is based in part on the dissertation of BDM under the guidance of his committee members SC, J. Barrick, and T. Lehman. We thank J. Boren and the Boren family for granting access to the site and the generous donation of the fossil material to the Museum of Texas Tech University. We thank the numerous Texas Tech students and volunteers who assisted in the field and lab. B. Meyers is acknowledged for discovery of the locality MOTT VPL 3881 and the left humerus (TTU-P10421). We also thank P. Holroyd and the UCMP for access to comparative material from the Placerias quarry. Special thanks to D. Cunningham, G. Gürtler, A. Hungerbühler, J. Martz, S. Nesbitt, and W. Parker for assistance in various aspects of this project. We also thank K. Angielczyk, C. Kammerer, and T. Sulej for their helpful feedback on our manuscript. This project was made possible through the support of the Museum of Texas Tech University.DISCLOSURE STATEMENTNo potential conflict of interest was reported by the author(s).AUTHOR CONTRIBUTIONSBDM designed the project and wrote sections for the initial draft as part of his unpublished doctoral dissertation. AKH and BJS collected data, revised and edited the manuscript, drafted and revised the figures, and performed the phylogenetic analyses. AKH and JLP collected additional comparative data a
{"title":"A new kannemeyeriiform dicynodont (Synapsida) from a Late Triassic vertebrate assemblage in west Texas, U.S.A.Citation for this article: Mueller, B. D., Huttenlocker, A. K., Small, B. J., Pinto, J. L., Dean-Wallace, K., & Chatterjee, S. (2023) A new kannemeyeriiform dicynodont (Synapsida) from a Late Triassic vertebrate assemblage in west Texas, U.S.A. <i>Journal of Vertebrate Paleontology</i> . https://doi.org/10.1080/02724634.2023.2255236","authors":"Bill D. Mueller, Adam K. Huttenlocker, Bryan J. Small, James L. Pinto, Kendra Dean-Wallace, Sankar Chatterjee","doi":"10.1080/02724634.2023.2255236","DOIUrl":"https://doi.org/10.1080/02724634.2023.2255236","url":null,"abstract":"ABSTRACTA new kannemeyeriiform dicynodont is described from the Upper Triassic Tecovas Formation (Dockum Group) of west Texas, U.S.A. The taxon, Argodicynodon boreni gen. et sp. nov., is diagnosed by numerous cranial characters including: squamosal-interparietal sutural contact broad and interdigitating; tall, narrow intertemporal region formed by the parietals with long postorbitals forming the lateral face of the dorsal platform; interparietal forms knobby, bilobed exostoses that wedge between the parietals to form a W-shaped outline in dorsal view; basioccipital and exoccipital contributions to the occipital condyle are distinct, and the dorsal fossa separating the exoccipitals is deeply incised and dorsoventrally deep; caniniform process of the maxilla is dorsoventrally deep and well developed; and an elongated tab-like medial process of the articular exceeds the width of the quadrate roller. A phylogenetic analysis based on 23 continuous and 176 discrete (numeric) morphological characters and 120 taxa finds Argodicynodon conservatively to be a placeriine near the Placerias + Moghreberia group, representing the oldest placeriine in the southwestern U.S.A. and the first named dicynodont genus from the Dockum Group of Texas. A review of Euramerican dicynodont records exposes their hidden diversity and abundance in Laurasia during the Late Triassic. The records of Argodicynodon and other previously undescribed dicynodont fossils from nearby localities underscores the diversity of non-Placerias dicynodonts in the North American Upper Triassic.http://zoobank.org/urn:lsid:zoobank.org:pub:AB9B7ABC-6C84-4B04-909F-F1DA114030AB ACKNOWLEDGMENTSThis study is based in part on the dissertation of BDM under the guidance of his committee members SC, J. Barrick, and T. Lehman. We thank J. Boren and the Boren family for granting access to the site and the generous donation of the fossil material to the Museum of Texas Tech University. We thank the numerous Texas Tech students and volunteers who assisted in the field and lab. B. Meyers is acknowledged for discovery of the locality MOTT VPL 3881 and the left humerus (TTU-P10421). We also thank P. Holroyd and the UCMP for access to comparative material from the Placerias quarry. Special thanks to D. Cunningham, G. Gürtler, A. Hungerbühler, J. Martz, S. Nesbitt, and W. Parker for assistance in various aspects of this project. We also thank K. Angielczyk, C. Kammerer, and T. Sulej for their helpful feedback on our manuscript. This project was made possible through the support of the Museum of Texas Tech University.DISCLOSURE STATEMENTNo potential conflict of interest was reported by the author(s).AUTHOR CONTRIBUTIONSBDM designed the project and wrote sections for the initial draft as part of his unpublished doctoral dissertation. AKH and BJS collected data, revised and edited the manuscript, drafted and revised the figures, and performed the phylogenetic analyses. AKH and JLP collected additional comparative data a","PeriodicalId":17597,"journal":{"name":"Journal of Vertebrate Paleontology","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2023-11-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135868820","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-11-02DOI: 10.1080/02724634.2023.2254360
Panagiotis Kampouridis, Georgia Svorligkou, Nikolaos Kargopoulos, Nikolai Spassov, Madelaine Böhme
Extant rhinoceroses are represented only by five species and are characterized by the presence of a nasal horn. In the past, they were much more diverse, with one of the best-known groups being the aceratheriines, i.e., hornless rhinoceroses. Chilotheres are a group of hornless rhinos that inhabited Eurasia during the Late Miocene. Their westernmost geographic range reached Eastern Europe, where overall eight species have been erected. Four of these were described based on material from the Upper Miocene of Samos Island (Greece), two of which are not considered valid anymore. Unfortunately, the type skulls of all four species are lost and there are several issues concerning their taxonomy. Therefore, we herein designate two skulls housed in historical collections from Samos as neotypes for the first two species, Chilotherium schlosseri (Weber, 1905) and Eochilotherium samium (Weber, 1905), and provide detailed comparisons for the separation of the species from each other and from any other chilotheres. Our results prove that the two species are valid and justify their separation on a generic level. Chilotherium schlosseri seems to be more closely affiliated with the other European Chilotherium species, whereas E. samium is more similar to the Chinese ‘Chilotherium’ wimani and ‘Chilotherium’ primigenium, based on their more plesiomorphic characters.
