(GSSP) of the Tortonian Stage (Upper Miocene) at Monte Dei Corvi
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Cambrian Phytoplankton of the Brunovistulicum – Taxonomy and Biostratigraphy
MONIKA JACHOWICZ-ZDANOWSKA Cambrian phytoplankton of the Brunovistulicum – taxonomy and biostratigraphy Polish Geological Institute Special Papers,28 WARSZAWA 2013 CONTENTS Introduction...........................................................6 Geological setting and lithostratigraphy.............................................8 Summary of Cambrian chronostratigraphy and acritarch biostratigraphy ...........................13 Review of previous palynological studies ...........................................17 Applied techniques and material studied............................................18 Biostratigraphy ........................................................23 BAMA I – Pulvinosphaeridium antiquum–Pseudotasmanites Assemblage Zone ....................25 BAMA II – Asteridium tornatum–Comasphaeridium velvetum Assemblage Zone ...................27 BAMA III – Ichnosphaera flexuosa–Comasphaeridium molliculum Assemblage Zone – Acme Zone .........30 BAMA IV – Skiagia–Eklundia campanula Assemblage Zone ..............................39 BAMA V – Skiagia–Eklundia varia Assemblage Zone .................................39 BAMA VI – Volkovia dentifera–Liepaina plana Assemblage Zone (Moczyd³owska, 1991) ..............40 BAMA VII – Ammonidium bellulum–Ammonidium notatum Assemblage Zone ....................40 BAMA VIII – Turrisphaeridium semireticulatum Assemblage Zone – Acme Zone...................41 BAMA IX – Adara alea–Multiplicisphaeridium llynense Assemblage Zone – Acme Zone...............42 Regional significance of the biostratigraphic -
Summary of the Paleontology of the Santa Fe Group (Mio-Pliocene), North-Central New Mexico Barry S
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/30 Summary of the paleontology of the Santa Fe Group (Mio-Pliocene), north-central New Mexico Barry S. Kues and Spencer G. Lucas, 1979, pp. 237-241 in: Santa Fe Country, Ingersoll, R. V. ; Woodward, L. A.; James, H. L.; [eds.], New Mexico Geological Society 30th Annual Fall Field Conference Guidebook, 310 p. This is one of many related papers that were included in the 1979 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Carnivora from the Late Miocene Love Bone Bed of Florida
Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 413-434 413 CARNIVORA FROM THE LATE MIOCENE LOVE BONE BED OF FLORIDA Jon A. Baskin1 Eleven genera and twelve species of Carnivora are known from the late Miocene Love Bone Bed Local Fauna, Alachua County, Florida. Taxa from there described in detail for the first time include the canid cf. Urocyon sp., the hemicyonine ursid cf. Plithocyon sp., and the mustelids Leptarctus webbi n. sp., Hoplictis sp., and ?Sthenictis near ?S. lacota. Postcrania of the nimravid Barbourofelis indicate that it had a subdigitigrade posture and most likely stalked and ambushed its prey in dense cover. The postcranial morphology of Nimravides (Felidae) is most similar to the jaguar, Panthera onca. The carnivorans strongly support a latest Clarendonian age assignment for the Love Bone Bed. Although the Love Bone Bed local fauna does show some evidence of endemism at the species level, it demonstrates that by the late Clarendonian, Florida had become part of the Clarendonian chronofauna of the midcontinent, in contrast to the higher endemism present in the early Miocene and in the later Miocene and Pliocene of Florida. Key Words: Carnivora; Miocene; Clarendonian; Florida; Love Bone Bed; Leptarctus webbi n. sp. INTRODUCTION can Museum of Natural History, New York; F:AM, Frick The Love Bone Bed Local Fauna, Alachua County, fossil mammal collection, part of the AMNH; UF, Florida Florida, has produced the largest and most diverse late Museum of Natural History, University of Florida. Miocene vertebrate fauna known from eastern North All measurements are in millimeters. The follow- America, including 43 species of mammals (Webb et al. -
