My observation. The paper cited is Emergence of peraluminous crustal magmas and implications for the early Earth, 14-May-2021,
http://www.geochemicalperspectivesletters.org/article2114/
Here are some interesting statements I see in the paper cited. “Detrital zircons from the Jack Hills (JH) metasedimentary belt of Western Australia are a record of the first ∼1.5 billion years of Earth history and can be used to help reconstruct the conditions of crust formation and secular changes therein. Beginning as early as ca. 4.3 Ga, but becoming more pronounced in the mid-Archean, a peraluminous signature begins to emerge from the JH zircon record…” Continental crust and its derivatives (e.g., detrital zircons) preserve a near continuous record of Earth’s history from ∼4.4. Ga to today (Voice et al., 2011) that can be used to investigate both individual magmatic systems (e.g., Reimink et al., 2014) and secular changes in Earth’s geodynamic and tectonic history (Bauer et al., 2020)… Whereas peraluminous granitic rocks dominate the bedrock geology in the AGC at ∼3.6 Ga (Reimink et al., 2019b), the peraluminous zircons that emerge in the JH record at ∼3.6 Ga are only a fraction of the total zircon population (∼10 %).”
These dates for very old samples of Earth is looking more and more crowded with astronomy. The Giant Impact for the origin of the Moon now can be dated some 4.4 to 4.45 billion years ago.
https://phys.org/news/2020-07-younger-age-earth-moon.html, THE MOON MIGHT BE YOUNGER THAN WE THOUGHT, Sky & Telescope 140(5):11, 2020 "Abstract The newly formed Moon could have taken up to 10 times longer to solidify than we thought. If so, our satellite might be younger than previously estimated."
We have meteorites with ages dated in this period too and younger.
https://ui.adsabs.harvard.edu/abs/2016LPICo1921.6440P/abstract, "Conclusion: Younger Ar/Ar step ages (3500 - 4400 Ma) for Bjurböle chondrule c2 suggest that the analysis of individual chondrules can yield more accurate meteorite ages than are obtainable from bulk samples."
https://ui.adsabs.harvard.edu/abs/2004GeCoA..68.3779D/abstract, "Older ages from high-T extractions may date an earlier impact event at 4.52 ± 0.08 Ga, whereas younger ages from lower-T extractions date a later impact event at 4.23 ± 0.03 Ga that may have caused annealing of feldspar and olivine."
https://ui.adsabs.harvard.edu/abs/2000GeCoA..64.2133B/abstract, "We made 39Ar- 40Ar age determinations of Watson, Techado, Miles, Colomera, and Sombrerete. Watson has an Ar-Ar age of 3.677 ± 0.007 Gyr, similar to previously reported ages for Kodaikanal and Netschaëvo. We suggest that the various determined radiometric ages of these three meteorites were probably reset by a common impact event."
We have microfossils dated 4.28 billion years old. 'Canadian bacteria-like fossils called oldest evidence of life',
https://www.reuters.com/article/us-science-life-idUSKBN16858B, 01-March-2017
Some of the more recent age dating using zircons on Earth and life appearing on Earth 4.28 billion years ago, can get very interesting with astronomical dates.