Subjects -> PALEONTOLOGY (Total: 46 journals)
Showing 1 - 21 of 21 Journals sorted alphabetically
Acta Palaeontologica Polonica     Open Access   (Followers: 6)
Alcheringa: An Australasian Journal of Palaeontology     Hybrid Journal   (Followers: 7)
Ameghiniana     Open Access   (Followers: 1)
Annales de Paléontologie     Full-text available via subscription   (Followers: 7)
Annals of Carnegie Museum     Full-text available via subscription   (Followers: 1)
Boreas: An International Journal of Quaternary Research     Hybrid Journal   (Followers: 12)
Comptes Rendus Palevol     Full-text available via subscription  
European Journal of Protistology     Hybrid Journal   (Followers: 6)
EvoDevo     Open Access   (Followers: 4)
Facies     Hybrid Journal   (Followers: 10)
Fossil Record     Open Access   (Followers: 5)
Geobios     Full-text available via subscription   (Followers: 6)
Historical Biology: An International Journal of Paleobiology     Hybrid Journal   (Followers: 9)
Ichnos: An International Journal for Plant and Animal Traces     Hybrid Journal  
International Journal of Speleology     Open Access   (Followers: 3)
Journal of Paleolimnology     Hybrid Journal   (Followers: 6)
Journal of Paleontology     Hybrid Journal   (Followers: 11)
Journal of Quaternary Science     Hybrid Journal   (Followers: 32)
Journal of Vertebrate Paleontology     Full-text available via subscription   (Followers: 12)
Marine Micropaleontology     Hybrid Journal   (Followers: 2)
Micropaleontology     Full-text available via subscription  
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen     Full-text available via subscription   (Followers: 4)
Novitates Paleoentomologicae     Open Access   (Followers: 1)
Open Quaternary     Open Access   (Followers: 1)
Palaeogeography, Palaeoclimatology, Palaeoecology     Hybrid Journal   (Followers: 13)
Palaeontology     Hybrid Journal   (Followers: 18)
Palaeoworld     Hybrid Journal   (Followers: 3)
PALAIOS     Hybrid Journal   (Followers: 7)
Paläontologische Zeitschrift     Hybrid Journal   (Followers: 4)
Paleobiology     Full-text available via subscription   (Followers: 6)
PaleoBios     Open Access   (Followers: 1)
Paleoceanography and Paleoclimatology     Full-text available via subscription   (Followers: 4)
Paleontological Journal     Full-text available via subscription   (Followers: 5)
Paleontological Research     Full-text available via subscription   (Followers: 3)
Palynology     Hybrid Journal   (Followers: 2)
Papers in Palaeontology     Hybrid Journal   (Followers: 1)
Quaternaire     Open Access   (Followers: 3)
Quaternary Research     Full-text available via subscription   (Followers: 20)
Quaternary Science Reviews     Hybrid Journal   (Followers: 25)
Review of Palaeobotany and Palynology     Hybrid Journal   (Followers: 2)
Revue de Micropaleontologie     Full-text available via subscription  
Rivista Italiana di Paleontologia e Stratigrafia (Research In Paleontology and Stratigraphy)     Open Access   (Followers: 2)
Spanish Journal of Palaeontology     Open Access  
Swiss Journal of Palaeontology     Hybrid Journal   (Followers: 4)
Vertebrate Anatomy Morphology Palaeontology     Open Access   (Followers: 2)
Zitteliana     Open Access   (Followers: 4)
Similar Journals
Journal Cover
Journal of Paleontology
Journal Prestige (SJR): 0.882
Citation Impact (citeScore): 2
Number of Followers: 11  
 
  Hybrid Journal Hybrid journal (It can contain Open Access articles)
ISSN (Print) 0022-3360 - ISSN (Online) 1937-2337
Published by Cambridge University Press Homepage  [395 journals]
  • JPA volume 95 issue 3 Cover and Front matter
    • PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2021.32
      Issue No: Vol. 95, No. 3 (2021)
       
  • JPA volume 95 issue 3 Cover and Back matter
    • PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2021.33
      Issue No: Vol. 95, No. 3 (2021)
       
