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Journal articles on the topic 'Hauterive'

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Published: 20 April 2024

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1

Benkert, Alain, and Heinz Egger. "Dendrochronologie d'un site du Bronze final, Hauterive-Champréveyres (Suisse)." Bulletin de la Société préhistorique française 83, no. 11 (1986): 486–502. http://dx.doi.org/10.3406/bspf.1986.8723.

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2

Daber, Rudolf. "Zur Paläogeographie und Biologie vonWeichselia reticulata im Hauterive-Barrěme (Unterkreide)." Feddes Repertorium 101, no. 5-6 (1990): 319–31. http://dx.doi.org/10.1002/fedr.4911010523.

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3

Daber, Rudolf. "Zur Paläogeographie und Biologie von Weichselia reticulata im Hauterive-Barrême (Unterkreide)." Feddes Repertorium 101, no. 5-6 (April 18, 2008): 319–31. http://dx.doi.org/10.1002/fedr.19901010523.

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4

Wild, Rupert. "Pterosaur remains (Reptilia, Pterosauria) from the Lower Cretaceous (Hauterivian) of Hannover (Lower Saxony)." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 181, no. 1-3 (December 10, 1990): 241–54. http://dx.doi.org/10.1127/njgpa/181/1990/241.

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5

Hajdas, I., G. Bonani, P. Hadorn, N. Thew, G. R. Coope, and G. Lemdahl. "Radiocarbon and absolute chronology of the Late-Glacial record from Hauterive/Rouges-Terres, Lake Neuchâtel (CH)." Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 223-224 (August 2004): 308–12. http://dx.doi.org/10.1016/j.nimb.2004.04.061.

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6

Straus, Lawrence Guy. "Un Campement Magdalénien au Bord du Lac de Neuchâtel: Contexte, Vestiges, Activités. Hauterive-Champréveyres 10. Denise LeeschUn Campement Magdalénien au Bord du Lac de Neuchâtel: Etude Archéozoologique. Hauterive-Champréveyres 11. Philippe Morel , Werner Müller , Denise Leesch." Journal of Anthropological Research 56, no. 1 (April 2000): 129–31. http://dx.doi.org/10.1086/jar.56.1.3630972.

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7

Leurquin, JeannineLéon. "Leuvrey J.M. : Hauterive-Champréveyres. L'industrie lithique du Bronze final. Etude typotechnologique (avec une contribution de T. Adatte)." L'Anthropologie 104, no. 4 (October 2000): 573. http://dx.doi.org/10.1016/s0003-5521(00)80038-2.

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8

Magny, Michel, Nigel Thew, and Philippe Hadorn. "Late-glacial and early Holocene changes in vegetation and lake-level at Hauterive/Rouges-Terres, Lake Neuchâtel (Switzerland)." Journal of Quaternary Science 18, no. 1 (November 28, 2002): 31–40. http://dx.doi.org/10.1002/jqs.699.

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9

Coope, G. Russell, and Scott A. Elias. "The environment of Upper Palaeolithic (Magdalenian and Azilian) hunters at Hauterive-Champr�veyres, Neuch�tel, Switzerland, interpreted from coleopteran remains." Journal of Quaternary Science 15, no. 2 (February 2000): 157–75. http://dx.doi.org/10.1002/(sici)1099-1417(200002)15:2<157::aid-jqs478>3.0.co;2-k.

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10

Straus, Lawrence Guy. "Hauterive-Champréveyres et Neuchâtel-Monruz. Témoins d'Implantations Magdaléniennes et Aziliennes sur la Rive Nord du Lac de Neuchâtel. Denise Leesch , Marie-Isabelle Cattin , Werner Müller." Journal of Anthropological Research 62, no. 1 (April 2006): 147–49. http://dx.doi.org/10.1086/jar.62.1.3630744.

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11

Peschaux, Caroline, François-Xavier Chauvière, and Dominique Henry-Gambier. "Les coquilles de mollusques des fouilles Émile Rivière aux Balzi Rossi (Vintimille, Italie) : apport des collections Goury (Musée Lorrain, Nancy, France) et Moll (Laténium, Hauterive, Suisse)." Paléo, Hors-série (November 15, 2023): 78–97. http://dx.doi.org/10.4000/paleo.7853.

