Two new genera have been identified in the Permian of Mexico: cf Bjuvia and Nils-sonia. Along with previously-known Taeniopteris , these confirm the presence of Cyca-dophytes in the upper Paleozoic of Mexico. This substantially increases the geographical and temporal distribution of this group and provides information on the type of environment in which these plants developed. The new reports come from two localities of the Matzitzi Formation, in the state of Puebla, Mexico, called Carretera (Ca) and Coatepec (Co). In the first locality, we identified material characterized by the presence of a simple leaf of large size with veins perpendicular to the rachis and always parallel, as well as a stomatal apparatus with papillae. The fragmentary nature of the material from Puebla allows only an affinity to Bjuvia of the order Cycadales. Other specimens are assigned to Taeniopteris and Nilssonia . The Nilssonia reported from Carretera, has a segmented lamina attached to the rachis on the upper side. Tae-niopteris is characterized by an entire lamina, generally narrow, with veins originating perpendicularly to the rachis that dichotomizes one or several times. The species T. lentriculiformis and T. crassinervis are reported for the first time from Coatepec. Together with these genera
{"title":"New records of Bjuvia and Nilssonia from the Permian of Mexico","authors":"Miguel A. Flores-Barragan, M. P. Velasco-de León","doi":"10.26879/1109","DOIUrl":"https://doi.org/10.26879/1109","url":null,"abstract":"Two new genera have been identified in the Permian of Mexico: cf Bjuvia and Nils-sonia. Along with previously-known Taeniopteris , these confirm the presence of Cyca-dophytes in the upper Paleozoic of Mexico. This substantially increases the geographical and temporal distribution of this group and provides information on the type of environment in which these plants developed. The new reports come from two localities of the Matzitzi Formation, in the state of Puebla, Mexico, called Carretera (Ca) and Coatepec (Co). In the first locality, we identified material characterized by the presence of a simple leaf of large size with veins perpendicular to the rachis and always parallel, as well as a stomatal apparatus with papillae. The fragmentary nature of the material from Puebla allows only an affinity to Bjuvia of the order Cycadales. Other specimens are assigned to Taeniopteris and Nilssonia . The Nilssonia reported from Carretera, has a segmented lamina attached to the rachis on the upper side. Tae-niopteris is characterized by an entire lamina, generally narrow, with veins originating perpendicularly to the rachis that dichotomizes one or several times. The species T. lentriculiformis and T. crassinervis are reported for the first time from Coatepec. Together with these genera","PeriodicalId":56100,"journal":{"name":"Palaeontologia Electronica","volume":"27 1","pages":""},"PeriodicalIF":2.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69147223","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}
Voltaire D. Paes Neto, J. Desojo, A. C. B. Brust, A. M. Ribeiro, C. Schultz, M. Soares
Aetosauroides scagliai, from the Ischigualasto Formation of Argentina and Santa Maria Supersequence of Brazil (Carnian-Norian), is one of the oldest members of Aetosauria, a diverse clade of armored crocodile-line archosaurs. Aetosauroides scagliai differs from other aetosaurs in having the maxilla excluded from the margin of the external nares, the length/width ratio of the postzygapophyses ≤ 0.75, and other features that place it as one of the earliest-diverging members of the clade. In this paper we provide a detailed description of the skull of A. scagliai based on a new Brazilian specimen, revealing that it lacks a pneumatic cavity on the medial surface of the maxilla and further differs from all other known aetosaurs by the presence of ≥ 12 dentary teeth. However, contra previous studies, the elongated posterior process of the jugal does articulate ventrally with the quadratojugal in A. scagliai, forming the posteroventral corner of the skull as in all other aetosaurs. Aetosauroides scagliai exhibits some characters typical of predatory archosaurs (like the recurved ziphodont teeth and