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Bacteriogenic iron oxides as an evidence of hydrothermal vent activity : case study from the Polish part of the Silesian Nappe and Tatra Massif

2014
journal article
conference proceedings
Journal
Buletini i Shkencave Gjeologjike
Author
Bąk Marta

Bąk Krzysztof

Wolska Anna

Górny Zbigniew

Stożek Beata
Title of volume
Special Issue : Proceedings XX Congress of the Carpathian-Balkan Geological Association
Volume
1
Pages
75-78
ISSN
0254-5276
eISSN
2306-9600
Keywords in English

Iron related bacteria

hydrothermal vents

Upper Albian-Cenomanian

Silesian Nappe of Outer Carpathians

Tatra Massif

URL
https://www.researchgate.net/profile/Zbigniew_Gorny/publication/272489349
Access date
2015-07-01
Language
English
Journal language
English
Abstract in English

Ferruginous (i.e. ferrous oxides/hydroxides) coatings occurring in the Upper Albian– Cenomanian marine sediments of the Carpathians, represent the occurrence of Iron Related Bacteria. The singular grain coatings consist of densely packed elongated capsules of 5 μm width, with a wall thickness of 0.1 μm. These structures are remnants of the original bacterial sheath. The chemical composition of the capsules and their morphology show that they may be representatives of the Sphaerotilus–Leptothrix group, living recently around low-temperature hydrothermal vents. Such vents are interpreted as the source of metals for bottom sediments in the Silesian Basin (Outer Carpathians) and most probably in the Tatric Basin (Inner Carpathians), too.