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12

Ullmann, Félix. "Kauz, D aniel: Du t abou au débat. Cent a ns de lutte contre le cancer en Suisse 1910–2010. P réface de Didier Burkhalter. Hauterive, Ed. A ttinger, 2010. 255 p. CHF 58.–. ISBN 978-2-940418-16-9." Gesnerus 68, no. 1 (November 11, 2011): 128–29. http://dx.doi.org/10.1163/22977953-06801019.

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13

Reboulet, Stéphane, François Atrops, Serge Ferry, and André Schaaf. "Renouvellement des ammonites en fosse vocontienne a la limite Valanginien-Hauterivien." Geobios 25, no. 4 (January 1992): 469–76. http://dx.doi.org/10.1016/s0016-6995(92)80074-n.

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14

Bessire, François. "Robert DARNTON, Michel SCHLUP (éds.), Le Rayonnement d'une maison d'édition dans l'Europe des Lumières : la Société typographique de Neuchâtel 1769-1789 , publiés avec la collaboration de Jacques RYCHNER. Index établi par Marie-Christine HAUSER, avec le concours de Marcel GUERDAT et Michael SCHMIDT, Neuchâtel-Hauterive, Bibliothèque publique et universitaire-Éditions Gilles Attinger, 2005, 620 p. + ill." Dix-huitième siècle 38, no. 1 (November 1, 2006): CXVI. http://dx.doi.org/10.3917/dhs.038.0643dl.

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15

Masse, Jean-Pierre, and Geneviève Termier. "Les Spongiaires du Crétacé inférieur (Hauterivien-Aptien inférieur) de Provence (Sud-Est de la France)." Géologie Méditerranéenne 19, no. 2 (1992): 89–123. http://dx.doi.org/10.3406/geolm.1992.1472.

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16

Schroeder, Rolf, Bernard Clavel, Antonietta Cherchi, and Jean Charollais. "Praedictyorbitolina busnardoi n. sp. (Foraminiferida) et évolution de la lignéePraedictyorbitolina — Dictyorbitolina (Hauterivien supérieur — Barrémien basal)." Paläontologische Zeitschrift 73, no. 3-4 (December 1999): 203–15. http://dx.doi.org/10.1007/bf02988035.

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17

Peybernès, B., and P. J. Combes. "Stratigraphie séquentielle du Crétacé basal (intervalle Berriasien-Hauterivien) des Pyrénées centrales et orientales franco-espagnoles." Cretaceous Research 15, no. 5 (October 1994): 535–46. http://dx.doi.org/10.1006/cres.1994.1032.

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18

Peybernès, Bernard, Richard Ciszak, Todor Nikolov, Marin lvanov, and Kristalina Stoykova. "Géométrie des formations et des séquences de dépôt éocrétacées (intervalle Hauterivien-Aptien) de Bulgarie nord-orientale." Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science 327, no. 8 (October 1998): 555–62. http://dx.doi.org/10.1016/s1251-8050(99)80038-x.

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19

Schroeder, Rolf, Bernard Clavel, and Jean Charollais. "Praedictyorbitolina carthusiana n. gen. n. sp., Orbitolinidé (Foraminiferida) de la limite Hauterivien-Barrémien des Alpes occidentales." Paläontologische Zeitschrift 64, no. 3-4 (December 1990): 193–202. http://dx.doi.org/10.1007/bf02985713.

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20

Alméras, Yves, Serge Ferry, Bruno R. C. Granier, and Yann Merran. "Jurassian brachiopods of the Valanginian - Hauterivian interval. Their contribution to the dating of the Salima Formation in Mount Lebanon." Carnets de géologie (Notebooks on geology) 21, no. 7 (March 24, 2021): 163–79. http://dx.doi.org/10.2110/carnets.2021.2107.