mandibular articulation at the level of the tooth row), but was probably an omnivore, as it also shares several probable adaptations for herbivory with aetosaurs generally (i.e., edentulous anterior premaxilla and dentary) and stagonolepidoids specifically (e.g., shovel-shaped snout). This suggests that there was greater trophic diversity in this clade than usually recognized, at least early in their evolutionary history. Voltaire Dutra Paes Neto. Programa de Pós-Graduação em Geociências. Av. Bento Gonçalves 9500, Prédio 43127, 91540-000, Porto Alegre, Brazil. voltairearts@gmail.com Julia Brenda Desojo. División Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n°, La Plata, B1900FWA, Buenos Aires, Argentina; Consejo Nacional de Investigaciones Científicas y Tecnológicas (CONICET). julideso@fcnym.unlp.edu.ar Ana Carolina Biacchi Brust. Centro de Estudos e Pesquisas em Direito e Internet. Av. Roraima, 1000, 74B (3427), 97105-900, Santa Maria, Brazil. anacarolinabrust@gmail.com Ana Maria Ribeiro. Museu de Ciências Naturais do Rio Grande do Sul – SEMA/RS. Dr. Salvador França, 1427 Jardim Botânico, Porto Alegre RS, 90690-000 amaria_ribeiro@yahoo.com.br PAES NETO ET AL.: AETOSAUROIDES SKULL 2 Cesar Leandro Schultz. Programa de Pós-Graduação em Geociências. Av. Bento Gonçalves 9500, Prédio 43127, 91540-000, Porto Alegre, Brazil. cesar.schultz@ufrgs.br Marina Bento Soares. Museu Nacional, Universidade Federal do Rio de Janeiro. Parque da Quinta da Boa vista s/n 20940-040, Rio de Janeiro, RJ, Brazil. marina.soares@mn.ufrj.br
Aetosauroides scagliai来自阿根廷的Ischigualasto组和巴西的Santa Maria超序(卡尼亚-诺里亚)，是最古老的Aetosauria成员之一，Aetosauria是一个多样化的装甲鳄鱼系祖龙分支。scagliai Aetosauroides scagliai与其他aetosaurus的不同之处在于，其上颌骨被排除在外鼻的边缘之外，后颧骨的长/宽比≤0.75，以及其他特征使其成为该分支中最早分化的成员之一。在这篇论文中，我们基于一个新的巴西标本对a . scagliai的头骨进行了详细的描述，揭示了它在上颌骨的内侧表面缺乏一个气动腔，并且与所有其他已知的aetosaurus的不同之处是存在≥12颗直齿。然而，与先前的研究相反，在A. scagliai中，长形的下颌后突确实在腹侧与方形下颌相连，形成了头骨的后腹侧角，就像所有其他直龙一样。scagliai Aetosauroides scagliai具有一些掠食性始祖龙的典型特征(如弯曲的ziphodon牙齿和齿列水平的下颌关节)，但它可能是杂食动物，因为它也与一般的aetosaurus(即无牙的前颌和有牙的)和stagonolepidoids(例如，铲子形的鼻子)有一些可能的食草性适应。这表明，至少在它们的进化史早期，这一分支的营养多样性比通常认为的要大。伏尔泰。Programa de Pós-Graduação em Geociênciasa . Bento gonalalves 9500, pracimdio 43127, 91540-000，巴西阿雷格里港。voltairearts@gmail.com Julia Brenda Desojo。División Paleontología维蒂布拉多斯，拉普拉塔博物馆，博斯克大道，拉普拉塔，B1900FWA，布宜诺斯艾利斯，阿根廷;国家调查委员会Científicas y Tecnológicas(调查委员会)。julideso@fcnym.unlp.edu.ar Ana Carolina Biacchi Brust。互联网研究与信息管理中心。罗赖马，1000,74b(3427)， 97105-900，巴西圣玛丽亚。anacarolinabrust@gmail.com安娜·玛丽亚·里贝罗。Ciências巴西大自然博物馆- SEMA/RS。萨尔瓦多·弗兰扎拉博士，1427 Jardim botnico, Porto Alegre RS, 90690000 amaria_ribeiro@yahoo.com.br PAES NETO等人:AETOSAUROIDES SKULL 2 Cesar Leandro Schultz。Programa de Pós-Graduação em Geociênciasa . Bento gonalalves 9500, pracimdio 43127, 91540-000，巴西阿雷格里港。cesar.schultz@ufrgs.br Marina Bento Soares。巴西国立博物馆，巴西联邦大学。金塔大道公园(20940-040)，巴西里约热内卢，RJ。marina.soares@mn.ufrj.br
{"title":"Skull osteology of Aetosauroides scagliai Casamiquela, 1960 (Archosauria: Aetosauria) from the Late Triassic of Brazil: New insights into the paleobiology of aetosaurs","authors":"Voltaire D. Paes Neto, J. Desojo, A. C. B. Brust, A. M. Ribeiro, C. Schultz, M. Soares","doi":"10.26879/1120","DOIUrl":"https://doi.org/10.26879/1120","url":null,"abstract":"Aetosauroides scagliai, from the Ischigualasto Formation of Argentina and Santa Maria Supersequence of Brazil (Carnian-Norian), is one of the oldest members of Aetosauria, a diverse clade of armored crocodile-line archosaurs. Aetosauroides scagliai differs from other aetosaurs in having the maxilla excluded from the margin of the external nares, the length/width ratio of the postzygapophyses ≤ 0.75, and other features that place it as one of the earliest-diverging members of the clade. In this paper we provide a detailed description of the skull of A. scagliai based on a new Brazilian specimen, revealing that it lacks a pneumatic cavity on the medial surface of the maxilla and further differs from all other known aetosaurs by the presence of ≥ 12 dentary teeth. However, contra previous studies, the elongated posterior process of the jugal does articulate ventrally with the quadratojugal in A. scagliai, forming the posteroventral corner of the skull as in all other