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Environmental changes over the past 25 000 years in the southern Middle Atlas, Morocco

Tabel, Jalal ; Khater, Carla ; Rhoujjati, Ali ; Dezileau, Laurent ; Bouimetarhan, Ilham ; Carre, Matthieu ; Vidal, Laurence ; Benkaddour, Abdelfattah ; Nourelbait, Majda ; Cheddadi, Rachid

Journal of quaternary science, 2016-02, Vol.31 (2), p.93-102 [Periódico revisado por pares]

Blackwell Publishing Ltd

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  • Título:
    Environmental changes over the past 25 000 years in the southern Middle Atlas, Morocco
  • Autor: Tabel, Jalal ; Khater, Carla ; Rhoujjati, Ali ; Dezileau, Laurent ; Bouimetarhan, Ilham ; Carre, Matthieu ; Vidal, Laurence ; Benkaddour, Abdelfattah ; Nourelbait, Majda ; Cheddadi, Rachid
  • Assuntos: Cedrus atlantica ; Earth Sciences ; Last Glacial Maximum ; Mediterranean environments ; Morocco ; pollen ; Sciences of the Universe
  • É parte de: Journal of quaternary science, 2016-02, Vol.31 (2), p.93-102
  • Notas: ark:/67375/WNG-3WZVM7JG-F
    French EC2CO programme
    istex:3DF259A1F0FDD63DF317C8A687EACBE9C54F6672
    ArticleID:JQS2841
  • Descrição: ABSTRACT A new fossil record from the southern Middle Atlas spans continuously the last 25 000 years and provides evidence of an increased amount of snow precipitation during the last glacial period and a warm early Holocene with rather dry climate conditions. This environmental reconstruction is based on a multi‐proxy approach that integrates pollen, micro‐charcoals, grain size and geochemical analysis. During the last glacial period we observe a strong presence of aquatic plants species that today flower during late spring and summer. These occurrences are related to an increased amount of snow precipitation on the surrounding mountains which fed the marsh during the summer season. Although the early Holocene reveals a slight and steady expansion of Mediterranean oaks, the semi‐arid Artemisia steppe remained dominant in the landscape until 6.8 ka cal BP. Thus, the early Holocene seems to have been less humid than elsewhere in North Africa. The Atlas cedars began to establish around 6 ka cal BP. This indicates that the amount of annual rainfall increased after the mid‐Holocene. The late Holocene is marked by an increase of fire events, which may be related to a strengthening of the dry season and/or a higher seasonality.
  • Editor: Blackwell Publishing Ltd
  • Idioma: Inglês

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