Articles | Volume 7, issue 3
https://doi.org/10.5194/gchron-7-427-2025
https://doi.org/10.5194/gchron-7-427-2025
Research article
 | 
16 Sep 2025
Research article |  | 16 Sep 2025

Nonparametric estimation of age–depth models from sedimentological and stratigraphic information

Niklas Hohmann, David De Vleeschouwer, Sietske Batenburg, and Emilia Jarochowska

Related authors

A revised marine fossil record of the Mediterranean before and after the Messinian salinity crisis
Konstantina Agiadi, Niklas Hohmann, Elsa Gliozzi, Danae Thivaiou, Francesca R. Bosellini, Marco Taviani, Giovanni Bianucci, Alberto Collareta, Laurent Londeix, Costanza Faranda, Francesca Bulian, Efterpi Koskeridou, Francesca Lozar, Alan Maria Mancini, Stefano Dominici, Pierre Moissette, Ildefonso Bajo Campos, Enrico Borghi, George Iliopoulos, Assimina Antonarakou, George Kontakiotis, Evangelia Besiou, Stergios D. Zarkogiannis, Mathias Harzhauser, Francisco Javier Sierro, Angelo Camerlenghi, and Daniel García-Castellanos
Earth Syst. Sci. Data, 16, 4767–4775, https://doi.org/10.5194/essd-16-4767-2024,https://doi.org/10.5194/essd-16-4767-2024, 2024
Short summary

Cited articles

Aadland, T., Sadler, P. M., and Helland-Hansen, W.: Geometric interpretation of time-scale dependent sedimentation rates, Sediment. Geol., 371, 32–40, https://doi.org/10.1016/j.sedgeo.2018.04.003, 2018. a, b, c
Abril-Hernández, J.: 210Pb-dating of sediments with models assuming a constant flux: CFCS, CRS, PLUM, and the novel χ-mapping. Review, performance tests, and guidelines, J. Environ. Radioactiv., 268–269, 107248, https://doi.org/10.1016/j.jenvrad.2023.107248, 2023. a, b, c
Appleby, P. and Oldfield, F.: The calculation of lead-210 dates assuming a constant rate of supply of unsupported 210Pb to the sediment, CATENA, 5, 1–8, https://doi.org/10.1016/S0341-8162(78)80002-2, 1978. a, b, c
Averbuch, O., Tribovillard, N., Devleeschouwer, X., Riquier, L., Mistiaen, B., and Van Vliet-Lanoe, B.: Mountain building-enhanced continental weathering and organic carbon burial as major causes for climatic cooling at the Frasnian–Famennian boundary (c. 376 Ma)?, Terra Nova, 17, 25–34, https://doi.org/10.1111/j.1365-3121.2004.00580.x, 2005. a
Barker, M., Chue Hong, N. P., Katz, D. S., Lamprecht, A.-L., Martinez-Ortiz, C., Psomopoulos, F., Harrow, J., Castro, L. J., Gruenpeter, M., Martinez, P. A., and Honeyman, T.: Introducing the FAIR Principles for research software, Sci. Data, 9, 622, https://doi.org/10.1038/s41597-022-01710-x, 2022. a
Download
Short summary
Age–depth models assign ages to sampling locations (e.g., in drill cores), making them crucial to the determined timing and pace of past changes. We present two methods to estimate age–depth models from sedimentological and stratigraphic information, resulting in richer and more empirically realistic age–depth models. As a use case, we (1)  determine the timing of the Frasnian–Famennian extinction and (2) examine the duration of the Paleocene–Eocene Thermal Maximum (PETM), a potential deep-time analog for anthropogenic climate change.
Share