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Les gisements jurassiens français ou suisses du Crétacé basal (Valanginien ou Hauterivien) recèlent de nombreuses espèces de brachiopodes parmi lesquelles 3 espèces inconnues au Liban : Lamellaerhynchia desori (Loriol in Pictet & Campiche, 1872), Sulcirhynchia valangiensis (Loriol, 1864) et Terebratulina arzierensis (Loriol, 1864). Le site fossilifère de la Formation de Salima à Zeghrine, une localité proche de Bikfaya (Mont Liban), recèle une association constituée de Belothyris pseudojurensis (Leymerie, 1842), Lamellaerhynchia hauteriviensis Burri, 1953, Loriolithyris valdensis (Loriol, 1868), Lor. latifrons (Pictet, 1872), Sellithyris carteroniana (Orbigny, 1847) et Terebratulina biauriculata Orbigny, 1850, toutes également présentes dans les localités jurassiennes. Sur la base de l'étude de son association de brachiopodes, la Formation de Salima est par conséquent attribuée au Valanginien indifférencié. [The Jurassian French or Swiss outcrops of the lowermost Cretaceous (Valanginian or Hauterivian) yield numerous brachiopod species including 3 species: Lamellaerhynchia desori (Loriol in Pictet & Campiche, 1872), Sulcirhynchia valangiensis (Loriol, 1864), and Terebratulina arzierensis (Loriol, 1864), which are not found in Lebanon. The fossiliferous site of the Salima Formation at Zeghrine, a locality close to Bikfaya (Mount Lebanon), yields an assemblage made of Belothyris pseudojurensis (Leymerie, 1842), Lamellaerhynchia hauteriviensis Burri, 1953, Loriolithyris valdensis (Loriol, 1868), Lor. latifrons (Pictet, 1872), Sellithyris carteroniana (Orbigny, 1847), and Terebratulina biauriculata Orbigny, 1850; all are also present in Jurassian localities. On the basis of the study of its brachiopod assemblage, the Salima Formation is therefore ascribed an undifferentiated Valanginian age.]

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21

Suberbiola, Xabier Pereda, Fidel Torcida, Luis Angel Izquierdo, Pedro Huerta, Diego Montero, and Gustavo Pérez. "First rebbachisaurid dinosaur (Sauropoda, Diplodocoidea) from the early Cretaceous of Spain : palaeobiogeographical implications." Bulletin de la Société Géologique de France 174, no. 5 (September 1, 2003): 471–79. http://dx.doi.org/10.2113/174.5.471.

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Abstract Sauropod remains from the early Cretaceous (late Barremian–early Aptian) of Salas de los Infantes (Burgos, Spain) are described. The material consists of several caudal vertebrae, chevrons, a pair of ischia and a femur that is presumed to belong to a single medium-sized individual. Based on the tall neural arches and broad neural spines of the anterior caudal vertebrae, the specimen is referred to the Diplodocoidea. Moreover, it shows affinities with the Rebbachisauridae, a basal clade of diplodocoids. Both the caudal vertebrae and ischium of the Burgos sauropod are similar in form to those of ‘Rebbachisaurus’ tessonei from the Albian-Cenomanian of South America. However, there are some differences with regard to this taxon, so the Burgos sauropod is provisionally referred to as Rebbachisauridae in-det. Rebbachisaurids are known in the Aptian-Cenomanian of the western Gondwanan landmasses (Africa and South America), although further remains have been reported from the Coniacian-Santonian of Argentina and the Hauteri-vian–Barremian of Croatia. The Burgos diplodocoid appears to be one of the earliest representative of the Rebbachisau-ridae. This discovery supports previous evidence of a land connection between Europe and Africa across the Tethys seaway sometime in the early Cretaceous.

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22

Concheyro, Andrea, Andrea Caramés, Cecilia R. Amenábar, and Marina Lescano. "Nannofossils, foraminifera and microforaminiferal linings in the Cenozoic diamictites of Cape Lamb, Vega Island, Antarctica." Polish Polar Research 35, no. 1 (March 1, 2014): 1–26. http://dx.doi.org/10.2478/popore-2014-0003.

