Mots-clés
Australie ; Holocène ; Mer de Tasmanie ; Pacifique ; Pacifique Sud ; Paléoclimat ; Poussière éolienne ; Précipitation ; Quaternaire ; Tardiglaciaire ; Vent ; VégétationAeolian dust ; Australia ; Holocene ; Lateglacial ; Pacific Region ; Palaeoclimate ; Precipitation ; Quaternary ; South Pacific Ocean ; Vegetation ; WindLast Glacial Maximum to early Holocene wind strength in the mid-latitudes of the Southern Hemisphere from aeolian dust in the Tasman Sea
Auteurs :HESSE, P.P.
MCTAINSH, G.H.
Description :
In this study, 2 deep-sea sediment cores, from near the center of the dust path that crosses the Tasman Sea from Australia, were sampled for particle-size analysis of eolian dusts deposited from the Last Glacial Maximum, (LGM), to the Holocene by the Southern Hemisphere zonal westerly winds. From these results it appears that activation of desert dunefields over 40% of Australia during the LGM was the result of a reduction in stabilizing vegetation and more frequent episodes of sand movement rather than of increased wind strength.
Type de document :
Article de périodique
Source :
Quaternary research, issn : 0033-5894, 1999, vol. 52, n°. 3, p. 343-349, Collation : Illustration, Références bibliographiques : 52 ref.
Date :
1999
Editeur :
Pays édition : Etats-Unis, San Diego, CA, Elsevier
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)