Dinosaur Tracks 2011
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New Dinosaur Tracksites from the Sousa Lower Cretaceous Basin (Paraíba, Brasil)
Studi Trent. Sci. Nat., Acta Geol., 81 (2004): 5-21 ISSN 0392-0534 © Museo Tridentino di Scienze Naturali, Trento 2006 New dinosaur tracksites from the Sousa Lower Cretaceous basin (Paraíba, Brasil) Giuseppe LEONARDI1* & MariadeFátimaC.F. DOS SANTOS2 1Istituto Cavansi, Dorsoduro 898, I-30123 Venezia, Italy 2Museu Câmara Cascudo, Avenida Hermes da Fonseca 1398, 59015-001 Natal – RN, Brasil *Corresponding author e-mail: [email protected] SUMMARY - New dinosaur tracksites from the Sousa Lower Cretaceous basin (Paraíba, Brasil) - During our 30th expedition to the Lower Cretaceous Rio do Peixe basins (Paraíba, Northeastern Brasil) the following new dinosaur tracksites were discovered: Floresta dos Borba (theropods, sauropods, ornithopods), Lagoa do Forno (theropods, sauropods), Lagoa do Forno II (one theropod), Várzea dos Ramos II (theropods), Várzea dos Ramos III (theropods). In the previously known sites the following new material was discovered: at Piau, a sauropod trackway; at Serrote do Letreiro a new theropod trackway; at Riacho do Cazé, some sauropod and theropod tracks; at Mãe d’Água, new sauropod, theropod and ornithopods footprints. At Fazenda Paraíso new theropod and sauropod tracks were discov- ered and a new map of the main rocky pavement including theropod tracks is provided here. The farms at Saguim de Cima, Várzea da Jurema, Tabuleiro, Catolé da Piedade (WNW of Sousa, in the Sousa Formation) and at Pau d’Arco (SE of Sousa, in the Piranhas Formation) were explored without results. RIASSUNTO - Nuove piste di dinosauri nel bacino di Sousa (Cretaceo inferiore, Paraíba, Brasile) - Durante la nostra 30ª spedizione ai bacini del Rio do Peixe (Cretaceo inferiore; Paraíba, Brasile nord orientale) sono stati sco- perti i seguenti nuovi siti con piste di dinosauri: Floresta dos Borba (teropodi, sauropodi, ornitopodi), Lagoa do Forno (teropodi, sauropodi), Lagoa do Forno II (un teropodo), Várzea dos Ramos II (teropodi), Várzea dos Ramos III (tero- podi). -
An Ornithopod Tracksite from the Helvetiafjellet Formation (Lower Cretaceous) of Boltodden, Svalbard
Downloaded from http://sp.lyellcollection.org/ at Universitetet i Oslo on January 11, 2016 The theropod that wasn’t: an ornithopod tracksite from the Helvetiafjellet Formation (Lower Cretaceous) of Boltodden, Svalbard JØRN H. HURUM1,2, PATRICK S. DRUCKENMILLER3, ØYVIND HAMMER1*, HANS A. NAKREM1 & SNORRE OLAUSSEN2 1Natural History Museum, University of Oslo, PO Box 1172, Blindern, 0318 Oslo, Norway 2The University Centre in Svalbard (UNIS), PO Box 156, 9171 Longyearbyen, Norway 3Department of Geosciences, University of Alaska Museum, University of Alaska Fairbanks, 907 Yukon Drive, Fairbanks, AK 99775, USA *Corresponding author (e-mail: [email protected]) Abstract: We re-examine a Lower Cretaceous dinosaur tracksite at Boltodden in the Kvalva˚gen area, on the east coast of Spitsbergen, Svalbard. The tracks are preserved in the Helvetiafjellet For- mation (Barremian). A sedimentological characterization of the site indicates that the tracks formed on a beach/margin of a lake or interdistributary bay, and were preserved by flooding. In addition to the two imprints already known from the site, we describe at least 34 additional, pre- viously unrecognized pes and manus prints, including one trackway. Two pes morphotypes and one manus morphotype are recognized. Given the range of morphological variation and the pres- ence of manus tracks, we reinterpret all the prints as being from an ornithopod rather than a thero- pod, as previously described. We assign the smaller (morphotype A, pes; morphotype B, manus) to Caririchnium billsarjeanti. The larger (morphotype C, pes) track is assigned to Caririchnium sp., differing in size and interdigital angle from the two described ichnospecies C. burreyi and C. -