{"title":"Revision of the Late Miocene hornless rhinocerotids from Samos Island (Greece) with the designation of neotypes and implications for the European chilotheresCitation for this article: Kampouridis, P., Svorligkou, G., Kargopoulos, N., Spassov, N., & Böhme, M. (2023) Revision of the Late Miocene hornless rhinocerotids from Samos Island (Greece) with the designation of neotypes and implications for the European chilotheres. <i>Journal of Vertebrate Paleontology</i> . https://doi.org/10.1080/…","authors":"Panagiotis Kampouridis, Georgia Svorligkou, Nikolaos Kargopoulos, Nikolai Spassov, Madelaine Böhme","doi":"10.1080/02724634.2023.2254360","DOIUrl":"https://doi.org/10.1080/02724634.2023.2254360","url":null,"abstract":"Extant rhinoceroses are represented only by five species and are characterized by the presence of a nasal horn. In the past, they were much more diverse, with one of the best-known groups being the aceratheriines, i.e., hornless rhinoceroses. Chilotheres are a group of hornless rhinos that inhabited Eurasia during the Late Miocene. Their westernmost geographic range reached Eastern Europe, where overall eight species have been erected. Four of these were described based on material from the Upper Miocene of Samos Island (Greece), two of which are not considered valid anymore. Unfortunately, the type skulls of all four species are lost and there are several issues concerning their taxonomy. Therefore, we herein designate two skulls housed in historical collections from Samos as neotypes for the first two species, Chilotherium schlosseri (Weber, 1905) and Eochilotherium samium (Weber, 1905), and provide detailed comparisons for the separation of the species from each other and from any other chilotheres. Our results prove that the two species are valid and justify their separation on a generic level. Chilotherium schlosseri seems to be more closely affiliated with the other European Chilotherium species, whereas E. samium is more similar to the Chinese ‘Chilotherium’ wimani and ‘Chilotherium’ primigenium, based on their more plesiomorphic characters.","PeriodicalId":17597,"journal":{"name":"Journal of Vertebrate Paleontology","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2023-11-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135935126","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-11-02DOI: 10.1080/02724634.2023.2261505
Mikhail V. Nazarkin
ABSTRACT†Serrivomer glehni, a new species of the Neogene saw-toothed eel (Anguilliformes, Serrivomeridae) is described based on the 55 specimens from the Middle–Upper Miocene Kurasi Formation of Sakhalin Island, Russia. This is the third record of fossil saw-toothed eels since the recovery of partial skeletons from the Miocene of Japan and Italy. The new species demonstrates close similarity to the extant Serrivomer species in overall body form and shape of separate bones and their complexes. The new species is characterized by the “longidentatus” type of vomerine dentition and by a single branchiostegal ray protruding beyond the hyoid bar, which suggests a close affinity to the modern S. sector. It can be reliably distinguished from all other species of Serrivomer by its lower number of vertebrae (134 vs. 140–172) and its larger cleithrum, which is positioned under the seventh instead of the eighth vertebral centrum.http://zoobank.org/urn:lsid:zoobank.org:pub:50673E06-602C-4CA1-8CFF-AD992BCAEBED ACKNOWLEDGMENTSI am grateful to A. I. Pinchuk (University of Alaska) for his great help with the English. Special thanks go to A. M. Prokofiev (A.N. Severtsov's Institute of Ecology and Evolution, Russian Academy of Sciences, Moscow, Russia) for donation of comparative materials. I thank the editors, along with anonymous reviewers for their valuable comments and corrections to the manuscript. The reported study was funded by the Russian Government Research Theme No. 122031100285-3.AUTHOR CONTRIBUTIONSThe author confirms sole responsibility for the study concept, data collection, analysis and interpretation of results, and preparation of the manuscript.DISCLOSURE STATEMENTNo potential conflict of interest was declared by the author.
