Sinemurian-Pliensbachian calcareous nannofossil biostratigraphy and organic carbon isotope stratigraphy in the Paris Basin: Calibration to the ammonite biozonation of NW Europe

被引:47
作者
Peti, Leonie [1 ,7 ]
Thibault, Nicolas [1 ]
Clemence, Marie-Emilie [2 ]
Korte, Christoph [1 ]
Dommergues, Jean-Louis [3 ]
Bougeault, Cedric [3 ]
Pellenard, Pierre [3 ]
Jelby, Mads E. [4 ]
Ullmann, Clemens V. [5 ,6 ]
机构
[1] Univ Copenhagen, Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark
[2] Univ Innsbruck, Inst Geol, Fac Geo & Atmospher Sci, Innrain 52, A-6020 Innsbruck, Austria
[3] Univ Bourgogne Franche Comte, UMR CNRS uB 6282, Biogeosci, 6 Blvd Gabriel, F-21000 Dijon, France
[4] Univ Copenhagen, Nat Hist Museum Denmark, DK-1350 Copenhagen K, Denmark
[5] Univ Exeter, Camborne Sch Mines, Penryn Campus, Penryn TR10 9FE, Cornwall, England
[6] Univ Exeter, Environm & Sustainabil Inst, Penryn Campus, Penryn TR10 9FE, Cornwall, England
[7] Univ Auckland, Sch Environm, PB 92019,23 Symonds St, Auckland, New Zealand
关键词
Coccoliths; Lower Jurassic; Semi-quantitative biostratigraphy; Sancerre-Couy; OCEANIC ANOXIC EVENT; NORTHERN SPAIN; LUSITANIAN BASIN; SEA-LEVEL; GEOCHEMICAL EVIDENCE; ASTURIAN BASIN; WESTERN TETHYS; LOWER TOARCIAN; COUY BOREHOLE; PHYTOPLANKTON;
D O I
10.1016/j.palaeo.2016.12.004
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The biostratigraphy of Sinemurian to lower Toarcian calcareous nannofossils has been investigated in the Sancerre-Couy core (Paris Basin), which contains a mixed assemblage of species with affinities to the northern and southern areas of the peri-tethyan realm, thus allowing for the use and calibration of the Mediterranean Province (Italy/S France) and NW Europe (UK) biozonation schemes. This study is based on semi-quantitative analyses of the calcareous nannofossil assemblage performed on 145 samples and the recorded bioevents are calibrated to the NW European Ammonite Zonation and to a new organic carbon isotope curve based on 385 data points. The main bioevents, i.e. the first occurrences of Parhabdolithus liasicus, Crepidolithus pliensbachensis, Crepidolithus crassus, Mitrolithus lenticularis, Similiscutum cruciulus sensu lato, Lotharingius hauffii, Crepidolithus cavus and Lotharingius sigillatus as well as the last occurrence of Parhabdolithus robustus, have been identified. However, we show that a large number of standard biostratigraphic markers show inconsistent occurrences at the base and top of their range, possibly accounting for some of the significant discrepancies observed between the different domains. In addition to the nine main bioevents used for the biozonation of the core, we document an additional 50 distinct bioevents, evaluate their reliability and discuss their potential significance by comparison to previous studies. A total of five significant negative organic carbon isotope excursions are identified and defined in the Paris Basin including the well-documented Sinemurian-Pliensbachian boundary event. One positive excursion is further defined in the Pliensbachian interval. Our calibration of high-resolution calcareous nannofossil biostratigraphy to ammonite biostratigraphy and organic carbon isotopes represents a new strati graphic reference for the Lower Jurassic series. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:142 / 161
页数:20
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