Impulsores antrópicos y climáticos en la evolución geoambiental de la región cantábrica durante el Antropocenointegrando evidencias geomorfológicas y registros sedimentarios costeros y lacustres

  1. M. Morellón 1
  2. Juan Remondo 2
  3. Jaime Bonachea 2
  4. V. Brusch 2
  5. J.L. Cavallotto
  6. J. Fernández-Lozano 2
  7. Luis María Forte 3
  8. J. E. Gómez-Arozamena
  9. Alberto González-Díez 2
  10. F. González-Soto 3
  11. I. Hernández-Almeida 7
  12. M. Leira 4
  13. César Morales del Molino 5
  14. V. Rivas 2
  15. C. Sierra-Fernández 6
  16. Antonio Cendrero 2
  1. 1 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

  2. 2 Universidad de Cantabria
    info

    Universidad de Cantabria

    Santander, España

    ROR https://ror.org/046ffzj20

  3. 3 Universidad Nacional de La Plata
    info

    Universidad Nacional de La Plata

    La Plata, Argentina

    ROR https://ror.org/01tjs6929

  4. 4 Universidade de Lisboa
    info

    Universidade de Lisboa

    Lisboa, Portugal

    ROR https://ror.org/01c27hj86

  5. 5 University of Bern
    info

    University of Bern

    Berna, Suiza

    ROR https://ror.org/02k7v4d05

  6. 6 Universidad de León
    info

    Universidad de León

    León, España

    ROR https://ror.org/02tzt0b78

  7. 7 Department of Earth Sciencies, ETH-Zürich
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Libro:
XV Reunión Nacional de Cuaternario Bizkaia Aretoa: Bilbao, 1-5 julio 2019. Libro de resúmenes

Editorial: Universidad del País Vasco = Euskal Herriko Unibertsitatea

ISBN: 978-84-17713-16-4

Año de publicación: 2019

Páginas: 199-202

Congreso: Reunión Nacional de Cuaternario (15. 2019. Bilbao)

Tipo: Aportación congreso

DIALNET GOOGLE SCHOLAR lock_openAcceso abierto editor

Resumen

This research aims at understanding how recent (19th to 21st centuries) warming and increasing human activities have affected the geomorphological dynamics of the Cantabrian region, subjected to a comparatively high human pressure during this period. In this work, we use a multi-archive and multi-site approach, integrating available high-resolution estuarine (Tina-Menor, San Vicente, Rabia, Suances, Maruca, Santander, Santoña, Muskiz and Urdaibai) and lake (La Cueva, Enol) sedimentary records located across W to E longitudinal and altitudinal (0-1500 m.a.s.l.) transects. Preliminary results indicate a marked increase in sedimentation rates during the so-called ‘Great Acceleration’, recorded after the second half of the 20th century and mainly driven by the economic growth and associated human impact in this area. The extension of this research to other lacustrine watersheds located at different altitudes and subjected to different levels of anthropic pressure and the application of other proxies (sedimentology and geochemistry) will clarify the relative contribution of climate change and human impact to reconstructed environmental changes.

Fuente de los datos: Dialnet