Barite (BaSO 4 ) biomineralization at Flybye Springs, a cold sulphur spring system in Canada's Northwest Territories

The Flybye Springs, Northwest Territories, consist of 10 active vents and numerous small seeps that discharge sulphide- and barium-rich spring waters at an average temperature 8.5 °C. Oxidation of sulphide to sulphate drives precipitation of stellate and platy barite microcrystals in the proximal fl...

Full description

Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Bonny, Sandy M, Jones, Brian
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2007
Subjects:
Online Access:http://dx.doi.org/10.1139/e06-126
http://www.nrcresearchpress.com/doi/pdf/10.1139/e06-126
id crcansciencepubl:10.1139/e06-126
record_format openpolar
spelling crcansciencepubl:10.1139/e06-126 2024-06-23T07:55:42+00:00 Barite (BaSO 4 ) biomineralization at Flybye Springs, a cold sulphur spring system in Canada's Northwest Territories Bonny, Sandy M Jones, Brian 2007 http://dx.doi.org/10.1139/e06-126 http://www.nrcresearchpress.com/doi/pdf/10.1139/e06-126 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 44, issue 6, page 835-856 ISSN 0008-4077 1480-3313 journal-article 2007 crcansciencepubl https://doi.org/10.1139/e06-126 2024-06-06T04:11:17Z The Flybye Springs, Northwest Territories, consist of 10 active vents and numerous small seeps that discharge sulphide- and barium-rich spring waters at an average temperature 8.5 °C. Oxidation of sulphide to sulphate drives precipitation of stellate and platy barite microcrystals in the proximal flow paths. Downstream, and in vent- and tributary-fed ponds, barite is precipitated among streamer and mat forming colonies of sulphur-tolerant microbes, including Thiothrix, Beggiatoa, Thioploca, Chromatium, Oscillatoria, fungi (dominantly Penicillium), and unicellular sulphate reducing bacteria. These microbes mediate barite saturation by adjusting redox gradients and via passive adsorption of barium ions to cell surfaces and extracellular polymeric substances. Passive biomineralization produces barite laminae in floating microbial mats, nanometric coatings, and micrometric encrustations around microbial cells and filaments, and local permineralization of Thiothrix, Beggiatoa, and Oscillatoria outer cell walls. Intracellular barium enrichment and (or) metabolic sulphur oxidation may be important to "active biomineralization" that produces nanometric barite globules on the tips of fungal hyphae, barite-filled cell cavities in Beggiatoa and Thiothrix, and baritized sulphur globules. Degradation of biomineralized cells generates detrital "microfossils," including barite tunnels, layered cylinders, solid cylindrical grains and chains of barite beads. The diversity of inorganic and biomineralized barite in the Flybye Springs flow path highlights the influence of ambient chemistry, microbial metabolism, and cellular structure on barite solubility and on the taphonomy of microfossils preserved in barite. Article in Journal/Newspaper Northwest Territories Canadian Science Publishing Northwest Territories Canadian Journal of Earth Sciences 44 6 835 856
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description The Flybye Springs, Northwest Territories, consist of 10 active vents and numerous small seeps that discharge sulphide- and barium-rich spring waters at an average temperature 8.5 °C. Oxidation of sulphide to sulphate drives precipitation of stellate and platy barite microcrystals in the proximal flow paths. Downstream, and in vent- and tributary-fed ponds, barite is precipitated among streamer and mat forming colonies of sulphur-tolerant microbes, including Thiothrix, Beggiatoa, Thioploca, Chromatium, Oscillatoria, fungi (dominantly Penicillium), and unicellular sulphate reducing bacteria. These microbes mediate barite saturation by adjusting redox gradients and via passive adsorption of barium ions to cell surfaces and extracellular polymeric substances. Passive biomineralization produces barite laminae in floating microbial mats, nanometric coatings, and micrometric encrustations around microbial cells and filaments, and local permineralization of Thiothrix, Beggiatoa, and Oscillatoria outer cell walls. Intracellular barium enrichment and (or) metabolic sulphur oxidation may be important to "active biomineralization" that produces nanometric barite globules on the tips of fungal hyphae, barite-filled cell cavities in Beggiatoa and Thiothrix, and baritized sulphur globules. Degradation of biomineralized cells generates detrital "microfossils," including barite tunnels, layered cylinders, solid cylindrical grains and chains of barite beads. The diversity of inorganic and biomineralized barite in the Flybye Springs flow path highlights the influence of ambient chemistry, microbial metabolism, and cellular structure on barite solubility and on the taphonomy of microfossils preserved in barite.
format Article in Journal/Newspaper
author Bonny, Sandy M
Jones, Brian
spellingShingle Bonny, Sandy M
Jones, Brian
Barite (BaSO 4 ) biomineralization at Flybye Springs, a cold sulphur spring system in Canada's Northwest Territories
author_facet Bonny, Sandy M
Jones, Brian
author_sort Bonny, Sandy M
title Barite (BaSO 4 ) biomineralization at Flybye Springs, a cold sulphur spring system in Canada's Northwest Territories
title_short Barite (BaSO 4 ) biomineralization at Flybye Springs, a cold sulphur spring system in Canada's Northwest Territories
title_full Barite (BaSO 4 ) biomineralization at Flybye Springs, a cold sulphur spring system in Canada's Northwest Territories
title_fullStr Barite (BaSO 4 ) biomineralization at Flybye Springs, a cold sulphur spring system in Canada's Northwest Territories
title_full_unstemmed Barite (BaSO 4 ) biomineralization at Flybye Springs, a cold sulphur spring system in Canada's Northwest Territories
title_sort barite (baso 4 ) biomineralization at flybye springs, a cold sulphur spring system in canada's northwest territories
publisher Canadian Science Publishing
publishDate 2007
url http://dx.doi.org/10.1139/e06-126
http://www.nrcresearchpress.com/doi/pdf/10.1139/e06-126
geographic Northwest Territories
geographic_facet Northwest Territories
genre Northwest Territories
genre_facet Northwest Territories
op_source Canadian Journal of Earth Sciences
volume 44, issue 6, page 835-856
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e06-126
container_title Canadian Journal of Earth Sciences
container_volume 44
container_issue 6
container_start_page 835
op_container_end_page 856
_version_ 1802648372850458624