Abstract Variations in Earth's orbit and axial tilt induce climatic changes which are recorded in sedimentary deposits. The frequencies of these cyclical variations are integer combinations of the main secular frequencies of the solar system. Analyzing these cycles in sedimentary records can help establish an astronomical time scale for the geological record by correlating geological proxies with computed variations in insolation on the Earth's surface that follows the gravitational laws. When the astronomical solution becomes uncertain when going back in time, the analysis of stratigraphic records can provide insights into the past states of the planetary system and the evolution of the Earth‐Moon system. A critical aspect of this analysis is the estimation of the sedimentary deposition rate, which determines the time‐depth transfer function, relating geological depth to relative or absolute time. We propose a novel approach for constructing astronomical time scales for geological stratigraphic records. The AstroGeoFit method establishes a time‐depth transfer function throughout the record, accommodating variable sedimentation rates, and extracts the primary astronomical signal from the geological sequence. This is achieved using a genetic algorithm that adapts to a wide range of sedimentation rate variations. This statistical analysis enables the reconstruction of an astronomical signal (e.g., eccentricity and/or precession) purely from the stratigraphic sequence with minimal subjective bias. When this template is correlated with an astronomical solution, an absolute time scale is obtained for the entire record. In addition, we show that uncertainties can be estimated at each stage of the AstroGeoFit process.
Hoang et al. (2025) studied this question.