aetosaurs. Aetosauroides scagliai exhibits some characters typical of predatory archosaurs (like the recurved ziphodont teeth and mandibular articulation at the level of the tooth row), but was probably an omnivore, as it also shares several probable adaptations for herbivory with aetosaurs generally (i.e., edentulous anterior premaxilla and dentary) and stagonolepidoids specifically (e.g., shovel-shaped snout). This suggests that there was greater trophic diversity in this clade than usually recognized, at least early in their evolutionary history. Voltaire Dutra Paes Neto. Programa de Pós-Graduação em Geociências. Av. Bento Gonçalves 9500, Prédio 43127, 91540-000, Porto Alegre, Brazil. voltairearts@gmail.com Julia Brenda Desojo. División Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n°, La Plata, B1900FWA, Buenos Aires, Argentina; Consejo Nacional de Investigaciones Científicas y Tecnológicas (CONICET). julideso@fcnym.unlp.edu.ar Ana Carolina Biacchi Brust. Centro de Estudos e Pesquisas em Direito e Internet. Av. Roraima, 1000, 74B (3427), 97105-900, Santa Maria, Brazil. anacarolinabrust@gmail.com Ana Maria Ribeiro. Museu de Ciências Naturais do Rio Grande do Sul – SEMA/RS. Dr. Salvador França, 1427 Jardim Botânico, Porto Alegre RS, 90690-000 amaria_ribeiro@yahoo.com.br PAES NETO ET AL.: AETOSAUROIDES SKULL 2 Cesar Leandro Schultz. Programa de Pós-Graduação em Geociências. Av. Bento Gonçalves 9500, Prédio 43127, 91540-000, Porto Alegre, Brazil. cesar.schultz@ufrgs.br Marina Bento Soares. Museu Nacional, Universidade Federal do Rio de Janeiro. Parque da Quinta da Boa vista s/n 20940-040, Rio de Janeiro, RJ, Brazil. marina.soares@mn.ufrj.br","PeriodicalId":56100,"journal":{"name":"Palaeontologia Electronica","volume":"1 1","pages":""},"PeriodicalIF":2.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69147296","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}
N. Nasser, B. Gregory, D. Singer, R. Patterson, H. Roe
Testate lobose amoebae of the order Arcellinida are a diverse, cosmopolitan group of shelled protists found in many environments, including freshwater habitats, peatlands, and soils. Their decay-resistant tests make them an important fossil group for reconstructing Quaternary environments. Within the family Difflugidae Stein, 1859 more than 300 species and 200 sub-species have been attributed to the genus Difflugia Leclerc, 1815. Although carried out on only a few taxa, molecular evidence has demonstrated that test morphology is more important than test composition in categorizing distinct taxa within the Arcellinida. The type species of Difflugia, D. proteiformis Lamarck, 1816, is characterized by a terminal aperture and an elongate acuminate test. The morphology of D. proteiformis is vastly different from most species assigned to Difflugia, explaining its polyphyletic status. We reclassify Difflugia bidens Penard, 1902 as type species of Erugomicula, a new genus within the Difflugidae, which is distinguished from other taxa within Difflugia by its broad, ovoid test, and distinct compression. Based on the compressed morphology of the test, which is not a characteristic of the Difflugiidae, we tentatively assign Erugomicula to the family Hyalospheniidae. Nawaf A. Nasser. Ottawa-Carleton Geoscience Centre and Department of Earth Sciences, Carleton University, Ottawa K1S 5B6, Canada. nawaf.nasser@carleton.ca Braden R.B. Gregory. Ottawa-Carleton Geoscience Centre and Department of Earth Sciences, Carleton University, Ottawa K1S 5B6, Canada. GregorBRB@gmail.com David Singer. Department of Zoology, Institute of Biosciences, University of São Paulo, São Paulo, Brazil and Ottawa-Carleton Geoscience Centre and Department of Earth Sciences, Carleton University, Ottawa K1S 5B6, Canada. david.singer.bio@outlook.com R. Timothy Patterson. Ottawa-Carleton Geoscience Centre and Department of Earth Sciences, Carleton University, Ottawa K1S 5B6, Canada. tim.patterson@carleton.ca Helen M. Roe. School of Natural and Built Environments, Queen’s University Belfast, Belfast, United Kingdom, BT7 1NN. h.roe@qub.ac.uk NASSER ET AL.: Erugomicula, A NEW GENUS OF ARCELLINIDA 2