An Overview of the Lower Cretaceous Dinosaur Tracksites from the Mirambel Formation in the Iberian Range (Ne Spain)
Khosla, A. and Lucas, S.G., eds., 2016, Cretaceous Period: Biotic Diversity and Biogeography. New Mexico Museum of Natural History and Science Bulletin 71. 65 AN OVERVIEW OF THE LOWER CRETACEOUS DINOSAUR TRACKSITES FROM THE MIRAMBEL FORMATION IN THE IBERIAN RANGE (NE SPAIN) D. CASTANERA1, I. DÍAZ-MARTÍNEZ2, M. MORENO-AZANZA3, J.I. CANUDO4, AND J.M. GASCA4 1 Bayerische Staatssammlung für Paläontologie und Geologie and GeoBioCenter, Ludwig-Maximilians-Universität, Richard-Wagner-Str. 10, 80333 Munich, Germany. [email protected]; 2 CONICET - Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, General Roca 1242, 8332 General Roca, Río Negro, [email protected]; 3 Departamento de Ciências da Terra, Geobiotec. Departamento de Ciências da Terra. Faculdade de Ciências e Tecnologia, FCT, Universidade Nova de Lisboa, 2829-526. Caparica, Portugal. Museu da Lourinhã. [email protected]; 4 Grupo Aragosaurus-IUCA, Paleontología, Departamento de Ciencias de la Tierra, Facultad de Ciencias, Universidad de Zaragoza, Calle Pedro Cerbuna, 12, 50009, Zaragoza, Spain. [email protected]; [email protected] Abstract—Up to now, the ichnological vertebrate record from the Barremian Mirambel Formation (NE Spain) has remained completely unknown despite the fact that osteological findings have been reported in recent years. Here we provide an overview of 11 new dinosaur tracksites found during a fieldwork campaign in the year 2011. The majority of these tracksites (seven) preserve small- to medium-sized tridactyl tracks here assigned to indeterminate theropods. Only one footprint presents enough characters to classify it as Megalosauripus isp. Ornithopod tracks identified asCaririchnium isp. and Iguanodontipodidae indet. -
A New European Albian Turtle That Extends the Known Stratigraphic Range of the Pleurosternidae (Paracryptodira)
Cretaceous Research 55 (2015) 74e83 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes A new European Albian turtle that extends the known stratigraphic range of the Pleurosternidae (Paracryptodira) * A. Perez-García a, b, , E. Espílez c, L. Mampel c, L. Alcala c a Centro de Geologia, Faculdade de Ci^encias da Universidade de Lisboa (FCUL), Edificio C6, Campo Grande, 1749-016 Lisbon, Portugal b Grupo de Biología Evolutiva, Facultad de Ciencias, UNED, Paseo Senda del Rey, 9, 28040 Madrid, Spain c Fundacion Conjunto Paleontologico de Teruel-Dinopolis (Museo Aragones de Paleontología), Avda. Sagunto s/n, E-44002 Teruel, Spain article info abstract Article history: Postcranial material corresponding to three specimens of freshwater turtles, from the lower Albian Received 23 December 2014 (upper Lower Cretaceous) of Arino~ (Teruel Province, Spain), is analysed in this paper. This study allows us Accepted in revised form 18 February 2015 to identify the presence of Pleurosternidae (Paracryptodira) outside its known stratigraphic range, from Available online Kimmeridgian to Barremian, and extends its distribution to the Albian. The species from Arino~ represents a new taxon, Toremys cassiopeia gen. et sp. nov., which is the only pleurosternid described so far in post- Keywords: Berriasian levels. Toremys cassiopeia is closely related to other taxa from Europe, to which the Cretaceous Pleurosternidae pleurosternids are restricted. Knowledge about the European freshwater turtle faunas distributed be- Toremys cassiopeia, gen. et sp. nov. fi Lower Cretaceous tween the Barremian and the uppermost Cretaceous is very limited. The new nding provides relevant Albian data on these poorly understood faunas. -
