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Geochemical extraction of ceratopsian remains from ironstone 从铁岩中提取角龙遗骸的地球化学研究
IF 1.4 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-12-15 DOI: 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...
许多化石周围都有铁岩,其硬度给全球化石保护人员带来了巨大挑战。铁矿石有多种形式,其中碳酸盐形式的菱铁矿...
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引用次数: 0
The origin of modern marlins (Teleostei: Istiophoridae): new fossil evidence from the Lower Miocene of Austria 现代海马(Teleostei: Istiophoridae)的起源:来自奥地利下中新世的新化石证据
IF 1.4 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-12-12 DOI: 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...
我们报告了奥地利帕金北阿尔卑斯前陆盆地(西帕拉特提斯)最古老的Istiophoridae化石记录(下中新世,下阿基坦统,∼22.4 Ma)。所研究的标本...
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引用次数: 0
A New Eutherian Mammal from the Upper Cretaceous Bayinshire Formation of Mongolia 蒙古上白垩统巴音夏组真兽哺乳动物一新种
IF 1.4 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-12-04 DOI: 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…
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引用次数: 0
A new hupehsuchian (Reptilia: Ichthyosauromorpha) from the Lower Triassic of South China with implications for the evolution of polydactyly 华南下三叠世一新虎爪目(爬行纲:鱼爪目)及其多趾进化意义
IF 1.4 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-24 DOI: 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...
Hupehsuchia是华南下三叠世的一种神秘的海洋爬行动物,其特征包括前肢和后肢的单侧或双侧多趾。合适的婚姻对象……
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引用次数: 0
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. Journal of Vertebrate Paleontology . https://doi.org/10.1080/02724634.2023.2255236 美国德克萨斯州西部晚三叠世脊椎动物组合中一种新的kannemeyeryiiform双齿兽(Synapsida)。本文引文:Mueller, b.d., Huttenlocker, a.k., Small, b.j., Pinto, j.l., Dean-Wallace, K., &;(2023)美国西部晚三叠世脊椎动物群中一种新的kannemeyeryiform dicynodon (Synapsida),古生物学报。https://doi.org/10.1080/02724634.2023.2255236
4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-03 DOI: 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
摘要:美国德克萨斯州西部上三叠统Tecovas组(Dockum群)发现了一种新的kannemeyeryiiform dicynodon (Argodicynodon boreni gen. et sp. nov.)。该分类群的颅骨特征包括:鳞状-壁间缝合接触广泛且交错;高而窄的颞间区由顶部形成,长后颊部形成背平台的侧面;壁间形成多节的,双裂片的外生物,楔入壁间形成一个w形的轮廓在背面视图;枕后髁和枕外髁对枕后髁的贡献是不同的,分离枕外髁的背窝是深切和背腹深的;上颌骨犬科突背腹深且发育良好;关节内侧有一个细长的锯齿状突起超过了方形滚轴的宽度。基于23个连续和176个离散(数字)形态特征和120个分类群的系统发育分析发现,Argodicynodon保守地属于Placerias + Moghreberia类群附近的一个placeriae,代表了美国西南部最古老的placeriae,也是德克萨斯州Dockum类群中第一个被命名的dicynodon属。通过对欧美双齿兽记录的回顾,揭示了晚三叠世Laurasia地区双齿兽的多样性和丰富性。Argodicynodon和其他先前在附近地区发现的双齿类化石的记录强调了北美上三叠统非placeria双齿类化石的多样性。http://zoobank.org/urn:lsid:zoobank.org:pub:AB9B7ABC-6C84-4B04-909F-F1DA114030AB致谢本研究部分基于BDM在其委员会成员SC、J. Barrick和T. Lehman的指导下完成的论文。我们感谢J. Boren和Boren家族允许进入现场,并慷慨地将化石材料捐赠给德克萨斯理工大学博物馆。我们感谢在现场和实验室中提供帮助的众多德克萨斯理工学院学生和志愿者。B. Meyers发现了局部MOTT VPL 3881和左肱骨(tu - p10421)。我们也感谢P. Holroyd和UCMP提供Placerias采石场的比较材料。特别感谢D. Cunningham、G. grtler、A. hungerb hler、J. Martz、S. Nesbitt和W. Parker在本项目各方面提供的帮助。我们还要感谢K. Angielczyk、C. Kammerer和T. Sulej对我们的手稿提供的有益反馈。这个项目是在德克萨斯理工大学博物馆的支持下实现的。披露声明作者未报告潜在的利益冲突。作者贡献sbdm设计了这个项目,并为他未发表的博士论文的初稿撰写了部分内容。AKH和BJS收集数据,修改和编辑稿件,起草和修改图表,并进行系统发育分析。AKH和JLP从Placerias收集了额外的比较数据和照片。KD-W和SC提供了额外的数据和照片。所有作者都编辑了这份手稿。补充文件补充数据1:详细方法(补充附录S1-S5)。补充数据2:用于分类分析的nexus格式文件(完整数据集)。补充数据3:用于分类分析的nexus格式文件(修剪后的kannemeyeriiform数据集)。补充资料4:tnt格式的完整分析文件。补充数据5:tnt格式的简化分析文件。
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引用次数: 0
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. Journal of Vertebrate Paleontology . https://doi.org/10.1080/… 希腊萨莫斯岛(Samos Island)晚中新世无角犀类的新类型命名及其对欧洲儿童的启示。本文引用本文:Kampouridis, P., Svorligkou, G., Kargopoulos, N., Spassov, N., &;Böhme, M.(2023)希腊Samos岛晚中新世无角犀类的新类型划分及其对欧洲chilotheres的启示。古脊椎动物杂志。https://doi.org/10.1080/..。
4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-02 DOI: 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.
