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Structure, morphology and crystal growth of bacterial magnetite
Recent high-resolution transmission electron microscopy (HRTEM) studies of the structure and morphology of bacterial magnetite (Fe 3 O 4 ) crystals isolated from a magnetotactic coccus 1 and from an unidentified bacterium extracted from sediment 2 have shown the crystals to be well ordered single-do...
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Published in: | Nature (London) 1984-01, Vol.310 (5976), p.405-407 |
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container_title | Nature (London) |
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creator | Mann, Stephen Frankel, Richard B. Blakemore, Richard P. |
description | Recent high-resolution transmission electron microscopy (HRTEM) studies of the structure and morphology of bacterial magnetite (Fe
3
O
4
) crystals isolated from a magnetotactic coccus
1
and from an unidentified bacterium extracted from sediment
2
have shown the crystals to be well ordered single-domain particles with a morphology based on a hexagonal prism of {011} faces truncated by specific low index planes. We report here a HRTEM study of intact magnetite crystals (magnetosomes) in the microaerophilic bacterium
Aquaspirillum magnetotacticum
, grown in pure culture
3,4
. Our aim has been to investigate the structure, morphology and crystal growth of the magnetite particles in the light of a recent Mossbauer spectroscopy study of this organism
5
which indicated, in addition to magnetite, the presence of hydrated iron(
III
) oxide phases together with the magnetosomes. Our results show that the mature particles are well ordered single-domain crystals of magnetite with a morphology very different from previously studied crystals and based on an octahedral prism of {111} faces truncated by {100} faces. We also show the first direct evidence for both crystalline and non-crystalline phases within individual magnetosomes. The results are important in aiding elucidation of the crystal growth mechanisms of biogenic magnetite. |
doi_str_mv | 10.1038/310405a0 |
format | article |
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3
O
4
) crystals isolated from a magnetotactic coccus
1
and from an unidentified bacterium extracted from sediment
2
have shown the crystals to be well ordered single-domain particles with a morphology based on a hexagonal prism of {011} faces truncated by specific low index planes. We report here a HRTEM study of intact magnetite crystals (magnetosomes) in the microaerophilic bacterium
Aquaspirillum magnetotacticum
, grown in pure culture
3,4
. Our aim has been to investigate the structure, morphology and crystal growth of the magnetite particles in the light of a recent Mossbauer spectroscopy study of this organism
5
which indicated, in addition to magnetite, the presence of hydrated iron(
III
) oxide phases together with the magnetosomes. Our results show that the mature particles are well ordered single-domain crystals of magnetite with a morphology very different from previously studied crystals and based on an octahedral prism of {111} faces truncated by {100} faces. We also show the first direct evidence for both crystalline and non-crystalline phases within individual magnetosomes. The results are important in aiding elucidation of the crystal growth mechanisms of biogenic magnetite.</description><identifier>ISSN: 0028-0836</identifier><identifier>EISSN: 1476-4687</identifier><identifier>DOI: 10.1038/310405a0</identifier><identifier>CODEN: NATUAS</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Humanities and Social Sciences ; letter ; Mineralogy ; multidisciplinary ; Non silicates ; Science ; Science (multidisciplinary)</subject><ispartof>Nature (London), 1984-01, Vol.310 (5976), p.405-407</ispartof><rights>Springer Nature Limited 1984</rights><rights>1985 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a442t-5d50c6382dc4f0f1705a9e5aefc1edad0748d5ba3a9113bc83819a30d07b52d73</citedby><cites>FETCH-LOGICAL-a442t-5d50c6382dc4f0f1705a9e5aefc1edad0748d5ba3a9113bc83819a30d07b52d73</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27903,27904</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=8973352$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Mann, Stephen</creatorcontrib><creatorcontrib>Frankel, Richard B.</creatorcontrib><creatorcontrib>Blakemore, Richard P.</creatorcontrib><title>Structure, morphology and crystal growth of bacterial magnetite</title><title>Nature (London)</title><addtitle>Nature</addtitle><description>Recent high-resolution transmission electron microscopy (HRTEM) studies of the structure and morphology of bacterial magnetite (Fe
3
O
4
) crystals isolated from a magnetotactic coccus
1
and from an unidentified bacterium extracted from sediment
2
have shown the crystals to be well ordered single-domain particles with a morphology based on a hexagonal prism of {011} faces truncated by specific low index planes. We report here a HRTEM study of intact magnetite crystals (magnetosomes) in the microaerophilic bacterium
Aquaspirillum magnetotacticum
, grown in pure culture
3,4
. Our aim has been to investigate the structure, morphology and crystal growth of the magnetite particles in the light of a recent Mossbauer spectroscopy study of this organism
