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D:L-Amino Acid Modeling Reveals Fast Microbial Turnover of Days to Months in the Subsurface Hydrothermal Sediment of Guaymas Basin

We investigated the impact of temperature on the microbial turnover of organic matter (OM) in a hydrothermal vent system in Guaymas Basin, by calculating microbial bio- and necromass turnover times based on the culture-independent D:L-amino acid model. Sediments were recovered from two stations near...

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Autores principales: Møller, Mikkel H., Glombitza, Clemens, Lever, Mark A., Deng, Longhui, Morono, Yuki, Inagaki, Fumio, Doll, Mechthild, Su, Chin-chia, Lomstein, Bente A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5963217/
https://www.ncbi.nlm.nih.gov/pubmed/29867871
http://dx.doi.org/10.3389/fmicb.2018.00967
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author Møller, Mikkel H.
Glombitza, Clemens
Lever, Mark A.
Deng, Longhui
Morono, Yuki
Inagaki, Fumio
Doll, Mechthild
Su, Chin-chia
Lomstein, Bente A.
author_facet Møller, Mikkel H.
Glombitza, Clemens
Lever, Mark A.
Deng, Longhui
Morono, Yuki
Inagaki, Fumio
Doll, Mechthild
Su, Chin-chia
Lomstein, Bente A.
author_sort Møller, Mikkel H.
collection PubMed
description We investigated the impact of temperature on the microbial turnover of organic matter (OM) in a hydrothermal vent system in Guaymas Basin, by calculating microbial bio- and necromass turnover times based on the culture-independent D:L-amino acid model. Sediments were recovered from two stations near hydrothermal mounds (<74°C) and from one cold station (<9°C). Cell abundance at the two hydrothermal stations dropped from 10(8) to 10(6) cells cm(-3) within ∼5 m of sediment depth resulting in a 100-fold lower cell number at this depth than at the cold site where numbers remained constant at 10(8) cells cm(-3) throughout the recovered sediment. There were strong indications that the drop in cell abundance was controlled by decreasing OM quality. The quality of the sedimentary OM was determined by the diagenetic indicators %T(AA)C (percentage of total organic carbon present as amino acid carbon), %T(AA)N (percentage of total nitrogen present as amino acid nitrogen), aspartic acid:β-alanine ratios, and glutamic acid:γ-amino butyric acid ratios. All parameters indicated that the OM became progressively degraded with increasing sediment depth, and the OM in the hydrothermal sediment was more degraded than in the uniformly cold sediment. Nonetheless, the small community of microorganisms in the hydrothermal sediment demonstrated short turnover times. The modeled turnover times of microbial bio- and necromass in the hydrothermal sediments were notably faster (biomass: days to months; necromass: up to a few hundred years) than in the cold sediments (biomass: tens of years; necromass: thousands of years), suggesting that temperature has a significant influence on the microbial turnover rates. We suggest that short biomass turnover times are necessary for maintance of essential cell funtions and to overcome potential damage caused by the increased temperature.The reduced OM quality at the hyrothemal sites might thus only allow for a small population size of microorganisms.
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spelling pubmed-59632172018-06-04 D:L-Amino Acid Modeling Reveals Fast Microbial Turnover of Days to Months in the Subsurface Hydrothermal Sediment of Guaymas Basin Møller, Mikkel H. Glombitza, Clemens Lever, Mark A. Deng, Longhui Morono, Yuki Inagaki, Fumio Doll, Mechthild Su, Chin-chia Lomstein, Bente A. Front Microbiol Microbiology We investigated the impact of temperature on the microbial turnover of organic matter (OM) in a hydrothermal vent system in Guaymas Basin, by calculating microbial bio- and necromass turnover times based on the culture-independent D:L-amino acid model. Sediments were recovered from two stations near hydrothermal mounds (<74°C) and from one cold station (<9°C). Cell abundance at the two hydrothermal stations dropped from 10(8) to 10(6) cells cm(-3) within ∼5 m of sediment depth resulting in a 100-fold lower cell number at this depth than at the cold site where numbers remained constant at 10(8) cells cm(-3) throughout the recovered sediment. There were strong indications that the drop in cell abundance was controlled by decreasing OM quality. The quality of the sedimentary OM was determined by the diagenetic indicators %T(AA)C (percentage of total organic carbon present as amino acid carbon), %T(AA)N (percentage of total nitrogen present as amino acid nitrogen), aspartic acid:β-alanine ratios, and glutamic acid:γ-amino butyric acid ratios. All parameters indicated that the OM became progressively degraded with increasing sediment depth, and the OM in the hydrothermal sediment was more degraded than in the uniformly cold sediment. Nonetheless, the small community of microorganisms in the hydrothermal sediment demonstrated short turnover times. The modeled turnover times of microbial bio- and necromass in the hydrothermal sediments were notably faster (biomass: days to months; necromass: up to a few hundred years) than in the cold sediments (biomass: tens of years; necromass: thousands of years), suggesting that temperature has a significant influence on the microbial turnover rates. We suggest that short biomass turnover times are necessary for maintance of essential cell funtions and to overcome potential damage caused by the increased temperature.The reduced OM quality at the hyrothemal sites might thus only allow for a small population size of microorganisms. Frontiers Media S.A. 2018-05-15 /pmc/articles/PMC5963217/ /pubmed/29867871 http://dx.doi.org/10.3389/fmicb.2018.00967 Text en Copyright © 2018 Møller, Glombitza, Lever, Deng, Morono, Inagaki, Doll, Su and Lomstein. http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
spellingShingle Microbiology
Møller, Mikkel H.
Glombitza, Clemens
Lever, Mark A.
Deng, Longhui
Morono, Yuki
Inagaki, Fumio
Doll, Mechthild
Su, Chin-chia
Lomstein, Bente A.
D:L-Amino Acid Modeling Reveals Fast Microbial Turnover of Days to Months in the Subsurface Hydrothermal Sediment of Guaymas Basin
title D:L-Amino Acid Modeling Reveals Fast Microbial Turnover of Days to Months in the Subsurface Hydrothermal Sediment of Guaymas Basin
title_full D:L-Amino Acid Modeling Reveals Fast Microbial Turnover of Days to Months in the Subsurface Hydrothermal Sediment of Guaymas Basin
title_fullStr D:L-Amino Acid Modeling Reveals Fast Microbial Turnover of Days to Months in the Subsurface Hydrothermal Sediment of Guaymas Basin
title_full_unstemmed D:L-Amino Acid Modeling Reveals Fast Microbial Turnover of Days to Months in the Subsurface Hydrothermal Sediment of Guaymas Basin
title_short D:L-Amino Acid Modeling Reveals Fast Microbial Turnover of Days to Months in the Subsurface Hydrothermal Sediment of Guaymas Basin
title_sort d:l-amino acid modeling reveals fast microbial turnover of days to months in the subsurface hydrothermal sediment of guaymas basin
topic Microbiology
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5963217/
https://www.ncbi.nlm.nih.gov/pubmed/29867871
http://dx.doi.org/10.3389/fmicb.2018.00967
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