Extrapolating the tidal dissipation rate back, the Moon and Earth are within the Roche limit about 1.5 billion years ago or near 3 earth radii separation. Other reports show the strata do not come so neatly in layers that unravel the story of the receding Moon so cleanly.
Ref paper - Milankovitch cycles in banded iron formations constrain the Earth–Moon system 2.46 billion years ago,
https://www.pnas.org/doi/abs/10.1073/pnas.2117146119, 26-Sep-2022. "Significance Milankovitch cycles recorded in 2.46-billion-year-old sediments indicate that Earth’s precession cycle had a significantly higher frequency than present, signaling shorter daylengths and Earth–Moon distance..."
My observation. Using the data provided here, Earth in the Precambrian model 2.46 Gyr had a LOD 16.9 hours and the Moon orbited about 50.45 earth radii distance compared to the present mean near 60.27 earth radii distance. Using a circular orbit for the Moon, the lunar month or period ~ 20.9 days. Earth spin at its equator with LOD 16.9 h = 0.6587 km/s. Other reports, Slowdown of Earth's spin caused an oxygen surge,
https://forums.space.com/threads/slowdown-of-earths-spin-caused-an-oxygen-surge.40239/, 21 h LOD 2 Gyr.
Thank the moon for Earth's lengthening day,
https://www.sciencedaily.com/releases/2018/06/180604151200.htm, "A new study that reconstructs the deep history of our planet's relationship to the moon shows that 1.4 billion years ago, a day on Earth lasted just over 18 hours"
My question, are these Earth-Moon system models using Precambrian strata consistent and reliably trace the past history of the orbit of the Earth-Moon system back perhaps 2.5 Gyr? Notice we have an 18 h LOD 1.4 Gyr, 21 h LOD 2 Gyr, and the phys.org report 16.9 h LOD 2.46 Gyr. When you examine the giant impact model(s) for the origin of the Moon, system spin rates and distances are very different, a number show the Moon about 3-7 earth radii when it forms with the proto-earth spinning with a 2-5 hour LOD.