Conference
XX Congress of the Carpathian-Balkan Geological Association
Conference start date
2014-09-24
End date conference
2014-09-26
Conference city
Tirana
Conference country
Albania
Conference type
international
Affiliation
Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych
dc.abstract.enFerruginous (i.e. ferrous oxides/hydroxides) coatings occurring in the Upper Albian– Cenomanian marine sediments of the Carpathians, represent the occurrence of Iron Related Bacteria. The singular grain coatings consist of densely packed elongated capsules of 5 μm width, with a wall thickness of 0.1 μm. These structures are remnants of the original bacterial sheath. The chemical composition of the capsules and their morphology show that they may be representatives of the Sphaerotilus–Leptothrix group, living recently around low-temperature hydrothermal vents. Such vents are interpreted as the source of metals for bottom sediments in the Silesian Basin (Outer Carpathians) and most probably in the Tatric Basin (Inner Carpathians), too.pl
dc.affiliationWydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznychpl
dc.conferenceXX Congress of the Carpathian-Balkan Geological Association
dc.conference.cityTirana
dc.conference.countryAlbania
dc.conference.datefinish2014-09-26
dc.conference.datestart2014-09-24
dc.contributor.authorBąk, Marta - 127266 pl
dc.contributor.authorBąk, Krzysztofpl
dc.contributor.authorWolska, Anna - 132729 pl
dc.contributor.authorGórny, Zbigniew - 182279 pl
dc.contributor.authorStożek, Beata - 142886 pl
dc.date.accession2015-07-01pl
dc.date.accessioned2015-07-01T15:54:54Z
dc.date.available2015-07-01T15:54:54Z
dc.date.issued2014pl
dc.date.openaccess5
dc.description.accesstimepo opublikowaniu
dc.description.conftypeinternationalpl
dc.description.physical75-78pl
dc.description.publication0,43pl
dc.description.versionostateczna wersja autorska (postprint)
dc.description.volume1pl
dc.identifier.eissn2306-9600pl
dc.identifier.issn0254-5276pl
dc.identifier.urihttp://ruj.uj.edu.pl/xmlui/handle/item/11067
dc.identifier.weblinkhttps://www.researchgate.net/profile/Zbigniew_Gorny/publication/272489349pl
dc.languageengpl
dc.language.containerengpl
dc.rightsDodaję tylko opis bibliograficzny*
dc.rights.licenceInna otwarta licencja
dc.rights.uri*
dc.share.typeinne
dc.subject.enIron related bacteriapl
dc.subject.enhydrothermal ventspl
dc.subject.enUpper Albian-Cenomanianpl
dc.subject.enSilesian Nappe of Outer Carpathianspl
dc.subject.enTatra Massifpl
dc.subtypeConferenceProceedingspl
dc.titleBacteriogenic iron oxides as an evidence of hydrothermal vent activity : case study from the Polish part of the Silesian Nappe and Tatra Massifpl
dc.title.journalBuletini i Shkencave Gjeologjikepl
dc.title.volumeSpecial Issue : Proceedings XX Congress of the Carpathian-Balkan Geological Associationpl
dc.typeJournalArticlepl
dspace.entity.typePublication
dc.abstract.enpl
Ferruginous (i.e. ferrous oxides/hydroxides) coatings occurring in the Upper Albian– Cenomanian marine sediments of the Carpathians, represent the occurrence of Iron Related Bacteria. The singular grain coatings consist of densely packed elongated capsules of 5 μm width, with a wall thickness of 0.1 μm. These structures are remnants of the original bacterial sheath. The chemical composition of the capsules and their morphology show that they may be representatives of the Sphaerotilus–Leptothrix group, living recently around low-temperature hydrothermal vents. Such vents are interpreted as the source of metals for bottom sediments in the Silesian Basin (Outer Carpathians) and most probably in the Tatric Basin (Inner Carpathians), too.
dc.affiliationpl
Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych
dc.conference
XX Congress of the Carpathian-Balkan Geological Association
dc.conference.city
Tirana
dc.conference.country
Albania
dc.conference.datefinish
2014-09-26
dc.conference.datestart
2014-09-24
dc.contributor.authorpl
Bąk, Marta - 127266
dc.contributor.authorpl
Bąk, Krzysztof
dc.contributor.authorpl
Wolska, Anna - 132729
dc.contributor.authorpl
Górny, Zbigniew - 182279
dc.contributor.authorpl
Stożek, Beata - 142886
dc.date.accessionpl
2015-07-01
dc.date.accessioned
2015-07-01T15:54:54Z
dc.date.available
2015-07-01T15:54:54Z
dc.date.issuedpl
2014
dc.date.openaccess
5
dc.description.accesstime
po opublikowaniu
dc.description.conftypepl
international
dc.description.physicalpl
75-78
dc.description.publicationpl
0,43
dc.description.version
ostateczna wersja autorska (postprint)
dc.description.volumepl
1
dc.identifier.eissnpl
2306-9600
dc.identifier.issnpl
0254-5276
dc.identifier.uri
http://ruj.uj.edu.pl/xmlui/handle/item/11067
dc.identifier.weblinkpl
https://www.researchgate.net/profile/Zbigniew_Gorny/publication/272489349
dc.languagepl
eng
dc.language.containerpl
eng
dc.rights*
Dodaję tylko opis bibliograficzny
dc.rights.licence
Inna otwarta licencja
dc.rights.uri*
dc.share.type
inne
dc.subject.enpl
Iron related bacteria
dc.subject.enpl
hydrothermal vents
dc.subject.enpl
Upper Albian-Cenomanian
dc.subject.enpl
Silesian Nappe of Outer Carpathians
dc.subject.enpl
Tatra Massif
dc.subtypepl
ConferenceProceedings
dc.titlepl
Bacteriogenic iron oxides as an evidence of hydrothermal vent activity : case study from the Polish part of the Silesian Nappe and Tatra Massif
dc.title.journalpl
Buletini i Shkencave Gjeologjike
dc.title.volumepl
Special Issue : Proceedings XX Congress of the Carpathian-Balkan Geological Association
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations
Wydział Biologii
Wolska, Anna
Stożek, Beata
Górny, Zbigniew
No affiliation
Bąk, Marta
Bąk, Krzysztof

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