5
which indicated, in addition to magnetite, the presence of hydrated iron(
III
) oxide phases together with the magnetosomes. Our results show that the mature particles are well ordered single-domain crystals of magnetite with a morphology very different from previously studied crystals and based on an octahedral prism of {111} faces truncated by {100} faces. We also show the first direct evidence for both crystalline and non-crystalline phases within individual magnetosomes. The results are important in aiding elucidation of the crystal growth mechanisms of biogenic magnetite.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Humanities and Social Sciences</subject><subject>letter</subject><subject>Mineralogy</subject><subject>multidisciplinary</subject><subject>Non silicates</subject><subject>Science</subject><subject>Science (multidisciplinary)</subject><issn>0028-0836</issn><issn>1476-4687</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1984</creationdate><recordtype>article</recordtype><recordid>eNplkE1LxDAQhoMouK6CP6EHEQWrkyZp0pPI4hcseFDPZZqm3S5tsyYpsv_eyKoXTwPzPjzMvIScUrimwNQNo8BBIOyRGeUyT3mu5D6ZAWQqBcXyQ3Lk_RoABJV8Rm5fg5t0mJy5SgbrNivb23ab4Fgn2m19wD5pnf0Mq8Q2SYU6GNfF3YDtaEIXzDE5aLD35uRnzsn7w_3b4ildvjw-L-6WKXKehVTUAnTOVFZr3kBDZTyxMAJNo6mpsQbJVS0qZFhQyiqtmKIFMohBJbJasjk533k3zn5Mxody6Lw2fY-jsZMvKacyzwSL4MUO1M5670xTblw3oNuWFMrvhsrfhiJ69uNEr7FvHI6683-8KiRjIovY5Q7zMRlb48q1ndwYv_2v_AIceXIt</recordid><startdate>19840101</startdate><enddate>19840101</enddate><creator>Mann, Stephen</creator><creator>Frankel, Richard B.</creator><creator>Blakemore, Richard P.</creator><general>Nature Publishing Group UK</general><general>Nature Publishing</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QL</scope><scope>C1K</scope></search><sort><creationdate>19840101</creationdate><title>Structure, morphology and crystal growth of bacterial magnetite</title><author>Mann, Stephen ; Frankel, Richard B. ; Blakemore, Richard P.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a442t-5d50c6382dc4f0f1705a9e5aefc1edad0748d5ba3a9113bc83819a30d07b52d73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1984</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Humanities and Social Sciences</topic><topic>letter</topic><topic>Mineralogy</topic><topic>multidisciplinary</topic><topic>Non silicates</topic><topic>Science</topic><topic>Science (multidisciplinary)</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Mann, Stephen</creatorcontrib><creatorcontrib>Frankel, Richard B.</creatorcontrib><creatorcontrib>Blakemore, Richard P.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Nature (London)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Mann, Stephen</au><au>Frankel, Richard B.</au><au>Blakemore, Richard P.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Structure, morphology and crystal growth of bacterial magnetite</atitle><jtitle>Nature (London)</jtitle><stitle>Nature</stitle><date>1984-01-01</date><risdate>1984</risdate><volume>310</volume><issue>5976</issue><spage>405</spage><epage>407</epage><pages>405-407</pages><issn>0028-0836</issn><eissn>1476-4687</eissn><coden>NATUAS</coden><abstract>Recent high-resolution transmission electron microscopy (HRTEM) studies of the structure and morphology of bacterial magnetite (Fe
3
O
4
) crystals isolated from a magnetotactic coccus
1
and from an unidentified bacterium extracted from sediment
2
have shown the crystals to be well ordered single-domain particles with a morphology based on a hexagonal prism of {011} faces truncated by specific low index planes. We report here a HRTEM study of intact magnetite crystals (magnetosomes) in the microaerophilic bacterium
Aquaspirillum magnetotacticum
, grown in pure culture
3,4
. Our aim has been to investigate the structure, morphology and crystal growth of the magnetite particles in the light of a recent Mossbauer spectroscopy study of this organism
5
which indicated, in addition to magnetite, the presence of hydrated iron(
III
) oxide phases together with the magnetosomes. Our results show that the mature particles are well ordered single-domain crystals of magnetite with a morphology very different from previously studied crystals and based on an octahedral prism of {111} faces truncated by {100} faces. We also show the first direct evidence for both crystalline and non-crystalline phases within individual magnetosomes. The results are important in aiding elucidation of the crystal growth mechanisms of biogenic magnetite.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><doi>10.1038/310405a0</doi><tpages>3</tpages><oa>free_for_read</oa></addata></record> |
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ispartof | Nature (London), 1984-01, Vol.310 (5976), p.405-407 |
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language | eng |
recordid | cdi_proquest_miscellaneous_14176253 |
source | Nature |
subjects | Earth sciences Earth, ocean, space Exact sciences and technology Humanities and Social Sciences letter Mineralogy multidisciplinary Non silicates Science Science (multidisciplinary) |
title | Structure, morphology and crystal growth of bacterial magnetite |
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