The bombardment history on the lunar farside revealed by <sup>40</sup> Ar/ <sup>39</sup> Ar geochronology of Chang’e-6 impact melt rocks

The reconstruction of the lunar bombardment history is pivotal to understanding the evolution of Earth-Moon system. So far, it heavily depends on geochronological studies of lunar nearside samples but lacks direct sample constraints from the lunar farside. Here, we present 28 single-clast 40 Ar/ 39 Ar ages of impact melt rocks returned by the Chang’e-6 mission. They reveal impact events spanning from ∼4.33 to ∼1.13 billion years (Ga). In particular, three melt clasts date to ∼4.16 Ga, consistent with the recent dating of the Apollo basin, and only two ages fall at 4.0 to 3.7 Ga. The presence of older ages (&gt;4.0 Ga) and lack of predominant age around ∼3.9 Ga suggest that the lunar farside bombardment was not dominated by a cataclysmic spike but by a smooth long-term decline punctuated by later impacts.

Authors

Institutions

Publication Details

Journal
Science Advances
Published
2026-07-23
DOI
https://doi.org/10.1126/sciadv.aee8718
Primary Topic
Planetary Science and Exploration
Type
article
Field-Weighted Citation Impact
0.00

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

The bombardment history on the lunar farside revealed by 40 Ar/ 39 Ar geochronology of Chang’e-6 impact melt rocks

Peng‐Li He, Xiaoping Xia, F. F. Huang, Mang Lin et al.
Science Advances
Planetary Science and Exploration
article

The bombardment history on the lunar farside revealed by 40 Ar/ 39 Ar geochronology of Chang’e-6 impact melt rocks

Peng‐Li He, Xiaoping Xia, F. F. Huang, Mang Lin, Qing Yang, Hua‐Ning Qiu, Fei Su, Jingyou Chen, Wanfeng Zhang, Ming Xiao, Huaiyu He, J Zhang, Zexian Cui, Yan‐Qiang Zhang, Fred Jourdan, Xiujuan Bai, Qin Zhou, Liekun Yang, Yi‐Gang Xu, Le Chen, Le Zhang, De‐wen Zheng, Bo Wei, Yi-Xiang Wang, Jun-Jie Wang, Yonghua Cao, Ying-De Jiang, Jun-Jie Li
article en

Abstract

The reconstruction of the lunar bombardment history is pivotal to understanding the evolution of Earth-Moon system. So far, it heavily depends on geochronological studies of lunar nearside samples but lacks direct sample constraints from the lunar farside. Here, we present 28 single-clast 40 Ar/ 39 Ar ages of impact melt rocks returned by the Chang’e-6 mission. They reveal impact events spanning from ∼4.33 to ∼1.13 billion years (Ga). In particular, three melt clasts date to ∼4.16 Ga, consistent with the recent dating of the Apollo basin, and only two ages fall at 4.0 to 3.7 Ga. The presence of older ages (&gt;4.0 Ga) and lack of predominant age around ∼3.9 Ga suggest that the lunar farside bombardment was not dominated by a cataclysmic spike but by a smooth long-term decline punctuated by later impacts.

Science AdvancesVol. 12(30)
Planetary Science Institute (US), Yangtze University (CN), Chinese Academy of Sciences (CN), Curtin University (AU), Guangzhou Institute of Geochemistry (CN), China University of Geosciences (CN), Institute of Geology and Geophysics (AZ), Institute of Geology and Geophysics (CN), Beijing Research Institute of Uranium Geology (CN), University of Hong Kong (HK), China Earthquake Administration (CN)
National Natural Science Foundation of China, Chinese Academy of Sciences, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences
Openalex Percentile: Top 9%
Planetary Science and Exploration
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.