现存的犀牛只有五个物种,它们的特征是有一个鼻角。在过去,它们的种类要多样得多,其中最著名的一种是无角犀牛,即无角犀牛。Chilotheres是一群在中新世晚期居住在欧亚大陆的无角犀牛。它们最西端的地理范围到达了东欧,在那里总共竖立了8种。其中四个是根据Samos岛(希腊)上中新世的材料描述的,其中两个被认为不再有效。不幸的是,这四个物种的头骨类型都丢失了,而且它们的分类学存在一些问题。因此,我们在此将萨摩斯历史藏品中的两个头骨指定为前两个物种的新类型,即Chilotherium schlosseri (Weber, 1905)和Eochilotherium samium (Weber, 1905),并对这两个物种之间以及与任何其他chilotheri之间的分离进行了详细的比较。我们的结果证明了这两个物种是有效的,并证明了它们在一般水平上的分离。Chilotherium schlosseri似乎与其他欧洲Chilotherium物种更接近,而E. samium则更接近中国的“Chilotherium”wimani和“Chilotherium”primigenium,基于它们更多的半形特征。
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引用次数: 0
A saw-toothed eel † Serrivomer glehni sp. nov. from the Miocene of Sakhalin Island, north-western PacificCitation for this article: Nazarkin, M. V. (2023) A saw-toothed eel † Serrivomer glehni sp. nov. from the Miocene of Sakhalin Island, north-western Pacific. Journal of Vertebrate Paleontology . https://doi.org/10.1080/02724634.2023.2261505 A saw-toothed鳝†Serrivomer glehni sp. nov. from中新世的库页岛,西北太平洋。古脊椎动物杂志。https://doi.org/10.1080/02724634.2023.2261505
4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-02 DOI: 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。
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引用次数: 0
The first articulated skull roof and braincase of Melvius chauliodous (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 Melvius chauliodous (Amiidae, Vidalamiinae) from the Upper Cretaceous Kirtland Formation, San Juan Basin, New Mexico. Journal of Vertebrate Paleontology . https://doi.org… 新墨西哥州圣胡安盆地上白垩统Kirtland组首次发现的Melvius chauliodous (Amiidae, vidalamiae)的关节头盖骨顶和脑壳。Williamson, t.e.(2023)新墨西哥州圣胡安盆地上白垩统Kirtland组首次发现的Melvius chauliodous (Amiidae, Vidalamiinae)的关节头盖骨顶和脑壳。古脊椎动物杂志。https://doi.org..。
4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-01 DOI: 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
来自美国新墨西哥州Kirtland地层的Melvius chauliodous新发现的保存异常完好的关节头盖和脑壳揭示了Melvius的新特征,为Melvius提供了详细的骨学信息,从而允许重新评估定义该属的特征,其两个公认的物种M. chauliodous和M. thomasi,以及其在Vidalamiinae中的系统发育关系。新的特征包括皮肤变异射线(“肋骨”)和顶骨射线束的存在,这两种梅尔维乌斯以前都不知道。细长的皮肤变形射线的存在,以前被认为是Calamopleurus属和Calamopleurini部落的特征,现在在Melvius中有记录,但这些射线在两种皮肤变形的后内侧角的起源点不同。在这两种麦尔维斯鱼的顶骨后外侧角下方也有记录显示出短的扇形射线束。Melvius先前被置于Vidalamiini部落(vidalamiae亚科),但由于它与Calamopleurini部落和Calamopleurus属成员具有一些独特的特征,因此它在Vidalamiini中的位置以及在Vidalamiinae中这两个不同的分支(部落)的识别在我们的系统发育分析中没有得到支持。以前区分梅尔维乌斯种的特征,特别是M. chauliodous和M. thomasi在眶后装饰上的差异,被认为是可疑的。然而,其他特征可能决定种间变异或差异。目前,我们保留这两个物种,直到更明确的材料的M. thomasi描述。