FN Archimer Export Format
PT J
TI Climatic cycles as expressed in sediments of the PROMESS1 borehole PRAD1-2, central Adriatic, for the last 370 ka: 1. Integrated stratigraphy - art. no. Q01R01
BT 
AF PIVA, A
   ASIOLI, A
   SCHNEIDER, R
   TRINCARDI, F
   ANDERSEN, N
   COLMENERO HIDALGO, E
   DENNIELOU, Bernard
   FLORES, J
   VIGLIOTTI, L
AS 1:1;2:2;3:3;4:1;5:4;6:5;7:6;8:7;9:1;
FF 1:;2:;3:;4:;5:;6:;7:PDG-DOP-DCB-GM-LES;8:;9:;
C1 CNR, ISMAR, I-40129 Bologna, Italy.
   CNR, IGG, I-35100 Padua, Italy.
   Univ Kiel, Inst Geowissensch, D-24118 Kiel, Germany.
   Univ Kiel, Leibniz Lab Radiomet Dating & Stable Isotope Res, D-24118 Kiel, Germany.
   Univ Salamanca, Fac Ciencies, Dept Geol, E-37008 Salamanca, Spain.
   IFREMER, Dept Geosci Marines, F-29280 Plouzane, France.
   Univ Salamanca, Dept Geol, E-37008 Salamanca, Spain.
C2 CNR, ITALY
   CNR, ITALY
   UNIV KIEL, GERMANY
   UNIV KIEL, GERMANY
   UNIV SALAMANCA, SPAIN
   IFREMER, FRANCE
   UNIV SALAMANCA, SPAIN
SI BREST
SE PDG-DOP-DCB-GM-LES
IN WOS Ifremer jusqu'en 2018
   copubli-europe
IF 2.979
TC 47
UR https://archimer.ifremer.fr/doc/2008/publication-3605.pdf
LA English
DT Article
DE ;Sapropel stratigraphy;Adriatic Sea;D O events;Foraminifera;Oxygen isotope stratigraphy;Late Quaternary
AB [1] A multiproxy integrated chronological framework, based on oxygen and carbon stable isotope stratigraphy, biostratigraphy (foraminifera and nannoplankton bioevents and foraminifer assemblage-based climate cyclicity), magnetostratigraphy, sapropel stratigraphy, and C-14 AMS radiometric dates, has been achieved for borehole PRAD1-2, collected in 185.5 m water depth in the central Adriatic. This work was carried out within the European Community project Profiles across Mediterranean Sedimentary Systems (PROMESS1). The 71.2 m long borehole spans a time interval between late MIS 11 and MIS 1 (the last 370 ka), showing a chronological resolution of 500 and 250 years per cm during interglacial and glacial intervals, respectively. At present, this record is the most expanded and continuous marine record available for the Adriatic Basin. Several orbital cycles can be recognized in the PRAD1-2 record: the 100 ka glacial-interglacial fluctuations and the 23 ka precession-related cycles, which in turn control the deposition of sapropel layers. An integrated analysis of short-term oscillations within the Last Glaciation interval (MIS 4-MIS 2) allowed the identification of the Adriatic signature of Dansgaard-Oeschger events, showing the potential to achieve a more refined chronostratigraphic framework for the top part of the PRAD1-2 record. Finally, the age model obtained by this study allowed the chronological integration of the main foraminifera bioevents detected in the borehole as well as of the volcanoclastic layers present in the upper part of the record. Despite its proximal location, PRAD1-2 presents a continuous record and shows the potential to be consistently correlated both with deep-sea and continental records in the Mediterranean region and beyond.
PY 2008
SO Geochemistry Geophysics Geosystems
SN 1525-2027
PU American Geophysical Union
VL 9
UT 000252361600004
DI 10.1029/2007GC001713
ID 3605
ER

EF