Abstract
Lunar chronology models are built by associating the radiometric ages of samples returned by the Apollo and Luna missions measured in the laboratory with compiled crater distributions of those sites. Such models have not only been widely used to determine the absolute ages of various regions on the Moon1,2,3,4,5,6, but have also been generalized to date the surfaces of the rocky bodies of the inner Solar System7,8,9,10,11,12. However, there is a gap in lunar samples ages between 3.0 Gyr ago and 1.0 Gyr ago13, which occupies almost half of the history of the Moon. Chang’e-5, the first lunar sample return mission since the Luna 24 lander in 1976, brought back basalt material from a young mare area that has been dated to the centre of this gap at 2.030 ± 0.004 Gyr old14. Using this radiometric age, we updated the most widely used chronology models, focusing in particular on the Neukum model13. We found that the updated model is consistent with a combination of an exponential decrease and a linear rate. The updated chronology gives older ages with respect to the Neukum model for most of the lunar history, with a maximum difference of 0.24 Gyr at 2.55 Gyr ago. Differences from other models are of comparable magnitude or greater. These results have important implications for the chronology and impact history of the inner Solar System.
This is a preview of subscription content, access via your institution
Access options
Access Nature and 54 other Nature Portfolio journals
Get Nature+, our best-value online-access subscription
$29.99 / 30 days
cancel any time
Subscribe to this journal
Receive 12 digital issues and online access to articles
$119.00 per year
only $9.92 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
Data availability
The data points used to fit the new chronology model include those from Neukum13, Hiesinger et al.23, Jia et al.19, Wu et al.22, Qian et al.17 and the radiometric age (2.030 ± 0.004 Ga) from Li et al.14. The mapped craters in the Chang'e-5 landing area can be found at https://zenodo.org/record/5615501#.YXvMT5pByF4.
Code availability
The code for fitting the new lunar cratering chronology function can be found at https://zenodo.org/record/5615459#.YXvHJppByF4.
Change history
11 March 2022
A Correction to this paper has been published: https://doi.org/10.1038/s41550-022-01649-4
References
Hiesinger, H. et al. Ages of mare basalts on the lunar nearside. J. Geophys. Res. 105, 29239–29275 (2000).
Hiesinger, H. et al. Ages and stratigraphy of mare basalts in Oceanus Procellarum, Mare Nubium, Mare Cognitum, and Mare Insularum. J. Geophys. Res. 108, 5065 (2003).
Hiesinger, H. et al. Ages and stratigraphy of lunar mare basalts in Mare Frigoris and other nearside maria based on crater size-frequency distribution measurements. J. Geophys. Res. 115, E03003 (2010).
Whitten, J. et al. Lunar mare deposits associated with the Orientale impact basin: new insights into mineralogy, history, mode of emplacement, and relation to Orientale Basin evolution from Moon Mineralogy Mapper (M3) data from Chandrayaan-1. J. Geophys. Res. 116, E00G9 (2011).
Kirchoff, M. R. et al. Ages of large lunar impact craters and implications for bombardment during the Moon’s middle age. Icarus 225, 325–341 (2013).
Yue, Z. et al. Refined model age for Orientale Basin derived from zonal crater dating of its ejecta. Icarus 346, 113804 (2020).
Ivanov, B. A. Mars/Moon cratering rate ratio estimates. Space Sci. Rev. 96, 87–104 (2001).
Michael, G. G. Planetary surface dating from crater size–frequency distribution measurements: multiple resurfacing episodes and differential isochron fitting. Icarus 226, 885–890 (2013).
Hartmann, W. K. & Neukum, G. Cratering chronology and the evolution of Mars. Space Sci. Rev. 96, 165–194 (2001).
Neukum, G., Ivanov, B. A. & Hartmann, W. K. Cratering records in the Inner Solar System in relation to thelunar reference. Space Sci. Rev. 96, 55–86 (2001).
Hartmann, W. K. Martian cratering 8: isochron refinement and the chronology of Mars. Icarus 174, 294–320 (2005).
Hartmann, W. K. & Daubar, I. J. Martian cratering 11. Utilizing decameter scale crater populations to study Martian history. Meteorit. Planet. Sci. 52, 493–510 (2017).
Neukum, G. Meteorite Bombardment and Dating of Planetary Surfaces. Habilitation thesis, Univ. Munich (1983).
Li, Q. L. et al. Two billion-year-old volcanism on the Moon from Chang’e-5 basalts. Nature 600, 54–58 (2021).
Wang, J. et al. Localization of the Chang’e-5 lander using radio-tracking and image-based methods. Remote Sens. 13, 590–601 (2021).
Qian, Y. et al. The regolith properties of the Chang’e-5 landing region and the ground drilling experiments using lunar regolith simulants. Icarus 337, 113508 (2020).
Qian, Y. et al. Young lunar mare basalts in the Chang’e-5 sample return region, northern Oceanus Procellarum. Earth Planet. Sci. Lett. 555, 116702 (2021).
Yue, Z. et al. Lunar regolith thickness deduced from concentric craters in the CE-5 landing area. Icarus 329, 46–54 (2019).
