A unique prokaryotic vertical distribution in the groundwaters of deep sedimentary geological settings in Hokkaido, Japan

IF 3.5 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Progress in Earth and Planetary Science Pub Date : 2024-01-04 DOI:10.1186/s40645-023-00604-9
Ayumi Sugiyama, Tetsuo Ibara, Kazuyo Nagaosa, Atsunao Marui, Kenji Kato
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Abstract

The purpose of this study is to clarify the vertical prokaryotic distribution in groundwater in a terrestrial subsurface sedimentary environment with a geological complex. Six groundwater samples were collected from a coastal 1200-m-deep borehole in which digging strata deposited between 2.3 and 1.5 Ma in Horonobe, Hokkaido, Japan. The studied succession was divided into three vertical zones that were geochemically differentiated according to their chloride contents and water-stable isotopes. The upper zone (UZ; shallower than 500 m) primarily contained fresh water supplied by penetrating meteoric water, the connate water zone (CWZ; deeper than 790 m) contained paleo-seawater, and the diffusion zone (DZ; 500–790 m depth) located between UZ and CWZ. Fluctuations in the prokaryotic density and constituents were observed across these three zones. The prokaryotic density decreased from UZ toward DZ, and the density of DZ was two orders of magnitude lower than that of UZ and CWZ. High prokaryotic activity was observed in CWZ below DZ. The upward expansion of prokaryotic distribution from CWZ, where high prokaryotic potential expressed by biomass can be maintained almost equivalent to that in the marine environment, probably occurred on a geological timescale from 80 ka to 1.3 Ma, as shown by the groundwater age of DZ. The DZ is a zone where the geochemistry has changed drastically owing to the mixing of penetrating meteoric water and the diffusion of deep paleo-seawater, preserving a unique subsurface environment. This chemically mixed zone might be considered as a buffering zone for prokaryotes to prevent the expansion of prokaryotic density and activity provided by diffusion and their in situ growth from both above and below the zones, which is expected to be maintained over a geological timescale. This zone is considered important for using subsurface space in the deep subsurface environment of the island arc.

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日本北海道深层沉积地质环境地下水中独特的原核生物垂直分布情况
本研究的目的是弄清具有地质复合体的陆地地下沉积环境中地下水中原核生物的垂直分布情况。研究人员从日本北海道堀之部一个 1200 米深的沿海钻孔中采集了六个地下水样本,该钻孔挖掘了沉积于 2.3 至 1.5 Ma 之间的地层。所研究的演替分为三个垂直区域,根据其氯化物含量和水稳定同位素进行地球化学区分。上层带(UZ;深度小于 500 米)主要包含由穿透性流星水提供的淡水,涵养水带(CWZ;深度大于 790 米)包含古海水,扩散带(DZ;深度为 500-790 米)位于 UZ 和 CWZ 之间。在这三个区域中,原核生物的密度和成分都有波动。原核生物密度从 UZ 向 DZ 降低,DZ 的密度比 UZ 和 CWZ 低两个数量级。在 DZ 以下的 CWZ 中,原核生物活动频繁。从 DZ 的地下水年龄可以看出,原核生物从 CWZ 开始向上扩展分布,其生物量所表现的高原核生物潜力几乎与海洋环境中的原核生物潜力相当。由于穿透性流星水和深层古海水的扩散,DZ 是一个地球化学发生了巨大变化的区域,保留了独特的地下环境。这一化学混合区可被视为原核生物的缓冲区,以防止原核生物密度和活动因扩散而扩大,以及原核生物在区上和区下的原地生长。这一区域被认为对利用岛弧深层地下环境的地下空间非常重要。
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来源期刊
Progress in Earth and Planetary Science
Progress in Earth and Planetary Science Earth and Planetary Sciences-General Earth and Planetary Sciences
CiteScore
6.50
自引率
5.10%
发文量
59
审稿时长
31 weeks
期刊介绍: Progress in Earth and Planetary Science (PEPS), a peer-reviewed open access e-journal, was launched by the Japan Geoscience Union (JpGU) in 2014. This international journal is devoted to high-quality original articles, reviews and papers with full data attached in the research fields of space and planetary sciences, atmospheric and hydrospheric sciences, human geosciences, solid earth sciences, and biogeosciences. PEPS promotes excellent review articles and welcomes articles with electronic attachments including videos, animations, and large original data files. PEPS also encourages papers with full data attached: papers with full data attached are scientific articles that preserve the full detailed raw research data and metadata which were gathered in their preparation and make these data freely available to the research community for further analysis.
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