Lateral facies variations in the Triassic Dachstein platform: A challenge for cyclostratigraphy
The Triassic Dachstein platform limestone at Steinernes Meer, Salzburg, Austria, includes 611 m of limestone with 222 peritidal cycles overlain by 273 m of subtidal, non‐cyclic and weakly cyclic limestone.
Elias Samankassou, Paul Enos
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Why the day is 24 hours long: The history of Earth's atmospheric thermal tide, composition, and mean temperature. [PDF]
Wu H +4 more
europepmc +1 more source
Low dinosaur biodiversity in central China 2 million years prior to the end-Cretaceous mass extinction. [PDF]
Han F +16 more
europepmc +1 more source
Although siliceous sediments have the potential to reveal an enigmatic Miocene climate evolution, problems with age model construction are tough to beat. Cyclostratigraphy is a useful tool for the construction of a high-resolution age model. In the Japan
Jumpei Yoshioka +2 more
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Planetary chaos and inverted climate phasing in the Late Triassic of Greenland. [PDF]
Mau M, Kent DV, Clemmensen LB.
europepmc +1 more source
87th Annual Meeting of the Meteoritical Society 2025: Abstracts
Meteoritics &Planetary Science, Volume 60, Issue S1, Page 30-350, August 2025.
wiley +1 more source
Initial Results of the Cyclostratigraphy Intercomparison Project 2
The study of astronomical climate forcing and the application of cyclostratigraphy grew spectacularly over the last decades. In cyclostratigraphy a wide range in methods are used to assess cyclicity and orbitally forced cyclicity. However, comparative studies between these different approaches remain too rare.
Christian Zeeden +5 more
openaire +2 more sources
Is One Sample Enough? Testing the Importance of Lateral Sedimentary Variability in Cyclostratigraphy
Cyclostratigraphic studies of sedimentary rocks traditionally sample assuming that one sample per sedimentary horizon is sufficient. But is one sample enough?
Fangfang Chen, Ross N. Mitchell
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Editorial: Multi-Disciplinary Applications in Magnetic Chronostratigraphy
Luigi Jovane +2 more
doaj +1 more source
Milankovitch cycles in banded iron formations constrain the Earth-Moon system 2.46 billion years ago. [PDF]
Lantink ML +3 more
europepmc +1 more source