Fahrplan Schulzentrum Helpsen Gültig Ab 01.09.2015 Anfahrten
Fahrplan Schulzentrum Helpsen gültig ab 01.09.2015 Fahrtrichtung Niedernwöhren/Meerbeck/Wiedensahl/Stadthagen Anfahrten Ort Haltestelle 1.Std 1.Std 2.Std Sonderveranstaltungen Wiedensahl Sportplatz 07:32 08:08 14:00 Wiedensahl Ronnenberg 07:34 08:09 14:01 Wiedensahl Mitte 07:35 08:10 14:02 Wiedensahl Niemitz 07:36 08:11 14:03 Niedernwöhren Abzw.Mittelbrink 07:38 08:13 14:04 Niedernwöhren Wilkening 07:39 08:14 14:05 Niedernwöhren Grundschule Niedernwöhren Suthmeier 07:41 08:16 14:06 Niedernwöhren Bahnhof Str. 07:42 08:18 14:08 Meerbeck Schweer 07:43 Hobbensen Ort 07:44 Levesen Kreuzung 07:46 Helpsen IGS 07:50 Niedernwöhren Alte Schule 07:32 08:00 Meerbeck Lange Str. 07:34 08:24 14:14 Meerbeck Bartels 07:37 08:25 14:16 Meerbeck Sparkasse 07:39 08:26 14:17 Meerbeck Gallweg 07:40 08:27 14:18 Volksdorf Kuckshagen 07:41 08:28 14:20 Volksdorf Mitte 07:42 08:29 14:21 Volksdorf Abzw.Hiddensen 07:44 08:30 14:23 Helpsen IGS 07:50 08:35 14:30 Stadthagen Hütten Str. 07:15 08:06 13:49 Breslauer Str. 07:16 08:05 13:47 ZOH 07:19 08:03 13:45 Untere Str. 07:35 13:32 Helpsen IGS 07:50 08:14 14:15 Fahrtrichtung Niedernwöhren/Meerbeck/Wiedensahl/Stadthagen Rückfahrten Ort Haltestelle 5.Std 5.Std 6.Std 6.Std 8.Std 8.Std Sonderveranstaltungen Helpsen IGS 12:33 12:33 13:23 13:20 15:55 15:45 18:15 17:50 HALTEPUNKT 4 6 4 6 4 4 6 Volksdorf Abzw Hiddensen 12:41 13:26 15:58 18:20 Volksdorf Mitte 12:42 13:27 15:59 18:21 Volksdorf Kuckshagen 12:43 13:28 16:00 18:22 Meerbeck Gallweg 12:44 13:29 16:01 18:23 Meerbeck Sparkasse 12:45 13:30 16:03 18:24 Niedernwöhren Bahnhof Str. -
A Review of Large Cretaceous Ornithopod Tracks, with Special Reference to Their Ichnotaxonomy
bs_bs_banner Biological Journal of the Linnean Society, 2014, 113, 721–736. With 5 figures A review of large Cretaceous ornithopod tracks, with special reference to their ichnotaxonomy MARTIN G. LOCKLEY1*, LIDA XING2, JEREMY A. F. LOCKWOOD3 and STUART POND3 1Dinosaur Trackers Research Group, University of Colorado at Denver, CB 172, PO Box 173364, Denver, CO 80217-3364, USA 2School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China 3Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, UK Received 30 January 2014; revised 12 February 2014; accepted for publication 13 February 2014 Trackways of ornithopods are well-known from the Lower Cretaceous of Europe, North America, and East Asia. For historical reasons, most large ornithopod footprints are associated with the genus Iguanodon or, more generally, with the family Iguanodontidae. Moreover, this general category of footprints is considered to be sufficiently dominant at this time as to characterize a global Early Cretaceous biochron. However, six valid ornithopod ichnogenera have been named from the Cretaceous, including several that are represented by multiple ichnospecies: these are Amblydactylus (two ichnospecies); Caririchnium (four ichnospecies); Iguanodontipus, Ornithopodichnus originally named from Lower Cretaceous deposits and Hadrosauropodus (two ichnospecies); and Jiayinosauropus based on Upper Cretaceous tracks. It has recently been suggested that ornithopod ichnotaxonomy is oversplit and that Caririchnium is a senior subjective synonym of Hadrosauropodus and Amblydactylus is a senior subjective synonym of Iguanodontipus. Although it is agreed that many ornithopod tracks are difficult to differentiate, this proposed synonymy is questionable because it was not based on a detailed study of the holotypes, and did not consider all valid ornithopod ichnotaxa or the variation reported within the six named ichnogenera and 11 named ichnospecies reviewed here. -
