Articles | Volume 12, issue 9
https://doi.org/10.5194/cp-12-1765-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-1765-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Testing the impact of stratigraphic uncertainty on spectral analyses of sedimentary series
Mathieu Martinez
CORRESPONDING AUTHOR
MARUM, Centrum for Marine Environmental Sciences, Leobenerstr., Universität Bremen, 28359 Bremen, Germany
Sergey Kotov
MARUM, Centrum for Marine Environmental Sciences, Leobenerstr., Universität Bremen, 28359 Bremen, Germany
David De Vleeschouwer
MARUM, Centrum for Marine Environmental Sciences, Leobenerstr., Universität Bremen, 28359 Bremen, Germany
Damien Pas
Pétrologie sédimentaire, B20, Géologie, Université de Liège, Sart Tilman, 4000 Liège, Belgium
Heiko Pälike
MARUM, Centrum for Marine Environmental Sciences, Leobenerstr., Universität Bremen, 28359 Bremen, Germany
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- Detection of Strong Precession Cycles from the Late Pliocene Sedimentary Records of Northeastern Tibetan Plateau Q. Su et al. 10.1029/2019GC008447
- Cyclostratigraphic calibration of the Eifelian Stage (Middle Devonian, Appalachian Basin, Western New York, USA) D. Pas et al. 10.1130/B35589.1
- A decomposition approach to cyclostratigraphic signal processing S. Wouters et al. 10.1016/j.earscirev.2021.103894
- Paleoclimate proxies for cyclostratigraphy: Comparative analysis using a Lower Triassic marine section in South China M. Li et al. 10.1016/j.earscirev.2019.01.011
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Short summary
Identification of Milankovitch cycles within the sedimentary record depends on spectral analyses, but these can be biased because there are always slight uncertainties in the sample position within a sedimentary column. Here, we simulate uncertainties in the sample position and show that a tight control on the inter-sample distance together with a density of 6–12 samples per precession cycle are needed to accurately reconstruct the contribution of the orbital forcing on past climate changes.
Identification of Milankovitch cycles within the sedimentary record depends on spectral...