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The Jurassic Fossil Wood Diversity from Western Liaoning, NE China
Jiang et al. Journal of Palaeogeography (2019) 8:1 https://doi.org/10.1186/s42501-018-0018-y Journal of Palaeogeography RESEARCH Open Access The Jurassic fossil wood diversity from western Liaoning, NE China Zi-Kun Jiang1,2, Yong-Dong Wang2,3*, Ning Tian4,5, Ao-Wei Xie2,6, Wu Zhang7, Li-Qin Li2 and Min Huang1 Abstract Western Liaoning is a unique region in China that bears diverse types of Jurassic plants, including leaves, fern rhizomes, and wood, providing significant proxy for vegetation and palaeoenvironment reconstruction of the well-known Yanliao Flora in East Asia. In particular, the silicified wood is very abundant in the fossil Lagerstätte of the Jurassic Tiaojishan Formation in Beipiao, western Liaoning. Previous and recent systematic investigations documented a high diversity of the Jurassic wood assemblages. These assemblages are dominated by conifers, followed by cycads and ginkgoaleans. In total, about 30 species belonging to 21 genera of fossil wood have been recorded so far, which are represented by Cycadopsida, Ginkgopsida, Coniferopsida, and Gymnospermae incertae sedis. The evolutionary implications of several distinctive fossil wood taxa as well as palaeoclimate implications are summarized based on their anatomical structures and growth ring patterns. This work approaches the vegetation development and evolutionary significances of the wood taxa and their relatives, and provides clues for the further understanding of the diversity of the Jurassic Yanliao Flora in East Asia. Keywords: Fossil wood, Diversity, Evolution, Tiaojishan Formation, Jurassic 1 Introduction 2004;Wangetal.,2009). Among these localities, western Fossil floras are a significant record for the vegetation Liaoning is a well-known fossil Lagerstätte with diverse and for the palaeoenvironment reconstructions of the and well-preserved fossil plant foliages and wood (Zhang Mesozoic. -
Anura: Brachycephalidae) Com Base Em Dados Morfológicos
Pós-graduação em Biologia Animal Laboratório de Anatomia Comparada de Vertebrados Departamento de Ciências Fisiológicas Instituto de Ciências Biológicas da Universidade de Brasília Sistemática filogenética do gênero Brachycephalus Fitzinger, 1826 (Anura: Brachycephalidae) com base em dados morfológicos Tese apresentada ao Programa de pós-graduação em Biologia Animal para a obtenção do título de doutor em Biologia Animal Leandro Ambrósio Campos Orientador: Antonio Sebben Co-orientador: Helio Ricardo da Silva Maio de 2011 Universidade de Brasília Instituto de Ciências Biológicas Programa de Pós-graduação em Biologia Animal TESE DE DOUTORADO LEANDRO AMBRÓSIO CAMPOS Título: “Sistemática filogenética do gêneroBrachycephalus Fitzinger, 1826 (Anura: Brachycephalidae) com base em dados morfológicos.” Comissão Examinadora: Prof. Dr. Antonio Sebben Presidente / Orientador UnB Prof. Dr. José Peres Pombal Jr. Prof. Dr. Lílian Gimenes Giugliano Membro Titular Externo não Vinculado ao Programa Membro Titular Interno Vinculado ao Programa Museu Nacional - UFRJ UnB Prof. Dr. Cristiano de Campos Nogueira Prof. Dr. Rosana Tidon Membro Titular Interno Vinculado ao Programa Membro Titular Interno Vinculado ao Programa UnB UnB Brasília, 30 de maio de 2011 Dedico esse trabalho à minha mãe Corina e aos meus irmãos Flávio, Luciano e Eliane i Agradecimentos Ao Prof. Dr. Antônio Sebben, pela orientação, dedicação, paciência e companheirismo ao longo do trabalho. Ao Prof. Dr. Helio Ricardo da Silva pela orientação, companheirismo e pelo auxílio imprescindível nas expedições de campo. Aos professores Carlos Alberto Schwartz, Elizabeth Ferroni Schwartz, Mácia Renata Mortari e Osmindo Pires Jr. pelos auxílios prestados ao longo do trabalho. Aos técnicos Pedro Ivo Mollina Pelicano, Washington José de Oliveira e Valter Cézar Fernandes Silveira pelo companheirismo e auxílio ao longo do trabalho. -
