@article{10272/8339,
year = {2007},
url = {http://hdl.handle.net/10272/8339},
abstract = {Samples from the Alboran Sea (Western Mediterranean) were studied in order to characterise the organic
rich layers recorded during marine isotope stage 7 from a geochemical point of view. X ray fluorescence
measurements were carried out at a 1cm-resolution and variations in terrigenous and biogenic elements
were observed during the whole studied interval (245-190 kyr), suggesting more carbonate production
during warmer periods, and more arrival of terrigenous material during lower-sea level substages. Organic
rich layers were characterized by high biogenic barium and low Si/Al, which can be interpreted as increasing
surface productivity or better preservation of the organic material, and more river discharge due to more
abundant precipitations},
title = {Caracterización geoquímica de las capas ricas en materia orgánica registradas durante el estadio isotópico marino 7 en el Mar de Alborán (Mediterráneo occidental)},
title = {Geochemical characterization of the organic rich layers recorded during marine isotope stage 7 in the Alboran Sea
(Western Mediterranean)},
author = {González Mora, Beatriz and Sierro, Francisco Javier},
}