{"title":"Erugomicula, a new genus of Arcellinida (testate lobose amoebae)","authors":"N. Nasser, B. Gregory, D. Singer, R. Patterson, H. Roe","doi":"10.26879/807","DOIUrl":"https://doi.org/10.26879/807","url":null,"abstract":"Testate lobose amoebae of the order Arcellinida are a diverse, cosmopolitan group of shelled protists found in many environments, including freshwater habitats, peatlands, and soils. Their decay-resistant tests make them an important fossil group for reconstructing Quaternary environments. Within the family Difflugidae Stein, 1859 more than 300 species and 200 sub-species have been attributed to the genus Difflugia Leclerc, 1815. Although carried out on only a few taxa, molecular evidence has demonstrated that test morphology is more important than test composition in categorizing distinct taxa within the Arcellinida. The type species of Difflugia, D. proteiformis Lamarck, 1816, is characterized by a terminal aperture and an elongate acuminate test. The morphology of D. proteiformis is vastly different from most species assigned to Difflugia, explaining its polyphyletic status. We reclassify Difflugia bidens Penard, 1902 as type species of Erugomicula, a new genus within the Difflugidae, which is distinguished from other taxa within Difflugia by its broad, ovoid test, and distinct compression. Based on the compressed morphology of the test, which is not a characteristic of the Difflugiidae, we tentatively assign Erugomicula to the family Hyalospheniidae. Nawaf A. Nasser. Ottawa-Carleton Geoscience Centre and Department of Earth Sciences, Carleton University, Ottawa K1S 5B6, Canada. nawaf.nasser@carleton.ca Braden R.B. Gregory. Ottawa-Carleton Geoscience Centre and Department of Earth Sciences, Carleton University, Ottawa K1S 5B6, Canada. GregorBRB@gmail.com David Singer. Department of Zoology, Institute of Biosciences, University of São Paulo, São Paulo, Brazil and Ottawa-Carleton Geoscience Centre and Department of Earth Sciences, Carleton University, Ottawa K1S 5B6, Canada. david.singer.bio@outlook.com R. Timothy Patterson. Ottawa-Carleton Geoscience Centre and Department of Earth Sciences, Carleton University, Ottawa K1S 5B6, Canada. tim.patterson@carleton.ca Helen M. Roe. School of Natural and Built Environments, Queen’s University Belfast, Belfast, United Kingdom, BT7 1NN. h.roe@qub.ac.uk NASSER ET AL.: Erugomicula, A NEW GENUS OF ARCELLINIDA 2","PeriodicalId":56100,"journal":{"name":"Palaeontologia Electronica","volume":"1 1","pages":""},"PeriodicalIF":2.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69156092","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}
Large horned brontotheres (Brontotheriidae) are abundantly represented in Duchesnean and early Chadronian mammal faunas from the Big Bend Area of West Texas and nearby Mexico. The majority of this material, which until now has never been fully examined, is identified and described. The first brontothere to be named from this region, Menodus bakeri Stovall, 1948, is found to be a nomen dubium. The majority of the fossil material is referrable to Protitanops curryi Stock, 1936. P. curryi, previously only known from a single specimen from the Titus Valley Formation of Southern California, is now recognized in both the Duchesnean and Chadronian land mammal ages of Texas. It occurs in the late Duchesnean Porvenir Local Fauna from the lower part of the Chambers Tuff Formation and from the early Chadronian Little Egypt local fauna from the upper part of the Chambers Tuff Formation and the lower Chisos Formation in the Big Bend National Park Texas. A single specimen from the early Chadronian Rancho Gaitan local fauna of the Prietos Formation of Mexico is also identified as P. curryi. The extensive Protitanops curryi material from Texas and Mexico broadens the biostratigraphic and geographic ranges of this species and provides a more extensive understanding of its morphology and phylogenetic position. Duchesneodus uintensis (Peterson, 1931) has been previously identified with diagnostic material in the Blue Cliff horizon of the lower Chambers Tuff. Duchesneodus was previously identified in the early Duchesnean Skyline Channels of the Devil’s Graveyard Formation, but this material is better identified as cf. Parvicornus occidentalis Mihlbachler and Deméré, 2009. D. uintensis is therefore restricted to the late Duchesnean in Texas. Matthew C. Mihlbachler. Department of Anatomy, New York Institute of Technology College of Osteopathic Medicine, Old Westbury, New York 11658, USA. mmihlbac@nyit.edu Donald R. Prothero, Department of Vertebrate Paleontology, Natural History Museum of L.A. County, 900 Exposition Blvd., Los Angeles, California 90007, USA. donaldprothero@att.net MIHLBACHLER & PROTHERO: TEXAS BRONTOTHERIIDAE 2
