Overview
- A Korea Institute of Geoscience and Mineral Resources team led by Jaesoo Lim published the peer-reviewed study in late May 2026 reporting stromatolites beneath the Hapcheon (Jeokjung–Chogye) crater.
- The researchers found multiple layered structures about 10 to 20 centimeters across buried in the northwestern part of the crater that match stromatolite morphology.
- Chemical analyses showed europium enrichment and elevated calcium, calcite, and sulfur, a suite of signals commonly linked to hot, mineral-rich hydrothermal fluids.
- Radiocarbon dates on stromatolite material fall roughly between 23,400 and 14,600 years ago, which suggests the post-impact hydrothermal lake lasted for tens of millennia but the team notes age reversals and possible older-carbon contamination that make exact timing uncertain.
- The authors propose impact-created crater lakes could have served as temporary microbial refuges and localized oxygen-producing zones on early Earth and that similar buried signals make crater-hydrothermal sites promising targets in the search for past life on Mars, but they call for more fieldwork and tighter dating to test those ideas.