Variabilidad climática durante la última deglaciación a partir del estudio del registro espeleotémico de la cueva de Stolo, Pirineos occidentales, España

  1. J.L. Bernal-Wormull 1
  2. A. Moreno 1
  3. M. Bartolomé 2
  4. A. Aranburu 3
  5. M. Arriolabengoa 3
  6. E. Iriarte
  7. C.Spötl 4
  8. H. Cheng 5
  1. 1 Instituto Pirenaico de Ecología
    info

    Instituto Pirenaico de Ecología

    Zaragoza, España

    ROR https://ror.org/039ssy097

  2. 2 Museo Nacional de Ciencias Naturales (CSIC)
  3. 3 Universidad del País Vasco/Euskal Herriko Unibertsitatea
    info

    Universidad del País Vasco/Euskal Herriko Unibertsitatea

    Lejona, España

    ROR https://ror.org/000xsnr85

  4. 4 University of Innsbruck
    info

    University of Innsbruck

    Innsbruck, Austria

    ROR https://ror.org/054pv6659

  5. 5 Xi'an Jiaotong University
    info

    Xi'an Jiaotong University

    Xi'an, China

    ROR https://ror.org/017zhmm22

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: 349-352

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

Mota: Biltzar ekarpena

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Laburpena

A new record of last deglaciation in northeastern Spain is presented here based on the 18O variations from two stalagmites from Ostolo cave (W Pyrenees). The two stalagmites replicate very well the signal of abrupt changes that took place during the last deglaciation (18 – 10 ka BP) in synchrony with temperature changes in Greenland ice cores. A comparison with other nearby records (marine cores, lacustrine sediments and speleothems from northern Spain and southern France) allows discriminating different trends during last deglaciation indicating a high heterogeneity in the paleoenvironmental response to climate variability at this latitude

Datuen iturria: Dialnet