{"title":"Eocene (Duchesnean and earliest Chadronian) brontotheres (Brontotheriidae), Protitanops curryi and cf. Parvicornus occidentalis, from west Texas and Mexico","authors":"Matthew C. Mihlbachler, D. Prothero","doi":"10.26879/944","DOIUrl":"https://doi.org/10.26879/944","url":null,"abstract":"Large horned brontotheres (Brontotheriidae) are abundantly represented in Duchesnean and early Chadronian mammal faunas from the Big Bend Area of West Texas and nearby Mexico. The majority of this material, which until now has never been fully examined, is identified and described. The first brontothere to be named from this region, Menodus bakeri Stovall, 1948, is found to be a nomen dubium. The majority of the fossil material is referrable to Protitanops curryi Stock, 1936. P. curryi, previously only known from a single specimen from the Titus Valley Formation of Southern California, is now recognized in both the Duchesnean and Chadronian land mammal ages of Texas. It occurs in the late Duchesnean Porvenir Local Fauna from the lower part of the Chambers Tuff Formation and from the early Chadronian Little Egypt local fauna from the upper part of the Chambers Tuff Formation and the lower Chisos Formation in the Big Bend National Park Texas. A single specimen from the early Chadronian Rancho Gaitan local fauna of the Prietos Formation of Mexico is also identified as P. curryi. The extensive Protitanops curryi material from Texas and Mexico broadens the biostratigraphic and geographic ranges of this species and provides a more extensive understanding of its morphology and phylogenetic position. Duchesneodus uintensis (Peterson, 1931) has been previously identified with diagnostic material in the Blue Cliff horizon of the lower Chambers Tuff. Duchesneodus was previously identified in the early Duchesnean Skyline Channels of the Devil’s Graveyard Formation, but this material is better identified as cf. Parvicornus occidentalis Mihlbachler and Deméré, 2009. D. uintensis is therefore restricted to the late Duchesnean in Texas. Matthew C. Mihlbachler. Department of Anatomy, New York Institute of Technology College of Osteopathic Medicine, Old Westbury, New York 11658, USA. mmihlbac@nyit.edu Donald R. Prothero, Department of Vertebrate Paleontology, Natural History Museum of L.A. County, 900 Exposition Blvd., Los Angeles, California 90007, USA. donaldprothero@att.net MIHLBACHLER & PROTHERO: TEXAS BRONTOTHERIIDAE 2","PeriodicalId":56100,"journal":{"name":"Palaeontologia Electronica","volume":"52 1","pages":""},"PeriodicalIF":2.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69155891","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}
R. Bicknell, J. Žalohar, Primož Miklavc, B. Celarc, M. Križnar, T. Hitij
Xiphosura are a group of marine euchelicerates with a fossil record spanning the majority of the Phanerozoic. Despite this longevity, horseshoe crab fossils are uncommon. This rarity is a result of their cuticular exoskeleton that limits the preservational potential of xiphosurid specimens. Nonetheless, a xiphosurid evolutionary radiation is recorded in Triassic-aged deposits. This event likely reflects the occupation of vacant niches after the end-Permian extinction. Here, we revisit Sloveniolimulus rudkini Bick-nell et al., 2019b—a Middle Triassic horseshoe crab from the Strelovec Formation that was previously known from one specimen—and include newly identified material to explore the validity of the taxon. We demonstrate that unique genal spine morphologies are observed in all specimens, supporting the maintenance of S. rudkini . In documenting this material, we also considered the preservational pathways for horseshoe crabs in limestone and document other metazoan groups from this as-of-yet underex-plored Konservat-Lagerstätte.