  • Glossifungites+gingrasi+n.+isp.,+a+probable+subaqueous+insect+domicile+from+the+Cretaceous+Ferron+Sandstone,+Utah&rft.title=Journal+of+Paleontology&rft.issn=0022-3360&rft.date=2021&rft.volume=95&rft.spage=427&rft.epage=439&rft.aulast=King&rft.aufirst=M.&rft.au=M.+Ryan+King&rft.au=Andrew+D.+La+Croix,+Terry+A.+Gates,+Paul+B.+Anderson,+Lindsay+E.+Zanno&rft_id=info:doi/10.1017/jpa.2020.115">Glossifungites gingrasi n. isp., a probable subaqueous insect domicile
           from the Cretaceous Ferron Sandstone, Utah
    • Authors: M. Ryan King; Andrew D. La Croix, Terry A. Gates, Paul B. Anderson, Lindsay E. Zanno
      Pages: 427 - 439
      Abstract: A new ichnospecies, Glossifungites gingrasi n. isp., is described from multiple locations in basal sand-filled coastal plain distributary channels of the Turonian (Upper Cretaceous) Ferron Sandstone (central Utah). Glossifungites gingrasi n. isp. is attributed to the ichnogenus Glossifungites based on the presence of scratch imprints, passive fill, and a tongue-shaped structure, yet the new ichnospecies is distinct because it displays transverse bioglyphs that run perpendicular to the planiform structure, which contrasts to the axis parallel bioglyphs present in the ichnospecies G. saxicava. The transverse arrangement of ornamentation exhibited by G. gingrasi n. isp. is observed in modern subaqueous insect burrows produced by mayfly and chironomid larvae, and constitutes a way to differentiate insect-generated burrows from structures produced by crustaceans that are known to create other Glossifungites ichnospecies. Differentiating insect- from crustacean-generated burrows is significant because it provides a way to distinguish bioturbation by marine-recruited fauna from that produced by freshwater fauna in the rock record, making G. gingrasi n. isp. a valuable ichnological tool for paleoenvironmental and stratigraphic interpretation. While G. gingrasi n. isp. may represent a burrow created by a variety of filter-feeding subaqueous insects, the large size of G. gingrasi n. isp. in the Ferron Sandstone suggests that the largest specimens are probable mayfly burrows and supports the assertion that burrowing mayflies (e.g., Polymitarcyidae and Ephemeridae) adapted to domicile filter-feeding during or prior to the Turonian.UUID: http://zoobank.org/a033b22f-bf09-481a-975e-3a1b096154cc
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.115
      Issue No: Vol. 95, No. 3 (2021)
       
  • Ediacaran metazoan fossils with siliceous skeletons from the Digermulen
           Peninsula of Arctic Norway
    • Authors: Małgorzata Moczydłowska; Benjamin P. Kear, Daniel Snitting, Lei Liu, Peter Lazor, Jarosław Majka
      Pages: 440 - 475
      Abstract: In this study, a new assemblage of Ediacaran metazoan fossils is reported from the basal Stáhpogieddi Formation on the Digermulen Peninsula of Arctic Norway, including Anulitubus n. gen. Moczydłowska in Moczydłowska et al., Anulitubus formosus n. gen. n. sp. Moczydłowska in Moczydłowska et al., Coniculus n. gen. Moczydłowska in Moczydłowska et al., Coniculus elegantis n. gen. n. sp. Moczydłowska in Moczydłowska et al., Fistula n. gen. Moczydłowska in Moczydłowska et al., and Fistula crenulata n. gen. n. sp. Moczydłowska in Moczydłowska et al. The specimens are three-dimensionally preserved and include tubular and conical skeletons that are morphologically distinguished by their body-wall constructions, radial symmetry, polarity, segmentation, and annulation. The skeletons are interpreted to be biomineralized by primary silica based on computed micro-tomographic, petrographic, geochemical, and spectroscopic evidence of originally rigid body wall with layers of constant thicknesses, composed of opal, microcrystalline quartz, and an admixture of carbonaceous material, which differ from the host sediment mineralogy and do not show replacement or encrustation. The fossil-bearing interval immediately overlies strata of Gaskiers age and can be bracketed within 580–541 Ma, but it is estimated to be ca. 575 Ma on the basis of averaged sedimentation rates and biostratigraphic correlations with Ediacaran biota found in up-section deposits of ca. 558–555 Ma. Future new findings of such fossils in different preservation modes and further multi-collector inductively coupled plasma mass spectrometry, which shows the silicon fractionation and traces its biogenic origin versus inorganic mineralization, may corroborate the interpretation of biogenic silicification of these earliest skeletal fossils.UUID: https://zoobank.org/6bccada1-870e-47b0-b819-82685152ea54
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.105
      Issue No: Vol. 95, No. 3 (2021)
       