Dinosaur Tracks from the Early Cretaceous (Albian) of Parede (Cascais, Portugal): New Contributions for the Sauropod Palaeobiology of the Iberian Peninsula
Journal of Iberian Geology 41 (1) 2015: 155-166 http://dx.doi.org/10.5209/rev_JIGE.2015.v41.n1.48662 www.ucm.es /info/estratig/journal.htm ISSN (print): 1698-6180. ISSN (online): 1886-7995 Dinosaur tracks from the Early Cretaceous (Albian) of Parede (Cascais, Portugal): new contributions for the sauropod palaeobiology of the Iberian Peninsula V.F. Santos1,2*, P.M. Callapez2,3, D. Castanera4, F. Barroso-Barcenilla5,6, N.P.C. Rodrigues1, C.A. Cupeto7 1Museu Nacional de História Natural e da Ciência, Rua da Escola Politécnica 58, 1250-102 Lisboa, Portugal 2Centro de Investigação da Terra e do Espaço da UC – CITEUC, Avenida Dr. Dias da Silva, 3000-134 Coimbra, Portugal 3Departamento de Ciências da Terra da Universidade de Coimbra, Largo Marquês de Pombal, 3001-401 Coimbra, Portugal 4Grupo Aragosaurus-IUCA, Paleontología, Facultad de Ciencias, Universidad de Zaragoza, Calle Pedro Cerbuna 12, 50009 Zaragoza, Spain 5Departamento de Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, 28040 Madrid, Spain 6Grupo de Investigación IberCreta, Universidad de Alcalá de Henares, 28871 Alcalá de Henares, Spain 7Departamento de Geociências da Universidade de Évora, Rua Romão Ramalho 59, 7000-671 Évora, Portugal e-mail addresses: [email protected] (V.F.S., *corresponding author); [email protected] (P.M.C.); [email protected] (D.C.); [email protected] (F.B.B.); [email protected] (N.P.C.R.); [email protected] (C.A.C.) Received: 17 January 2014 / Accepted: 18 December 2014 / Available online: 25 March 2015 Abstract A recently discovered Early Cretaceous (early late Albian) dinosaur tracksite at Parede beach (Cascais, Portugal) reveals evidence of dinoturbation and at least two sauropod trackways. -
Zircon U-Pb SHRIMP Dating of the Yixian Formation in Sihetun, Northeast China
Cretaceous Research 28 (2007) 177e182 www.elsevier.com/locate/CretRes New evidence for Cretaceous age of the feathered dinosaurs of Liaoning: zircon U-Pb SHRIMP dating of the Yixian Formation in Sihetun, northeast China Wei Yang a, Shuguang Li a,*, Baoyu Jiang b a Department of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China b Department of Earth Sciences, Nanjing University, Nanjing 210093, China Accepted 30 May 2006 Available online 25 January 2007 Abstract We present the first report of U-Pb SHRIMP dating of zircons from three tuffs interbedded within the ‘‘feathered dinosaur’’-bearing deposits in western Liaoning, China. One is a sample from the Bed 6 tuff (LX-SHT-12) of the Yixian Formation in Sihetun, for which our zircon U-Pb SHRIMP analyses gave a Cretaceous age (124.7 Æ 2.7 Ma), in agreement with a previously published sanidine 40Ar/39Ar age (124.60 Æ 0.25 Ma). The other two are from the Bed 1 tuff (LX-HBJ-1) and Bed 8 tuff (LX-HBJ-6) of the Yixian Formation in Huangbanjigou; the former gave an age of 124.9 Æ 1.7 Ma, the latter an age of 122.8 Æ 1.6 Ma. The three consistent ages indicate that the Yixian Formation was deposited in the Early Cretaceous within a very short time period (ca. 2 Ma). Ó 2006 Published by Elsevier Ltd. Keywords: Zircon U-Pb SHRIMP dating; Yixian Formation; Feathered dinosaurs; Liaoning; Jehol Biota 1. Introduction still the subject of disagreement. Previously K-Ar and Rb-Sr dat- ing results for the volcanic rocks of the formation have yielded Recently, a wide variety of spectacular fossils, including the Jurassic ages of 137 Æ 7 Ma and 142.5 Æ 4Ma(Wang and Diao, ‘‘feathered dinosaurs’’ Sinosauropteryx (Chen et al., 1998), Pro- 1984). -