Pterosaur Distribution in Time and Space: an Atlas 61
Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Pa lä on to lo gie und Geologie B28 DAVID W. E. HONE & ERIC BUFFETAUT (Eds) Flugsaurier: pterosaur papers in honour of Peter Wellnhofer CONTENTS/INHALT Dedication 3 PETER WELLNHOFER A short history of pterosaur research 7 KEVIN PADIAN Were pterosaur ancestors bipedal or quadrupedal?: Morphometric, functional, and phylogenetic considerations 21 DAVID W. E. HONE & MICHAEL J. BENTON Contrasting supertree and total-evidence methods: the origin of the pterosaurs 35 PAUL M. BARRETT, RICHARD J. BUTLER, NICHOLAS P. EDWARDS & ANDREW R. MILNER Pterosaur distribution in time and space: an atlas 61 LORNA STEEL The palaeohistology of pterosaur bone: an overview 109 S. CHRISTOPHER BENNETT Morphological evolution of the wing of pterosaurs: myology and function 127 MARK P. WITTON A new approach to determining pterosaur body mass and its implications for pterosaur fl ight 143 MICHAEL B. HABIB Comparative evidence for quadrupedal launch in pterosaurs 159 ROSS A. ELGIN, CARLOS A. GRAU, COLIN PALMER, DAVID W. E. HONE, DOUGLAS GREENWELL & MICHAEL J. BENTON Aerodynamic characters of the cranial crest in Pteranodon 167 DAVID M. MARTILL & MARK P. WITTON Catastrophic failure in a pterosaur skull from the Cretaceous Santana Formation of Brazil 175 MARTIN LOCKLEY, JERALD D. HARRIS & LAURA MITCHELL A global overview of pterosaur ichnology: tracksite distribution in space and time 185 DAVID M. UNWIN & D. CHARLES DEEMING Pterosaur eggshell structure and its implications for pterosaur reproductive biology 199 DAVID M. MARTILL, MARK P. WITTON & ANDREW GALE Possible azhdarchoid pterosaur remains from the Coniacian (Late Cretaceous) of England 209 TAISSA RODRIGUES & ALEXANDER W. -
The Black Hills, South Dakota
The Black Hills, South Dakota 2-3 Local Area Events 4-5 Resident Services 6 Custer County History 7 Custer County Communities 8 Lawrence County History 9 Lawrence County Communities 10 Meade County History 11 Meade County Communities 12 Pennington County History 13 Pennington County Communities 14-15 Parks & Recreation 16-17 Local Area Attractions 18-19 South Dakota Hunting Seasons 20-21 DNR License Centers 23 Fishing Licensing & Limits 30 Local Area Snowmobile Trails 31 George S. Mickelson Bicycle Trails Custer County Lawrence County Meade County Pennington County Scan the QR Codes to go to the individual county pages. Local Area Events JANUARY JUNE (CONTD.) SEPTEMBER OCTOBER (CONTD.) Black Hills Stock Show & Rodeo | Rapid City Annual Black Hills Quilt Show & Sale | Rapid City Crazy Horse Autumn Volksmarch | Rapid City Spearfish Corn Maze | Spearfish Red Dirt Music Festival | Deadwood Cavalry Days | Rapid City Crazy Horse Night Blast | Rapid City Wild West Songwriter’s Festival | Deadwood ISOC Deadwood Snocross Shootout | Deadwood Crazy Horse Stampede | Rapid City Fireball Run Adventurally | Rapid City Deadweird | Deadwood Snow Jam Winter Carnival | Lead Crazy Horse Volksmarch | Rapid City Dakota Polka Festival | Rapid City Pumpkin Fest | Belle Fourche Jammin’ The Peak Music Series | Lead West Boulevard Summer Festival | Rapid City Deadwood Jam | Rapid City Halloween Parade | Belle Fourche Wild Bill Days | Rapid City Mickelson Trail Trek | Rapid City FEBRUARY Youth Rodeo Series | Sturgis Pumpkin Festival | Rapid City NOVEMBER Northern -
