La deglaciación temprana en el Pirineo centralel registro de la turbera de El Portalet

  1. P. González Sampériz 1
  2. B.L. Valero Garcés 2
  3. J.M. García Ruiz 2
  4. G. Jalut 3
  5. A. Moreno 2
  6. A. Navas 4
  7. C. Martí Bono 2
  8. T. Otto 3
  9. A. Delgado Huertas 5
  10. J.J. Dedoubat 3
  1. 1 Instituto Pirenaico de Ecología-CSIC
  2. 2 Instituto Pirenaico de Ecología-C
  3. 3 ADYBIO Univ. Paul Sabatier - UMR, Toulouse, Francia
  4. 4 Estación Experimental de Aula Dei
    info

    Estación Experimental de Aula Dei

    Zaragoza, España

    ROR https://ror.org/056a37x91

  5. 5 EEZ-CSIC
Erakutsi afiliazioak +
Aldizkaria:
Geotemas (Madrid)

ISSN: 1576-5172

Argitalpen urtea: 2004

Zenbakien izenburua: VI CONGRESO GEOLÓGICO DE ESPAÑA, ZARAGOZA, 12-15 JULIO, 2004

Zenbakia: 6

Orrialdeak: 101-104

Mota: Artikulua

DIALNET GOOGLE SCHOLAR lock_openSarbide irekia editor

Beste argitalpen batzuk: Geotemas (Madrid)

Laburpena

Palynological, sedimentological, and stable isotope analyses performed in El Portalet sequence (Gállego River headwaters, Spanish Central Pyrenees) reflect the climate evolution and vegetational changes in the Central Pyrenean Range since Oxygen Isotope Stage 3 mid Holocene (ca.30.000-5000 yr B.P.) The results confirm the early déglaciation in the Pyrenees compared to northern European and other Alpine mountain ranges. A minor glacial readvance at about 20 ka coincided with the global Last Glacial Maximum. The new data illustrate similarities and differences ofclimate and vegetation evolution during the last déglaciation between the Mediterranean and the central and northern European mountain regions.

Datuen iturria: Dialnet