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Preliminary Survey on the Tetori Group in Southern Ishikawa, Japan 石川
石川県立自然史資料館研究報告 第3号 Bulletin of the Ishikawa Museum of Natural History, 3: 49-62 (2013) Preliminary survey on the Tetori Group in southern Ishikawa, Japan Yoshihiro KATSURA 石川県南部に分布する手取層群に対する予備調査 桂嘉志浩 Abstract The Lower Cretaceous Itoshiro and overlying Akaiwa subgroups of the Tetori Group are distributed in the Shiramine Area of Hakusan City, Ishikawa Prefecture, Japan. The Kuwajima Formation, the upper division of the lower subgroup, is considered to have been deposited under lacustrine and associated alluvial environments. It has yielded a reasonable number of vertebrate remains that are small, allochthonous, and mostly disarticulated. The Akaiwa Formation, the lower division of the upper subgroup, is suggested to have been formed by fluvial systems with strong currents and rapid deposition. Except for plant fragments, fossils are uncommon. Vertebrates, including dinosaurs, occur in the Kitadani Formation, the upper division of the upper subgroup, in northeastern Fukui Prefecture, and this formation crops out in the Shiramine Area. Therefore, there is a chance that articulated large vertebrate fossils are preserved in the subgroups exposed in the area. However, the indurated nature of the rocks, precipitous topology, thick vegetation cover, and overall poor exposures represent significant challenges to making such a discovery. Further, based on the taphonomy of the observed vertebrates, finding well-preserved large vertebrates in the area will be difficult and require much time and financial support. Organizing a survey group of trained -
A Neoceratopsian Dinosaur from the Early Cretaceous of Mongolia And
ARTICLE https://doi.org/10.1038/s42003-020-01222-7 OPEN A neoceratopsian dinosaur from the early Cretaceous of Mongolia and the early evolution of ceratopsia ✉ Congyu Yu 1 , Albert Prieto-Marquez2, Tsogtbaatar Chinzorig 3,4, Zorigt Badamkhatan4,5 & Mark Norell1 1234567890():,; Ceratopsia is a diverse dinosaur clade from the Middle Jurassic to Late Cretaceous with early diversification in East Asia. However, the phylogeny of basal ceratopsians remains unclear. Here we report a new basal neoceratopsian dinosaur Beg tse based on a partial skull from Baruunbayan, Ömnögovi aimag, Mongolia. Beg is diagnosed by a unique combination of primitive and derived characters including a primitively deep premaxilla with four pre- maxillary teeth, a trapezoidal antorbital fossa with a poorly delineated anterior margin, very short dentary with an expanded and shallow groove on lateral surface, the derived presence of a robust jugal having a foramen on its anteromedial surface, and five equally spaced tubercles on the lateral ridge of the surangular. This is to our knowledge the earliest known occurrence of basal neoceratopsian in Mongolia, where this group was previously only known from Late Cretaceous strata. Phylogenetic analysis indicates that it is sister to all other neoceratopsian dinosaurs. 1 Division of Vertebrate Paleontology, American Museum of Natural History, New York 10024, USA. 2 Institut Català de Paleontologia Miquel Crusafont, ICTA-ICP, Edifici Z, c/de les Columnes s/n Campus de la Universitat Autònoma de Barcelona, 08193 Cerdanyola del Vallès Sabadell, Barcelona, Spain. 3 Department of Biological Sciences, North Carolina State University, Raleigh, NC 27695, USA. 4 Institute of Paleontology, Mongolian Academy of Sciences, ✉ Ulaanbaatar 15160, Mongolia. -
Papers in Press
Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2018PR013 Features and paleoecological significance of the shark fauna from the Upper Cretaceous Hinoshima Formation, Himenoura Group, Southwest Japan Accepted Naoshi Kitamura 4-8-7 Motoyama, Chuo-ku Kumamoto, Kumamoto 860-0821, Japan (e-mail: [email protected]) Abstract. The shark fauna of the Upper Cretaceous Hinoshima Formation (Santonian: 86.3–83.6 Ma) of the manuscriptHimenoura Group (Kamiamakusa, Kumamoto Prefecture, Kyushu, Japan) was investigated based on fossil shark teeth found at five localities: Himedo Park, Kugushima, Wadanohana, Higashiura, and Kotorigoe. A detailed geological survey and taxonomic analysis was undertaken, and the habitat, depositional environment, and associated mollusks of each locality were considered in the context of previous studies. Twenty-one species, 15 genera, 11 families, and 6 orders of fossil sharks are recognized from the localities. This assemblage is more diverse than has previously been reported for Japan, and Lamniformes and Hexanchiformes were abundant. Three categories of shark fauna are recognized: a coastal region (Himedo Park; probably a breeding site), the coast to the open sea (Kugushima and Wadanohana), and bottom-dwelling or near-seafloor fauna (Kugushima, Wadanohana, Higashiura, and Kotorigoe). -
A New Assemblage of Plant Mesofossils (Late Turonian– Middle Santonian; Upper Cretaceous) from the Tamagawa Formation, Kuji Group, in Northeastern Japan
120Paleontological Research, vol. 25, no. 2, pp. 120–126, MasamichiApril 1, 2021 Takahashi et al. © by the Palaeontological Society of Japan doi:10.2517/2020PR015 A new assemblage of plant mesofossils (late Turonian– middle Santonian; Upper Cretaceous) from the Tamagawa Formation, Kuji Group, in northeastern Japan MASAMICHI TAKAHASHI1, PATRICK S. HERENDEEN2, FABIANY HERRERA2, REN HIRAYAMA3, HISAO ANDO4, KAZUHISA SASAKI5 and PETER R. CRANE6,7 1Department of Environmental Sciences, Niigata University, 8050, 2-cho, Ikarashi, Nishi-ku, Niigata 950-2181, Japan (e-mail: [email protected]) 2Chicago Botanic Garden, 1000 Lake Cook Road, Glencoe, Illinois 60022, USA 3School of International Liberal Studies, Waseda University, 1-7-14, Nishiwaseda, Shinjuku-ku, Tokyo 169-0051, Japan 4Department of Earth Sciences, Faculty of Science, Ibaraki University, 2-1-1, Bunkyo, Mito 310-8512, Japan 5Kuji Amber Museum, 19-156-133, Kokujicho, Kuji, Iwate 028-0071, Japan 6Yale School of the Environment, Yale University, 195, Prospect Street, New Haven, Connecticut 06511, USA 7Oak Spring Garden Foundation, 1776, Loughborough Lane, Upperville, Virginia 20184, USA Received November 14, 2019; Revised manuscript accepted March 4, 2020 Abstract. A preliminary description is provided of a new assemblage of small, three-dimensional and char- coalified mesofossils from the Tamagawa Formation (late Turonian–middle Santonian; Upper Cretaceous) of the Kuji Group in northeastern Japan. The new mesofossils yield excellent structural details and include well- preserved circinate shoots of ferns together with conifer leafy-shoots, seeds and probable pollen cones, and vari- ety of angiosperm fruits and seeds, including fruits of Cornales and seeds of Nymphaeales. The new mesofossil assemblage is complementary to the previously published macrofossil flora from the Kuji Group. -
Titanosauriform Teeth from the Cretaceous of Japan
“main” — 2011/2/10 — 15:59 — page 247 — #1 Anais da Academia Brasileira de Ciências (2011) 83(1): 247-265 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 www.scielo.br/aabc Titanosauriform teeth from the Cretaceous of Japan HARUO SAEGUSA1 and YUKIMITSU TOMIDA2 1Museum of Nature and Human Activities, Hyogo, Yayoigaoka 6, Sanda, 669-1546, Japan 2National Museum of Nature and Science, 3-23-1 Hyakunin-cho, Shinjuku-ku, Tokyo 169-0073, Japan Manuscript received on October 25, 2010; accepted for publication on January 7, 2011 ABSTRACT Sauropod teeth from six localities in Japan were reexamined. Basal titanosauriforms were present in Japan during the Early Cretaceous before Aptian, and there is the possibility that the Brachiosauridae may have been included. Basal titanosauriforms with peg-like teeth were present during the “mid” Cretaceous, while the Titanosauria with peg-like teeth was present during the middle of Late Cretaceous. Recent excavations of Cretaceous sauropods in Asia showed that multiple lineages of sauropods lived throughout the Cretaceous in Asia. Japanese fossil records of sauropods are conformable with this hypothesis. Key words: Sauropod, Titanosauriforms, tooth, Cretaceous, Japan. INTRODUCTION humerus from the Upper Cretaceous Miyako Group at Moshi, Iwaizumi Town, Iwate Pref. (Hasegawa et al. Although more than twenty four dinosaur fossil local- 1991), all other localities provided fossil teeth (Tomida ities have been known in Japan (Azuma and Tomida et al. 2001, Tomida and Tsumura 2006, Saegusa et al. 1998, Kobayashi et al. 2006, Saegusa et al. 2008, Ohara 2008, Azuma and Shibata 2010). -