Fast-Running Theropods Tracks from the Early Cretaceous of La Rioja, Spain
Fast-Running Theropods Tracks From the Early Cretaceous of La Rioja, Spain Pablo Navarro-Lorbés ( [email protected] ) Universidad de La Rioja (UR), C/ Luis de Ulloa Javier Ruiz Universidad Complutense de Madrid Ignacio Díaz-Martínez Universidad Nacional de Río Negro-IIPG Erik Isasmendi Universidad del País Vasco/Euskal Herriko Unibertsitatea (UPV/EHU) Patxi Sáez-Benito Centro de Interpretación Paleontológica de La Rioja, C/ Mayor, 10, 26525, Igea, La Rioja Luis Viera Centro de Interpretación Paleontológica de La Rioja, C/ Mayor, 10, 26525, Igea, La Rioja Xabier Pereda-Suberbiola Universidad del País Vasco/Euskal Herriko Unibertsitatea (UPV/EHU) Angélica Torices Universidad de La Rioja (UR), C/ Luis de Ulloa Research Article Keywords: Fast-running theropods tracks, Early Cretaceous, La Rioja, Spain, Theropod behaviour, biodynamics, aleontology, biomechanical models Posted Date: August 5th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-764084/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Page 1/23 Abstract Theropod behaviour and biodynamics are intriguing questions that paleontology has been trying to resolve for a long time. The lack of extant groups with similar bipedalism has made it hard to answer some of the questions on the matter, yet theoretical biomechanical models have shed some light on the question of how fast theropods could run and what kind of movement they showed. The study of dinosaur tracks can help answer some of these questions due to the very nature of tracks as a product of the interaction of these animals with the environment. Two trackways belonging to fast-running theropods from the Lower Cretaceous Enciso Group of Igea (La Rioja) are presented here and compared with other fast-running theropod trackways published to date. -
The Giant Pliosaurid That Wasn't—Revising the Marine Reptiles From
The giant pliosaurid that wasn’t—revising the marine reptiles from the Kimmeridgian, Upper Jurassic, of Krzyżanowice, Poland DANIEL MADZIA, TOMASZ SZCZYGIELSKI, and ANDRZEJ S. WOLNIEWICZ Madzia, D., Szczygielski, T., and Wolniewicz, A.S. 2021. The giant pliosaurid that wasn’t—revising the marine reptiles from the Kimmeridgian, Upper Jurassic, of Krzyżanowice, Poland. Acta Palaeontologica Polonica 66 (1): 99–129. Marine reptiles from the Upper Jurassic of Central Europe are rare and often fragmentary, which hinders their precise taxonomic identification and their placement in a palaeobiogeographic context. Recent fieldwork in the Kimmeridgian of Krzyżanowice, Poland, a locality known from turtle remains originally discovered in the 1960s, has reportedly provided additional fossils thought to indicate the presence of a more diverse marine reptile assemblage, including giant pliosaurids, plesiosauroids, and thalattosuchians. Based on its taxonomic composition, the marine tetrapod fauna from Krzyżanowice was argued to represent part of the “Matyja-Wierzbowski Line”—a newly proposed palaeobiogeographic belt comprising faunal components transitional between those of the Boreal and Mediterranean marine provinces. Here, we provide a de- tailed re-description of the marine reptile material from Krzyżanowice and reassess its taxonomy. The turtle remains are proposed to represent a “plesiochelyid” thalassochelydian (Craspedochelys? sp.) and the plesiosauroid vertebral centrum likely belongs to a cryptoclidid. However, qualitative assessment and quantitative analysis of the jaws originally referred to the colossal pliosaurid Pliosaurus clearly demonstrate a metriorhynchid thalattosuchian affinity. Furthermore, these me- triorhynchid jaws were likely found at a different, currently indeterminate, locality. A tooth crown previously identified as belonging to the thalattosuchian Machimosaurus is here considered to represent an indeterminate vertebrate. -