Chronology, Causes and Progression of the Messinian Salinity Crisis
letters to nature the cause, and the effects, of the isolation of the Mediterranean; the two basic explanations are (1) a large glacio-eustatic sea-level drop, Chronology, causes and related to expanding polar ice volume6, and (2) orogenic uplift accompanied by gravity-driven sliding of large nappe complexes in progression of the the Gibraltar arc7. Until now, correlations of stable-isotope (d18O and d13C) records from open-ocean sequences to the Messinian Messinian salinity crisis event stratigraphy of the Mediterranean have been ambiguous because of the absence of a reliable time frame for the MSC. The W. Krijgsman*, F. J. Hilgen², I. Raf®³, F. J. Sierro§ establishment of astronomical polarity timescales for the past & D. S. Wilsonk 10 Myr (refs 3, 11) provided a signi®cant advance in dating the * Paleomagnetic Laboratory ``Fort Hoofddijk'', Utrecht University, geological record and promised a solution for the MSC controver- Budapestlaan 17, 3584 CD Utrecht, The Netherlands sies. Unfortunately, the Mediterranean-based astronomical polarity ² Department of Geology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, timescale showed a gap during much of the Messinian (6.7±5.3 Myr The Netherlands ago)3, related to the presence of less-favourable sediments and the ³ Dipartimento di Scienze della Terra, UniversitaÁ ``G. D'Annunzio'', notoriously complex geological history of the Mediterranean in Campus Universitario, Via dei Vestini 31, 66013 Chieti Scalo, Italy this time interval. However, the classic Messinian sediments § Department de -
Pamphlet to Accompany Geologic Map of the Apache Canyon 7.5
GEOLOGIC MAP AND DIGITAL DATABASE OF THE APACHE CANYON 7.5’ QUADRANGLE, VENTURA AND KERN COUNTIES, CALIFORNIA By Paul Stone1 Digital preparation by P.M. Cossette2 Pamphlet to accompany: Open-File Report 00-359 Version 1.0 2000 This report is preliminary and has not been reviewed for conformity with U. S. Geological Survey editorial standards. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U. S. Government. This database, identified as "Geologic map and digital database of the Apache Canyon 7.5’ quadrangle, Ventura and Kern Counties, California," has been approved for release and publication by the Director of the USGS. Although this database has been reviewed and is substantially complete, the USGS reserves the right to revise the data pursuant to further analysis and review. This database is released on condition that neither the USGS nor the U. S. Government may be held liable for any damages resulting from its use. U.S. Geological Survey 1 345 Middlefield Road, Menlo Park, CA 94025 2 West 904 Riverside Avenue, Spokane, WA 99201 1 CONTENTS Geologic Explanation............................................................................................................. 3 Introduction................................................................................................................................. 3 Stratigraphy................................................................................................................................ 4 Structure .................................................................................................................................... -
Oreodonts of the Tick Canyon Formation , Southern California