Research Paper Inventory and Management of Dinosaurs Traces
International Journal of Global Science Research ISSN: 2348-8344 (Online) Vol. 5, Issue. 2, October 2018, pp. 793-814 DOI: 10.26540/ijgsr.v5.i2.2018.106 Available Online at www.ijgsr.com © Copyright 2014 | ijgsr.com | All Rights Reserved Research Paper Inventory and Management of Dinosaurs Traces: A case Study of Azilal Region, Morocco Fayçal AMINE, M’Hamed BERRAHMA and Abdellatif AARAB Mohamed V University, ENS, Department of Earth Sciences, Geosciences, Natural Resources and Development Laboratory, Avenue Mohamed Bel Hassan El Ouazzani, P.O. Box 5118 Takaddoum, Rabat, Morocco. *Corresponding author E-mail: [email protected] Received: 30/09/2018 Revised: 13/10/2018 Accepted: 18/10/2018 Abstract: The preservation of geosites in under considerations has been the scope of the heritage framework is necessary at a numerous geological studies since the 20th time when urbanization, the exploitation of Century and particularly in the past 30 years. fossils and minerals are real threats to this Recent advances have revealed that irreversible heritage. This work is a geotourism is an emerging and still contribution to the preservation and underdeveloped face of tourism, mainly in development of dinosaur trace deposits by Morocco, and mapping the geoheritage of geological and geomorphological Azilal region remains lacunars. The description of the study area, then by importance of study of geoheritage of the mapping using Geographic Information Azilal Region is related the dinosaurs traces, Systems (GIS) and finally by the proposal of worked by many paleontologists and the models of development and preservation geologists (Dresnay, 1971, 1975; Couvreur, of these geosites. 1977; Dutuit & Ouazzou, 1980; Jenny et al., Keywords: Azilal region, Morocco, 1981a,b; Laville, 1981; Monbaron, 1978, Geoheritage, Geo-Routes, GIS, Geotouristic 1980, 1981, 1982a, b, 1983; Biron, 1982; Interess Local, Dinosaurs. -
Late Mesozoic to Paleogene Stratigraphy of the Salar De Atacama Basin, Antofagasta, Northern Chile: Implications for the Tectonic Evolution of the Central Andes
Late Mesozoic to Paleogene stratigraphy of the Salar de Atacama Basin, Antofagasta, Northern Chile: Implications for the tectonic evolution of the Central Andes Constantino Mpodozisa,T,Ce´sar Arriagadab, Matilde Bassoc, Pierrick Roperchd, Peter Cobbolde, Martin Reichf aServicio Nacional de Geologı´a y Minerı´a, now at Sipetrol. SA, Santiago, Chile bDepartamento de Geologı´a, Universidad de Chile, Santiago, Chile cServicio Nacional de Geologı´a y Minerı´a, Santiago, Chile dIRD/Dep. de Geologı´a, Universidad de Chile, Santiago, Chile eGe´osciences-Rennes (UMR6118 du CNRS), France fDepartment of Geological Sciences University of Michigan, United States Abstract The Salar de Atacama basin, the largest bpre-AndeanQ basin in Northern Chile, was formed in the early Late Cretaceous as a consequence of the tectonic closure and inversion of the Jurassic–Early Cretaceous Tarapaca´ back arc basin. Inversion led to uplift of the Cordillera de Domeyko (CD), a thick-skinned basement range bounded by a system of reverse faults and blind thrusts with alternating vergence along strike. The almost 6000-m-thick, upper Cretaceous to lower Paleocene sequences (Purilactis Group) infilling the Salar