微生物对日本Yunotaki瀑布锰矿形成的影响

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Island Arc Pub Date : 2022-05-27 DOI:10.1111/iar.12448
Fumito Shiraishi, Ryoji Chihara, Risa Tanimoto, Kazuya Tanaka, Yoshio Takahashi
{"title":"微生物对日本Yunotaki瀑布锰矿形成的影响","authors":"Fumito Shiraishi,&nbsp;Ryoji Chihara,&nbsp;Risa Tanimoto,&nbsp;Kazuya Tanaka,&nbsp;Yoshio Takahashi","doi":"10.1111/iar.12448","DOIUrl":null,"url":null,"abstract":"<p>Microorganisms are considered to play an important role in the formation of manganese oxide in natural environments. At Yunotaki Fall in north Japan, manganese-oxidizing bacteria were previously assumed to have oxidized manganese to precipitate birnessite, which relied on oxygen released from algae (i.e., indirect oxidation sensu <i>lato</i>). However, it remained unclear whether larger-scale manganese oxide precipitation was actually occurring under light conditions. This study therefore evaluated the contribution of indirect oxidation using microelectrodes to analyze local water chemistry, in addition to bulk water chemistry and DNA analyses. With the downward flow of hot spring water, pH increases because of CO<sub>2</sub> degassing and causes the saturation index of birnessite to increase downstream. Manganese concentrations in the hot spring water decrease downstream even if it was undersaturated in birnessite, suggesting the dominance of manganese oxide deposition by microorganisms. Indeed, the deposit surface was covered by thick microbial mats, and microscopic observations and DNA analysis of the mats indicate the presence of cyanobacteria, eukaryotic algae (green algae), and manganese-oxidizing bacteria. Microelectrode measurements at the surface of a deposit covered with eukaryotic algae showed that pH and O<sub>2</sub> concentration profiles are characteristic of oxygenic photosynthesis and aerobic respiration. On the other hand, the light and dark conditions show nearly identical Mn(II) concentration profiles decreasing within the algal mats. These results demonstrate that low bulk pH values in the hot spring water hindered indirect oxidation despite the occurrence of active oxygenic photosynthesis and that direct oxidation by manganese-oxidizing bacteria is considered to dominate in the investigated sample.</p>","PeriodicalId":14791,"journal":{"name":"Island Arc","volume":null,"pages":null},"PeriodicalIF":1.0000,"publicationDate":"2022-05-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Microbial influences on manganese deposit formation at Yunotaki Fall, Japan\",\"authors\":\"Fumito Shiraishi,&nbsp;Ryoji Chihara,&nbsp;Risa Tanimoto,&nbsp;Kazuya Tanaka,&nbsp;Yoshio Takahashi\",\"doi\":\"10.1111/iar.12448\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Microorganisms are considered to play an important role in the formation of manganese oxide in natural environments. At Yunotaki Fall in north Japan, manganese-oxidizing bacteria were previously assumed to have oxidized manganese to precipitate birnessite, which relied on oxygen released from algae (i.e., indirect oxidation sensu <i>lato</i>). However, it remained unclear whether larger-scale manganese oxide precipitation was actually occurring under light conditions. This study therefore evaluated the contribution of indirect oxidation using microelectrodes to analyze local water chemistry, in addition to bulk water chemistry and DNA analyses. With the downward flow of hot spring water, pH increases because of CO<sub>2</sub> degassing and causes the saturation index of birnessite to increase downstream. Manganese concentrations in the hot spring water decrease downstream even if it was undersaturated in birnessite, suggesting the dominance of manganese oxide deposition by microorganisms. Indeed, the deposit surface was covered by thick microbial mats, and microscopic observations and DNA analysis of the mats indicate the presence of cyanobacteria, eukaryotic algae (green algae), and manganese-oxidizing bacteria. Microelectrode measurements at the surface of a deposit covered with eukaryotic algae showed that pH and O<sub>2</sub> concentration profiles are characteristic of oxygenic photosynthesis and aerobic respiration. On the other hand, the light and dark conditions show nearly identical Mn(II) concentration profiles decreasing within the algal mats. These results demonstrate that low bulk pH values in the hot spring water hindered indirect oxidation despite the occurrence of active oxygenic photosynthesis and that direct oxidation by manganese-oxidizing bacteria is considered to dominate in the investigated sample.</p>\",\"PeriodicalId\":14791,\"journal\":{\"name\":\"Island Arc\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":1.0000,\"publicationDate\":\"2022-05-27\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Island Arc\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1111/iar.12448\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Island Arc","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1111/iar.12448","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0

