Showing 121 - 140 results of 684 for search '"Pyrenees"', query time: 0.07s Refine Results
  1. 121

    New palaeobotanical data from Carboniferous Culm deposits constrain the age of the Variscan deformation in the eastern Pyrenees by C. MARTÍN-CLOSAS, S. TRIAS, J.M. CASAS

    Published 2018-06-01
    “… The pre-Variscan rocks of the Pyrenees exhibit a polyphase deformation linked to the Variscan crustal shortening and a low-pressure–high-temperature metamorphism. …”
    Get full text
    Article
  2. 122

    Winter tourism under climate change in the Pyrenees and the French Alps: relevance of snowmaking as a technical adaptation by P. Spandre, P. Spandre, H. François, D. Verfaillie, D. Verfaillie, M. Pons, M. Vernay, M. Lafaysse, E. George, S. Morin

    Published 2019-04-01
    “…The reliability elevation using snowmaking is projected to rise by 200 to 300 m in the Alps and by 400 to 600 m in the Pyrenees in the near future (2030–2050) compared to the reference period for all climate scenarios. …”
    Get full text
    Article
  3. 123

    La mise en oeuvre des chartes forestières de territoire : exemple des Pyrénées-Orientales by D. BOURGOUIN, G. VAN PETEGHEM

    Published 2002-04-01
    “…L'exemple concret de l'aménagement des suberaies dans les Pyrénées-Orientales illustre parfaitement cette nouvelle politique.…”
    Get full text
    Article
  4. 124
  5. 125

    The Perspective of Arctic–Alpine Species in Southernmost Localities: The Example of <i>Kalmia procumbens</i> in the Pyrenees and Carpathians by Łukasz Walas, Marcin Pietras, Małgorzata Mazur, Ángel Romo, Lydia Tasenkevich, Yakiv Didukh, Adam Boratyński

    Published 2023-09-01
    “…The realized niches of <i>K. procumbens</i> in the Pyrenees are compact, while those in the Carpathians are dispersed. …”
    Get full text
    Article
  6. 126
  7. 127

    Increasing size and abundance of microbialites (oncoids) in connection with the K/T boundary in non-marine environments in the South Central Pyrenees by H. ASTIBIA, N. LÓPEZ-MARTÍNEZ, J.J. ELORZA, E. VICENS

    Published 2012-10-01
    “… A layer rich in giant microbialites, developed within continental deposits of the Tremp Formation (South-Central Pyrenees) in the aftermath of the end-Cretaceous mass extinctions, is here reported for the first time. …”
    Get full text
    Article
  8. 128

    Climatic and Anthropogenic Drivers of Forest Succession in the Iberian Pyrenees during the Last 500 Years: A Statistical Approach by Valentí Rull, Teresa Vegas-Vilarrúbia

    Published 2022-04-01
    “…This paper uses independent high-resolution palynological and paleoclimatic reconstructions to statistically analyze the long-term effects of external drivers on regional forest succession in the central Iberian Pyrenees during the last 500 years. The statistical methods used are Gaussian response analysis, cluster analysis, rate-of-change analysis, principal component analysis, and redundancy analysis. …”
    Get full text
    Article
  9. 129

    The early/middle Eocene transition at the Ésera valley (South Central Pyrenees): Implications in Shallow Benthic Zones (SBZ) by Adriana Rodríguez-Pintó, Josep Serra-Kiel, Gilen Bernaola, Antonio Barnolas, Emilio L. Pueyo, Josep Tosquella, Pau Arbués, Robert Scholger

    Published 2022-07-01
    “…This work was performed in shallow marine siliciclastics rich in larger foraminifera, around the Ypresian/Lutetian boundary in the Ésera valley (South-Central Pyrenees). Although the calcareous nannofossil content in the studied interval is low, not allowing a precise Y/L boundary to be recognised, the taxa found are enough to support the chronostratigraphic attribution. …”
    Get full text
    Article
  10. 130

    The early/middle Eocene transition at the Ésera valley (South Central Pyrenees): Implications in Shallow Benthic Zones (SBZ) by Adriana Rodríguez-Pintó, Josep Serra-Kiel, Gilen Bernaola, Antonio Barnolas, Emilio L. Pueyo, Josep Tosquella, Pau Arbués, Robert Scholger

    Published 2022-07-01
    “…This work was performed in shallow marine siliciclastics rich in larger foraminifera, around the Ypresian/Lutetian boundary in the Ésera valley (South-Central Pyrenees). Although the calcareous nannofossil content in the studied interval is low, not allowing a precise Y/L boundary to be recognised, the taxa found are enough to support the chronostratigraphic attribution. …”
    Get full text
    Article
  11. 131
  12. 132
  13. 133
  14. 134
  15. 135

    Nannofossils from the Middle Eocene Sabiñánigo Sandstone Formation in the Jaca Basin (southern Pyrenees): biostratigraphy and paleoenvironmental implications by E. R. Lasluisa, O. Oms, E. Remacha, A. González-Lanchas, H. Blanchar-Roca, J. A. Flores

    Published 2024-04-01
    “…<p>This study presents the first detailed data on calcareous nannofossil assemblages from the Sabiñánigo Sandstone Formation in the Jaca Basin (central south Pyrenees). This formation is mainly composed of deltaic and outer-shelf sediments. …”
    Get full text
    Article
  16. 136
  17. 137
  18. 138

    A new look at old debates about the Corbières (NE-Pyrenees) geology: salt tectonics and gravity gliding by Parizot Oriane, Frizon de Lamotte Dominique, Missenard Yves

    Published 2023-01-01
    “…This geological object is located at the NE of the Pyrenees, close to the Gulf of Lions. At this place, the chain changes in orientation from E-W to NE-SW and presents in detail, a great complexity. …”
    Get full text
    Article
  19. 139

    Detection of tick-borne pathogens in questing Ixodes ricinus in the French Pyrenees and first identification of Rickettsia monacensis in France by Akl Toufic, Bourgoin Gilles, Souq Marie-Line, Appolinaire Joël, Poirel Marie-Thérèse, Gibert Philippe, Abi Rizk Georges, Garel Mathieu, Zenner Lionel

    Published 2019-01-01
    “…In this study, we estimated the prevalence of important tick-borne infections in questing ticks from an area in Southwestern France (Hautes-Pyrénées) inhabited by Pyrenean chamois (Rupicapra pyrenaica pyrenaica) experiencing high tick burden. …”
    Get full text
    Article
  20. 140