摘要/ ABSTRACT摘要:本文根据俄罗斯库页岛中新世中上统Kurasi组55份标本,描述了新近系锯齿鳗(鳗形目,锯齿鳗科)的一新种Serrivomer glehni。这是自日本和意大利中新世发现部分锯齿鳗鱼骨骼以来,第三次发现锯齿鳗鱼化石。新种与现存的serriomer物种在整体形态和独立骨骼及其复合体的形状上表现出非常接近的相似性。这个新物种的特征是长齿状牙列和一条突出在舌骨棒之外的鳃骨射线,这表明它与现代的s系有密切的关系。由于它的椎骨数量较少(134对140-172),其更大的椎骨位于第七椎体而不是第八椎体之下,因此可以可靠地将其与所有其他种类的Serrivomer区分出来。http://zoobank.org/urn:lsid:zoobank.org:pub:50673E06-602C-4CA1-8CFF-AD992BCAEBED感谢A. I. Pinchuk(阿拉斯加大学)在英语方面的巨大帮助。特别感谢A. M. Prokofiev (A. n . Severtsov的生态与进化研究所,俄罗斯科学院,莫斯科)捐赠的比较材料。我感谢编辑,以及匿名审稿人对手稿的宝贵意见和更正。报告的研究由俄罗斯政府研究主题No. 122031100285-3资助。作者确认对研究概念、数据收集、结果分析和解释以及稿件的准备负全部责任。声明作者未声明存在潜在的利益冲突。
{"title":"A saw-toothed eel † <i>Serrivomer glehni</i> sp. nov. from the Miocene of Sakhalin Island, north-western PacificCitation for this article: Nazarkin, M. V. (2023) A saw-toothed eel † <i>Serrivomer glehni</i> sp. nov. from the Miocene of Sakhalin Island, north-western Pacific. <i>Journal of Vertebrate Paleontology</i> . https://doi.org/10.1080/02724634.2023.2261505","authors":"Mikhail V. Nazarkin","doi":"10.1080/02724634.2023.2261505","DOIUrl":"https://doi.org/10.1080/02724634.2023.2261505","url":null,"abstract":"ABSTRACT†Serrivomer glehni, a new species of the Neogene saw-toothed eel (Anguilliformes, Serrivomeridae) is described based on the 55 specimens from the Middle–Upper Miocene Kurasi Formation of Sakhalin Island, Russia. This is the third record of fossil saw-toothed eels since the recovery of partial skeletons from the Miocene of Japan and Italy. The new species demonstrates close similarity to the extant Serrivomer species in overall body form and shape of separate bones and their complexes. The new species is characterized by the “longidentatus” type of vomerine dentition and by a single branchiostegal ray protruding beyond the hyoid bar, which suggests a close affinity to the modern S. sector. It can be reliably distinguished from all other species of Serrivomer by its lower number of vertebrae (134 vs. 140–172) and its larger cleithrum, which is positioned under the seventh instead of the eighth vertebral centrum.http://zoobank.org/urn:lsid:zoobank.org:pub:50673E06-602C-4CA1-8CFF-AD992BCAEBED ACKNOWLEDGMENTSI am grateful to A. I. Pinchuk (University of Alaska) for his great help with the English. Special thanks go to A. M. Prokofiev (A.N. Severtsov's Institute of Ecology and Evolution, Russian Academy of Sciences, Moscow, Russia) for donation of comparative materials. I thank the editors, along with anonymous reviewers for their valuable comments and corrections to the manuscript. The reported study was funded by the Russian Government Research Theme No. 122031100285-3.AUTHOR CONTRIBUTIONSThe author confirms sole responsibility for the study concept, data collection, analysis and interpretation of results, and preparation of the manuscript.DISCLOSURE STATEMENTNo potential conflict of interest was declared by the author.","PeriodicalId":17597,"journal":{"name":"Journal of Vertebrate Paleontology","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2023-11-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135934066","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-11-01DOI: 10.1080/02724634.2023.2264341
Robert M. Sullivan, Steven E. Jasinski, Thomas E. Williamson
ABSTRACTA new, exceptionally well-preserved articulated skull roof and braincase of Melvius chauliodous, from the Kirtland Formation of New Mexico, reveals new features that provide detailed osteological information for Melvius, thus allowing for a reassessment of characters that defines the genus, its two recognized species M. chauliodous and M. thomasi, and its phylogenetic relationships within Vidalamiinae. The new features include the presence of dermopterotic rays (‘ribs’) and parietal ray bundles, previously unknown for both species of Melvius. The presence of elongated dermopterotic rays, a feature previously considered to be distinctive for the genus Calamopleurus, and tribe Calamopleurini, is now documented in Melvius, but these rays differ in their point of origination at the posteromedial corners of both dermopterotics. Bundles of short fan-shaped rays emanating from below the posterolateral corners of the parietals are also documented in both species of Melvius. Melvius was previously placed in the tribe Vidalamiini (Subfamily Vidalamiinae), but because it shares some unique features with members of the tribe Calamopleurini