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AbstractMicropaleontological and palynological samples from three Cenozoic diamictites at Cape Lamb, Vega Island, James Ross Basin were analysed. Fossiliferous samples yielded reworked and autochthonous assemblages of Mesozoic calcareous nanno− fossils, impoverished Cretaceous foraminifera together with Neogene species, as well as Late Cretaceous dinoflagellate cysts, pollen, spores and abundant Cenozoic micro− foraminiferal linings. The recovered nannoflora indicates Early Cretaceous (Hauteri− vian-Albian) and Late Cretaceous (Santonian-Early Campanian) ages, suggesting an in− tensive reworking of marine sediments. The presence of the Early Cretaceous species Nannoconus circularis Deres et Acheriteguy in the diamictite represents its first record for the James Ross Basin. The scarce foraminiferal fauna includes Pullenia jarvisi Cushman, which indicates reworking from lower Maastrichtian-lower Paleocene sediments, and also the Neogene autochthonous Trochammina sp. aff. T. intermedia. The in− ner−organic layer observed inside this specimen appears to be identical to microfora− miniferal linings recovered from the same sample. Palynomorphs found in the studied samples suggest erosion from the underlying Snow Hill Island and the Lopez de Bertodano Formation beds (upper Campanian-upper Maastrichtian). These recovered assemblages indicate either different periods of deposition or reworking from diverse sources during Cenozoic glaciation, originating in James Ross Island and the Antarctic Peninsula with the influence of local sediment sources.

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23

Mortimer, N., P. B. Gans, and D. C. Mildenhall. "A middle-late Quaternary age for the adakitic arc volcanics of Hautere (Solander Island), Southern Ocean." Journal of Volcanology and Geothermal Research 178, no. 4 (December 2008): 701–7. http://dx.doi.org/10.1016/j.jvolgeores.2008.09.003.

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24

Elfjiji, H., A. Boukdir, and A. Zitouni. "Application of the Electrical (Geophysical) Method for the Identification of the Sealed Bevel in the Coastal Region of Walidia Province of el Jadida – Morocco." E3S Web of Conferences 37 (2018): 05003. http://dx.doi.org/10.1051/e3sconf/20183705003.

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The Walidia area knows a great development of agricultural, industrial, maritime activities and a very great demographic expansion. This development is accompanied by a growing demand for water. On the other hand, any intense abstraction of fresh water at a coastal aquifer capture field causes a decrease in groundwater flow and a lowering of the piezometric surface. There is therefore a danger of advancing towards the land of the saltwater bevel and salinization of groundwater which is gradually loaded into mineral salts and can reach abnormally high levels. This work deals with the application of geophysics by electrical sounding method to the in-depth study of the freshwater-salt water interface (salted bevel) on the one hand and the study of the lateral and vertical evolution of the geometry of the different aquifers. The principle of the method is, when performing an electrical survey, to research how varies, at a given point on the surface, the resistivity of the subsoil vertically. For this one executes in a same place a succession of measurements, increasing each time the dimensions of the device and thus the depth of investigation which is proportional to them. At this site, we explore a slice of ground increasingly thick and thus highlights the changes in geological constitution along the vertical. The electrical soundings were carried out with the classic Schlumberger device. The interpretation and the exploitation of the data of the electric soundings carried out made it possible to : Follow the evolution of the salted bevel roof, Draw the upstream limit (marine invasion) of salted bevel Hauterivian, on the one hand, and Valanginian and Jurassic on the other hand, Follow the roof structure of Dridrat limestone (Hauterivien) and limestones of Valanginien and Upper Jurassic, Draw the map of the marl roof of Safi (Hauterivian) constituting the impermeable substratum of Dridrat limestones.

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25

Tchoumatchenco, Platon, Todor Nikolov, Dimitar Kozhoukharov, Benyo Benev, Petar Gočev, Nikola Katzkov, Khrischo Khrischev, et al. "Le Crétacé inférieur dans le Massif de lʼOuarsenis et les Monts de Tiaret (Algérie du Nord)." Geologica Balcanica 25, no. 2 (April 30, 1995): 27–60. http://dx.doi.org/10.52321/geolbalc.25.2.27.

