Symbiont‐driven sulfur crystal formation in a thiotrophic symbiosis from deep‐sea hydrocarbon seeps

Summary The siboglinid tubeworm Sclerolinum contortum symbiosis inhabits sulfidic sediments at deep‐sea hydrocarbon seeps in the G ulf of M exico. A single symbiont phylotype in the symbiont‐housing organ is inferred from phylogenetic analyses of the 16 S ribosomal ribonucleic acid (16 S rRNA ) gene...

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Published in:Environmental Microbiology Reports
Main Authors: Eichinger, Irmgard, Schmitz‐Esser, Stephan, Schmid, Markus, Fisher, Charles R., Bright, Monika
Other Authors: Austrian Science Fund
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2014
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Online Access:http://dx.doi.org/10.1111/1758-2229.12149
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spelling crwiley:10.1111/1758-2229.12149 2024-09-09T19:26:00+00:00 Symbiont‐driven sulfur crystal formation in a thiotrophic symbiosis from deep‐sea hydrocarbon seeps Eichinger, Irmgard Schmitz‐Esser, Stephan Schmid, Markus Fisher, Charles R. Bright, Monika Austrian Science Fund 2014 http://dx.doi.org/10.1111/1758-2229.12149 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2F1758-2229.12149 https://onlinelibrary.wiley.com/doi/pdf/10.1111/1758-2229.12149 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/1758-2229.12149 http://onlinelibrary.wiley.com/wol1/doi/10.1111/1758-2229.12149/fullpdf en eng Wiley http://creativecommons.org/licenses/by/4.0/ Environmental Microbiology Reports volume 6, issue 4, page 364-372 ISSN 1758-2229 1758-2229 journal-article 2014 crwiley https://doi.org/10.1111/1758-2229.12149 2024-08-20T04:16:14Z Summary The siboglinid tubeworm Sclerolinum contortum symbiosis inhabits sulfidic sediments at deep‐sea hydrocarbon seeps in the G ulf of M exico. A single symbiont phylotype in the symbiont‐housing organ is inferred from phylogenetic analyses of the 16 S ribosomal ribonucleic acid (16 S rRNA ) gene and fluorescent in situ hybridization. The phylotype we studied here, and a previous study from an arctic hydrocarbon seep population, reveal identical 16 S rRNA symbiont gene sequences. While sulfide is apparently the energy source for the symbionts (and ultimately the gutless host), both partners also have to cope with its toxicity. This study demonstrates abundant large sulfur crystals restricted to the trophosome area. Based on R aman microspectroscopy and energy dispersive X ‐ray analysis, these crystals have the same S 8 sulfur configuration as the recently described small sulfur vesicles formed in the symbionts. The crystals reside adjacent to the symbionts in the trophosome. This suggests that their formation is either extra‐ or intracellular in symbionts. We propose that formation of these crystals provides both energy‐storage compounds for the symbionts and serves the symbiosis by removing excess toxic sulfide from host tissues. This symbiont‐mediated sulfide detoxification may have been crucial for the establishment of thiotrophic symbiosis and continues to remain an important function of the symbionts. Article in Journal/Newspaper Arctic Wiley Online Library Arctic Environmental Microbiology Reports 6 4 364 372
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Summary The siboglinid tubeworm Sclerolinum contortum symbiosis inhabits sulfidic sediments at deep‐sea hydrocarbon seeps in the G ulf of M exico. A single symbiont phylotype in the symbiont‐housing organ is inferred from phylogenetic analyses of the 16 S ribosomal ribonucleic acid (16 S rRNA ) gene and fluorescent in situ hybridization. The phylotype we studied here, and a previous study from an arctic hydrocarbon seep population, reveal identical 16 S rRNA symbiont gene sequences. While sulfide is apparently the energy source for the symbionts (and ultimately the gutless host), both partners also have to cope with its toxicity. This study demonstrates abundant large sulfur crystals restricted to the trophosome area. Based on R aman microspectroscopy and energy dispersive X ‐ray analysis, these crystals have the same S 8 sulfur configuration as the recently described small sulfur vesicles formed in the symbionts. The crystals reside adjacent to the symbionts in the trophosome. This suggests that their formation is either extra‐ or intracellular in symbionts. We propose that formation of these crystals provides both energy‐storage compounds for the symbionts and serves the symbiosis by removing excess toxic sulfide from host tissues. This symbiont‐mediated sulfide detoxification may have been crucial for the establishment of thiotrophic symbiosis and continues to remain an important function of the symbionts.
author2 Austrian Science Fund
format Article in Journal/Newspaper
author Eichinger, Irmgard
Schmitz‐Esser, Stephan
Schmid, Markus
Fisher, Charles R.
Bright, Monika
spellingShingle Eichinger, Irmgard
Schmitz‐Esser, Stephan
Schmid, Markus
Fisher, Charles R.
Bright, Monika
Symbiont‐driven sulfur crystal formation in a thiotrophic symbiosis from deep‐sea hydrocarbon seeps
author_facet Eichinger, Irmgard
Schmitz‐Esser, Stephan
Schmid, Markus
Fisher, Charles R.
Bright, Monika
author_sort Eichinger, Irmgard
title Symbiont‐driven sulfur crystal formation in a thiotrophic symbiosis from deep‐sea hydrocarbon seeps
title_short Symbiont‐driven sulfur crystal formation in a thiotrophic symbiosis from deep‐sea hydrocarbon seeps
title_full Symbiont‐driven sulfur crystal formation in a thiotrophic symbiosis from deep‐sea hydrocarbon seeps
title_fullStr Symbiont‐driven sulfur crystal formation in a thiotrophic symbiosis from deep‐sea hydrocarbon seeps
title_full_unstemmed Symbiont‐driven sulfur crystal formation in a thiotrophic symbiosis from deep‐sea hydrocarbon seeps
title_sort symbiont‐driven sulfur crystal formation in a thiotrophic symbiosis from deep‐sea hydrocarbon seeps
publisher Wiley
publishDate 2014
url http://dx.doi.org/10.1111/1758-2229.12149
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2F1758-2229.12149
https://onlinelibrary.wiley.com/doi/pdf/10.1111/1758-2229.12149
https://onlinelibrary.wiley.com/doi/full-xml/10.1111/1758-2229.12149
http://onlinelibrary.wiley.com/wol1/doi/10.1111/1758-2229.12149/fullpdf
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