RT Journal Article
T1 Evolución paleoambiental del tránsito Eoceno-Oligoceno en el Atlántico sur (Sondeo 1263) basada en foraminíferos bentónicos
T1 Paleoenvironmental evolution of the Eocene-Oligocene transition in the South Atlantic (Site 1263) based onbenthic foraminifera
A1 Fenero, Raquel
A1 Thomas, Ellen
A1 Alegret, Laia
A1 Molina, Eustoquio
AB Quantitative análisis of benthic foraminiferal assemblages at South Atlantic Site 1263 providedinformation about paleobathymetry and changes in benthic foraminiferal faunas across the Eocene-Oligoceneboundary. Benthic foraminifera indicate an upper abyssal depth (~ 2000 m). Changes in relative abundancesof Epistominella exigua, Epistominella vitrea, Globocassidulina subglobosa and Nuttallides umbonifera,probably indicate variability in seasonality of export productivity, bottom current intensity and carbonatecorrosivity. The transition into glaciation event Oi-1 is characterized by highly seasonal productivity, Oi-1itself by less variability, probably at fairly active bottom currents
PB Universidad de Huelva
YR 2010
FD 2010
LK http://hdl.handle.net/10272/7471
UL http://hdl.handle.net/10272/7471
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 14 jul 2026