Microbial fabrics of geyserites around hot spring pools in Daggyai, Tibet, China
The Daggyai geyserites serve as hosts for cesium deposits; however, their origin, whether by chemical deposition or biological formation, is a topic of debate. To decipher the origin of geyserites, the petrographic features of the geyserite samples were examined. The geyserites exhibited columnar la...
Gespeichert in:
| Veröffentlicht in: | Terra nova (Oxford, England) England), 2020-10, Vol.32 (5), p.355-368 |
|---|---|
| Hauptverfasser: | , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 368 |
|---|---|
| container_issue | 5 |
| container_start_page | 355 |
| container_title | Terra nova (Oxford, England) |
| container_volume | 32 |
| creator | Li, Rong Wu, Geng Jones, Brian Shi, Taiheng |
| description | The Daggyai geyserites serve as hosts for cesium deposits; however, their origin, whether by chemical deposition or biological formation, is a topic of debate. To decipher the origin of geyserites, the petrographic features of the geyserite samples were examined. The geyserites exhibited columnar laminated, planar laminated and spicular morphologies. Furthermore, they contained morphological and confocal microscopic evidence of the coccoid, bacilliform and filamentous microbes that formed them. Minor calcite and quartz crystals were found locally in the columnar laminated and spicular geyserites. Cyanobacteria tentatively assigned to the genus Calothrix dominated in the planar and columnar laminated geyserites, but were rare in the spicular geyserites. The results demonstrated that the microbes contributed to the Daggyai geyserite formation. |
| doi_str_mv | 10.1111/ter.12465 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2442033440</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2442033440</sourcerecordid><originalsourceid>FETCH-LOGICAL-c3325-157ad7f0bd66bb96c5faa150f15e3253d3f0cd6bb4515709c0808d245ea51c5e3</originalsourceid><addsrcrecordid>eNp1kEtPwzAQhC0EEqVw4B9Y4oTUlPUraY6olIdUBELlbDmOnboKcbFTofx7DOHKXvYw3-xqBqFLAnOS5qY3YU4oz8URmhCWi4wRSo7RBErBM74oylN0FuMOAIqClhP0-ux08JVTLbaqCk5H7C1uzBBNcL2JWAV_6Gq89T2O--C6Bu-9byN2Hb5TTTMoN8MbV5l-hpdb16lzdGJVG83F356i9_vVZvmYrV8enpa360wzRkVGRKHqwkJV53lVlbkWVikiwBJhks5qZkHXSeIioVBqWMCiplwYJYhOzBRdjXf3wX8eTOzlzh9Cl15KyjkFxjiHRF2PVAoZYzBWpgwfKgySgPwpTKbC5G9hib0Z2S_XmuF_UG5Wb6PjG7_sa8w</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2442033440</pqid></control><display><type>article</type><title>Microbial fabrics of geyserites around hot spring pools in Daggyai, Tibet, China</title><source>Wiley Online Library All Journals</source><creator>Li, Rong ; Wu, Geng ; Jones, Brian ; Shi, Taiheng</creator><creatorcontrib>Li, Rong ; Wu, Geng ; Jones, Brian ; Shi, Taiheng</creatorcontrib><description>The Daggyai geyserites serve as hosts for cesium deposits; however, their origin, whether by chemical deposition or biological formation, is a topic of debate. To decipher the origin of geyserites, the petrographic features of the geyserite samples were examined. The geyserites exhibited columnar laminated, planar laminated and spicular morphologies. Furthermore, they contained morphological and confocal microscopic evidence of the coccoid, bacilliform and filamentous microbes that formed them. Minor calcite and quartz crystals were found locally in the columnar laminated and spicular geyserites. Cyanobacteria tentatively assigned to the genus Calothrix dominated in the planar and columnar laminated geyserites, but were rare in the spicular geyserites. The results demonstrated that the microbes contributed to the Daggyai geyserite formation.</description><identifier>ISSN: 0954-4879</identifier><identifier>EISSN: 1365-3121</identifier><identifier>DOI: 10.1111/ter.12465</identifier><language>eng</language><publisher>Oxford: Blackwell Publishing Ltd</publisher><subject>Caesium ; Calcite ; Cesium ; Crystals ; fabric ; geyserite ; Hot springs ; microbe ; morphology ; Tibet</subject><ispartof>Terra nova (Oxford, England), 2020-10, Vol.32 (5), p.355-368</ispartof><rights>2020 John Wiley & Sons Ltd</rights><rights>Copyright © 2020 John Wiley & Sons Ltd</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3325-157ad7f0bd66bb96c5faa150f15e3253d3f0cd6bb4515709c0808d245ea51c5e3</citedby><cites>FETCH-LOGICAL-c3325-157ad7f0bd66bb96c5faa150f15e3253d3f0cd6bb4515709c0808d245ea51c5e3</cites><orcidid>0000-0003-4642-8312</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2Fter.12465$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fter.12465$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,27924,27925,45574,45575</link.rule.ids></links><search><creatorcontrib>Li, Rong</creatorcontrib><creatorcontrib>Wu, Geng</creatorcontrib><creatorcontrib>Jones, Brian</creatorcontrib><creatorcontrib>Shi, Taiheng</creatorcontrib><title>Microbial fabrics of geyserites around hot spring pools in Daggyai, Tibet, China</title><title>Terra nova (Oxford, England)</title><description>The Daggyai geyserites serve as hosts for cesium deposits; however, their origin, whether by chemical deposition or biological formation, is a topic of debate. To decipher the origin of geyserites, the petrographic features of the geyserite samples were examined. The geyserites exhibited columnar laminated, planar laminated and spicular morphologies. Furthermore, they contained morphological and confocal microscopic evidence of the coccoid, bacilliform and filamentous microbes that formed them. Minor calcite and quartz crystals were found locally in the columnar laminated and spicular geyserites. Cyanobacteria tentatively assigned to the genus Calothrix dominated in the planar and columnar laminated geyserites, but were rare in the spicular geyserites. The results demonstrated that the microbes contributed to the Daggyai geyserite formation.