and the genus Calamopleurus, its placement within Vidalamiini, and the recognition of these two distinct clades (tribes) within Vidalamiinae, are not supported in our phylogenetic analysis. Previous characters distinguishing Melvius species, particularly differences in postinfraorbital ornamentation between M. chauliodous and M. thomasi, are considered dubious. However, other features may serve to determine interspecific variation or differences. For the present, we retain both species until more definitive material of M. thomasi is described. ACKNOWLEDGMENTSForemost, RMS thanks J. Petersen (discoverer) and T. Knopick who helped collect the specimen, and who have been invaluable field assistants to RMS in collecting fossil vertebrates from the San Juan Basin for over a decade. We are especially grateful to P. Holroyd (UCMP) for providing photos of UCMP 131707 and UCMP 129681 that were crucial in identifying this latter element. Thanks are also extended to M. Sims (KU Biodiversity Institute and Natural History Museum) for verifying the locality information of the KUVP specimens mentioned within and for providing us with high resolution photos of KUVP 88378 that helped in interpreting and reconfirming the identity of this element. Special thanks to T. Tokaryk and M. Gilbert for additional information regarding Canadian occurrences of Melvius. RMS thanks D. Fowler (Dickinson Museum Center and Badlands Dinosaur Museum) for discussions regarding phylogenetic analyses and paleogeography as they pertain to this study. N. Volden (NMMNH) aided in securing information regarding the fossil amiid specimens previously housed in the collections of the University of New Mexico and we thank her for her help. L. Rinehart prepared the ventral side of NMMNH P-88899 and RMS prepared the dorsal side of the specimen. RMS thanks P. Reser
{"title":"The first articulated skull roof and braincase of <i>Melvius chauliodous</i> (Amiidae, Vidalamiinae) from the Upper Cretaceous Kirtland Formation, San Juan Basin, New MexicoCitation for this article: Sullivan, R. M., Jasinski, S. E., & Williamson, T. E. (2023) The first articulated skull roof and braincase of <i>Melvius chauliodous</i> (Amiidae, Vidalamiinae) from the Upper Cretaceous Kirtland Formation, San Juan Basin, New Mexico. <i>Journal of Vertebrate Paleontology</i> . https://doi.org…","authors":"Robert M. Sullivan, Steven E. Jasinski, Thomas E. Williamson","doi":"10.1080/02724634.2023.2264341","DOIUrl":"https://doi.org/10.1080/02724634.2023.2264341","url":null,"abstract":"ABSTRACTA new, exceptionally well-preserved articulated skull roof and braincase of Melvius chauliodous, from the Kirtland Formation of New Mexico, reveals new features that provide detailed osteological information for Melvius, thus allowing for a reassessment of characters that defines the genus, its two recognized species M. chauliodous and M. thomasi, and its phylogenetic relationships within Vidalamiinae. The new features include the presence of dermopterotic rays (‘ribs’) and parietal ray bundles, previously unknown for both species of Melvius. The presence of elongated dermopterotic rays, a feature previously considered to be distinctive for the genus Calamopleurus, and tribe Calamopleurini, is now documented in Melvius, but these rays differ in their point of origination at the posteromedial corners of both dermopterotics. Bundles of short fan-shaped rays emanating from below the posterolateral corners of the parietals are also documented in both species of Melvius. Melvius was previously placed in the tribe Vidalamiini (Subfamily Vidalamiinae), but because it shares some unique features with members of the tribe Calamopleurini and the genus Calamopleurus, its placement within Vidalamiini, and the recognition of these two distinct clades (tribes) within Vidalamiinae, are not supported in our phylogenetic analysis. Previous characters distinguishing Melvius species, particularly differences in postinfraorbital ornamentation between M. chauliodous and M. thomasi, are considered dubious. However, other features may serve to determine interspecific variation or differences. For the present, we retain both species until more definitive material of M. thomasi is described. ACKNOWLEDGMENTSForemost, RMS thanks J. Petersen (discoverer) and T. Knopick who helped collect the specimen, and who have been