PALE0B10s Contributions from the University of California Museum of Paleontology, Berkeley No. I June 15, 1967 OREODONTS OF THE TICK CANYON FORMATION , SOUTHERN CALIFORNIA by David P. Whistler OREODONTS OF THE TICK CANYON FORMATION, SOUTHERN CALIFORNIA BY DAVID P. WHISTLER In 1940, Richard H. Jahns reviewed the stratigraphy of the nonmarine Mint Canyon Formation in the eastern part of the Ventura Basin and separated from it a new formation and fauna. Previous to this work, a controversy existed as to the age of the Mint Canyon Formation, for it contained vertebrates considered indicative of both the Miocene and Pliocene (Kew, 1924, Maxson, 1930, and Stirton, 1933). As a partial solut,ion to this controversy, Jahns demonstrated the presence of an erosional unconformity low in the nonmarine sequence which indicated a shift in source area. He redefined the beds below the unconformity as the Tick Canyon Formation (Jahns, 1940, pp. 163-66). Additional fossils discovered in the Tick Canyon Formation since Maxson's work, and certain of the forms described by Maxson, comprise the Tick Canyon fauna. Only two specimens described by Maxson are from the Tick Canyon Formation, UCMP 30046, the type of Miolabis californicus and UCMP 23852, a dentary fragment of a Parahippus. Neither of these permitted a definitive age determination. The additional fauna described by Jahns indicates an Arikareean mammalian age (early Miocene), and there is a noteworthy temporal hiatus between the Tick Canyon fauna and the over lying Mint Canyon fauna. In addition, faunas comprising three mammalian ages, late Barstovian, and earlier and late Clarendonian, are now recognized from the Mint Canyon Formation, but this is not the principal concern of this paper. -
208 Cia: STRETTE DI PERTUSO - M.TE BARILLARO • Settore 1: Tortona
CARTOGRAFIA I SENTIERI IN PROVINCIA DI ALESSANDRIA Estratto dalla CTR 1:50.000 in formato vettoriale Regione Piemonte - Settore Cartografico La Regione Piemonte ha promosso negli ultimi anni un pro- Autorizzazione N. 7/2007 del 9/5/2007 gramma di censimento, recupero e promozione della rete sen- (riproduzione vietata) tieristica regionale, con la creazione del Catasto Regionale dei Sentieri . La Provincia di Alessandria, facendo seguito alle indicazioni della Regione, ha istituito nel Febbraio 2006 la Consulta Provincia di Alessandria Provinciale Per la Sentieristica , costituita dagli enti e dalle Direzione Tutela e Valorizzazione Ambientale associazioni che operano nel settore, con compiti di indivi- Servizio Parchi, Protezione Naturalistica duazione dei sentieri da inserire nel catasto, di coordinamen- e Forestazione to e programmazione degli interventi sul territorio e di con- sulenza a enti e associazioni. Consulta Provinciale per la Sentieristica Il territorio provinciale è stato suddiviso in 8 settori, facen- ti capo alle sezioni del Club Alpino Italiano presenti in provin- SENTIERO 208 cia: STRETTE DI PERTUSO - M.TE BARILLARO • Settore 1: Tortona • “ 2: Novi Ligure • “ 3 e 4: Ovada • “ 5: Acqui Terme • “ 6: S. Salvatore e Valenza LOGISTICA • “ 7: Casale M.to In auto • “ 8: Alessandria Autostrade A7 Milano-Genova Uscita Vignole Borbera –Arquata Scrivia Il Servizio Parchi individua i sentieri più significativi degli 8 SP 140 della Val Borbera fino al km 13,4 in località Baracche settori al fine di promuovere forme di turismo a basso -
Of the Serravallian Stage (Middle Miocene)