Deep Sea Drilling Project Initial Reports Volume 6
39. PLANKTONIC MICROFOSSIL BIOSTRATIGRAPHY OF THE NORTHWESTERN PACIFIC OCEAN David Bukry1, U.S. Geological Survey, La Jolla, California, Robert G. Douglas, Case Western Reserve University, Cleveland, Ohio, Stanley A. Kling, Cities Service Oil Company, Tulsa, Oklahoma, and Valeri Krasheninnikov, Academy of Sciences of the U.S.S.R., Moscow CONTENTS Page Page Introduction 1253 Regional Correlation 1281 Zonal Comparison 1254 Calcareous Nannoplankton 1281 Planktonic Foraminifera, Mesozoic 1281 Upper Cretaceous-Paleocene Boundary 1255 California 1281 Paleocene-Eocene Boundary 1259 Japan 1285 Eocene-Oligocene Boundary 1259 West Pacific 1286 Oligocene-Miocene Boundary 1259 Australia 1287 Miocene-Pliocene Boundary 1260 Planktonic Foraminifera, Cenozoic 1288 Pliocene-Pleistocene Boundary 1261 Solomon Islands 1288 Zonal Summary 1261 Mariana Islands 1288 The Philippines 1288 Paleoecology 1261 Taiwan 1289 Calcareous Nannoplankton 1261 Japan 1289 Radiolaria 1267 Kamchatka Penisula 1290 California 1290 Preservation 1267 Radiolaria 1291 Calcareous Nannoplankton 1267 Sedimentation Rates 1291 Foraminifera 1269 Relationship to Acoustostratigraphy 1294 Radiolaria 1279 References 1296 INTRODUCTION A comparison of zonal units of calcareous nannoplank- ton, foraminifera, and radiolarians in the same strata Biostratigraphic evidence obtained from the north- shows only few cases of exact coincidence of zonal western Pacific Ocean as a result of coring carried out limits, especially if coincidences at the top or bottom by the Glomar Challenger during Leg 6 of the Deep of the standard 9-meter coring runs are dismissed as Sea Drilling Project from Hawaii to Guam is considered artificially induced owing to gaps in sediment recovery. here mainly from the standpoint of three dominant Exact coincidence of zonal limits within coring runs marine planktonic microfossil groups—calcareous nan- are most notable for the Upper Paleocene sediment of noplankton, foraminifers, and radiolarians. -
2A Palaeozoic Basement and Associated Cover
Palaeozoic basement 2a and associated cover MASAYUKI EHIRO (COORDINATOR), TATSUKI TSUJIMORI, KAZUHIRO TSUKADA & MANCHUK NURAMKHAAN Pre-Cenozoic rocks of the Japanese islands are largely composed of Complex is separated by a mylonite zone from Barrovian-type, latest Palaeozoic to Cretaceous accretionary complexes and Creta- medium-pressure, pelitic schists (‘Unazuki Schist’) which crop out ceous granitic intrusives. Exposures of older rocks are restricted to as a north–south-aligned elongated, narrow subunit 2–3 km wide a limited number of narrow terranes, notably the Hida, Oeyama and 17 km long (e.g. Kano 1990; Takagi & Hara 1994). Another and Hida Gaien belts (Inner Zone of SW Japan), the Kurosegawa important tectonic boundary within the Hida Belt is the ‘Funatsu Belt (Outer Zone of SW Japan) and the South Kitakami Belt Shear Zone’, which comprises dextrally sheared, mostly metagrani- (NE Japan). In these belts, early Palaeozoic basement rocks are toid mylonitic rocks (Komatsu et al. 1993). typically overlain by a cover of middle Palaeozoic to Mesozoic The presence in the Hida Gneiss Complex of high-aluminous shelf facies strata. This chapter describes these basement inliers metapelites, metamorphosed acidic volcanic rocks and abundant and their cover, grouping them under four subheadings: Hida, impure siliceous marble associated with orthogneiss suggest a Oeyama, Hida Gaien and South Kitakami/Kurosegawa belts. passive-margin lithology for the protoliths, probably as continental Although opinions are varied among authors whether the Unazuki shelf sediments and basement rock on a rifted continental margin Schist should be placed in the Hida Belt (TT) or in the Hida Gaien (e.g. Sohma & Kunugiza 1993; Isozaki 1996, 1997; Wakita 2013). -
