Dinámica climática y de la vegetación durante el Interestadial Würmiense (60-25ky bp) en el NW ibérico

  1. Luis Gómez Orellana 1
  2. Pablo Ramil Rego 1
  1. 1 Universidade de Santiago de Compostela
    info

    Universidade de Santiago de Compostela

    Santiago de Compostela, España

    ROR https://ror.org/030eybx10

Journal:
Férvedes: Revista de investigación

ISSN: 1134-6787

Year of publication: 2015

Issue: 8

Pages: 55-64

Type: Article

DIALNET GOOGLE SCHOLAR

More publications in: Férvedes: Revista de investigación

Abstract

Isotopic sequences show the existence of numerous climatic oscillations occurred during the last glacial period in the North Atlantic, particularly during the Würm interstadial (MIS 3). This episode shows a glacial retreat northward and an intensification of the climatic oscillations. Along the NW Iberian coast there is an important set of fossilized deposits, which records this and other periods of the last glacial. The sequence reflects an alternation of phases of expansion and detraction of forests. The data reveal the strategic situation of the Iberian Northwest to assessing the vegetation response to changes in the North Atlantic, and the presence of areas of refuge for mesophilous and thermophilous trees.

Data source: Dialnet