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Refining the Early Devonian time scale using Milankovitch cyclicity in Lochkovian–Pragian sediments (Prague Synform, Czech Republic)

Authors :
da Silva, Anne-Christine
Hladil, J.
Chadimová, L.
Slavík, L.
Hilgen, F.J.
Bábek, O.
Dekkers, M.J.
da Silva, Anne-Christine
Hladil, J.
Chadimová, L.
Slavík, L.
Hilgen, F.J.
Bábek, O.
Dekkers, M.J.
Source :
Earth and Planetary Science Letters vol.455 (2016) date: 2016-11-30 p.125-139 [ISSN 0012-821X]
Publication Year :
2016

Abstract

The Early Devonian geological time scale (base of the Devonian at , Becker et al., 2012) suffers from poor age control, with associated large uncertainties between 2.5 and 4.2 Myr on the stage boundaries. Identifying orbital cycles from sedimentary successions can serve as a very powerful chronometer to test and, where appropriate, improve age models. Here, we focus on the Lochkovian and Pragian, the two lowermost Devonian stages. High-resolution magnetic susceptibility ( – 5 to 10 cm sampling interval) and gamma ray spectrometry (GRS – 25 to 50 cm sampling interval) records were gathered from two main limestone sections, Požár-CS (118 m, spanning the Lochkov and Praha Formations) and Pod Barrandovem (174 m; Praha Formation), both in the Czech Republic. An additional section (Branžovy, 65 m, Praha Formation) was sampled for GRS (every 50 cm). The and GRS records are very similar, so variations are driven by variations in the samples' paramagnetic clay mineral content, reflecting changes in detrital input. Therefore, climatic variations are very likely captured in our records. Multiple spectral analysis and statistical techniques such as: Continuous Wavelet Transform, Evolutive Harmonic Analysis, Multi-taper method and Average Spectral Misfit, were used in concert to reach an optimal astronomical interpretation. The Požár-CS section shows distinctly varying sediment accumulation rates. The Lochkovian (essentially equivalent to the Lochkov Formation (Fm.)) is interpreted to include a total of nineteen 405 kyr eccentricity cycles, constraining its duration to . The Praha Fm. includes fourteen 405 kyr eccentricity cycles in the three sampled sections, while the Pragian Stage only includes about four 405 kyr eccentricity cycles, thus exhibiting durations of and respectively. Because the Lochkov Fm. contains an interval with very low sediment accumulation rate and because the Praha Fm. was cross-validated in three different

Details

Database :
OAIster
Journal :
Earth and Planetary Science Letters vol.455 (2016) date: 2016-11-30 p.125-139 [ISSN 0012-821X]
Notes :
DOI: 10.1016/j.epsl.2016.09.009, English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1445796530
Document Type :
Electronic Resource