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The Lower Cretaceous sediments in the Monts de Tiaret (Oranian High Plains) (Tlemcenian Palaeogeographic Domain) and the Western Ouarsenis (Tellian Palaeogeographic Domain) are subdivided in lithostratigraphic units which differ for the Tlemcenian and the Tellian Domains. In the first one, a specific feature is the development of shalow, and in the second – of deep water sediments. The following formal lithostratigraphic units are distinguished in the Tlemcenian Domain: (1) Remaïlia Carbonate Formation – limestones, marls and dolomites (Berriasian – Early Hauterivian (p.p.); (2) Berthelot Sandstone Formation (Early Hauterivien (p.p.) – Aptian); (3) Djebel Tenfeld Carbonate Formation – alternation of marls and limestones, rich in shallow water molluscs. Within the Tellian Atlas (Tell ian Domain) are distinguished: (l) Oued Fodda Carbonate Formation (Late Tithonian – Early Aptian); (2) El Melaab Turbiditic Formation (new unit of Aptian (p.p.) – Early Albian age) subdivided in 2 new Members: (a) Oued Sidi Mohamed Member (Aptian) – marls with turbiditic sandstones – distal flysch; (b) Oued Mezdar Member (Early Albian) – sandstones with intercalations of marls – proximal flysch; (3) Rhedadoua Marls Formation (Middle – Late (p.p.) Albian; (4) Hassi ben Ziane Carbonate Formation – marls and limestones (Late Albian (p.p.) – Early Cenomanian). In the Chouala region crop out the allochtonous sediments of the Sidi Seba Achir Limestones-Marls Formation (new unit of Berriasian-Middle Aptian Age) subdivided in 3 new members: (a) Oued el Ouakal Member – alternation of marls and limestones (Berriasian – Valanginian); (b) Oued Malah Member - marls (Hauterivian); (c) Sidi Ounes Member – marls and limestones (Barremian – Middle Aptian). The region of the High Plains (Monts de Tiaret) was uplifted at the end of the Jurassic, and the Berriasian sea transgressed over it. The subsidence of the Tellian Domain continued since the Late Jurassic and became an area of turbiditic sedimentation during the Aptian-Early Albian. The sedimentation in the Tlemcenian and Tellian Domains continued without interruption into the Cenomanian.

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26

François, Éric, and Bruno David. "Variations morphologiques des Toxaster (Echinoida : Spatangoida) en regard des fluctuations spatiales (Arc de Castellane, SE France) et temporelles (Valanginien-Hauterivien) du milieu sédimentaire : expression d'un potentiel adaptatif restreint." Geobios 39, no. 3 (May 2006): 355–71. http://dx.doi.org/10.1016/j.geobios.2005.01.002.

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27

Haddoumi, Hamid, André Charrière, Monique Feist, and Bernard Andreu. "Nouvelles datations (Hauterivien supérieur–Barrémien inférieur) dans les « Couches rouges » continentales du Haut Atlas central marocain ; conséquences sur l’âge du magmatisme et des structurations mésozoïques de la chaîne Atlasique." Comptes Rendus Palevol 1, no. 5 (December 2002): 259–66. http://dx.doi.org/10.1016/s1631-0683(02)00039-8.

