TY - JOUR
T1 - High-resolution cyclostratigraphic analysis of multiple climate proxies from a short Langhian pelagic succession in the Co`nero Riviera, Ancona (Italy)
AU - Mader, Dieter
AU - Cleaveland, L
AU - Bice, D M
AU - Montanari, Alessandro
AU - Köberl, Christian
N1 - Zeitschrift: Palaeogeography, Palaeoclimatology, Palaeoecology
DOI: 10.1016/j.palaeo.2004.06.001
Coden: PPPYA
Affiliations: Department of Geological Sciences, University of Vienna, Althanstrasse 14, A-1090 Vienna, A.; Department of Geology, Carleton College, Northfield, Minnesota 55057, USA; Osservatorio Geologico di Coldigioco, 62020 Frontale di Apiro, Italy
Adressen: Department of Geological Sciences; University of Vienna; Althanstrasse 14, A-1090 Vienna, A.email: [email protected]
Source-File: EarthScienceScopus_iso.csv
Import aus Scopus: 2-s2.0-4344640108
Importdatum: 27.11.2006 19:26:57
30.10.2007: Datenanforderung 1951 (Import Sachbearbeiter)
PY - 2004
Y1 - 2004
N2 - A high-resolution analysis of multiple climate proxies from a rhythmic mid-Langhian pelagic limestone - marl succession (northeastern Apennines of Italy) yields information on the pacing and nature of palaeoenvironmental changes in this part of the mid-Miocene Mediterranean. The variations in stable isotopes, magnetic susceptibility, and a variety of geochemical parameters through the section, although modified by diagenetic changes, are broadly consistent with a model of climate cycles in which the limestones represent cold/dry periods and the marls represent warm/wet periods. Fourier analysis of the multiple proxies, constrained by radioisotopic dates, and aided by partial tuning to either eccentricity or obliquity show that these proxies respond in synchrony to orbitally forced climate changes, with obliquity being the dominant influence in this succession. Π2004 Elsevier B.V. All rights reserved.
AB - A high-resolution analysis of multiple climate proxies from a rhythmic mid-Langhian pelagic limestone - marl succession (northeastern Apennines of Italy) yields information on the pacing and nature of palaeoenvironmental changes in this part of the mid-Miocene Mediterranean. The variations in stable isotopes, magnetic susceptibility, and a variety of geochemical parameters through the section, although modified by diagenetic changes, are broadly consistent with a model of climate cycles in which the limestones represent cold/dry periods and the marls represent warm/wet periods. Fourier analysis of the multiple proxies, constrained by radioisotopic dates, and aided by partial tuning to either eccentricity or obliquity show that these proxies respond in synchrony to orbitally forced climate changes, with obliquity being the dominant influence in this succession. Π2004 Elsevier B.V. All rights reserved.
M3 - Article
SN - 0031-0182
VL - 211
SP - 325
EP - 344
JO - Palaeogeography, Palaeoclimatology, Palaeoecology
JF - Palaeogeography, Palaeoclimatology, Palaeoecology
IS - 3-4
ER -