invaluable field assistants to RMS in collecting fossil vertebrates from the San Juan Basin for over a decade. We are especially grateful to P. Holroyd (UCMP) for providing photos of UCMP 131707 and UCMP 129681 that were crucial in identifying this latter element. Thanks are also extended to M. Sims (KU Biodiversity Institute and Natural History Museum) for verifying the locality information of the KUVP specimens mentioned within and for providing us with high resolution photos of KUVP 88378 that helped in interpreting and reconfirming the identity of this element. Special thanks to T. Tokaryk and M. Gilbert for additional information regarding Canadian occurrences of Melvius. RMS thanks D. Fowler (Dickinson Museum Center and Badlands Dinosaur Museum) for discussions regarding phylogenetic analyses and paleogeography as they pertain to this study. N. Volden (NMMNH) aided in securing information regarding the fossil amiid specimens previously housed in the collections of the University of New Mexico and we thank her for her help. L. Rinehart prepared the ventral side of NMMNH P-88899 and RMS prepared the dorsal side of the specimen. RMS thanks P. Reser","PeriodicalId":17597,"journal":{"name":"Journal of Vertebrate Paleontology","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2023-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135271589","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-11-01DOI: 10.1080/02724634.2023.2256812
Christian A. Sidor, Arjan Mann, Kenneth D. Angielczyk
ABSTRACTFossils referable to the gorgonopsian Gorgonops sp. and to the dicynodont Endothiodon sp. are described from the Permian Madumabisa Mudstone Formation of the Mid-Zambezi Basin of southern Zambia. Specimens of the former taxon conform to recent diagnoses of the genus (e.g., five postcanine teeth, transverse flange of the pterygoid backswept, postorbital bar rugose and moderately expanded), but differ slightly from South African material in some respects (e.g., reduced dentition on the transverse flange of the pterygoid). Fossils of the latter are less complete, but show diagnostic features such as a dentary with numerous teeth, a ventral boss, and a shallow posterior dentary sulcus, oval palatine pads, and a narrow intertemporal region of the skull, although a species-level identification is not currently possible. Although the relevant fossils were never described, a vertebrate fossil assemblage including Endothiodon was previously reported from the Madumabisa Mudstone Formation in northern Zimbabwe (i.e., K5d), suggesting that this biozone was relatively broadly distributed across the Mid-Zambezi Basin. The Mid-Zambezi Basin of southern Zambia was previously demonstrated to host Guadalupian Tapinocephalus Assemblage Zone-equivalent strata, with rhinesuchids, burnetiamorphs, tapinocephalids, and dicynodonts recognized. The recognition of Lopingian Endothiodon Assemblage Zone-age rocks expands the stratigraphic range of vertebrate-bearing horizons in southern Zambia. ACKNOWLEDGMENTSOur research in Zambia has been supported by the National Geographic Society (CRE 8571-088 to S. Steyer, CRE 8961-11 to C.A.S.), with additional support from The Grainger Foundation and the Field Museum/IDP, Inc. African Partner’s Program (to K.D.A.) and NSF EAR-1337569 (to C.A.S.) and EAR-1337291 (to K.D.A. and S. Nesbitt). We thank K. Mwamulowe and J. Museba (NHCC) for assistance in arranging and carrying out the fieldwork. In addition, N. Barbolini, C. Beightol, A. Goulding, J. Museba, S. Nesbitt, R. Smith, S. Steyer, N. Tabor, and S. Tolan were part of the field teams in 2012 and 2014 and helped to collect the fossils discussed here. Preparation was skillfully performed by K. Abrams, S. Egberts, A. Shinya, and C. Van Beek. Finally, we thank M. Day, C. Kammerer, and B. Rubidge for their helpful reviews and J. Fröbisch for his editorial assistance.AUTHOR CONTRIBUTIONSCAS designed the project. CAS, KDA, and AM gathered and analyzed the data, and all three wrote and edited the manuscript.DISCLOSURE STATEMENTNo potential conflict of interest was declared by the author(s).