{"title":"Revisiting horseshoe crab fossils from the Middle Triassic (Anisian) Strelovec Formation Konservat-Lagerstätte of Slovenia","authors":"R. Bicknell, J. Žalohar, Primož Miklavc, B. Celarc, M. Križnar, T. Hitij","doi":"10.26879/1168","DOIUrl":"https://doi.org/10.26879/1168","url":null,"abstract":"Xiphosura are a group of marine euchelicerates with a fossil record spanning the majority of the Phanerozoic. Despite this longevity, horseshoe crab fossils are uncommon. This rarity is a result of their cuticular exoskeleton that limits the preservational potential of xiphosurid specimens. Nonetheless, a xiphosurid evolutionary radiation is recorded in Triassic-aged deposits. This event likely reflects the occupation of vacant niches after the end-Permian extinction. Here, we revisit Sloveniolimulus rudkini Bick-nell et al., 2019b—a Middle Triassic horseshoe crab from the Strelovec Formation that was previously known from one specimen—and include newly identified material to explore the validity of the taxon. We demonstrate that unique genal spine morphologies are observed in all specimens, supporting the maintenance of S. rudkini . In documenting this material, we also considered the preservational pathways for horseshoe crabs in limestone and document other metazoan groups from this as-of-yet underex-plored Konservat-Lagerstätte.","PeriodicalId":56100,"journal":{"name":"Palaeontologia Electronica","volume":"1 1","pages":""},"PeriodicalIF":2.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69147152","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}
{"title":"Patagonia’s diverse but homogeneous early Paleocene forests: Angiosperm leaves from the Danian Salamanca and Peñas Coloradas formations, San Jorge Basin, Chubut, Argentina","authors":"A. Iglesias, P. Wilf, E. Stiles, Rebecca Wilf","doi":"10.26879/1124","DOIUrl":"https://doi.org/10.26879/1124","url":null,"abstract":"","PeriodicalId":56100,"journal":{"name":"Palaeontologia Electronica","volume":"24 1","pages":"1-88"},"PeriodicalIF":2.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69147306","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}
Teeth can provide important insight into diet and evolution of extinct vertebrates. Tooth enamel microstructure records functional and phylogenetic signals beyond the gross morphology of the dentition. Here , we provide the first systematic sampling of phytosaur tooth enamel to address questions of intra-and interspecific variation, and thus taxonomic identification, biogeographic connectivity, and heterodonty. We sampled 23 phytosaur teeth from five localities throughout the American Southwest and one locality from the Newark Supergroup of North Carolina. These teeth probably represent five heterodont genera and are tentatively assigned to Angistorhinus, Smilosu-chus, Machaeroprosopus, Redondasaurus, and “Rutiodon” . We used scanning electron microscopy to examine their enamel microstructure from transverse, longitudinal, and tangential cross-sections. All sampled teeth are composed of columnar enamel ranging in thickness from 20 to 150 µm, typically 50–100 µm, across all
{"title":"Tooth enamel microstructure in North American Phytosauria (Diapsida:Archosauriformes): Implications for biogeography and ecology of a Late Triassic clade of crocodylian-like predators","authors":"Devin K. Hoffman, Jess Miller-Camp, A. Heckert","doi":"10.26879/1162","DOIUrl":"https://doi.org/10.26879/1162","url":null,"abstract":"Teeth can provide important insight into diet and evolution of extinct vertebrates. Tooth enamel microstructure records functional and phylogenetic signals beyond the gross morphology of the dentition. Here , we provide the first systematic sampling of phytosaur tooth enamel to address questions of intra-and interspecific variation, and thus taxonomic identification, biogeographic connectivity, and heterodonty. We sampled 23 phytosaur teeth from five localities throughout the American Southwest and one locality from the Newark Supergroup of North Carolina. These teeth probably represent five heterodont genera and are tentatively assigned to Angistorhinus, Smilosu-chus, Machaeroprosopus, Redondasaurus, and “Rutiodon” . We used scanning electron microscopy to examine their enamel microstructure from transverse, longitudinal, and tangential cross-sections. All sampled teeth are composed of columnar enamel ranging in thickness from 20 to 150 µm, typically 50–100 µm, across all","PeriodicalId":56100,"journal":{"name":"Palaeontologia Electronica","volume":"1 1","pages":""},"PeriodicalIF":2.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69147036","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}