摘要

微生物被认为在自然环境中氧化锰的形成中起着重要作用。在日本北部的Yunotaki瀑布,锰氧化细菌以前被认为是通过氧化锰来沉淀birnite,这依赖于藻类释放的氧气(即间接氧化感应)。然而,尚不清楚是否在光照条件下确实发生了更大规模的氧化锰沉淀。因此,除了散装水化学和DNA分析外,本研究还利用微电极分析了间接氧化对局部水化学的贡献。随着温泉水的向下流动,由于CO2脱气,pH值升高,导致碧玉矿的饱和指数在下游升高。温泉水中锰的浓度在下游降低,即使它在碧玉矿中是不饱和的,表明微生物沉积锰氧化物的优势。事实上,沉积物表面覆盖着厚厚的微生物垫,显微镜观察和对垫的DNA分析表明存在蓝藻,真核藻类(绿藻)和锰氧化细菌。在被真核藻类覆盖的沉积物表面的微电极测量表明,pH和O2浓度分布具有氧光合作用和有氧呼吸的特征。另一方面,在光照和黑暗条件下,藻垫内Mn(II)浓度曲线几乎相同,呈下降趋势。这些结果表明,尽管发生了活跃的含氧光合作用,但温泉水中较低的体积pH值阻碍了间接氧化,而锰氧化细菌的直接氧化被认为在所研究的样品中占主导地位。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Microbial influences on manganese deposit formation at Yunotaki Fall, Japan

Microorganisms are considered to play an important role in the formation of manganese oxide in natural environments. At Yunotaki Fall in north Japan, manganese-oxidizing bacteria were previously assumed to have oxidized manganese to precipitate birnessite, which relied on oxygen released from algae (i.e., indirect oxidation sensu lato). However, it remained unclear whether larger-scale manganese oxide precipitation was actually occurring under light conditions. This study therefore evaluated the contribution of indirect oxidation using microelectrodes to analyze local water chemistry, in addition to bulk water chemistry and DNA analyses. With the downward flow of hot spring water, pH increases because of CO2 degassing and causes the saturation index of birnessite to increase downstream. Manganese concentrations in the hot spring water decrease downstream even if it was undersaturated in birnessite, suggesting the dominance of manganese oxide deposition by microorganisms. Indeed, the deposit surface was covered by thick microbial mats, and microscopic observations and DNA analysis of the mats indicate the presence of cyanobacteria, eukaryotic algae (green algae), and manganese-oxidizing bacteria. Microelectrode measurements at the surface of a deposit covered with eukaryotic algae showed that pH and O2 concentration profiles are characteristic of oxygenic photosynthesis and aerobic respiration. On the other hand, the light and dark conditions show nearly identical Mn(II) concentration profiles decreasing within the algal mats. These results demonstrate that low bulk pH values in the hot spring water hindered indirect oxidation despite the occurrence of active oxygenic photosynthesis and that direct oxidation by manganese-oxidizing bacteria is considered to dominate in the investigated sample.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Island Arc
Island Arc 地学-地球科学综合
CiteScore
2.90
自引率
26.70%
发文量
32
审稿时长
>12 weeks
期刊介绍: Island Arc is the official journal of the Geological Society of Japan. This journal focuses on the structure, dynamics and evolution of convergent plate boundaries, including trenches, volcanic arcs, subducting plates, and both accretionary and collisional orogens in modern and ancient settings. The Journal also opens to other key geological processes and features of broad interest such as oceanic basins, mid-ocean ridges, hot spots, continental cratons, and their surfaces and roots. Papers that discuss the interaction between solid earth, atmosphere, and bodies of water are also welcome. Articles of immediate importance to other researchers, either by virtue of their new data, results or ideas are given priority publication. Island Arc publishes peer-reviewed articles and reviews. Original scientific articles, of a maximum length of 15 printed pages, are published promptly with a standard publication time from submission of 3 months. All articles are peer reviewed by at least two research experts in the field of the submitted paper.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信