NOAA/WDS Paleoclimatology - Astronomical Solutions 3.49-0 Ga for Earth's Orbital Eccentricity and Inclination, Obliquity, and Climatic Precession

The planets' gravitational interaction causes rhythmic changes in Earth's orbital parameters (also called Milankovic cycles), which have powerful applications in geology and astrochronology. For instance, the primary astronomical eccentricity cycle due to the secular frequency term (g2-g5) (~405 kyr in the recent past) utilized in deep-time analyses is dominated by Venus' and Jupiter's orbits, aka long eccentricity cycle. The widely accepted and long-held view is that (g2-g5) was practically stable in the past and may hence be used as a "metronome" to reconstruct accurate ages and chronologies. However, using state-of-the-art integrations of the solar system, we show here that (g2-g5) can become unstable over long time scales, without major changes in, or destabilization of, planetary orbits. The (g2-g5) disruption is due to the secular resonance o12 = (g1 - g2) + (s1 - s2), a major contributor to solar system chaos. We demonstrate that entering/exiting the o12 resonance is a common phenomenon on long time scales, occurring in ~40% of our solutions. During o12-resonance episodes, (g2-g5) is very weak or absent and Earth's orbital eccentricity and climate-forcing spectrum are unrecognizable compared to the recent past. Our results have fundamental implications for geology and astrochronology, as well as climate forcing because the paradigm that the longest Milankovic cycle dominates Earth's astronomical forcing, is stable, and has a period of ~405 kyr requires revision.