Registro edáfico de los cambios paleoambientales en la depresión del Guadalentín durante el Holoceno (Murcia, SE España)

  1. Elvria Roquero 1
  2. P.G.Silva 2
  3. J. Élez 2
  4. M.A. Rodríguez-Pascua 3
  5. A. Medialdea 4
  6. Jorge L. Giner 5
  7. R. Pérez López 3
  8. Teresa Bardají 6
  1. 1 Universidad Politécnica de Madrid
    info

    Universidad Politécnica de Madrid

    Madrid, España

    ROR https://ror.org/03n6nwv02

  2. 2 Universidad de Salamanca
    info

    Universidad de Salamanca

    Salamanca, España

    ROR https://ror.org/02f40zc51

  3. 3 Instituto Geológico y Minero de España (IGME)
  4. 4 University of Cologne
    info

    University of Cologne

    Colonia, Alemania

    ROR https://ror.org/00rcxh774

  5. 5 Universidad Autónoma de Madrid
    info

    Universidad Autónoma de Madrid

    Madrid, España

    ROR https://ror.org/01cby8j38

  6. 6 Universidad de Alcalá
    info

    Universidad de Alcalá

    Alcalá de Henares, España

    ROR https://ror.org/04pmn0e78

Erakutsi afiliazioak +
Liburua:
XV Reunión Nacional de Cuaternario Bizkaia Aretoa: Bilbao, 1-5 julio 2019. Libro de resúmenes

Argitaletxea: Universidad del País Vasco = Euskal Herriko Unibertsitatea

ISBN: 978-84-17713-16-4

Argitalpen urtea: 2019

Orrialdeak: 235-238

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

Mota: Biltzar ekarpena

DIALNET GOOGLE SCHOLAR lock_openSarbide irekia editor

Laburpena

The Guadalentín Depression is the more outstanding landscape feature generated by strike-slip faulting within the central segment of the Eastern Betic Shear Zone (EBSZ).This depression evolved under lacustrine to palustrine (playa-lake) conditions until at least roman times. This work-study paleosols interbedded in the sedimentary sequence of the Espuña Karting profile anddeveloped on calcium carbonate rich fine parent material. Soil morphology and properties from two dated paleosols represent twodifferent environmental crisis, the oldest paleosol from the Bronce Age, developed under conditions that are more humid and indicates a long rupture in sedimentary depression. Roman period paleosol, developed under Mediterranean semiarid conditions, also indicates an important rupture in the depression evolving from palustrine to the present fluvial environment.

Datuen iturria: Dialnet