The late early Miocene Béon 1 locality has yielded an abundant vertebrate fauna with more than 5,000 remains assigned to four rhinocerotid species: the stem rhinocerotine Plesiaceratherium mirallesi, the teleoceratines Prosantorhinus douvillei and Brachypotherium brachypus , and the early-diverging elasmotheriine Hispanotherium beonense . Such a profusion of closely related large herbivore species co-occurring raises questions about habitat capacity and niche partitioning. To investigate potential niche partitioning of Béon 1 rhinocerotids, we studied their ecology through texture microwear stress between the low scores suggesting browsing preferences, microwear subtle dietary
{"title":"Paleoecology of the Rhinocerotidae (Mammalia, Perissodactyla) from Béon 1, Montréal-du-Gers (late early Miocene, SW France): Insights from dental microwear texture analysis, mesowear, and enamel hypoplasia","authors":"M. Hullot, Y. Laurent, G. Merceron, P. Antoine","doi":"10.26879/1163","DOIUrl":"https://doi.org/10.26879/1163","url":null,"abstract":"The late early Miocene Béon 1 locality has yielded an abundant vertebrate fauna with more than 5,000 remains assigned to four rhinocerotid species: the stem rhinocerotine Plesiaceratherium mirallesi, the teleoceratines Prosantorhinus douvillei and Brachypotherium brachypus , and the early-diverging elasmotheriine Hispanotherium beonense . Such a profusion of closely related large herbivore species co-occurring raises questions about habitat capacity and niche partitioning. To investigate potential niche partitioning of Béon 1 rhinocerotids, we studied their ecology through texture microwear stress between the low scores suggesting browsing preferences, microwear subtle dietary","PeriodicalId":56100,"journal":{"name":"Palaeontologia Electronica","volume":"1 1","pages":""},"PeriodicalIF":2.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69147049","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}
Sauropod dinosaurs were the dominant large-bodied herbivores in many Mesozoic terrestrial ecosystems. Such predominance took place after a faunal replacement event linked to a global environmental change during the Early Jurassic (Pliensbachian–Toarcian), when the smaller basal sauropodomorphs were replaced by giant forms in the subclade Eusauropoda. Two main characteristics of this latter group are large body size (exceeding 10 tons) and a remarkably long neck. New data is presented on the axial anatomy of one of the earliest known eusauropods, Bagualia alba from the Toarcian levels of the Cañadón Asfalto Formation (Chubut Province, Argentina), which bear on the origins of these characteristics. Optimizing relevant axial characters on sauropodomorph phylogeny highlights important changes in cervical anatomy in the evolution of Sauropoda: a greater elongation of the neck due to both an increase in the vertebral count and the elongation of each cervical vertebra, and the appearance of pneumatic structures, first on the external surface (e.g., pleurocoels, laminae within the pleurocoels, accessory laminae of the neural arch) and subsequently invading the internal body of the vertebrae. These two changes have been considered essentials for body mass increase in Eusauropoda. The Toarcian age of Bagualia indicates that several important modifications in the axial skeleton and especially the neck occurred early in eusauropod evolution. These modifications are of ecomorphological importance and likely influenced the success of the eusauropods during the climatic changes surrounding the Pliensbachian–Toarcian crisis. Kevin Leonel Gomez. Consejo Nacional de Investigaciones Científicas y Técnicas, Museo Paleontológico Egidio Feruglio, Fontana 140, 9100, Trelew, Argentina. kgomez@mef.org.ar Jose Luis Carballido. Consejo Nacional de Investigaciones Científicas y Técnicas, Museo Paleontológico Egidio Feruglio, Fontana 140, 9100, Trelew, Argentina. jcarballido@mef.org.ar Diego Pol. Consejo Nacional de Investigaciones Científicas y Técnicas, Museo Paleontológico Egidio Feruglio, Fontana 140, 9100, Trelew, Argentina. dpol@mef.org.ar