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28

Abbott, Steve. "Other journals - The cloisters of Hauterive, by Benno Artmann. Mathematical Intelligencer 13 2 pp 44–49 - A portrait of Alfred Tarski, by Steven R. Givant. Mathematical Intelligencer 13 3 pp 16–32 - The ultimate jigsaw puzzle, by Ian Stewart. New Scientist 13.4.91 pp 30–33. - Mathematical modelling in senior school mathematics: implementing an innovation, by Neville J. Clatworthy and Peter L. Galbraith. Teaching Mathematics and its Applications 10 1 pp 6–28. - Infinity and geometry, by Joseph Rosenblatt. Mathematical Spectrum 23 4 pp 132–136. - The fiftieth William Lowell Putnam mathematical competition, by Leonard F. Klosinski, Gerald L. Alexanderson, and Loren C. Larson. American Mathematical Monthly 98 4 pp 319–327. - Multiple pythagorean number triples, by Albert Fässler. American Mathematical Monthly 98 6 pp 505–517. - Majorization and the birthday inequality, by M. Lawrence Clevenson and William Watkins. Mathematics Magazine 64 3 pp 183–188. - The Evolution of stochastic strategies in the prisoner’s dilemma, by Martin Nowak and Karl Sigmund. Acta Applicandae Mathematicae 20 3 pp 247–265." Mathematical Gazette 75, no. 474 (December 1991): 460–62. http://dx.doi.org/10.1017/s0025557200150521.

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29

Thévenin, Éric. "Magneux-Hauterive." ADLFI. Archéologie de la France - Informations, August 11, 2015. http://dx.doi.org/10.4000/adlfi.15261.

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30

Chabrié, Christophe, and Jean-François Garnier. "Pinel-Hauterive." ADLFI. Archéologie de la France - Informations, March 1, 2008. http://dx.doi.org/10.4000/adlfi.2736.

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31

Bellon, Catherine. "Magneux-Hauterive." ADLFI. Archéologie de la France - Informations, March 1, 2007. http://dx.doi.org/10.4000/adlfi.7107.

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32

Cahen, Raphaël. "Hauterive et l’école des diplomates (1800-1830)." Histoire du droit international, no. 18 (February 23, 2021). http://dx.doi.org/10.35562/cliothemis.335.

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Le comte d’Hauterive, qui fut l’une des figures majeures de la diplomatie française de la fin du Directoire au début de la monarchie de Juillet, a consacré une grande partie de sa carrière à la formation des diplomates à travers la création d’une école rattachée au ministère des Affaires étrangères. L’école entretenait des relations ambiguës avec le droit de gens et n’a jamais vraiment réussi à professionnaliser le métier de diplomate. En revanche, les trajectoires de trois des anciens élèves-aspirants, qui ont occupé le poste de président du Comité consultatif du contentieux du ministère des Affaires étrangères, peuvent témoigner d’une certaine juridicisation des relations internationales.

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33

HAJDAS, I. "Radiocarbon and absolute chronology of the Late-Glacial record from Hauterive/Rouges-Terres, Lake Neuch�tel (CH)." Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, May 2004. http://dx.doi.org/10.1016/s0168-583x(04)00586-5.

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34

Petiteau, Natalie. "Philippe HENRY [dir.], La mémoire de la Révolution neuchâteloise de 1848. Du Cinquantenaire au Centenaire, 1898-1948, Hauterive, Éditions Gilles Attinger, 1997, 251 p." Cahiers d’histoire, no. 43-2 (March 1, 1998). http://dx.doi.org/10.4000/ch.186.

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35

Bardachevskiy, V. N., N. I. Shestakova, and S. V. Ershov. "Features of formation of Gydan Peninsula Hauteriv-Barremian clinoform." Neftegazovaya Geologiya. Teoriya I Praktika 14, no. 4 (2019). http://dx.doi.org/10.17353/2070-5379/45_2019.

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36

MOJON, Pierre-Olivier, Antonio MUSOLINO, Stefan BUCHER, and Bernard CLAUDE. "Nouvelles données sur les ammonites du Valanginien - Hauterivien de la région stratotypique de Neuchâtel (Jura suisse) : implications biostratigraphiques." Carnets de géologie (Notebooks on geology), August 2013, 237–54. http://dx.doi.org/10.4267/2042/51216.

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37

CLAVEL, Bernard, Robert BUSNARDO, Jean CHAROLLAIS, Marc CONRAD, and Bruno GRANIER. "Répartition biostratigraphique des orbitolinidés dans la biozonation à ammonites (plate-forme urgonienne du Sud-Est de la France) Partie 1 : Hauterivien supérieur - Barrémien basal." Carnets de géologie (Notebooks on geology), ar (2010). http://dx.doi.org/10.4267/2042/33369.

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