摘要在赞比亚南部赞比西盆地中二叠纪Madumabisa泥岩组中描述了gorgonopsian Gorgonops sp.和dicynodon Endothiodon sp.的化石。前分类群的标本符合该属最近的诊断(例如,五颗后犬齿,翼状体的横向翼缘后掠,后齿条皱襞和适度扩张),但在某些方面与南非材料略有不同(例如,翼状体横向翼缘上的齿列减少)。后者的化石不太完整,但显示出诊断特征,如具有许多牙齿的牙齿,腹侧凸起,浅后牙沟,椭圆形腭垫和颅骨狭窄的颞间区,尽管目前还不可能进行物种水平的鉴定。尽管相关化石从未被描述过,但在津巴布韦北部的Madumabisa泥岩组(即K5d)中曾报道过包括Endothiodon在内的脊椎动物化石组合,这表明该生物带在赞比西盆地中部分布相对广泛。赞比亚南部的中赞比西盆地先前已被证明拥有瓜达卢普系Tapinocephalus组合带等效地层,已识别出rhinesuchids, burnetiamorphs, tapinocephalids和dicynodonts。洛平期内齿兽组合带时代岩石的发现,扩大了赞比亚南部脊椎动物层位的地层范围。致谢我们在赞比亚的研究得到了国家地理学会的支持(CRE 8571-088 to S. Steyer, CRE 8961-11 to C.A.S.),并得到了格兰杰基金会和Field Museum/IDP, Inc.的额外支持。非洲合作伙伴计划(给K.D.A.)和NSF EAR-1337569(给C.A.S.)和EAR-1337291(给K.D.A.和S. Nesbitt)。我们感谢K. Mwamulowe和J. Museba (NHCC)在安排和开展实地工作方面的协助。此外,N. Barbolini、C. Beightol、A. Goulding、J. Museba、S. Nesbitt、R. Smith、S. Steyer、N. Tabor和S. Tolan是2012年和2014年实地考察小组的成员,他们帮助收集了这里讨论的化石。准备工作由K. Abrams, S. Egberts, A. Shinya和C. Van Beek熟练地完成。最后,我们感谢M. Day、C. Kammerer和B. Rubidge的有益评论,以及J. Fröbisch的编辑协助。scas设计了这个项目。CAS, KDA和AM收集和分析数据,三人共同撰写和编辑稿件。披露声明作者未声明存在潜在利益冲突。
{"title":"<i>Gorgonops</i> and <i>Endothiodon</i> (Synapsida: Therapsida) from the Madumabisa Mudstone Formation: evidence of a previously unreported tetrapod biozone in the Mid-Zambezi Basin of southern ZambiaCitation for this article: Sidor, C. A., Mann, A., & Angielczyk, K. D. (2023) <i>Gorgonops</i> and <i>Endothiodon</i> (Synapsida: Therapsida) from the Madumabisa Mudstone Formation: evidence of a previously unreported tetrapod biozone in the Mid-Zambezi Basin of southern Zambia. <i>Journal of …","authors":"Christian A. Sidor, Arjan Mann, Kenneth D. Angielczyk","doi":"10.1080/02724634.2023.2256812","DOIUrl":"https://doi.org/10.1080/02724634.2023.2256812","url":null,"abstract":"ABSTRACTFossils referable to the gorgonopsian Gorgonops sp. and to the dicynodont Endothiodon sp. are described from the Permian Madumabisa Mudstone Formation of the Mid-Zambezi Basin of southern Zambia. Specimens of the former taxon conform to recent diagnoses of the genus (e.g., five postcanine teeth, transverse flange of the pterygoid backswept, postorbital bar rugose and moderately expanded), but differ slightly from South African material in some respects (e.g., reduced dentition on the transverse flange of the pterygoid). Fossils of the latter are less complete, but show diagnostic features such as a dentary with numerous teeth, a ventral boss, and a shallow posterior dentary sulcus, oval palatine pads, and a narrow intertemporal region of the skull, although a species-level identification is not currently possible. Although the relevant fossils were never described, a vertebrate fossil assemblage including Endothiodon was previously reported from the Madumabisa Mudstone Formation in northern Zimbabwe (i.e., K5d), suggesting that this biozone was relatively broadly distributed across the Mid-Zambezi Basin. The Mid-Zambezi Basin of southern Zambia was previously demonstrated to host Guadalupian Tapinocephalus Assemblage Zone-equivalent strata, with rhinesuchids, burnetiamorphs, tapinocephalids, and dicynodonts recognized. The recognition of Lopingian Endothiodon Assemblage Zone-age rocks expands the stratigraphic range of vertebrate-bearing horizons in southern Zambia. ACKNOWLEDGMENTSOur research in Zambia has been supported by the National Geographic Society (CRE 8571-088 to S. Steyer, CRE 8961-11 to C.A.S.), with additional support from The Grainger Foundation and the Field Museum/IDP, Inc. African Partner’s Program (to K.D.A.) and NSF EAR-1337569 (to C.A.S.) and EAR-1337291 (to K.D.A. and S. Nesbitt). We thank K. Mwamulowe and J. Museba (NHCC) for assistance in arranging and carrying out the fieldwork. In addition, N. Barbolini, C. Beightol, A. Goulding, J. Museba, S. Nesbitt, R. Smith, S. Steyer, N. Tabor, and S. Tolan were part of the field teams in 2012 and 2014 and helped to collect the fossils discussed here. Preparation was skillfully performed by K. Abrams, S. Egberts, A. Shinya, and C. Van Beek. Finally, we thank M. Day, C. Kammerer, and B. Rubidge for their helpful reviews and J. Fröbisch for his editorial assistance.AUTHOR CONTRIBUTIONSCAS designed the project. CAS, KDA, and AM gathered and analyzed the data, and all three wrote and edited the manuscript.DISCLOSURE STATEMENTNo potential conflict of interest was declared by the author(s).","PeriodicalId":17597,"journal":{"name":"Journal of Vertebrate Paleontology","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2023-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135221437","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2023-10-27DOI: 10.1080/02724634.2023.2265445
