Reconstruccion de la vegetación asociada a depósitos tobáceos fluviales holocenos del sistema ibérico

  1. Josu Aranbarri 1
  2. C. Sancho 2
  3. C. Arenas 2
  4. M. Bartolomé 3
  5. M. Alcolea 4
  6. A. Celant 5
  7. M. Leunda 2
  8. P. González-Sampériz 6
  1. 1 Universidad del País Vasco/Euskal Herriko Unibertsitatea
    info

    Universidad del País Vasco/Euskal Herriko Unibertsitatea

    Lejona, España

    ROR https://ror.org/000xsnr85

  2. 2 Universidad de Zaragoza
    info

    Universidad de Zaragoza

    Zaragoza, España

    ROR https://ror.org/012a91z28

  3. 3 Museo Nacional de Ciencias Naturales-CSIC
  4. 4 Universidade de Santiago de Compostela
    info

    Universidade de Santiago de Compostela

    Santiago de Compostela, España

    ROR https://ror.org/030eybx10

  5. 5 Università de Roma La Sapienza
    info

    Università de Roma La Sapienza

    Roma, Italia

    ROR https://ror.org/02be6w209

  6. 6 Instituto Pirenaico de Ecología-CSIC
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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: 293-296

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

Tipo: Aportación congreso

DIALNET GOOGLE SCHOLAR lock_openAcceso abierto editor

Resumen

Fluvial tufa build-ups located in the Queiles, Val and Las Parras del Martín river valleys (Iberian Range, NE Iberia), are investigated following radiocarbon dating, palynological and anthracological analyses. The studied tufa deposits have been framed within the Early-MidHolocene (ca. 9500 to 4000 cal yr BP) in agreement with regional palaeoenvironmental evidences. The obtained palaeobotanical results highlight the existence of dense riparian woodland where diverse broadleaved trees defined the main vegetation features in the river valleys.Deciduous and evergreen oaks were the main spread regional forests accompanied by many warm-loving taxa. Pinewoods were usually confined to high-altitude elevations, although their presence is also relevant around El Batán deposit (in Las Parras del Río Martín) during the Early Holocene. The transition towards the Late Holocene is evidenced by the rise of nitrophilous and ruderal taxa, which are linked to the spread of agricultural and grazing practices along the river valleys.

Fuente de los datos: Dialnet