de Atacama basin reflects rapid local subsidence to the east of the CD. Its oldest outcropping unit (Tonel Formation) comprises more than 1000 m of continental red sandstones and evaporites, which began to accumulate as syntectonic growth strata during the initial stages of CD uplift. Tonel strata are capped by almost 3000 m of sandstones and conglomerates of western provenance, representing the sedimentary response to renewed pulses of tectonic shortening, which were deposited in alluvial fan, fluvial and eolian settings together with minor lacustrine mudstone (Purilactis Formation). -
Appendix A. Supplementary Material
Appendix A. Supplementary material Comprehensive taxon sampling and vetted fossils help clarify the time tree of shorebirds (Aves, Charadriiformes) David Cernˇ y´ 1,* & Rossy Natale2 1Department of the Geophysical Sciences, University of Chicago, Chicago 60637, USA 2Department of Organismal Biology & Anatomy, University of Chicago, Chicago 60637, USA *Corresponding Author. Email: [email protected] Contents 1 Fossil Calibrations 2 1.1 Calibrations used . .2 1.2 Rejected calibrations . 22 2 Outgroup sequences 30 2.1 Neornithine outgroups . 33 2.2 Non-neornithine outgroups . 39 3 Supplementary Methods 72 4 Supplementary Figures and Tables 74 5 Image Credits 91 References 99 1 1 Fossil Calibrations 1.1 Calibrations used Calibration 1 Node calibrated. MRCA of Uria aalge and Uria lomvia. Fossil taxon. Uria lomvia (Linnaeus, 1758). Specimen. CASG 71892 (referred specimen; Olson, 2013), California Academy of Sciences, San Francisco, CA, USA. Lower bound. 2.58 Ma. Phylogenetic justification. As in Smith (2015). Age justification. The status of CASG 71892 as the oldest known record of either of the two spp. of Uria was recently confirmed by the review of Watanabe et al. (2016). The younger of the two marine transgressions at the Tolstoi Point corresponds to the Bigbendian transgression (Olson, 2013), which contains the Gauss-Matuyama magnetostratigraphic boundary (Kaufman and Brigham-Grette, 1993). Attempts to date this reversal have been recently reviewed by Ohno et al. (2012); Singer (2014), and Head (2019). In particular, Deino et al. (2006) were able to tightly bracket the age of the reversal using high-precision 40Ar/39Ar dating of two tuffs in normally and reversely magnetized lacustrine sediments from Kenya, obtaining a value of 2.589 ± 0.003 Ma. -
A New Narrow-Gauge Sauropod Trackway from the Cenomanian Candeleros Formation, Northern Patagonia, Argentina
Accepted Manuscript A new narrow-gauge sauropod trackway from the Cenomanian Candeleros Formation, northern Patagonia, Argentina Arturo Miguel Heredia, Pablo José Pazos, Diana Elizabeth Fernández, Ignacio Díaz Martínez, Marcos Comerio PII: S0195-6671(18)30249-0 DOI: https://doi.org/10.1016/j.cretres.2018.11.016 Reference: YCRES 4019 To appear in: Cretaceous Research Received Date: 14 June 2018 Revised Date: 8 October 2018 Accepted Date: 20 November 2018 Please cite this article as: Heredia, A.M., Pazos, P.J., Fernández, D.E., Martínez, I.D., Comerio, M., A new narrow-gauge sauropod trackway from the Cenomanian Candeleros Formation, northern Patagonia, Argentina, Cretaceous Research, https://doi.org/10.1016/j.cretres.2018.11.016. This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT MANUSCRIPT ACCEPTED A new narrow-gauge sauropod trackway from the Cenomanian Candeleros Formation, northern Patagonia, Argentina Arturo Miguel Heredia1, 2, Pablo José Pazos1, 2, Diana Elizabeth Fernández1, 2, Ignacio Díaz Martínez3, Marcos Comerio4 1- Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas. Buenos Aires, Argentina. 2- CONICET - Universidad de Buenos Aires. Instituto de Estudios Andinos Don Pablo Groeber (IDEAN). Buenos Aires, Argentina. -
