• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

钾过量和其他稀有气体可鉴定出一个具有十亿年历史的放射成因富水系统。

Kr excess and other noble gases identify a billion-year-old radiogenically-enriched groundwater system.

机构信息

Department of Earth Sciences, University of Toronto, Toronto, ON, M5S 3B1, Canada.

Department of Earth Sciences, University of Oxford, Oxford, OX1 3AN, UK.

出版信息

Nat Commun. 2022 Jun 30;13(1):3768. doi: 10.1038/s41467-022-31412-2.

DOI:10.1038/s41467-022-31412-2
PMID:35773264
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9246980/
Abstract

Deep within the Precambrian basement rocks of the Earth, groundwaters can sustain subsurface microbial communities, and are targets of investigation both for geologic storage of carbon and/or nuclear waste, and for new reservoirs of rapidly depleting resources of helium. Noble gas-derived residence times have revealed deep hydrological settings where groundwaters are preserved on millions to billion-year timescales. Here we report groundwaters enriched in the highest concentrations of radiogenic products yet discovered in fluids, with an associated Kr excess in the free fluid, and residence times >1 billion years. This brine, from a South African gold mine 3 km below surface, demonstrates that ancient groundwaters preserved in the deep continental crust on billion-year geologic timescales may be more widespread than previously understood. The findings have implications beyond Earth, where on rocky planets such as Mars, subsurface water may persist on long timescales despite surface conditions that no longer provide a habitable zone.

摘要

在地球的前寒武纪基底岩石深处,地下水可以维持地下微生物群落,是地质封存碳和/或核废物以及氦等迅速枯竭资源新储层的研究目标。稀有气体衍生的停留时间揭示了深层水文环境,地下水在数百万到十亿年的时间尺度上得以保存。在这里,我们报告了富含放射性产物的地下水,这是迄今为止在流体中发现的最高浓度,同时自由流体中的 Kr 过剩,停留时间>10 亿年。这种卤水来自南非地表以下 3 公里的金矿,表明保存在大陆地壳深处的古老地下水可能比以前认为的更为普遍。这些发现不仅对地球有意义,在火星等岩石行星上,尽管表面条件不再提供宜居区域,但地下水可能会在很长时间内持续存在。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8996/9246980/2ef8db776ec7/41467_2022_31412_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8996/9246980/e162f24b2292/41467_2022_31412_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8996/9246980/d978e0b3e12b/41467_2022_31412_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8996/9246980/2ef8db776ec7/41467_2022_31412_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8996/9246980/e162f24b2292/41467_2022_31412_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8996/9246980/d978e0b3e12b/41467_2022_31412_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8996/9246980/2ef8db776ec7/41467_2022_31412_Fig3_HTML.jpg

相似文献

1
Kr excess and other noble gases identify a billion-year-old radiogenically-enriched groundwater system.钾过量和其他稀有气体可鉴定出一个具有十亿年历史的放射成因富水系统。
Nat Commun. 2022 Jun 30;13(1):3768. doi: 10.1038/s41467-022-31412-2.
2
Deep fracture fluids isolated in the crust since the Precambrian era.深断裂流体自前寒武纪以来就被隔离在地壳中。
Nature. 2013 May 16;497(7449):357-60. doi: 10.1038/nature12127.
3
Hydrogeological controls on microbial activity and habitability in the Precambrian continental crust.对前寒武纪大陆地壳中微生物活动和生存能力的水文地质控制。
Geobiology. 2024 Mar-Apr;22(2):e12592. doi: 10.1111/gbi.12592.
4
Hydrogeologic controls on episodic H2 release from precambrian fractured rocks--energy for deep subsurface life on earth and mars.前寒武纪裂隙岩石中 episodic H2 释放的水文地质控制——地球和火星深层地下生命的能量
Astrobiology. 2007 Dec;7(6):971-86. doi: 10.1089/ast.2006.0096.
5
Earth-like Habitable Environments in the Subsurface of Mars.火星地下的类地宜居环境。
Astrobiology. 2021 Jun;21(6):741-756. doi: 10.1089/ast.2020.2386. Epub 2021 Apr 15.
6
Noble gas excess air applied to distinguish groundwater recharge conditions.应用惰性气体过量空气来区分地下水补给条件。
Environ Sci Technol. 2007 Mar 15;41(6):1949-55. doi: 10.1021/es061115r.
7
Paleo-Rock-Hosted Life on Earth and the Search on Mars: A Review and Strategy for Exploration.古岩石上的地球生命与火星探索:综述与勘探策略。
Astrobiology. 2019 Oct;19(10):1230-1262. doi: 10.1089/ast.2018.1960. Epub 2019 Jun 25.
8
Noble Gas Analyses to Distinguish Between Surface and Subsurface Brine Releases at a Legacy Oil Site.利用稀有气体分析区分遗留石油场地的地表和地下盐水排放
Ground Water. 2024 Jul-Aug;62(4):645-655. doi: 10.1111/gwat.13412. Epub 2024 Apr 13.
9
Microbial Life in Impact Craters.撞击坑中的微生物生命。
Curr Issues Mol Biol. 2020;38:75-102. doi: 10.21775/cimb.038.075. Epub 2020 Jan 22.
10
Using Kr and isotopic tracers to characterise old groundwater in the Bangkok metropolitan and vicinity areas.利用氪和同位素示踪剂表征曼谷大都市区及周边地区的古老地下水。
Isotopes Environ Health Stud. 2023 Oct 9:1-28. doi: 10.1080/10256016.2023.2261613.

