@article{10272/8594,
year = {2006},
url = {http://hdl.handle.net/10272/8594},
abstract = {In this work, preliminary chronostratigaphic features of the Upper Pleistocene-Holocene morphosedimentary
alluvial unit covering the bottom of the Bardena Blanca depression are described. This unit is made up by
1) gravels and sands related to a braided channel system, 2) laminated sands and clays accumulated in
distal flats of alluvial fans and 3) clays and gypsums corresponding to a playa-lake environment. According
the first chronological data supplied by OSL and 14C the age of this sequence ranges between 18 and 5 ka.
The prevailed paleoclimatic conditions were cold and humid during Last Glacial Maximum-Oldest Dryas
and arid during Lower Holocene},
title = {Cronoestratigrafía de los registros aluviales del tránsito Pleistoceno superior-Holoceno en la depresión de la Bardena Blanca (Navarra)},
title = {Chronostratigraphy of Late Pleistocene-Early Holocene alluvial records in the Bardena Blanca depression
(Navarra, Spain)},
author = {Muñoz Jiménez, Arsenio and Sancho, Carlos and Peña, José Luis and Benito, Gerardo and Rhodes, Edward and McDonald, Eric and Longares, Luis Alberto},
}