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Sedimentary response to climate and sea level changes during the past similar to 400 ka from borehole PRAD1-2 (Adriatic margin) - art. no. Q09R04 5
Ridente, D; Trincardi, F; Piva, A; Asioli, A; Cattaneo, Antonio.
[1] Borehole PRAD1-2 was drilled in similar to 186 m water depth on the upper slope of the central Adriatic, in the frame of Profiles across Mediterranean Sedimentary Systems (PROMESS1) European Union-funded project. The borehole penetrated 71.2 m through a stratigraphic interval characterized by subparallel seismic reflections and uniform seismic units. According to an age-depth model based on several independent proxies (including foraminifera and nannoplankton stratigraphy, delta O-18 curves, and magnetostratigraphy) the cored interval records Marine Isotope Stages and Substages (MIS) from MIS1 to the top of MIS11, thus encompassing the past similar to 370 ka. PRAD1-2 therefore represents an unprecedented continuous record through the last four...
Tipo: Text Palavras-chave: Adriatic Sea; Depositional sequences; High frequency climate cycles; Quaternary.
Ano: 2008 URL: http://archimer.ifremer.fr/doc/2008/publication-4759.pdf
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On the Barremian - lower Albian stratigraphy of Colombia 16
Hoedemaeker, P.J..
The biostratigraphy and sequence stratigraphy of the Barremian deposits, and the biostratigraphy of the Aptian deposits in the Villa de Leyva area in Colombia are briefly described.
Tipo: Article / Letter to the editor Palavras-chave: Stratigraphy; Barremian; Aptian; Depositional sequences; Colombia; 38.16.
Ano: 2004 URL: http://www.repository.naturalis.nl/record/214456
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