New Sauropod Trackways from the Middle Jurassic of Portugal
New sauropod trackways from the Middle Jurassic of Portugal Vanda F. Santos, José J. Moratalla, and Rafael Royo-Torres Acta Palaeontologica Polonica 54 (3), 2009: 409-422 doi: http://dx.doi.org/10.4202/app.2008.0049 The Galinha tracksite reveals a sequence of Bajocian–Bathonian limestones belonging to the Serra de Aire Formation (West−Central Portugal) and is one of the few sites in the world where Middle Jurassic sauropod dinosaur tracks can be found. This tracksite is characterised by the presence of long, wide gauge sauropod trackways, the Middle Jurassic age of which suggests these dinosaurs were more widely distributed over time than previously thought. Two trackways contain unique pes and manus prints with morphologies that allow a new sauropod ichnotaxon to be described: Polyonyx gomesi igen. et isp. nov. On the basis of different manus/pes prints and trackway features, the proposal is made to subdivide Sauropodomorpha ichno−morphotypes into five groups: Tetrasauropus−like, Otozoum −like, Breviparopus/Parabrontopodus−like; Brontopodus−like, and Polyonyx−like. Polyonyx gomesi igen. et isp. nov. is thought to represent a nonneosauropod eusauropod, with a well developed manus digit I. The posterior orientation of this digit print suggests they were made by a eusauropod dinosaur with a posteriorly rotated pollex. The manus print morphologies observed in two trackways suggest a stage of manus structure intermediate between the primitive non−tubular sauropod manus and the tubular metacarpal arrangement characteristic of more derived sauropods. The low heteropody (manus:pes area ratio 1:2) of the trackway renders it possible they could have been made by eusauropods such as Turiasaurus riodevensis, which has a similar manus:pes area ratio. -
A NEW LOCALITY RECORDS of Stellagama Stellio (LINNAEUS, 1758) (SAURIA: AGAMIDAE) in ANATOLIA Yusuf Kumlutaş, 1 İsmail Hakkı U
Russian Journal of Herpetology Vol. 22, No. 2, 2015, pp. 149 – 153 A NEW LOCALITY RECORDS OF Stellagama stellio (LINNAEUS, 1758) (SAURIA: AGAMIDAE) IN ANATOLIA Yusuf Kumlutaþ,1 Ýsmail Hakký Uðurtaþ,2 Mustafa Koyun,3 Çetin Ilgaz1* Submitted July 17, 2014. As a result of our study, the new data on distribution of Stellagama stellio (Linnaeus, 1758) in Anatolia were ob- tained. The meristic pholidolial, metric (morphometric) characters and color-pattern features of specimens of S. stellio collected from five new localities in Turkey were given in detail and compared with regard to literature. Specimens examined in the present study were similar to S. s. daani specimens mentioned in the literature. Keywords: Stellagama stellio; new localities; distribution; meristic pholidolial; metric (morphometric) characters; Turkey. Stellagama stellio, Roughtail Rock Agama, was first populations as A. s. stellio. Kayseri specimens captured described as Lacerta stellio by Linnaeus in 1758. Greece by Mertens (1952) were considered as melanistic form. is the western boundary of this species, which is distrib- The most extensive morphological study (286 specimens uted through Turkey, Syria, Lebanon, northwestern Iraq, from 12 different populations) on S. stellio populations northern Saudi Arabia, Cyprus, northern and western was performed by Daan (1967) and he stated that Anato- Jordan, Israel and northern Egypt (Baran et al., 2012; Va- lian populations represent L. s. stellio. Clark and Clark lakos et al., 2008). S. stellio is represented by seven sub- (1973) stated that different populations of this species species [S. s. stellio (Linnaeus, 1758), S. s. vulgaris (Son- have different coloration in Turkey. Beutler and Frör nini and Latreille, 1802), S. -