首先,RMS感谢J. Petersen(发现者)和T. Knopick,他们帮助收集了标本,十多年来,他们一直是RMS在圣胡安盆地收集脊椎动物化石的宝贵现场助手。我们特别感谢P. Holroyd (UCMP)提供UCMP 131707和UCMP 129681的照片,这些照片对识别后一个元素至关重要。同时也要感谢M. Sims (KU生物多样性研究所和自然历史博物馆),他为我们提供了KUVP 88378的高分辨率照片,帮助我们解释和再次确认该元素的身份。特别感谢T. Tokaryk和M. Gilbert提供关于加拿大梅尔维厄斯发生情况的更多资料。RMS感谢D. Fowler (Dickinson博物馆中心和Badlands恐龙博物馆)对系统发育分析和古地理的讨论,因为它们与这项研究有关。N. Volden (NMMNH)协助获得了有关以前存放在新墨西哥大学收藏的化石标本的信息,我们感谢她的帮助。L. Rinehart制备NMMNH P-88899的腹侧,RMS制备标本的背侧。RMS感谢P. Reser提出的关于颅骨背侧准备的建议,这是非常赞赏的。我们非常感谢L. Cavin (musum d’histoire Naturelle, Geneva)对鱼类化石的深刻评论和补充信件以及对我们论文的审阅。我们还要感谢p.l. Godoy和一位匿名审稿人,他极大地改进了本文的早期版本。我们感谢JVP编辑T. Argyriou和J. Harris在我们的手稿出版过程中的指导。最后,我们感谢P. Gensler土地管理局(BLM)继续支持我们在新墨西哥州圣胡安盆地的研究,并为我们的实地工作发放了必要的许可证。两份新纳入的标本(NMMNH P-88899和P-88901)均在BLM古生物资源使用许可证号下采集。NM 14-09S(续期)发给S. Lucas, T. Williamson和G. Morgan。srms和SEJ构思并执行了该项目,起草了手稿,为人物评分,并编辑了手稿。SEJ进行了分析。RMS, SEJ和TEW对数据进行了分析,并对该版本进行了评审。补充资料1:包含图的文件。S1, S2,表S1 - s4,特征列表,数据矩阵,讨论Grande和Bemis (Citation1998)系统发育结果,和补充参考文献。补充数据2:NEXUS文件。补充数据3:TNT文件。补充数据4:最节俭的树文件。
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引用次数: 0
Gorgonops and Endothiodon (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) Gorgonops and Endothiodon (Synapsida: Therapsida) from the Madumabisa Mudstone Formation: evidence of a previously unreported tetrapod biozone in the Mid-Zambezi Basin of southern Zambia. Journal of … 来自Madumabisa泥岩组的Gorgonops和Endothiodon (Synapsida: Therapsida):赞比亚南部赞比西盆地中部以前未报道的四足动物生物带的证据。Angielczyk, K. D. (2023) Madumabisa泥岩组的Gorgonops和Endothiodon (Synapsida: Therapsida):赞比亚南部赞比西盆地中部以前未报道的四足动物生物带的证据。杂志…
4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-01 DOI: 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。
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引用次数: 0
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). Journal of Vertebrate Paleontology . https://doi.org/10.1080/02724634.2023.2265445 来自Miedary(波兰南部)的一个新的中三叠世脊椎动物组合本文引用:Czepiński, Ł, Pawlak, W., Rytel, A., Tałanda, M., Szczygielski, T., &;Sulej, T.(2023)波兰南部miary地区中三叠世脊椎动物新组合。古脊椎动物杂志。https://doi.org/10.1080/02724634.2023.2265445
4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-10-27 DOI: 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。
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引用次数: 0
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Journal of Vertebrate Paleontology
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