152 152 Articles by F.J. Hilgen1, H.A. Abels1, S. Iaccarino2, W. Krijgsman3, I. Raffi4, R. Sprovieri5, E. Turco2 and W.J. Zachariasse1 The Global Stratotype Section and Point (GSSP) of the Serravallian Stage (Middle Miocene) 1Department of Earth Sciences, Faculty of Geosciences, Utrecht University, The Netherlands. Email: [email protected] 2Dipartimento di Scienze della Terra, Università degli Studi di Parma, Parma, Italy. 3Paleomagnetic Laboratory “Fort Hoofddijk”, Budapestlaan 17, 3584 CD Utrecht, The Netherlands. 4Dipartimento di Geotecnologie per l’Ambiente e il Territorio, Università “G. d’Annunzio”, Chieti, Italy. 5Dipartimento di Geologia e Gedesia della Terra, Università degli Studi di Palermo, Palermo, Italy. The Global Stratotype Section and Point (GSSP) for point in a continuous marine section facilitates communication among the Base of the Serravallian Stage (Middle Miocene) is Earth Scientists as it permits to export the boundary as a timeline away from the GSSP, using multiple stratigraphic tools. defined in the Ras il Pellegrin section located in the During the last decade, much progress has been made in the coastal cliffs along the Fomm Ir-Rih Bay on the west Neogene by defining GSSPs of the Zanclean (Van Couvering et al., coast of Malta (35°54'50"N, 14°20'10"E). The GSSP is 2000), Piacenzian (Castradori et al., 1998) and Gelasian (Rio et al., at the base of the Blue Clay Formation (i.e., top of the 1998) Stages of the Pliocene, and the Messininan and Tortonian Stages transitional bed of the uppermost Globigerina of the (Upper) Miocene (Hilgen et al., 2000a; Hilgen et al., 2005). -
Deliberazione Della Giunta Regionale 1 Marzo 2019, N. 26-8491
REGIONE PIEMONTE BU12 21/03/2019 Deliberazione della Giunta Regionale 1 marzo 2019, n. 26-8491 Definizione degli ambiti territoriali di scelta dell' ASL AL entro i quali l'assistito puo' esercitare il proprio diritto di scelta/revoca del medico di assistenza primaria. A relazione del Presidente Chiamparino: Visto l’art. 19, comma 2, della Legge n. 833/78 che prevede la possibilità di libera scelta del medico, da parte dell’assistibile, nei limiti oggettivi dell’organizzazione sanitaria; visto l’art. 33, comma 3, dell’Accordo Collettivo Nazionale per la disciplina dei rapporti con i Medici di Medicina generale del 23 marzo 2005 e s.m.i. (nel prosieguo ACN MMG) che conferisce alle Regioni la competenza ad articolare il livello organizzativo dell’assistenza primaria in ambiti territoriali di comuni, gruppi di comuni o distretti; dato atto che attualmente l’ASL AL è articolata in 4 Distretti qui di seguito elencati: • Distretto di Acqui Terme-Ovada (risultante dalla fusione dell’ ex Distretto di Acqui -Terme con l’ ex Distretto di Ovada); • Distretto di Alessandria-Valenza (risultante dalla fusione dell’ ex Distretto di Alessandria con l’ ex Distretto di Valenza); • Distretto di Casale Monferrato; • Distretto di Novi Ligure- Tortona (risultante dalla fusione dell’ ex Distretto di Novi Ligure con l’ ex Distretto di Tortona); preso atto della deliberazione n. 782 del 28 novembre 2018, a firma del Direttore Generale dell'ASL AL (agli atti della Direzione Sanità, Settore Sistemi organizzativi e Risorse umane del SSR) nella quale viene posto in evidenza che: a) con legge regionale n. 4 del 5 aprile 2017 è stato istituito, con decorrenza dal 1° gennaio 2018, il Comune di Cassano Spinola , afferente il Distretto di Novi Ligure-Tortona, risultante dalla fusione dei Comuni di Cassano Spinola e di Gavazzana; b) con legge regionale n. -
LEGENDA 229,4 P 211,8 S 245,8 Fabbricone ! ! ! ! 230,8 Confine Comunale Serravalle Scrivia 203,2 232,1 O Rar 253,9 Eg
Sant'Agata Fossili Sant'Agata Fossili a Gavazzana i v i r c S . T 195,5 197,4 197,5 T . S 6 c r i v i a 199,5 1 197,9 193,1 217 Cassano Spinola T . S c 194,3 r 3 i Sardigliano 15 v SP i a 217,5 194 Casa San Bartolommeo Stazzano Casa Nuova 238,8 Villa Federici 217,6 Villa Parodi 209,9 4 Lordinio Sant`Andrea Torre 195,2 238,8 235,6 Novi Ligure 197 S P T . 3 S 5 c Il Capannone r i v i a 2 Masseria Tabacca 203 203,3 231,4 Villa Campea 203,3 210,5 217,1 203,7 203,8 Casa Gagliana 240,5 224,3 205,9 Villa Borgonuovo T. 5 S c 3 r iv Villa Clelia ia P 221,1 S Villa San Giorgio 224,3 T. Scrivia Villa Maria 221,1 253,7 206,3 Masseria Spalangrana 221,3 Casa Mornesi Macellaia 210,1 209,1 244,3 208,9 Casa Balotrina 250,4 1 210,4 7 204,2 1 P S a ivi cr 227,9 . S 219,9 T 221,6 Il R 195,6 io 229 193,2 ia iv r 210,1 c 5 S 219,7 . 3 5 T 1 Cascina Colombino LEGENDA 229,4 P 211,8 S 245,8 Fabbricone ! ! ! ! 230,8 Confine comunale Serravalle Scrivia 203,2 232,1 o rar 253,9 eg . N 8 R Lastrico a i P 143 v S 193,5 i r c S 217,5 230,1 RISCHIO INCENDI D'INTERFACCIA URBANO-FORESTA 231,4 . -