Aspects of the Microvertebrate Fauna of the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, Southern England
ASPECTS OF THE MICROVERTEBRATE FAUNA OF THE EARLY CRETACEOUS (BARREMIAN) WESSEX FORMATION OF THE ISLE OF WIGHT, SOUTHERN ENGLAND By STEVEN CHARLES SWEETMAN M.A. (Oxon.) 1980 F.G.S. A thesis submitted in partial fulfilment of the requirements for the award of the degree of Doctor of Philosophy of the University of Portsmouth School of Earth and Environmental Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, Portsmouth, PO1 3QL, U.K. April, 2007 0 Disclaimer Whilst registered for this degree, I have not registered for any other award. No part of this work has been submitted for any other academic award. 1 Acknowledgements At inception of this project there was a significant risk that the Wessex Formation would not yield a microvertebrate fauna. I would, therefore, like to express special thanks to Dave Martill (University of Portsmouth) for his initial support and for securing the research scholarship which made this study possible. I would also like to thank him for his supervision, generous support, encouragement and advice thereafter. Special thanks also to Susan Evans (UCL) for her enthusiastic help and advice on all matters relating to microvertebrates in general, and lizards in particular, and to Jerry Hooker (NHM) for everything relating to mammals; also to Brian Gasson for his support in the field and for the generous donation of many exceptional specimens from his private collection. The broad scope of this study has engendered the help, support and advice of many others and I am grateful to all. At the University -
Palaeontological Society of Japan
Transactions and Proceedings of the Palaeontological Society of Japan New Series No. 77 Palaeontological Society of Japan April lOth, 1970 Editor: Tokio SHIKAMA Associate Editor: Kiyotaka CHINZEI Officers for 1969-1970 President: Fuyuji T AKAI Councillors (*Executives): Kiyoshi ASANO*, Tetsuro HANAI* (Secretary), Kotora HATAI, Itaru HAYAMI, Koichiro ICHIKAWA, Taro KANAYA, Kametoshi KAN MERA, Teiichi KOBAYASHI, Kenji KO NISHI, Tamio KOTAKA, Tatsuro MATSU MOTO*, Masao MrNATO, Hiroshi OZAKI* (Treasurer), Tokio SHIKAMA*, Fuyuji TAKA!* Executive Committee (Chairman: Fuyuji T AKAI) General Affairs: Tetsuro HANAI, Takashi HAMADA, Yasuhide IwASAKI Membership: Takashi HAMADA Finance: Hiroshi OzAKI, Saburo KANNO Planning: Hiroshi OZAKI, Hiroshi UJUE Publications Transactions: Tokio SHIKAMA, Kiyotaka CHINZEI Special Papers: Tatsuro MATSUMOTO, Tomowo OZAWA "Fossils": Kiyoshi ASANO, Yokichi TAKA YANAGI Fossils on the cover is Globorotalia truncatulinoides (D '0RBIGNY, 1839). The photograph was taken on a scanning electron microscope, JEOL-JSM-2, x 100. All communications relating to this journal should be addressed to the PALAEONTOLOGICAL SOCIETY OF JAPAN Geological Institute, Faculty of Science, University of Tokyo, Tokyo 113, Japan Sole agent: University of Tokyo Press Trans. Proc. Palaeont. Soc. Japan, N. S., No. 77, pp. 205-228, pl. 23, April 10, 1970 561. A MIOCENE MOLLUSCAN FAUNA IN THE PHILIPPINES Y ASUHIDE IWASAKI Department of Geology, University Museum, University of Tokyo 71 !I -:;l:::':,-~f.Jlb~O)I=j:l~Ji'i!t~1t.fi"Wf: 1966~fnllfi!i::.Jv'/ :,-lfb Tayabas !tk!KO)!l[\'.i(f\'4 1i!iiDij:J!l:~fT-:>f.:=*:ftlilt!$ • fRiii.IJPJrjiljj!!;f;J:, f*:ffv;J:.Li!. < t.;:v'i.l;ml: r.d~ili-t Mllifb;~ :Q c ,'(l:l,:b;h, :Q~1t.15r~*~· 2 -7FJftP;J:.U~Lt1f'011!l--:>f.:. -
Orthotropous to Hemi‐Anatropous Angiosperm Seeds from the Early Cretaceou