  • Biostratigraphy and taxonomy of fusulinid foraminifera across the Upper
           Mississippian (upper Serpukhovian)–Lower Pennsylvanian (Bashkirian)
           successions from the Hadim Nappe, Central Taurides, southern Turkey
    • Authors: Melikan Akbaş; Cengiz Okuyucu
      Pages: 476 - 496
      Abstract: The Hadim Nappe, which is one of the allochthonous tectonic units in the Tauride Belt, in southern Turkey, includes a continuous stratigraphic succession from the Middle(')–Late Devonian to Late Cretaceous. A relatively complete succession of the upper Serpukhovian to Bashkirian is exposed in the Central Taurides, where two sections (Yassıpınar and Gölbelen) have been selected for detailed biostratigraphic investigations. The Mississippian-Pennsylvanian boundary in these sections was determined by the first appearance datum of the Plectostaffella jakhensis and located in the oolitic limestone facies indicating a shallow-water depositional environment. The uppermost Serpukhovian and regional Bashkirian substages (Syuranian, Akavasian, Askynbashian, and Arkhangelskian) were determined by index taxa, namely Plectostaffella jakhensis, P. bogdanovkensis, P. varvariensis, Pseudostaffella antiqua, Staffellaeformes staffellaeformis, Tikhonovichiella tikhonovichi, and Verella spicata. Fifty fusulinid species belonging to fourteen genera were determined in two sections, in which two species are new: Depratina turani Akbaş new species and Tikhonovichiella praetikhonovichi Akbaş new species. The taxonomic positions of two fusulinid species (Depratina convoluta n. comb. and Staffellaeformes parva robusta n. comb.) are revised. The studied fusulinid assemblages correlate with fusulinid assemblages from the southern Urals, Russian Platform, Donetz Basin, Darvaz, Spain, central Iran, and some other regions of the Tethyan Realm.UUID: http://zoobank.org/bcbb6c72-f6f9-4e77-9cf9-3572bd731ff3
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.116
      Issue No: Vol. 95, No. 3 (2021)
       
  • Early Cambrian (Stage 4) brachiopods from the Shipai Formation in the
           Three Gorges area of South China
    • Authors: Xiaolin Duan; Marissa J. Betts, Lars E. Holmer, Yanlong Chen, Fan Liu, Yue Liang, Zhifei Zhang
      Pages: 497 - 526
      Abstract: Diverse and abundant fossil taxa have been described in the lower Cambrian Shipai Formation in the Three Gorges area of Hubei Province, South China, but the taxonomy and diversity of the co-occurring brachiopod fauna are still far from clear. Here we describe the brachiopod fauna recovered from the Shipai Formation in the Three Gorges area of South China, including representatives of the subphylum Linguliformea: linguloids (Lingulellotreta ergalievi, Eoobolus malongensis, and Neobolidae gen. indet. sp. indet.), and an acrotretoid (Linnarssonia sapushanensis); and representatives from the subphylum Rhynchonelliformea: the calcareous-shelled Kutorginates (Kutorgina sinensis, Kutorgina sp., and Nisusia liantuoensis). This brachiopod assemblage and the first occurrence of Linnarssonia sapushanensis shell beds permit correlation of the Shipai Formation in the Three Gorges area of Hubei Province with the Stage 4 Wulongqing Formation in the Wuding area of eastern Yunnan. This correlation is further strengthened by the first appearance datum (FAD) of the rhynchonelliform brachiopod Nisusia in the upper silty mudstone of both the Shipai and Wulongqing formations. The new well-preserved material, derived from siliciclastic rocks, also gives critical new insights into the fine shell structure of L. sapushanensis. Microstructural studies on micromorphic acrotretoids (like Linnarssonia) have previously been restricted to fossils that were acid-etched from limestones. This is the first study to carry out detailed comparative ultrastructural studies on acrotretoid shells preserved in siliciclastic rocks. This work reveals a hollow tube and solid column microstructure in the acrotretoid shells from the Shipai Formation, which is likely to be equivalent of traditional column and central canal observed in shells dissolved from limestones.
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.117
      Issue No: Vol. 95, No. 3 (2021)
       