</description><subject>Caesium</subject><subject>Calcite</subject><subject>Cesium</subject><subject>Crystals</subject><subject>fabric</subject><subject>geyserite</subject><subject>Hot springs</subject><subject>microbe</subject><subject>morphology</subject><subject>Tibet</subject><issn>0954-4879</issn><issn>1365-3121</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1kEtPwzAQhC0EEqVw4B9Y4oTUlPUraY6olIdUBELlbDmOnboKcbFTofx7DOHKXvYw3-xqBqFLAnOS5qY3YU4oz8URmhCWi4wRSo7RBErBM74oylN0FuMOAIqClhP0-ux08JVTLbaqCk5H7C1uzBBNcL2JWAV_6Gq89T2O--C6Bu-9byN2Hb5TTTMoN8MbV5l-hpdb16lzdGJVG83F356i9_vVZvmYrV8enpa360wzRkVGRKHqwkJV53lVlbkWVikiwBJhks5qZkHXSeIioVBqWMCiplwYJYhOzBRdjXf3wX8eTOzlzh9Cl15KyjkFxjiHRF2PVAoZYzBWpgwfKgySgPwpTKbC5G9hib0Z2S_XmuF_UG5Wb6PjG7_sa8w</recordid><startdate>202010</startdate><enddate>202010</enddate><creator>Li, Rong</creator><creator>Wu, Geng</creator><creator>Jones, Brian</creator><creator>Shi, Taiheng</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0003-4642-8312</orcidid></search><sort><creationdate>202010</creationdate><title>Microbial fabrics of geyserites around hot spring pools in Daggyai, Tibet, China</title><author>Li, Rong ; Wu, Geng ; Jones, Brian ; Shi, Taiheng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3325-157ad7f0bd66bb96c5faa150f15e3253d3f0cd6bb4515709c0808d245ea51c5e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Caesium</topic><topic>Calcite</topic><topic>Cesium</topic><topic>Crystals</topic><topic>fabric</topic><topic>geyserite</topic><topic>Hot springs</topic><topic>microbe</topic><topic>morphology</topic><topic>Tibet</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Li, Rong</creatorcontrib><creatorcontrib>Wu, Geng</creatorcontrib><creatorcontrib>Jones, Brian</creatorcontrib><creatorcontrib>Shi, Taiheng</creatorcontrib><collection>CrossRef</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Terra nova (Oxford, England)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Li, Rong</au><au>Wu, Geng</au><au>Jones, Brian</au><au>Shi, Taiheng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Microbial fabrics of geyserites around hot spring pools in Daggyai, Tibet, China</atitle><jtitle>Terra nova (Oxford, England)</jtitle><date>2020-10</date><risdate>2020</risdate><volume>32</volume><issue>5</issue><spage>355</spage><epage>368</epage><pages>355-368</pages><issn>0954-4879</issn><eissn>1365-3121</eissn><abstract>The Daggyai geyserites serve as hosts for cesium deposits; however, their origin, whether by chemical deposition or biological formation, is a topic of debate. To decipher the origin of geyserites, the petrographic features of the geyserite samples were examined. The geyserites exhibited columnar laminated, planar laminated and spicular morphologies. Furthermore, they contained morphological and confocal microscopic evidence of the coccoid, bacilliform and filamentous microbes that formed them. Minor calcite and quartz crystals were found locally in the columnar laminated and spicular geyserites. Cyanobacteria tentatively assigned to the genus Calothrix dominated in the planar and columnar laminated geyserites, but were rare in the spicular geyserites. The results demonstrated that the microbes contributed to the Daggyai geyserite formation.</abstract><cop>Oxford</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/ter.12465</doi><tpages>14</tpages><orcidid>https://orcid.org/0000-0003-4642-8312</orcidid><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0954-4879 |
| ispartof | Terra nova (Oxford, England), 2020-10, Vol.32 (5), p.355-368 |
| issn | 0954-4879 1365-3121 |
| language | eng |
| recordid | cdi_proquest_journals_2442033440 |
| source | Wiley Online Library All Journals |
| subjects | Caesium Calcite Cesium Crystals fabric geyserite Hot springs microbe morphology Tibet |
| title | Microbial fabrics of geyserites around hot spring pools in Daggyai, Tibet, China |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-07T02%3A19%3A04IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Microbial%20fabrics%20of%20geyserites%20around%20hot%20spring%20pools%20in%20Daggyai,%20Tibet,%20China&rft.jtitle=Terra%20nova%20(Oxford,%20England)&rft.au=Li,%20Rong&rft.date=2020-10&rft.volume=32&rft.issue=5&rft.spage=355&rft.epage=368&rft.pages=355-368&rft.issn=0954-4879&rft.eissn=1365-3121&rft_id=info:doi/10.1111/ter.12465&rft_dat=%3Cproquest_cross%3E2442033440%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2442033440&rft_id=info:pmid/&rfr_iscdi=true |