2023
DOI: 10.1029/2022pa004555
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North Atlantic Drift Sediments Constrain Eocene Tidal Dissipation and the Evolution of the Earth‐Moon System

Abstract: Cyclostratigraphy and astrochronology are now at the forefront of geologic timekeeping. While this technique heavily relies on the accuracy of astronomical calculations, solar system chaos limits how far back astronomical calculations can be performed with confidence. High-resolution paleoclimate records with Milankovitch imprints now allow reversing the traditional cyclostratigraphic approach: Middle Eocene drift sediments from Newfoundland Ridge are well-suited for this purpose, due to high sedimentation rat… Show more

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Cited by 7 publications
(5 citation statements)
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“…The two approaches made essentially no difference in our computations and both yielded solutions including σ 12 -resonance intervals at a similar frequency (see below). For the observational constraints on R, we selected robust data sets based on the reconstruction of Earth's axial precession frequency obtained by cyclostratigraphic studies (Meyers & Malinverno 2018;Sørensen et al 2020;Lantink et al 2022;De Vleeschouwer et al 2023; see Figure 3). The classical integration of precession equations starting at the present rate dR 0 /dt (see Figure 3, green dashed line) follows MacDonald (1964); Goldreich (1966); Touma & Wisdom (1994).…”
Section: Past Earth-moon Distancementioning
confidence: 99%
“…The two approaches made essentially no difference in our computations and both yielded solutions including σ 12 -resonance intervals at a similar frequency (see below). For the observational constraints on R, we selected robust data sets based on the reconstruction of Earth's axial precession frequency obtained by cyclostratigraphic studies (Meyers & Malinverno 2018;Sørensen et al 2020;Lantink et al 2022;De Vleeschouwer et al 2023; see Figure 3). The classical integration of precession equations starting at the present rate dR 0 /dt (see Figure 3, green dashed line) follows MacDonald (1964); Goldreich (1966); Touma & Wisdom (1994).…”
Section: Past Earth-moon Distancementioning
confidence: 99%
“…Note that due to its small effect, selecting OS input option 1 or 2 for a L made essentially no difference in our long-term OS ensembles. For the observational constraints, we selected robust data sets based on the reconstruction of Earth's axial precession frequency obtained by cyclostratigraphic studies (Meyers & Malinverno, 2018;Sørensen et al, 2020;Lantink et al, 2022;De Vleeschouwer et al, 2023) (Figure 1b). Other methods for estimating past a L (and precession frequency) include the analysis of tidal rhythmites and fossil growth laminae, but these approaches are generally associated with large uncertainties and ambiguities in interpretation, especially for Precambrian time intervals (Lantink et al, 2022;Laskar et al, 2024).…”
Section: Tidal Friction In the Pastmentioning
confidence: 99%
“…If restricted to robust data sets from cyclostratigraphic studies, only two data points are available with ages older than 1 Ga (see Figure 1b). For more information on the cyclostratigraphic studies (Meyers & Malinverno, 2018; Sørensen et al, 2020; Lantink et al, 2022; De Vleeschouwer et al, 2023), see Section 3.7.…”
Section: Precession‐tilt Solutions and Frameworkmentioning
confidence: 99%
“…The NAFF software is available through https://paloz.marum.de/confluence/ display/ESPUBLIC/NAFF (Pälike, 2021b). The R scripts used to generate Figures 4-12 are available through Zenodo (De Vleeschouwer, 2023).…”
Section: Data Availability Statementmentioning
confidence: 99%