  • Lower Famennian (Upper Devonian) rhynchonellide and athyride brachiopods
           from the South Armenian Block
    • Authors: Vahram Serobyan; Taniel Danelian, Catherine Crônier, Araik Grigoryan, Bernard Mottequin
      Pages: 527 - 552
      Abstract: The lower Famennian ‘Cyrtospirifer’ orbelianus brachiopod Zone established in Armenia by Abrahamyan (1957) (coeval to the crepida conodont Zone) contains an abundant and diverse brachiopod fauna that still remains poorly studied. In an effort to revise and update its systematic classification and to assess the brachiopod diversity in this area after the Kellwasser extinction event at the end of the Frasnian, our attention is here focused on rhynchonellides and athyrides. Six rhynchonellide species are described belonging to five genera as well as a single athyride species (Crinisarina pseudoglobularis n. sp.), which is new to science. The genus Crinisarina is reported for the first time in the South Armenian Block (SAB), which was then part of the northern margin of Gondwana. Some of the rhynchonellides identified were previously recognized in this area, but they require modern documentation and taxonomic reassessment. More particularly, it is the first time that the internal structure of Sartenaerus baitalensis (Reed, 1922) is illustrated, taking into account that it is the type species of a biostratigraphically significant Famennian genus. One of the oldest punctate rhynchonellide species, Greira transcaucasica Erlanger, 1993, is described for the first time from Armenia and its intraspecific morphological variability is documented quantitatively. From a paleobiogeographic viewpoint, the studied brachiopod fauna clearly shares affinities with contemporaneous ones from other regions of the Gondwanan northern margin that extend eastwards of the SAB to Afghanistan and Pamir, although there are also some endemic elements.UUID: http://zoobank.org/798eb5f9-ad15-4d90-bc6a-ff22ee936438
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.114
      Issue No: Vol. 95, No. 3 (2021)
       
  • Brachial supporting structure of Spiriferida (Brachiopoda)
    • Authors: Zhiwei Yuan; Wen Guo, Dan Lyu, Yuanlin Sun
      Pages: 553 - 567
      Abstract: The filter-feeding organ of some extinct brachiopods is supported by a skeletal apparatus called the brachidium. Although relatively well studied in Atrypida and Athyridida, the brachidial morphology is usually neglected in Spiriferida. To investigate the variations of brachidial morphology in Spiriferida, 65 species belonging to eight superfamilies were analyzed. Based on the presence/absence of the jugal processes and normal/modified primary lamellae of the spiralia, four types of brachidium are recognized. Type-I (with jugal processes) and Type-II (without jugal processes), both having normal primary lamellae, could give rise to each other by losing/re-evolving the jugal processes. Type-III, without jugal processes, originated from Type-II through evolution of the modified lateral-convex primary lamellae, and it subsequently gave rise to Type-IV by evolving the modified medial-convex primary lamellae. The evolution of brachidia within individual evolutionary lineages must be clarified because two or more types can be present within a single family. Type-III and Type-IV are closely associated with the prolongation of the crura, representing innovative modifications of the feeding apparatus in response to possible shift in the position of the mouth towards the anterior, allowing for more efficient feeding on particles entering the mantle cavity from the anterior gape. Meanwhile, the modified primary lamellae adjusted/regulated the feeding currents. The absence of spires in some taxa with Type-IV brachidium might suggest that they developed a similar lophophore to that in some extant brachiopods, which can extend out of the shell.
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.106
      Issue No: Vol. 95, No. 3 (2021)
       
  • Three new cribrimorph bryozoans (order Cheilostomatida) from the early
           Miocene of Argentina, with a discussion on spinocystal shield morphologies
           
