2025-08-22 北海道大学
本研究で対象とした長野県中房温泉地域の珪華。70℃以上の熱水と珪華、発達した森林が共存する独特の景観を呈する。
＜関連情報＞
- https://www.hokudai.ac.jp/news/2025/08/post-2027.html
- https://www.hokudai.ac.jp/news/pdf/250822_pr2.pdf
- https://www.sciencedirect.com/science/article/pii/S0031018225004614
弧環境における現生珪華堆積物とその植物化石保存ポテンシャル Modern silica sinter deposits from an island-arc setting and their potential for fossilizing plants
Aya Kubota, Ryo Taniguchi, Tomoyuki Ueda, Yasuhiro Iba
Palaeogeography, Palaeoclimatology, Palaeoecology Available online: 5 August 2025
DOI:https://doi.org/10.1016/j.palaeo.2025.113176
Highlights
- A new facies model for silica sinter is proposed from a forested island-arc in Japan.Modern silica sinter deposits preserve abundant plant remains at cellular resolution.
- Sinter facies assemblages reflect thermal gradients and vegetation on steep slopes.
- Solar-driven evaporation is identified as the key driver of sinter growth.
- The model provides a modern analog for silica sinter Lagerstätten in the geological record.
Abstract
Silica sinters deposited by hot-spring activities form Lagerstätten with numerous three-dimensional, cell-preserved fossils. The formation processes and depositional facies of silica sinters have been documented in large-scale geothermal provinces, including mantle-plume hotspots and mid-ocean ridges. Silica sinters in these areas preserve plants and microbes which are adapted to survive under geothermal stress, and which live inside the hot-spring system. Most plants are, however, intolerant to this specific environment. They are growing outside the hot springs, their chance for being embedded and preserved in the silica sinters is thus limited. Paleodiversity estimates and paleoecological reconstructions of past silica sinter Lagerstätten are therefore considered to be ambiguous. Here, we present a new depositional facies model of silica sinter from a forested island-arc setting, and discuss the taphonomy of richly preserved plants from these settings. At Nakabusa Hot Springs in central Japan, numerous small seep points emerge on densely forested slopes, where they form silica sinters. These sinters are characterized by the incorporation of abundant modern plants and insects from the adjoining forests, in addition to temperature-specific microbes. Because narrow channels flow down steep slopes with little disturbance of the forests, a distinctive bio- and lithofacies has developed that richly preserves the present-day native vegetation. The facies model presented here can serve as a valuable modern analog for better understanding the depositional processes of plant-rich fossil silica sinters. It may further help to understand the factors controlling the fossilization of land-based vegetation, thereby improving its relevance for interpretations throughout the geologic record.