Sub Ambito 01 – Alessandrino Istat Comune 6003
SUB AMBITO 01 – ALESSANDRINO ISTAT COMUNE 6003 ALESSANDRIA 6007 ALTAVILLA MONFERRATO 6013 BASSIGNANA 6015 BERGAMASCO 6019 BORGORATTO ALESSANDRINO 6021 BOSCO MARENGO 6031 CARENTINO 6037 CASAL CERMELLI 6051 CASTELLETTO MONFERRATO 6052 CASTELNUOVO BORMIDA 6054 CASTELSPINA 6061 CONZANO 6068 FELIZZANO 6071 FRASCARO 6075 FRUGAROLO 6076 FUBINE 6078 GAMALERO 6193 LU E CUCCARO MONFERRATO 6091 MASIO 6105 MONTECASTELLO 6122 OVIGLIO 6128 PECETTO DI VALENZA 6129 PIETRA MARAZZI 6141 QUARGNENTO 6142 QUATTORDIO 6145 RIVARONE 6154 SAN SALVATORE MONFERRATO 6161 SEZZADIO 6163 SOLERO 6177 VALENZA SUB AMBITO 02 – CASALESE ISTAT COMUNE 6004 ALFIANO NATTA 6011 BALZOLA 6020 BORGO SAN MARTINO 6023 BOZZOLE 6026 CAMAGNA 6027 CAMINO 6039 CASALE MONFERRATO 6050 CASTELLETTO MERLI 6056 CELLA MONTE 6057 CERESETO 6059 CERRINA MONFERRATO ISTAT COMUNE 6060 CONIOLO 6072 FRASSINELLO MONFERRATO 6073 FRASSINETO PO 6077 GABIANO 6082 GIAROLE 6094 MIRABELLO MONFERRATO 6097 MOMBELLO MONFERRATO 5069 MONCALVO 6099 MONCESTINO 6109 MORANO SUL PO 6113 MURISENGO 6115 OCCIMIANO 6116 ODALENGO GRANDE 6117 ODALENGO PICCOLO 6118 OLIVOLA 6120 OTTIGLIO 6123 OZZANO MONFERRATO 6131 POMARO MONFERRATO 6133 PONTESTURA 6135 PONZANO MONFERRATO 6149 ROSIGNANO MONFERRATO 6150 SALA MONFERRATO 6153 SAN GIORGIO MONFERRATO 6159 SERRALUNGA DI CREA 6164 SOLONGHELLO 6171 TERRUGGIA 6173 TICINETO 6175 TREVILLE 6178 VALMACCA 6179 VIGNALE MONFERRATO 6182 VILLADEATI 6184 VILLAMIROGLIO 6185 VILLANOVA MONFERRATO SUB AMBITO 03 – NOVESE TORTONESE ACQUESE E OVADESE ISTAT COMUNE 6001 ACQUI TERME 6002 ALBERA LIGURE 6005 -
Barren Ridge FEIS-Volume IV Paleo Tech Rpt Final March
March 2011 BARREN RIDGE RENEWABLE TRANSMISSION PROJECT Paleontological Resources Assessment Report PROJECT NUMBER: 115244 PROJECT CONTACT: MIKE STRAND EMAIL: [email protected] PHONE: 714-507-2710 POWER ENGINEERS, INC. PALEONTOLOGICAL RESOURCES ASSESSMENT REPORT Paleontological Resources Assessment Report PREPARED FOR: LOS ANGELES DEPARTMENT OF WATER AND POWER 111 NORTH HOPE STREET LOS ANGELES, CA 90012 PREPARED BY: POWER ENGINEERS, INC. 731 EAST BALL ROAD, SUITE 100 ANAHEIM, CA 92805 DEPARTMENT OF PALEOSERVICES SAN DIEGO NATURAL HISTORY MUSEUM PO BOX 121390 SAN DIEGO, CA 92112 ANA 032-030 (PER-02) LADWP (MARCH 2011) SB 115244 POWER ENGINEERS, INC. PALEONTOLOGICAL RESOURCES ASSESSMENT REPORT TABLE OF CONTENTS 1.0 INTRODUCTION ........................................................................................................................... 1 1.1 STUDY PERSONNEL ....................................................................................................................... 2 1.2 PROJECT DESCRIPTION .................................................................................................................. 2 1.2.1 Construction of New 230 kV Double-Circuit Transmission Line ........................................ 4 1.2.2 Addition of New 230 kV Circuit ......................................................................................... 14 1.2.3 Reconductoring of Existing Transmission Line .................................................................. 14 1.2.4 Construction of New Switching Station .............................................................................