    • Authors: Juan López-Gappa; Leandro M. Pérez, Ana C.S. Almeida, Débora Iturra, Dennis P. Gordon, Leandro M. Vieira
      Pages: 568 - 582
      Abstract: Bryozoans with calcified frontal shields formed by the fusion of costae, collectively constituting a spinocyst, are traditionally assigned to the family Cribrilinidae. Today, this family is regarded as nonmonophyletic. In the Argentine Cenozoic, cribrilinids were until recently represented by only two fossil species from the Paleocene of Patagonia. This study describes the first fossil representatives of Jolietina and Parafigularia: J. victoria n. sp. and P. pigafettai n. sp., respectively. A fossil species of Figularia, F. elcanoi n. sp., is also described. The material comes from the early Miocene of the Monte León and Chenque formations (Patagonia, Argentina). For comparison, we also provide redescriptions of the remaining extant species of Jolietina: J. latimarginata (Busk, 1884) and J. pulchra Canu and Bassler, 1928a. The systematic position of some species previously assigned to Figularia is here discussed. Costafigularia n. gen. is erected, with Figularia pulcherrima Tilbrook, Hayward, and Gordon, 2001 as type species. Two species previously assigned to Figularia are here transferred to Costafigularia, resulting in C. jucunda n. comb. and C. tahitiensis n. comb. One species of Figularia is reassigned to Vitrimurella, resulting in V. ampla n. comb. The family Vitrimurellidae is here reassigned to the superfamily Cribrilinoidea. The subgenus Juxtacribrilina is elevated to genus rank. Inferusia is regarded as a subjective synonym of Parafigularia. Parafigularia darwini Moyano, 2011 is synonymized with I. taylori Kuklinski and Barnes, 2009, resulting in Parafigularia taylori n. comb. Morphological data suggest that these genera comprise different lineages, and a discussion on the disparities among cribrilinid (sensu lato) spinocysts is provided.UUID: http://zoobank.org/215957d3-064b-47e2-9090-d0309f6c9cd8
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.108
      Issue No: Vol. 95, No. 3 (2021)
       
  • Oriostoma+(Gastropoda)+with+an+in+situ+operculum+from+the+Silurian+of+Indiana&rft.title=Journal+of+Paleontology&rft.issn=0022-3360&rft.date=2021&rft.volume=95&rft.spage=583&rft.epage=585&rft.aulast=Rohr&rft.aufirst=David&rft.au=David+M.+Rohr&rft.au=Gregory+P.+Wahlman&rft_id=info:doi/10.1017/jpa.2020.103">Oriostoma (Gastropoda) with an in situ operculum from the Silurian of
           Indiana
    • Authors: David M. Rohr; Gregory P. Wahlman
      Pages: 583 - 585
      Abstract: A single specimen of Oriostoma globosum (von Schlotheim, 1820) from the Silurian-age (Wenlockian) Laurel Limestone in southeastern Indiana preserves a partial, multispiral operculum in situ within the aperture. Only eight specimens of in situ Oriostoma opercula have previously been illustrated from Canada and Europe, and this is the first from the United States. Oriostoma huntingtonensis Kindle, 1904, from younger Silurian (Ludlovian–Pridolian) strata in northern Indiana is considered a synonym of the more widespread O. globosum, and it was described as having associated loose multispiral calcareous opercula in the same strata.
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.103
      Issue No: Vol. 95, No. 3 (2021)
       