Im Weserbergland
2021 UrlaubIM WESERBERGLAND Herausgeber: Weserbergland Tourismus e. V. Postfach 10 03 39 31753 Hameln Fon 05151/9300-0 [email protected] www.weserbergland-tourismus.de ausgezeichnet WWW.WESERBERGLAND-TOURISMUS.DE mit dem Gütesiegel: Das Weserbergland auf einen Blick. LIEBE GÄSTE, Fachwerk und Weserrenaissance, Burgen und Schlösser sowie die eindrucksvolle Natur mit sanften Hügeln und die durch die Region fließende Weser - all das zeichnet das Weserbergland aus. Unsere Urlaubsregion erstreckt sich von Hann. Münden im Süden bis Porta Westfalica im Norden und bietet A2 Porta Westfalica eine Reihe einzigartiger Erlebnisse für Ihre nächste Reise. Wie wäre es Elze beispielsweise mit einer Radreise auf A2 Gronau dem ausgezeichneten Weser-Radweg Eime entlang der Weser? Sie schnüren lieber W e s die Wanderschuhe? Kein Problem! e r Duingen b Lamspringe Dann erwandern Sie doch einen der e Alfeld zertifizierten Qualitätswanderwege wie r zum Beispiel den Weserbergland-Weg g Freden oder den Ith-Hils-Weg. l a Auch Kulturliebhaber kommen bei n uns auf ihre Kosten: Sie können sich d auf die Spuren der historischen Städte und Stätten begeben und in die über 1.000-jährige Geschichte des Weserberglandes eintauchen. Entspannung und Ruhe sowie Wesertal genussvolle Momente sollen bei Ihrem Aufenthalt natürlich nicht zu kurz kommen und können in den Kur- und Heilbädern oder bei kulinarischen Ausflügen genossen werden. Ganz gleich, was Sie bei uns erleben möchten: das Weserbergland ist zu jeder Jahreszeit eine Reise wert! Wir freuen uns auf Ihren Besuch und wünschen Ihnen eine erlebnisreiche Zeit! 2 IHRE URLAUBSTHEMEN IHRE FERIENORTE Bad Karlshafen .......................................16 RADFAHREN Bad Pyrmont ............................................17 Weser-Radweg & Co. -
Amtsblatt 2008
Amtsblatt für den Landkreis Schaumburg --------------------------------------------------------------------------------------------------------------------------- Inhaltsverzeichnis 2008 Stichwort Einsender Seite Abfallentsorgung Landkreis Schaumburg 41 (Satzungen, Gebühren) Landkreis Schaumburg 42 Abwasserbeseitigung Samtgemeinde Eilsen 18 (Satzungen, Gebühren) Stadt Stadthagen 70 Samtgemeinde Lindhorst 72 Samtgemeinde Niedernwöhren 75 Samtgemeinde Lindhorst 101 Stadt Obernkirchen 105 Samtgemeinde Niedernwöhren 110 Stadt Bückeburg 125 Stadt Rinteln 128 Stadt Stadthagen 129 Samtgemeinde Nenndorf 138 Aufwandsentschädigungen / Landkreis Schaumburg 10 Auslagenersatz Gemeinde Auetal 133 Bebauungspläne Stadt Bückeburg Nr. 53 + 240 2 Gemeinde Suthfeld Nr. R5 3 Stadt Bad Nenndorf Nr. 15a 11 Gemeinde Nienstädt Nr. 08 12 Flecken Lauenau Nr. 44 14 Stadt Rinteln Nr. 7 18 Stadt Obernkirchen Nr. K6 25 Stadt Obernkirchen Nr. K7 25 Gemeinde Hespe Nr. 13 33 Stadt Bad Nenndorf Nr. 17A 50 Stadt Bad Nenndorf Nr. 77 51 Stadt Bückeburg Nr. 72 56 Stadt Rinteln Nr. 65 58 Gemeinde Meerbeck Nr. 23 76 Gemeinde Niedernwöhren Nr. 15 77 Flecken Lauenau Nr. 44 78 Stadt Rinteln Nr. 73 82 Gemeinde Lauenhagen Nr. 8 85 Gemeinde Nienstädt Nr. 5 95 Gemeinde Pohle Nr. 13 95 Stadt Bückeburg Nr. 4D + 220 98 Stadt Rinteln Nr. 9 100 Stadt Stadthagen Nr. 88 107 Gemeinde Bad Eilsen Nr. 19 107 Gemeinde Heeßen Nr. 17 108 Gemeinde Haste Nr. 21 109 Gemeinde Hespe Nr. 19 110 Stadt Bückeburg Nr. 71 125 Stadt Obernkirchen Nr. V7 125 1 Beförderungsentgelte/-bedingungen Landkreis Schaumburg