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Microbial siderophores as molecular shuttles for metal cations: sources, sinks and application perspectives
Iron is one of the highly abundant elements on the earth’s crust, an essential micronutrient for a majority of life forms, and exists in two frequent oxidation states such as ferrous (Fe 2+ ) and ferric (Fe 3+ ). These two oxidation states are interconvertible by redox reactions and form complexes w...
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| Published in: | Archives of microbiology 2023-09, Vol.205 (9), p.322-322, Article 322 |
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| Main Authors: | , , , |
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| cites | cdi_FETCH-LOGICAL-c352t-100e4a88f0a4203a6a35274de00050dcb3f0f8648913482d18b200129281aa043 |
| container_end_page | 322 |
| container_issue | 9 |
| container_start_page | 322 |
| container_title | Archives of microbiology |
| container_volume | 205 |
| creator | Vijay, Karuppiah Shibasini, Murugan Sivasakthivelan, Panneerselvam Kavitha, Thangavel |
| description | Iron is one of the highly abundant elements on the earth’s crust, an essential micronutrient for a majority of life forms, and exists in two frequent oxidation states such as ferrous (Fe
2+
) and ferric (Fe
3+
). These two oxidation states are interconvertible by redox reactions and form complexes with a wide range of siderophores. At neutral pH in soil, Fe
2+
is highly soluble upto 100 mM but have less biological value, whereas Fe
3+
is less soluble upto 10
–9
M. This reduced bioavailability of Fe
3+
induces competition among microorganisms. As many microorganisms need at least 10
–6
M of Fe
3+
form of iron for their growth, siderophores from these microbes readily withdraw Fe
3+
iron from a variety of habitats for their survival. In this review, we bring into light the several recent investigations related to diverse chemistry of microbial siderophores, mechanisms of siderophore uptake, biosynthetic gene clusters in microbial genomes, various sources of heavy metal cations in soil, siderophore-binding protein receptors and commercialisation perspectives of siderophores. Besides, this review unearths the recent advancements in the characterisation of novel siderophores and its heavy metal complexes alongside the interaction kinetics with receptors. |
| doi_str_mv | 10.1007/s00203-023-03644-3 |
| format | article |
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2+
) and ferric (Fe
3+
). These two oxidation states are interconvertible by redox reactions and form complexes with a wide range of siderophores. At neutral pH in soil, Fe
2+
is highly soluble upto 100 mM but have less biological value, whereas Fe
3+
is less soluble upto 10
–9
M. This reduced bioavailability of Fe
3+
induces competition among microorganisms. As many microorganisms need at least 10
–6
M of Fe
3+
form of iron for their growth, siderophores from these microbes readily withdraw Fe
3+
iron from a variety of habitats for their survival. In this review, we bring into light the several recent investigations related to diverse chemistry of microbial siderophores, mechanisms of siderophore uptake, biosynthetic gene clusters in microbial genomes, various sources of heavy metal cations in soil, siderophore-binding protein receptors and commercialisation perspectives of siderophores. Besides, this review unearths the recent advancements in the characterisation of novel siderophores and its heavy metal complexes alongside the interaction kinetics with receptors.</description><identifier>ISSN: 0302-8933</identifier><identifier>EISSN: 1432-072X</identifier><identifier>DOI: 10.1007/s00203-023-03644-3</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Bioavailability ; Biochemistry ; Biomedical and Life Sciences ; Biotechnology ; Cations ; Cell Biology ; Commercialization ; Coordination compounds ; Earth crust ; Ecology ; Gene clusters ; Genomes ; Heavy metals ; Iron ; Life Sciences ; Metal complexes ; Metal ions ; Microbial Ecology ; Microbiology ; Microorganisms ; Mini Review ; Oxidation ; Receptors ; Redox reactions ; Siderophores ; Soil pH ; Soils</subject><ispartof>Archives of microbiology, 2023-09, Vol.205 (9), p.322-322, Article 322</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c352t-100e4a88f0a4203a6a35274de00050dcb3f0f8648913482d18b200129281aa043</citedby><cites>FETCH-LOGICAL-c352t-100e4a88f0a4203a6a35274de00050dcb3f0f8648913482d18b200129281aa043</cites><orcidid>0000-0002-3167-0803 ; 0000-0003-2148-1109 ; 0000-0002-7554-3080 ; 0000-0001-7950-7899</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Vijay, Karuppiah</creatorcontrib><creatorcontrib>Shibasini, Murugan</creatorcontrib><creatorcontrib>Sivasakthivelan, Panneerselvam</creatorcontrib><creatorcontrib>Kavitha, Thangavel</creatorcontrib><title>Microbial siderophores as molecular shuttles for metal cations: sources, sinks and application perspectives</title><title>Archives of microbiology</title><addtitle>Arch Microbiol</addtitle><description>Iron is one of the highly abundant elements on the earth’s crust, an essential micronutrient for a majority of life forms, and exists in two frequent oxidation states such as ferrous (Fe
2+
) and ferric (Fe
3+
). These two oxidation states are interconvertible by redox reactions and form complexes with a wide range of siderophores. At neutral pH in soil, Fe
2+
is highly soluble upto 100 mM but have less biological value, whereas Fe
3+
is less soluble upto 10
–9
