Astronomical calibration of the Valanginian "Weissert" episode: The Orpierre marl-limestone succession (Vocontian Basin, southeastern France)

被引:35
作者
Charbonnier, Guillaume [1 ]
Boulila, Slah [2 ]
Gardin, Silvia [3 ]
Duchamp-Alphonse, Stephanie [1 ]
Adatte, Thierry [4 ]
Spangenberg, Jorge E. [4 ]
Foellmi, Karl B. [4 ]
Colin, Christophe [1 ]
Galbrun, Bruno [2 ]
机构
[1] Univ Paris 11, UMR CNRS IDES 8148, F-91405 Orsay, France
[2] Univ Paris 06, UMR CNRS ISTeP 7193, Inst Sci Terre Paris, F-75252 Paris 5, France
[3] Univ Paris 06, UMR CNRS CR2P 7072, Ctr Rech Paleobiodiversite & Paleoenvironm, F-75252 Paris 5, France
[4] Quartier UNIL Mouline, Inst Sci Terre, CH-1015 Lausanne, Switzerland
关键词
Positive carbon isotope excursion; Magnetic susceptibility; Cyclostratigraphy; Valanginian; Calcareous nannofossils; Vocontian Basin; CARBON-ISOTOPE STRATIGRAPHY; ORBITAL TIME-SCALE; CALCAREOUS NANNOFOSSILS; SOUTHERN ALPS; MAGNETIC-SUSCEPTIBILITY; MAIOLICA FORMATION; EVENT; BOUNDARY; PLATFORM; DELTA-C-13;
D O I
10.1016/j.cretres.2013.07.003
中图分类号
P5 [地质学];
学科分类号
070403 [天体物理学];
摘要
A high-resolution, biostratigraphic (calcareous nannofossils, calpionellids), chemostratigraphic (C-isotope) and cyclostratigraphic (magnetic susceptibility) study was performed on the marl-limestone alternations of the Upper Berriasian-Valanginian Orpierre section, deposited in the hemipelagic setting of the Vocontian Basin (SE France). The main aims of this study were to detect orbital forcing, to estimate the duration of the Valanginian "Weissert" episode, and to discuss the palaeoenvironmental implications. Detailed calcareous nannofossil biochronology allowed the recognition of Upper Berriasian-Lower Hauterivian biohorizons. The general trends of the delta C-13 curve and the major positive C-isotope excursion (amplitude of 1.8 parts per thousand) recorded at the Orpierre section are very similar to those found in other sections worldwide. Spectral analysis applied on high-resolution magnetic susceptibility (MS) variations coupled with frequency ratio method reveals a strong cyclic pattern related to the Earth's orbital parameters (precession, obliquity and eccentricity). The prominent 405 kyr eccentricity cycle in the MS signal and has been used as a geochronometer to time calibrate the section. The duration of the Weissert episode was estimated as 2.08 Myr. This duration is coherent with those obtained from the Umbria Marche Basin (similar to 2.3 Myr) and from the Angles section (similar to 2.14 Myr). Durations of more than 2 Myr suggest that a long perturbation in the dynamic of the global carbon cycle that is not compatible with the rapid and intense volcanic activity. Our cyclostratigraphic study indicates a minimal duration of 4.29 Myr for the Valanginian stage. The comparison between the MS signal at Orpierre and the spectral gamma-ray signal recently obtained in two composite sections of the Vocontian Basin allows to propose a revised duration for the Valanginian stage of 4.695 Myr instead of 5.08 Myr. Crown Copyright (C) 2013 Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:25 / 42
页数:18
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