在许多中生代陆地生态系统中，蜥脚类恐龙是主要的大型食草动物。这种优势是在早侏罗世(Pliensbachian-Toarcian)与全球环境变化有关的动物替换事件之后发生的，当时较小的基础蜥脚类被亚分支真蜥足类的巨大形式所取代。后者的两个主要特征是巨大的体型(超过10吨)和非常长的脖子。关于已知最早的真蜥脚类动物之一，来自Cañadón Asfalto组(Chubut省，阿根廷)Toarcian层的Bagualia alba的轴向解剖，提出了新的数据，这些数据与这些特征的起源有关。优化蜥脚类动物系统发育的相关轴向特征，凸显了蜥脚类动物进化过程中颈椎解剖学的重要变化:由于椎体数量的增加和每个颈椎的伸长，颈部的更大伸长，以及气动结构的出现，首先在外表面(例如，胸膜腔、胸膜腔内的椎板、神经弓的副椎板)，随后侵入椎体内部。这两种变化被认为是真爪足类动物体重增加的必要因素。巴瓜利亚的托瓦西亚时代表明，在真蜥脚类动物进化的早期，轴向骨骼，特别是颈部发生了一些重要的变化。这些变化在生态形态学上具有重要意义，并可能影响了在pliensbach - toarcian危机期间气候变化的真蜥脚类动物的成功。凯文·莱昂内尔·戈麦斯。国家调查委员会Científicas y tacimnicas, Paleontológico Egidio Feruglio博物馆，Fontana 144,9100，阿根廷Trelew。kgomez@mef.org.ar何塞·路易斯·卡巴利多。国家调查委员会Científicas y tacimnicas, Paleontológico Egidio Feruglio博物馆，Fontana 144,9100，阿根廷Trelew。jcarballido@mef.org.ar迭戈·波尔。国家调查委员会Científicas y tacimnicas, Paleontológico Egidio Feruglio博物馆，Fontana 144,9100，阿根廷Trelew。dpol@mef.org.ar
{"title":"The axial skeleton of Bagualia alba (Dinosauria: Eusauropoda) from the Early Jurassic of Patagonia","authors":"K. Gómez, J. Carballido, D. Pol","doi":"10.26879/1176","DOIUrl":"https://doi.org/10.26879/1176","url":null,"abstract":"Sauropod dinosaurs were the dominant large-bodied herbivores in many Mesozoic terrestrial ecosystems. Such predominance took place after a faunal replacement event linked to a global environmental change during the Early Jurassic (Pliensbachian–Toarcian), when the smaller basal sauropodomorphs were replaced by giant forms in the subclade Eusauropoda. Two main characteristics of this latter group are large body size (exceeding 10 tons) and a remarkably long neck. New data is presented on the axial anatomy of one of the earliest known eusauropods, Bagualia alba from the Toarcian levels of the Cañadón Asfalto Formation (Chubut Province, Argentina), which bear on the origins of these characteristics. Optimizing relevant axial characters on sauropodomorph phylogeny highlights important changes in cervical anatomy in the evolution of Sauropoda: a greater elongation of the neck due to both an increase in the vertebral count and the elongation of each cervical vertebra, and the appearance of pneumatic structures, first on the external surface (e.g., pleurocoels, laminae within the pleurocoels, accessory laminae of the neural arch) and subsequently invading the internal body of the vertebrae. These two changes have been considered essentials for body mass increase in Eusauropoda. The Toarcian age of Bagualia indicates that several important modifications in the axial skeleton and especially the neck occurred early in eusauropod evolution. These modifications are of ecomorphological importance and likely influenced the success of the eusauropods during the climatic changes surrounding the Pliensbachian–Toarcian crisis. Kevin Leonel Gomez. Consejo Nacional de Investigaciones Científicas y Técnicas, Museo Paleontológico Egidio Feruglio, Fontana 140, 9100, Trelew, Argentina. kgomez@mef.org.ar Jose Luis Carballido. Consejo Nacional de Investigaciones Científicas y Técnicas, Museo Paleontológico Egidio Feruglio, Fontana 140, 9100, Trelew, Argentina. jcarballido@mef.org.ar Diego Pol. Consejo Nacional de Investigaciones Científicas y Técnicas, Museo Paleontológico Egidio Feruglio, Fontana 140, 9100, Trelew, Argentina. dpol@mef.org.ar","PeriodicalId":56100,"journal":{"name":"Palaeontologia Electronica","volume":"1 1","pages":""},"PeriodicalIF":2.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69147447","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}
{"title":"Late Cretaceous Elopomorpha (Actinopterygii: Teleostei) from the Mahajanga Basin of Madagascar and impacts on paleobiogeography","authors":"Summer Ostrowski","doi":"10.26879/1151","DOIUrl":"https://doi.org/10.26879/1151","url":null,"abstract":",","PeriodicalId":56100,"journal":{"name":"Palaeontologia Electronica","volume":"1 1","pages":""},"PeriodicalIF":2.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69146880","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}
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