RESEARCH ARTICLE INVITED SPECIAL ARTICLE For the Special Issue: The Tree of Death: The Role of Fossils in Resolving the Overall Pattern of Plant Phylogeny Tanispermum, a new genus of hemi- orthotropous to hemi- anatropous angiosperm seeds from the Early Cretaceous of eastern North America Else Marie Friis1,5, Peter R. Crane2,3, and Kaj Raunsgaard Pedersen4 Manuscript received 29 November 2017; revision accepted 21 May PREMISE OF THE STUDY: Exotestal seeds with characters that indicate relationship to 2018. extant Austrobaileyales and Nymphaeales are abundant in Early Cretaceous sediments 1 Department of Palaeobiology, Swedish Museum of Natural History, from Portugal and eastern North America, but their variety and unique features provide Box 50007, SE-104 05 Stockholm, Sweden evidence of extensive extinct diversity among early angiosperms. 2 Oak Spring Garden Foundation, 1176 Loughborough Lane, Upperville, VA 20184, USA METHODS: The fossils were extracted from Early Cretaceous sediments from Virginia 3 School of Forestry and Environmental Studies, Yale University, New and Maryland, United States, by sieving in water. After cleaning with HF, HCl and water, Haven, CT 06511, USA they were examined using SEM and SRXTM and compared to seeds of extant and fossil 4 Department of Geoscience, University of Aarhus, Høegh-Guldbergs angiosperms. Gade 2, DK-8000, Aarhus, C Denmark KEY RESULTS: A new genus, Tanispermum gen. nov., with four species (T. hopewellense sp. 5 Author for correspondence (e-mail: [email protected]) nov., T. marylandense sp. nov., T. drewriense sp. nov., and T. antiquum sp. nov.) is recognized. Citation: Friis, E. M., P. R. Crane, and K. -
This Article Appeared in a Journal Published by Elsevier. the Attached
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Cretaceous Research 37 (2012) 319e340 Contents lists available at SciVerse ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes Review paper A review of the Upper Cretaceous marine reptiles from Japan T. Sato a,*, T. Konishi b, R. Hirayama c, M.W. Caldwell d,e a Department of Astronomy and Earth Sciences, Tokyo Gakugei University, Nukui-Kita-Machi 4-1-1, Koganei City, Tokyo 184-8501, Japan b Royal Tyrrell Museum of Palaeontology, PO Box 7500, Drumheller, Alberta T0J 0Y0, Canada c School of International Liberal Studies, Waseda University, Nishiwaseda 1-6-1, Shinjuku-ku, Tokyo 169-8050, Japan d Department of Biological Sciences, University of Alberta, Edmonton, Alberta T6G 2E9, Canada e Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E9, Canada article info abstract Article history: Taxonomy and stratigraphic distribution of the Upper Cretaceous marine reptiles from Japan are Received 10 March 2011 reviewed. -
The Lower Cretaceous Kuwajima Formation, Tetori Group, Japan
Bull. Kitakyushu Mus. Nat. Hist. Hum. Hist., Ser. A, 3: 123-133, March 31, 2005 Depositional environments and taphonomy of the bone-bearing beds of the Lower Cretaceous Kuwajima Formation, Tetori Group, Japan Shinji Isaji1 Hiroko Okazaki1 Ren Hirayama2 Hiroshige Matsuoka3 Paul M. Barrett4 Takehisa Tsubamoto5 Mikiko Yamaguchi6 Ichio Yamaguchi6 Tatsuya Sakumoto6 INatural History Museum and Institute, Chiba, 955-2 Aoba-cho, Chuo-ku, Chiba 260-8682, Japan 2School of International Liberal Studies, Waseda University, 1-17-14 Nishiwaseda Shinjuku-ku, Tokyo 169-0051, Japan 3Department of Geology and Mineralogy, Faculty of Science, Kyoto University, Kitashirakawa-oiwake-cho, Sakyo-ku, Kyoto 606-8224, Japan ^Department of Palaeontology, The Natural History Museum, London, Cromwell Road, London SW 7 5BD, UK 5Primate Research Institute, Kyoto University, Inuyama, Aichi 484-8506, Japan 6Shiramine Institute of Paleontology, 10-1-20 Kuwajima, Hakusan, Ishikawa 920-2502, Japan (Received August 21, 2004; accepted September 12, 2004) ABSTRACT—The bone-bearing beds of the Lower Cretaceous Kuwajima Formation (Tetori Group) are described. Three facies of bone-bearing beds (Facies I: carbonaceous sandstones; Facies II: dark grey fine-grained silty sandstones; Facies III: dark greenish-grey mudstones) are present in inter-channel deposits that originated on a floodplain. The grain size of the sediments, and plant and molluscan fossils occurring in each bone-bearing bed, indicate that Facies I was deposited in a peat marsh, Facies II in a shallow lake, and Facies III in a vegetated swamp. Isolated small bones and teeth are the most abundant vertebrate fossils. Common elements in Facies II are aquatic vertebratessuch as fishes and turtles.