  • Permian millipedes from the Fort Sill fissures of southwestern Oklahoma,
           with comments on allied taxa and millipedes preserved in karstic
           environments
    • Authors: Joseph T. Hannibal; William J. May
      Pages: 586 - 600
      Abstract: Permian millipedes are rare, especially so considering the relative abundance of millipedes in Carboniferous rocks. We report an early Permian millipede fauna containing three new genera and species of millipedes (Oklahomasoma richardsspurense new genus new species, Karstiulus fortsillensis new genus new species, and Dolesea subtila new genus new species) found in fossil-producing pockets of the Fort Sill fissures exposed in the Dolese Quarry near Richards Spur, southwest Oklahoma, USA. These are the first new genera of invertebrates to be described from this site, one of the most prolific fossil-vertebrate sites in the world. We also comment on taxa with morphological similarities and note previously described occurrences of Permian millipedes as well as occurrences of fossil myriapods (millipedes and centipedes) in karst deposits (caves and fissure fills) in Europe, Africa, Asia, North America, and the Caribbean. In contrast with the forms found at Richards Spur, most of these previous accounts of millipedes found in caves and fissure fills are of Pleistocene forms that are closely allied to modern taxa. The taxa from Richards Spur bear some similarities to Pennsylvanian forms. Karst (cave and fissure) faunas should be ranked with concretion faunas, cannel coals, and amber faunas as a major source of fossil myriapods.UUID: http://zoobank.org/5d58e1fb-4e5b-4597-9cd9-5cc9e2096b4d
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.100
      Issue No: Vol. 95, No. 3 (2021)
       
  • A new, giant ricinuleid (Arachnida, Ricinulei), from the Pennsylvanian of
           Illinois, and the identification of a new, ontogenetically stable,
           diagnostic character
    • Authors: Niall Whalen; Paul Selden
      Pages: 601 - 612
      Abstract: A new fossil ricinuleid, Curculioides bohemondi n. sp., from the Pennsylvanian Energy Shale of Illinois is described from a single specimen. It is the largest ricinuleid species yet described, living or extinct. The Energy Shale represents a new geographic locale for fossil ricinuleids, a sparsely distributed group. The species is distinguished from other members within the genus by the possession of very large (0.09 mm) carapace tubercles at a very low (30 mm-2) density. Statistical analyses are performed on extant and fossil ricinuleids to determine how their tubercles change throughout ontogeny, culminating in the recovery of a new ontogenetically stable diagnostic character: the tubercle coefficient (a measure of the size of the tubercles relative to body size).UUID: http://zoobank.org/aa9f2de5-c49d-4f70-bba5-db12fdee406f.
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.104
      Issue No: Vol. 95, No. 3 (2021)
       
  • Phylogeny and biogeography of some Cretaceous spatangoid echinoids with
           special emphasis on taxa from the Western Interior Seaway
    • Authors: Steven Byrum; Bruce S. Lieberman
      Pages: 613 - 623
      Abstract: Members of the echinoid order Spatangoida, a highly diverse and abundant marine invertebrate clade, were important denizens of the Cretaceous Western Interior Seaway (WIS), an epicontinental seaway that divided North America in two during an interval of greenhouse conditions between roughly 100 and 65 million years ago. A phylogenetic analysis of spatangoids was conducted using a character matrix of 32 characters from 21 species. Species that occur in the WIS were considered comprehensively, and species from other regions such as South America, Europe, and North Africa were also incorporated into the analysis. Phylogenetic patterns retrieved are largely congruent with preexisting family-level classifications; however, species within several genera, especially Hemiaster and Heteraster, need to be reassigned so that classification better reflects phylogeny. The genera Washitaster and Heteraster are closely related, as are Mecaster, Palhemiaster, and Proraster; Pliotoxaster, Macraster, and Hemiaster; and Micraster and Diplodetus. Biogeographic patterns were also considered using the phylogeny, and several episodes of vicariance and range expansion were identified. These were possibly related to some of the various major episodes of sea-level rise and fall during the Cretaceous. In particular, Valangian–mid-Aptian regressions may have caused vicariance within Heteraster and Washitaster while other early spatangoid vicariance may be related to regressions during the late Aptian–early Cenomanian. Further, vicariance caused by regressions during the mid-Cenomanian–Maastrichtian may have driven diversification within Micraster and Diplodetus. Last, transgressions during the late Aptian–early Cenomanian seem to have spurred prominent range expansions in Mecaster and Hemiaster.
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.102
      Issue No: Vol. 95, No. 3 (2021)
       