Jia, M. et al. A catalogue of impact craters larger than 200 m and surface age analysis in the Chang’e-5 landing area. Earth Planet. Sci. Lett. 541, 116272 (2020).
Hu, S. et al. A dry lunar mantle reservoir for young mare basalts of Chang’e-5. Nature 600, 49–53 (2021).
Qian, Y. Q. et al. Geology and scientific significance of the Rümker region in northern Oceanus Procellarum: China’s Chang’E-5 landing region. J. Geophys. Res. Planets 123, 1407–1430 (2018).
Wu, B. et al. Rock abundance and crater density in the candidate Chang’E-5 landing region on the Moon. J. Geophys. Res. Planets 123, 3256–3272 (2018).
Hiesinger, H. et al. How old are young lunar craters? J. Geophys. Res. 117, E00H10 (2012).
Wagner, R., Head, J. W. III, Wolf, U. & Neukum, G. Stratigraphic sequence and ages of volcanic units in the Gruithuisen region of the Moon. J. Geophys. Res. 107, E00H10 (2002).
Le Feuvre, M. & Wieczorek, M. A. Nonuniform cratering of the Moon and a revised crater chronology of the inner Solar System. Icarus 214, 1–20 (2011).
Marchi, S. et al. A New chronology for the Moon and Mercury. Astrophys. J. 137, 4936–4948 (2009).
Robbins, S. J. New crater calibrations for the lunar crater-age chronology. Earth Planet. Sci. Lett. 403, 188–198 (2014).
Marchi, S. et al. Small crater populations on Vesta. Planet. Space Sci. 103, 96–103 (2014).
Schmedemann, N. et al. The cratering record, chronology and surface ages of (4) Vesta in comparison to smaller asteroids and the ages of HED meteorites. Planet. Space Sci. 103, 104–130 (2014).
Chapman, C. R. et al. Cratering on Ida. Icarus 120, 77–86 (1996).
Shoemaker, E. M., Hackman, R. J. & Eggleton, R. E. Interplanetary correlation of geologic time. Adv. Astronaut. Sci. 8, 70–79 (1962).
Michael, G. G. & Neukum, G. Planetary surface dating from crater size–frequency distribution measurements: partial resurfacing events and statistical age uncertainty. Earth Planet. Sci. Lett. 294, 223–229 (2010).
Stöffler, D. & Ryder, G. Stratigraphy and isotope ages of lunar geologic units: chronological standard for the inner solar system. Space Sci. Rev. 96, 9–54 (2001).
Hartmann, W. K. Martian cratering VI: crater count isochrons and evidence for recent volcanism from Mars Global Surveyor. Meteorit. Planet. Sci. 34, 167–177 (1999).
Morota, T., Ukai, T. & Furumoto, M. Influence of the asymmetrical cratering rate on the lunar cratering chronology. Icarus 173, 322–332 (2005).
Le Feuvre, M. & Wieczorek, M. A. Nonuniform cratering of the terrestrial planets. Icarus 197, 291–306 (2008).
Gallant, J., Gladman, B. & Cuk, M. Current bombardment of the Earth-Moon system: emphasis on cratering asymmetries. Icarus 202, 371–382 (2009).
Coleman, T. F. & Li, Y. An interior trust region approach for nonlinear minimization subject to bounds. SIAM J. Optim. 6, 418–445 (1996).
Coleman, T. F. & Li, Y. On the convergence of reflective Newton methods for large-scale nonlinear minimization subject to bounds. Math. Program. 67, 189–224 (1994).
Acknowledgements
The Change'e-5 mission was carried out by the Chinese Lunar Exploration Program. This work was supported by the Strategic Priority Program of the Chinese Academy of Sciences (grant no. XDB41000000), the National Natural Science Foundation of China (grant nos 41941003, 41773065 and 41972321) and the Key Research Program of Frontier Sciences, CAS (grant no. QYZDY-SSW-DQC028).
Author information
Authors and Affiliations
Contributions
Z.Y. and K.D. planned the research and prepared the manuscript with the help of Z.O. K.D., W.W., Z.L., S.G., B.L., M.P., Y.W., M.J. and J. L. processed the data.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing interests.
Peer review
Peer review information
Nature Astronomy thanks Nicolle Zellner, Michelle Kirkhoff and the other, anonymous, reviewer(s) for their contribution to the peer review of this work.
Additional information
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary information
Supplementary Information
Supplementary Figs. 1 and 2.
Rights and permissions
About this article
Cite this article
Yue, Z., Di, K., Wan, W. et al. Updated lunar cratering chronology model with the radiometric age of Chang’e-5 samples. Nat Astron 6, 541–545 (2022). https://doi.org/10.1038/s41550-022-01604-3
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1038/s41550-022-01604-3
This article is cited by
-
Mineralogy and chronology of the young mare volcanism in the Procellarum-KREEP-Terrane
Nature Astronomy (2023)
-
Progresses and prospects of impact crater studies
Science China Earth Sciences (2023)
-
Innovative developments in lunar and planetary science promoted by China’s lunar exploration
Science China Earth Sciences (2023)
-
Spectral interpretation of late-stage mare basalt mineralogy unveiled by Chang’E-5 samples
Nature Communications (2022)