アウトクンプの岩盤が意外な発見をもたらす (Outokumpu’s bedrock reveals a smelly surprise)

ad

2025-02-05 フィンランド技術研究センター (VTT)

Tarkkasuurennoskiviaineksenpinnanmikrobeista

フィンランドのVTT技術研究センターは、アウトカンプ地域の地下深部から採取した岩石サンプルを分析し、約20億年前の海洋環境に由来する硫化水素ガスを発見しました。このガスは腐卵臭を放ち、地球の初期生命環境や大気組成の理解に新たな手がかりを提供します。

<関連情報>

深部岩盤地下水中の天然起源揮発性有機化合物 Naturally occurring volatile organic compounds in deep bedrock groundwater

Riikka Kietäväinen,Mari Nyyssönen,Maija Nuppunen-Puputti & Malin Bomberg
Communications Earth Environment  Published:29 January 2025
DOI:https://doi.org/10.1038/s43247-025-02053-2

Fig. 1

Abstract

In deep continental bedrock groundwater, volatile organic compounds pose intriguing questions about their occurrence. Although their natural sources remain poorly characterized, they potentially have profound effects on global elemental cycles and safety assessment of underground facilities. Our investigation focused on non-methane volatile organic compounds in five groundwater-filled Precambrian bedrock fracture zones at 500 m to 2300 m depth in the Outokumpu Deep Drill Hole, Finland. The system revealed a range of indigenous volatile organic compounds, including alcohols, ketones, aldehydes, alkanes, aromatics, and sulfur-compounds. Metagenomic sequencing demonstrated spatially widely distributed genetic potential for microbial volatile organic compound metabolism. Integrating these findings with local geology and hydrogeochemistry, our results suggest that volatile organic compounds are not only formed in or released to groundwater but also degraded in the continental bedrock through interconnected abiotic and biotic processes.

1702地球物理及び地球化学
ad
ad
Follow
ad
タイトルとURLをコピーしました