Łukasz Czepiński, Wojciech Pawlak, Adam Rytel, Mateusz Tałanda, Tomasz Szczygielski, Tomasz Sulej
ABSTRACTThe Middle Triassic remains a poorly understood time in the evolution of land vertebrates. Here, we report a new Ladinian-age vertebrate assemblage from Miedary (southern Poland). It consists of more than 20 taxa including fish (four species of Hybodontiformes, cf. Gyrolepis, Redfieldiiformes, ‘Thelodus’, Saurichthys, Serrolepis, Prohalecites, Ptychoceratodus), amphibians (Mastodonsaurus, Gerrothorax, Plagiosternum, chroniosuchian Bystrowiella), and reptiles (Owenettidae, Blezingeria, Nothosaurus, Tanystropheus, an additional, yet unidentified tanystropheid, the doswelliid Jaxtasuchus, and another archosauromorph, as well as eight archosauriform tooth morphotypes). Preliminary comparisons suggest biogeographic and environmental similarities with roughly contemporaneous localities known from the southwestern part of the Germanic Basin. Among differences in these two areas are the presence of a new armored archosauromorph and a surprising abundance of Tanystropheus remains in the new Polish site. Miedary is currently the richest source of three-dimensionally preserved Tanystropheus material in the world, which will be crucial for a better understanding of the preferred environment and lifestyle of this highly specialized reptile. ACKNOWLEDGMENTSWe thank M. Stachacz and G. Niedźwiedzki who were the first to examine the Miedary outcrop. We are grateful to E. Maxwell, E. Mujal, R. Schoch, and S. Spiekman (SMNS), C. Klug, T. Scheyer, and B. Scheffold (PIMUZ), H. Hagdorn (MHI), and I. Werneburg and A. Krahl (GPIT) for their hospitality and help during the visits and examination of their collections. We are grateful to editor H.-D. Sues, H. Hagdorn, two anonymous reviewers, and K. De Beats, and J. Dzik for discussion of the manuscript and for their helpful suggestions. We thank R. Motani, A. Wolniewicz, and A. Tintori for their help in identification of the vertebral centra assigned to Blezingeria. We thank K. Przestrzelska and P. Bajdek for their help in specimen preparation, and M. Dziewiński and J. Jabłoński for help in fossil transportation and photography. We express our gratitude to the authorities of the Zbrosławice municipality, as well as the mayors (W. Nawrocki, H. Kupka) and the community of the Miedary village for their long-standing hospitality. We thank K. Pielka, owner of the Miedary claypit area for support during the excavations, and S. Szczygiel for help with obtaining archival pictures of the Miedary claypit. We thank all students and volunteers taking part in the fieldwork in the Miedary site since 2015, particularly those who directly contributed to the discovery of the specimens described in the herein study: J. Armatys, M. Baranowska, M. Bieniaszewski, J. Chrostowski, M. Gierek, M. Granica, K. Grygorczyk, D. Hałubek, S. Kaczmarczyk, S. Kawecki, A. Kawińska, L. Kłosińska, A. Kowalewska, T. Kozyk, B. Kulus, A. Lewczuk, A. Lis, S. López-Torres, A. Minich, K. Nawrot, R. Nowakowski, R. Pelczar, K. Peszek, J. Rabińska, P. Rozwala
在陆生脊椎动物的进化过程中,中三叠世仍然是一个鲜为人知的时期。在这里,我们报告了一个来自波兰南部mimiary的新的拉丁时代脊椎动物组合。它由20多个分类群组成,包括鱼类(四种Hybodontiformes,如Gyrolepis, Redfieldiiformes, ' Thelodus ', Saurichthys, Serrolepis, Prohalecites, Ptychoceratodus),两栖动物(乳齿龙,Gerrothorax, Plagiosternum, chroniosuchia Bystrowiella)和爬行动物(Owenettidae, Blezingeria, Nothosaurus, Tanystropheus,另一种尚未确定的Tanystropheus, doswelliid Jaxtasuchus,另一种始祖龙,以及八种始祖龙牙齿形态)。初步比较表明,生物地理和环境与日耳曼盆地西南部已知的大致同时期的地方相似。这两个地区的不同之处在于,在波兰的新遗址中发现了一种新的带盔甲的始祖龙,以及数量惊人的剑龙化石。Miedary是目前世界上保存最丰富的三维剑齿虎材料的来源,这对于更好地了解这种高度专业化的爬行动物的首选环境和生活方式至关重要。我们感谢M. Stachacz和G. Niedźwiedzki,他们是第一个检查军事露头的人。我们感谢E. Maxwell、E. Mujal、R. Schoch和S. Spiekman (SMNS)、C. Klug、T. Scheyer和B. Scheffold (PIMUZ)、H. Hagdorn (MHI)和I. Werneburg和A. Krahl (GPIT)在参观和检查藏品期间的热情好客和帮助。我们感谢h . d .编辑。sue, H. Hagdorn,两位匿名审稿人,以及K. De Beats和J. Dzik对手稿的讨论和他们有益的建议。我们感谢R. Motani, A. Wolniewicz和A. Tintori在鉴定Blezingeria椎体中心方面所提供的帮助。我们感谢K. Przestrzelska和P. Bajdek在标本制备方面的帮助,以及M. Dziewiński和J. Jabłoński在化石运输和摄影方面的帮助。我们对Zbrosławice市政当局以及市长(纳瓦罗基、库普卡)和米达里村社区长期以来的盛情款待表示感谢。我们感谢Miedary粘土坑的所有者K. Pielka在挖掘过程中的支持,以及S. Szczygiel帮助获得Miedary粘土坑的档案图片。我们感谢所有自2015年以来在军事基地参与实地工作的学生和志愿者,特别是那些直接为发现本文研究中描述的标本做出贡献的人:j . Armatys m . Baranowska m . Bieniaszewski j . Chrostowski m . Gierek m . Granica K . Grygorczyk d Hałubek, S . Kaczmarczyk S Kawecki a Kawiń平方公里列阵,l·Kłosiń平方公里列阵,a . Kowalewska t . Kozyk库鲁,a . Lewczuk Lis), S . Lopez-Torres a . Minich K Nawrot, r . Nowakowski r . Pelczar K . Peszek j·拉比ń平方公里列阵,p . Rozwalak m . Ruminowicz m . Samborska i skowron4月份K . Sładkiewicz, b . Surmacz d Szelągowski, p . Ulwań滑雪,a . Witkowski a . Wojcicka和美国Ziarko。挖掘和研究得到了波兰国家科学中心的支持(资助2017/27/B/NZ8/01543, 2020/39/O/NZ8/02301授予T. su, 2019/35/N/NZ8/03806授予Ł)。c)。作者CONTRIBUTIONSŁC, AR, WP, MT和TSu领导了在军事遗址的发掘工作,从而收集了所描述的材料。WP和AR编写了地质剖面的描述。ŁC和AR分析了数值数据。ŁC和WP编制了数据。所有作者共同撰写和编辑了手稿。披露声明作者未声明存在潜在利益冲突。