引用本文的文献

1
Deep terrestrial indigenous microbial community dominated by Frackibacter.以弗拉克杆菌为主导的深层陆地本土微生物群落。
Commun Earth Environ. 2024;5(1):795. doi: 10.1038/s43247-024-01966-8. Epub 2024 Dec 29.
2
Radiolytic support for oxidative metabolism in an ancient subsurface brine system.古代地下卤水系统中氧化代谢的辐射分解支持
ISME Commun. 2024 Nov 5;4(1):ycae138. doi: 10.1093/ismeco/ycae138. eCollection 2024 Jan.
3
Subsurface Microbial Colonization at Mineral-Filled Veins in 2-Billion-Year-Old Mafic Rock from the Bushveld Igneous Complex, South Africa.

本文引用的文献

1
Rapid microbial methanogenesis during CO storage in hydrocarbon reservoirs.碳氢化合物储层中二氧化碳封存期间微生物的快速甲烷生成
Nature. 2021 Dec;600(7890):670-674. doi: 10.1038/s41586-021-04153-3. Epub 2021 Dec 22.
2
Earth-like Habitable Environments in the Subsurface of Mars.火星地下的类地宜居环境。
Astrobiology. 2021 Jun;21(6):741-756. doi: 10.1089/ast.2020.2386. Epub 2021 Apr 15.
3
Evolutionary stasis of a deep subsurface microbial lineage.深层地下微生物谱系的进化停滞。
南非布什维尔德火成杂岩体 20 亿年前富矿脉中地下微生物的定殖。
Microb Ecol. 2024 Oct 2;87(1):116. doi: 10.1007/s00248-024-02434-8.
4
Exploring the evidence of Middle Amazonian aquifer sedimentary outburst residues in a Martian chaotic terrain.探索火星混沌地形中亚马逊中部含水层沉积爆发残留物的证据。
Sci Rep. 2023 Oct 18;13(1):17524. doi: 10.1038/s41598-023-39060-2.
5
Radiolytically reworked Archean organic matter in a habitable deep ancient high-temperature brine.在一个宜居的深部古老高温盐水中经辐射作用重塑的太古宙有机质。
Nat Commun. 2023 Oct 3;14(1):6163. doi: 10.1038/s41467-023-41900-8.
ISME J. 2021 Oct;15(10):2830-2842. doi: 10.1038/s41396-021-00965-3. Epub 2021 Apr 6.
4
The contribution of water radiolysis to marine sedimentary life.水的辐射分解对海洋沉积物生命的贡献。
Nat Commun. 2021 Feb 26;12(1):1297. doi: 10.1038/s41467-021-21218-z.
5
Paleo-Rock-Hosted Life on Earth and the Search on Mars: A Review and Strategy for Exploration.古岩石上的地球生命与火星探索:综述与勘探策略。
Astrobiology. 2019 Oct;19(10):1230-1262. doi: 10.1089/ast.2018.1960. Epub 2019 Jun 25.
6
New ecosystems in the deep subsurface follow the flow of water driven by geological activity.深部地下的新生态系统遵循地质活动驱动的水流。
Sci Rep. 2019 Mar 1;9(1):3310. doi: 10.1038/s41598-019-39699-w.
7
Cassini finds molecular hydrogen in the Enceladus plume: Evidence for hydrothermal processes.卡西尼号在土卫二羽流中发现了分子氢:热液活动的证据。
Science. 2017 Apr 14;356(6334):155-159. doi: 10.1126/science.aai8703.
8
Sulfur mass-independent fractionation in subsurface fracture waters indicates a long-standing sulfur cycle in Precambrian rocks.地下断裂水中的硫质量非依赖性分馏表明前寒武纪岩石中存在长期的硫循环。
Nat Commun. 2016 Oct 27;7:13252. doi: 10.1038/ncomms13252.
9
The contribution of the Precambrian continental lithosphere to global H2 production.前寒武纪大陆岩石圈对全球 H2 产量的贡献。
Nature. 2014 Dec 18;516(7531):379-82. doi: 10.1038/nature14017.
10
Deep fracture fluids isolated in the crust since the Precambrian era.深断裂流体自前寒武纪以来就被隔离在地壳中。
Nature. 2013 May 16;497(7449):357-60. doi: 10.1038/nature12127.