  • Spiracarneyella,+a+new+carneyellid+edrioasteroid+from+the+Upper+Ordovician+(Katian)+of+Kentucky+and+Ohio+and+comments+on+carneyellid+heterochrony&rft.title=Journal+of+Paleontology&rft.issn=0022-3360&rft.date=2021&rft.volume=95&rft.spage=624&rft.epage=629&rft.aulast=Sumrall&rft.aufirst=Colin&rft.au=Colin+D.+Sumrall&rft.au=Daniel+Phelps&rft_id=info:doi/10.1017/jpa.2020.97">Spiracarneyella, a new carneyellid edrioasteroid from the Upper Ordovician
           (Katian) of Kentucky and Ohio and comments on carneyellid heterochrony
    • Authors: Colin D. Sumrall; Daniel Phelps
      Pages: 624 - 629
      Abstract: A new genus and species of carneyellid edrioasteroid, Spiracarneyella florencei n. gen. n. sp., is described from the Upper Ordovician (Kaitian) Point Pleasant Formation of northern Kentucky and southern Ohio. Spiracarneyella n. gen. is characterized by having all five ambulacra curving clockwise around the theca, having small node-bearing interambulacral plates in the distal interambulacra, and having the periproct placement slightly offset to the right side of the CD interambulacrum. The oral area of carneyellids evolved by paedomorphosis of the oral plates covering the mouth. The straight ambulacra of Cryptogoleus and the spiraling ambulacra of Spiracarneyella n. gen. evolved by paedomorphosis and peramorphosis, respectively.UUID: http://zoobank.org/79733c8f-0bc8-4e7e-8f77-8508f576755c
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.97
      Issue No: Vol. 95, No. 3 (2021)
       
  • A new cobia (Teleostei, Rachycentridae) species from the Miocene St. Marys
           Formation along Calvert Cliffs, Maryland, USA
    • Authors: Stephen J. Godfrey; Giorgio Carnevale
      Pages: 630 - 637
      Abstract: The highly fossiliferous St. Marys Formation is exposed along Calvert Cliffs, Maryland, and comprises one of the best available records of late Miocene life in the northeastern United States. Rachycentron stremphaencus new species, a cobia from the late Miocene (Tortonian) of the St. Marys Formation is described herein on the basis of a single three-dimensional neurocranium. This fossil represents the earliest known occurrence of neurocranial remains of the genus Rachycentron in the record. Rachycentron stremphaencus differs from Rachycentron canadum (Linnaeus, 1766) in many ways. The most obvious include a different ornamentation of the outer surface of the cranial bones; a notably pronounced lateral ridge resulting in a considerable gradient from the dorsal-medial exposure of the frontal to its lateralmost supraorbital margin; the size, shape, and position of the sphenotic that is located in the posterior half of the neurocranium and its lateralmost edge being adjacent to the anteriormost extent of the wedge-shaped trough in the dorsal surface of the skull formed by the lateral and medial ridges; the two contralateral medial ridges forming a proportionately much wider trough on either side of the supraoccipital; the epioccipitals not reaching the rear edge of the neurocranium; and the lack of a conspicuous posterolateral prong of the intercalar.UUID: http://zoobank.org/c8523bb4-2de2-4318-9a37-027f463a0441
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.107
      Issue No: Vol. 95, No. 3 (2021)
       
  • A new dissorophoid temnospondyl from the Allegheny Group (late
           Carboniferous) of Five Points, Mahoning County, Ohio (USA)
    • Authors: Rainer R. Schoch; Amy C. Henrici, Robert W. Hook
      Pages: 638 - 651
      Abstract: A small temnospondyl skull from the upper Carboniferous Allegheny Group of Five Points, Ohio, is referred to a new dissorophoid, Palodromeus bairdi n. gen n. sp. The complete skull with mandibles is preserved in counterparts. It is characterized by, (1) elongated slit-like choana; (2) postfrontal, postorbital, and supratemporal bearing a distinct ridge; and (3) reduced parietal only two-thirds the length of the frontal. Phylogenetic analysis confirms a dichotomy between amphibamiforms and olsoniforms and places Palodromeus bairdi n. gen. n. sp. at the base of the olsoniforms, revealing an early stage in the evolution of that clade.UUID: http://zoobank.org/3871e443-7888-4439-a7c1-9463bc4d87ab
      PubDate: 2021-05-01T00:00:00.000Z
      DOI: 10.1017/jpa.2020.101
      Issue No: Vol. 95, No. 3 (2021)
       
 
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