Decline in Vertebrate Biodiversity in Bethlehem, Palestine
Volume 7, Number 2, June .2014 ISSN 1995-6673 JJBS Pages 101 - 107 Jordan Journal of Biological Sciences Decline in Vertebrate Biodiversity in Bethlehem, Palestine Mazin B. Qumsiyeh1,* , Sibylle S. Zavala1 and Zuhair S. Amr2 1 Faculty of Science, Bethlehem University 9 Rue des Freres, Bethlehem, Palestine. 2 Department of Biology, Jordan University of Science and Technology, Irbid, Jordan. Received: December 10, 2013 Revised: January 15, 2014 Accepted: January 20, 2014 Abstract Our data showed that in the 1960s/1970s some 31 species of mammals and 78 species of birds were present in the area of the Bethlehem governorate, between Bethlehem and Deir Mar Saba. Comparison with observations done in 2008-2013 showed significant declines in vertebrate biodiversity in this area, which has increasingly become urbanized, with an increase in temperature and a decrease in annual rainfall over the past four decades. Keywords: Biodiversity, Palestine, Mammals, Birds, Reptiles. the human pressure in all areas (ARIJ, 1995). However, 1. Introduction the impact of these changes on nature was not studied. To estimate the impact of this human development Research on vertebrate biodiversity in the occupied on nature is difficult. Most studies of fauna and flora of West Bank is limited compared to that in the nearby the area South of Jerusalem (Bethlehem Governorate) areas of Palestine and Jordan; Palestinian research in was done by Western visitors who came on short trips to general still lags behind (Qumsiyeh and Isaac, 2012). tour the "Holy Land". One of the first native More work is needed to study habitat destruction Palestinians who engaged in faunal studies was Dr. -
Group Living, Parental Care, Age Structure, and Genetic Relatedness in Liolaemus Leopardinus, a High-Elevation Lizard from the Andes of Chile
GROUP LIVING, PARENTAL CARE, AGE STRUCTURE, AND GENETIC RELATEDNESS IN LIOLAEMUS LEOPARDINUS , A HIGH-ELEVATION LIZARD FROM THE ANDES OF CHILE By ENRIQUE SANTOYO BRITO Licenciatura en Biología Universidad Veracruzana Córdoba, Veracruz, México 2006 Master of Science in Wildlife Management and Conservation Colegio de Postgraduados Texcoco de Mora, Estado de México, México 2009 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of DOCTOR OF PHILOSOPHY December, 2017 GROUP LIVING, PARENTAL CARE, AGE STRUCTURE, AND GENETIC RELATEDNESS IN LIOLAEMUS LEOPARDINUS , A HIGH-ELEVATION LIZARD FROM THE ANDES OF CHILE Dissertation Approved: Dr. Stanley F. Fox Dissertation Adviser Dr. Jennifer Grindstaff Dr. Matthew Lovern Dr. Timothy O’Connell . ii ACKNOWLEDGEMENTS To my dissertation adviser, who believed in me and gave me the opportunity to grow as a scientist; thank you Dr. Fox! To my Advisory Committee, Dr. Grindstaff, Dr. Lovern, and Dr. O’Connell, thank you for your effort, time, and advice! To the faculty members at the Department of Integrative Biology, OSU, thank you for sharing your knowledge and for always having time to answer my questions. To the fantastic staff: G. Mulder, T. Neighbors, and N. Coleman for always keeping an eye on me, and always (or almost always) making sure I did not miss a deadline. To all my past and present labmates, but especially to Dan, Matt, Justin, and Jodie. To the Foxes, for opening the doors of your home to me, for always making me feel welcome, and for letting me be part of your family and life; I will always be thankful to you.