Quaternary Science Reviews· 2026Q1
First discovery of the Kobayashi-Kasamori (Kb-Ks) tephra layer in terrestrial sediments of the Korean Peninsula
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- Q1SCImago
- 2026year
Short summary
The Kobayashi-Kasamori (Kb-Ks) tephra layer, originating from a Kyushu, Japan eruption ~520 ka, has been identified for the first time in terrestrial lake sediments on the Korean Peninsula.
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Key points
- The Kobayashi-Kasamori (Kb-Ks) tephra layer was identified in lake sediments in a Korean Quaternary basin.
- Geochemical composition and refractive index of glass shards confirmed the tephra originated from a Kyushu, Japan eruption approximately 520,000 years ago.
- This marks the first discovery of Kb-Ks tephra in terrestrial sediments on the Korean Peninsula.
- The finding indicates the lake sediments are older than previously thought (older than 520 ka), and a meteorite impact occurred before this eruption.
AI-generated from the title and abstract; the full text is not read.
Abstract
Abstract It was recently reported that a Quaternary basin in southeastern Korea was formed by a meteorite impact, and a 12-cm-thick tephra layer was found in lake sediments in this basin. In this study, we analyzed the geochemical composition and refractive index of glass shards to identify the unknown tephra. Based on both results, this tephra was identified as Kb-Ks tephra that erupted in the Kyushu area, Japan, approximately 520 ka. To our knowledge, this is the first report of Kb-Ks tephra in terrestrial sediments in the Korean Peninsula. These findings indicate that the depositional age of the lake sediments is much older than previously suspected (ca. 63 ka), and that the meteorite impact occurred before 520 ka. Although more detailed studies are needed, the discovery of Kb-Ks tephra provides important information concerning the paleoclimate during the middle Pleistocene, as well as the prediction of volcanic hazards in the Korean Peninsula.
The authors' abstract, as published at the source. Quaternary Science Reviews, 2026 · DOI ↗
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