{"title":"A new Middle Triassic vertebrate assemblage from Miedary (southern Poland)Citation for this article: Czepiński, Ł, Pawlak, W., Rytel, A., Tałanda, M., Szczygielski, T., & Sulej, T. (2023) A new Middle Triassic vertebrate assemblage from Miedary (southern Poland). <i>Journal of Vertebrate Paleontology</i> . https://doi.org/10.1080/02724634.2023.2265445","authors":"Łukasz Czepiński, Wojciech Pawlak, Adam Rytel, Mateusz Tałanda, Tomasz Szczygielski, Tomasz Sulej","doi":"10.1080/02724634.2023.2265445","DOIUrl":"https://doi.org/10.1080/02724634.2023.2265445","url":null,"abstract":"ABSTRACTThe Middle Triassic remains a poorly understood time in the evolution of land vertebrates. Here, we report a new Ladinian-age vertebrate assemblage from Miedary (southern Poland). It consists of more than 20 taxa including fish (four species of Hybodontiformes, cf. Gyrolepis, Redfieldiiformes, ‘Thelodus’, Saurichthys, Serrolepis, Prohalecites, Ptychoceratodus), amphibians (Mastodonsaurus, Gerrothorax, Plagiosternum, chroniosuchian Bystrowiella), and reptiles (Owenettidae, Blezingeria, Nothosaurus, Tanystropheus, an additional, yet unidentified tanystropheid, the doswelliid Jaxtasuchus, and another archosauromorph, as well as eight archosauriform tooth morphotypes). Preliminary comparisons suggest biogeographic and environmental similarities with roughly contemporaneous localities known from the southwestern part of the Germanic Basin. Among differences in these two areas are the presence of a new armored archosauromorph and a surprising abundance of Tanystropheus remains in the new Polish site. Miedary is currently the richest source of three-dimensionally preserved Tanystropheus material in the world, which will be crucial for a better understanding of the preferred environment and lifestyle of this highly specialized reptile. ACKNOWLEDGMENTSWe thank M. Stachacz and G. Niedźwiedzki who were the first to examine the Miedary outcrop. We are grateful to E. Maxwell, E. Mujal, R. Schoch, and S. Spiekman (SMNS), C. Klug, T. Scheyer, and B. Scheffold (PIMUZ), H. Hagdorn (MHI), and I. Werneburg and A. Krahl (GPIT) for their hospitality and help during the visits and examination of their collections. We are grateful to editor H.-D. Sues, H. Hagdorn, two anonymous reviewers, and K. De Beats, and J. Dzik for discussion of the manuscript and for their helpful suggestions. We thank R. Motani, A. Wolniewicz, and A. Tintori for their help in identification of the vertebral centra assigned to Blezingeria. We thank K. Przestrzelska and P. Bajdek for their help in specimen preparation, and M. Dziewiński and J. Jabłoński for help in fossil transportation and photography. We express our gratitude to the authorities of the Zbrosławice municipality, as well as the mayors (W. Nawrocki, H. Kupka) and the community of the Miedary village for their long-standing hospitality. We thank K. Pielka, owner of the Miedary claypit area for support during the excavations, and S. Szczygiel for help with obtaining archival pictures of the Miedary claypit. We thank all students and volunteers taking part in the fieldwork in the Miedary site since 2015, particularly those who directly contributed to the discovery of the specimens described in the herein study: J. Armatys, M. Baranowska, M. Bieniaszewski, J. Chrostowski, M. Gierek, M. Granica, K. Grygorczyk, D. Hałubek, S. Kaczmarczyk, S. Kawecki, A. Kawińska, L. Kłosińska, A. Kowalewska, T. Kozyk, B. Kulus, A. Lewczuk, A. Lis, S. López-Torres, A. Minich, K. Nawrot, R. Nowakowski, R. Pelczar, K. Peszek, J. Rabińska, P. Rozwala","PeriodicalId":17597,"journal":{"name":"Journal of Vertebrate Paleontology","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2023-10-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"136261557","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}