M. This reduced bioavailability of Fe
3+
induces competition among microorganisms. As many microorganisms need at least 10
–6
M of Fe
3+
form of iron for their growth, siderophores from these microbes readily withdraw Fe
3+
iron from a variety of habitats for their survival. In this review, we bring into light the several recent investigations related to diverse chemistry of microbial siderophores, mechanisms of siderophore uptake, biosynthetic gene clusters in microbial genomes, various sources of heavy metal cations in soil, siderophore-binding protein receptors and commercialisation perspectives of siderophores. Besides, this review unearths the recent advancements in the characterisation of novel siderophores and its heavy metal complexes alongside the interaction kinetics with receptors.</description><subject>Bioavailability</subject><subject>Biochemistry</subject><subject>Biomedical and Life Sciences</subject><subject>Biotechnology</subject><subject>Cations</subject><subject>Cell Biology</subject><subject>Commercialization</subject><subject>Coordination compounds</subject><subject>Earth crust</subject><subject>Ecology</subject><subject>Gene clusters</subject><subject>Genomes</subject><subject>Heavy metals</subject><subject>Iron</subject><subject>Life Sciences</subject><subject>Metal complexes</subject><subject>Metal ions</subject><subject>Microbial Ecology</subject><subject>Microbiology</subject><subject>Microorganisms</subject><subject>Mini Review</subject><subject>Oxidation</subject><subject>Receptors</subject><subject>Redox reactions</subject><subject>Siderophores</subject><subject>Soil pH</subject><subject>Soils</subject><issn>0302-8933</issn><issn>1432-072X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp9kE1LxDAQhoMouK7-AU8BLx6sTj7apt5k8QtWvCh4C9k2dbubbWqmFfz3ZreC4MFDGBied8j7EHLK4JIB5FcIwEEkwOMTmZSJ2CMTJgVPIOdv-2QCAniiCiEOyRHiCoBxpdSErJ-aMvhFYxzFprLBd0sfLFKDdOOdLQdnAsXl0Pcubmsf6Mb2ES5N3_gWryn6IZQWL2K8XcdcW1HTda4ZAdrZgJ0t--bT4jE5qI1De_Izp-T17vZl9pDMn-8fZzfzpBQp75NYyEqjVA1GxlImM3Gdy8oCQApVuRA11CqTqmBCKl4xteDbPgVXzBiQYkrOx7td8B-DxV5vGiytc6a1fkDNVaoKleWZiujZH3QV-7TxdztKFipN80jxkYqqEIOtdReajQlfmoHe-tejfx39651_LWJIjCGMcPtuw-_pf1LfjlKIXA</recordid><startdate>20230901</startdate><enddate>20230901</enddate><creator>Vijay, Karuppiah</creator><creator>Shibasini, Murugan</creator><creator>Sivasakthivelan, Panneerselvam</creator><creator>Kavitha, Thangavel</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QL</scope><scope>7U9</scope><scope>7X7</scope><scope>7XB</scope><scope>88A</scope><scope>88E</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>H94</scope><scope>HCIFZ</scope><scope>K9.</scope><scope>LK8</scope><scope>M0S</scope><scope>M1P</scope><scope>M7N</scope><scope>M7P</scope><scope>P64</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>RC3</scope><scope>7X8</scope><orcidid>https://orcid.org/0000-0002-3167-0803</orcidid><orcidid>https://orcid.org/0000-0003-2148-1109</orcidid><orcidid>https://orcid.org/0000-0002-7554-3080</orcidid><orcidid>https://orcid.org/0000-0001-7950-7899</orcidid></search><sort><creationdate>20230901</creationdate><title>Microbial siderophores as molecular shuttles for metal cations: sources, sinks and application perspectives</title><author>Vijay, Karuppiah ; 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2+
) and ferric (Fe
3+
). These two oxidation states are interconvertible by redox reactions and form complexes with a wide range of siderophores. At neutral pH in soil, Fe
2+
is highly soluble upto 100 mM but have less biological value, whereas Fe
3+
is less soluble upto 10
–9
M. This reduced bioavailability of Fe
3+
induces competition among microorganisms. As many microorganisms need at least 10
–6
M of Fe
3+
form of iron for their growth, siderophores from these microbes readily withdraw Fe
3+
iron from a variety of habitats for their survival. In this review, we bring into light the several recent investigations related to diverse chemistry of microbial siderophores, mechanisms of siderophore uptake, biosynthetic gene clusters in microbial genomes, various sources of heavy metal cations in soil, siderophore-binding protein receptors and commercialisation perspectives of siderophores. Besides, this review unearths the recent advancements in the characterisation of novel siderophores and its heavy metal complexes alongside the interaction kinetics with receptors.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00203-023-03644-3</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0002-3167-0803</orcidid><orcidid>https://orcid.org/0000-0003-2148-1109</orcidid><orcidid>https://orcid.org/0000-0002-7554-3080</orcidid><orcidid>https://orcid.org/0000-0001-7950-7899</orcidid></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0302-8933 |
| ispartof | Archives of microbiology, 2023-09, Vol.205 (9), p.322-322, Article 322 |
| issn | 0302-8933 1432-072X |
| language | eng |
| recordid | cdi_proquest_miscellaneous_2858986768 |
| source | Springer Nature |
| subjects | Bioavailability Biochemistry Biomedical and Life Sciences Biotechnology Cations Cell Biology Commercialization Coordination compounds Earth crust Ecology Gene clusters Genomes Heavy metals Iron Life Sciences Metal complexes Metal ions Microbial Ecology Microbiology Microorganisms Mini Review Oxidation Receptors Redox reactions Siderophores Soil pH Soils |
| title | Microbial siderophores as molecular shuttles for metal cations: sources, sinks and application perspectives |
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