RT Journal Article
T1 Evolución sedimentaria y geoquímica del Lago de Estanya (Huesca) durante los últimos 21.000 años
T1 Depositional and geochemical evolution of Lake Estanya (Huesca) during the last 21.000 years
A1 Morellón, Mario
A1 Valero Garcés, Blas
A1 Rico, Mayte
A1 Mata, Pilar
A1 Delgado Huertas, Antonio
A1 Romero, Óscar
AB The sedimentary and geochemical evolution of Lake Estanya (NE Spain) documents arid conditions,reflected by shallow water levels, high salinity and low organic productivity during lateglacial times, withintensified aridity during the so-called Mystery Interval (17,500 – 14,500 cal. years BP), the Younger Dryas(13,300 – 11,600 cal. years BP) and prior to the Holocene (11,600 – 9,400 cal. years BP). Higher wateravailability characterized the last 9,400 years, as recorded by most Iberian marine and continental records.The Estanya records demonstrate a high impact of suborbital global climate fluctuations in lake hydrology.Increase in lake level and detrital sediment delivery during the last millenium also indicate changes in landuses in the watershed since Medieval times
YR 2009
FD 2009
LK http://hdl.handle.net/10272/8037
UL http://hdl.handle.net/10272/8037
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026