Occurrence and degradation of peptidoglycan in aquatic environments

Mechanisms controlling microbial degradation of dissolved organic matter (DOM) in aquatic environments are poorly understood, although microbes are crucial to global nutrient cycling. Bacterial cell wall components may be one of the keys in understanding the presence of slowly degrading DOM in natur...

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Published inFEMS microbiology ecology Vol. 46; no. 3; pp. 269 - 280
Main Authors Jørgensen, Niels O.G, Stepanaukas, Ramunas, Pedersen, Anne-Grethe U, Hansen, Michael, Nybroe, Ole
Format Journal Article Conference Proceeding
LanguageEnglish
Published Oxford, UK Elsevier B.V 01.12.2003
Blackwell Publishing Ltd
Blackwell
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Abstract Mechanisms controlling microbial degradation of dissolved organic matter (DOM) in aquatic environments are poorly understood, although microbes are crucial to global nutrient cycling. Bacterial cell wall components may be one of the keys in understanding the presence of slowly degrading DOM in nature. We found that dominant components of bacterial cell walls ( D-amino acids ( D-AA), glucosamine (GluA) and diaminopimelic acid (DAPA)) comprised up to 11.4% of the dissolved organic nitrogen in 50 diverse rivers entering the Baltic Sea. Occurrence of DAPA, a characteristic component of Gram-negative (G −) bacteria, in the rivers suggests that G − bacteria rather than Gram-positive (G +) were the major source of the cell wall material. In laboratory studies, the degradation of whole bacterial cells, cell wall material and purified peptidoglycan was studied to characterize degradation of cell wall material by natural aquatic bacteria. Addition of whole killed G − and G + bacteria to cultures of estuarine bacteria demonstrated fragmentation and loss of cell structure of the G + bacteria, while the G − bacteria maintained an intact cell shape during the entire 69-day period. In another experiment, estuarine bacteria degraded 39–69% of GluA, D-AA and DAPA in added cell wall material of a representative G − bacterial species during 8 days, as compared to a 72–89% degradation of GluA, D-AA and DAPA in cell material of a G + bacterial species. When cultures of estuarine bacteria were enriched with purified G − and G + peptidoglycan (1 mg l −1), at least 49% (G −) and 58% (G +) of D-AA in the peptidoglycan was degraded. No major changes in GluA were obvious. Interpretation of the results was difficult as a portion of the purified peptidoglycan was of similar size to the bacteria and could not be differentiated from cells growing in the cultures. Addition of the purified peptidoglycan stimulated the bacterial growth, and after 6 days the cell density in the enriched cultures was 4-fold higher than in the controls. A regrowth of bacteria after addition of L-broth at 105 days caused a 50- to 75-fold increase in dissolved D-AA and GluA. Most of the D-AA and GluA were taken up during the following 10 days, indicating that cell wall constituents are dynamic compounds. Our results show that a variable portion of peptidoglycan in G − and G + bacteria can be degraded by natural bacteria, and that peptidoglycan in G − bacteria is more resistant to bacterial attack than that in G + bacteria. Thus, the presence of cell wall constituents in natural DOM may reflect the recalcitrant nature of especially G − peptidoglycan.
AbstractList Mechanisms controlling microbial degradation of dissolved organic matter (DOM) in aquatic environments are poorly understood, although microbes are crucial to global nutrient cycling. Bacterial cell wall components may be one of the keys in understanding the presence of slowly degrading DOM in nature. We found that dominant components of bacterial cell walls (D-amino acids (D-AA), glucosamine (GluA) and diaminopimelic acid (DAPA)) comprised up to 11.4% of the dissolved organic nitrogen in 50 diverse rivers entering the Baltic Sea. Occurrence of DAPA, a characteristic component of Gram-negative (G(-)) bacteria, in the rivers suggests that G(-) bacteria rather than Gram-positive (G(+)) were the major source of the cell wall material. In laboratory studies, the degradation of whole bacterial cells, cell wall material and purified peptidoglycan was studied to characterize degradation of cell wall material by natural aquatic bacteria. Addition of whole killed G(-) and G(+) bacteria to cultures of estuarine bacteria demonstrated fragmentation and loss of cell structure of the G(+) bacteria, while the G(-) bacteria maintained an intact cell shape during the entire 69-day period. In another experiment, estuarine bacteria degraded 39-69% of GluA, D-AA and DAPA in added cell wall material of a representative G(-) bacterial species during 8 days, as compared to a 72-89% degradation of GluA, D-AA and DAPA in cell material of a G(+) bacterial species. When cultures of estuarine bacteria were enriched with purified G(-) and G(+) peptidoglycan (1 mg l(-1)), at least 49% (G(-)) and 58% (G(+)) Of D-AA in the peptidoglycan was degraded. No major changes in GluA were obvious. Interpretation of the results was difficult as a portion of the purified peptidoglycan was of similar size to the bacteria and could not be differentiated from cells growing in the cultures. Addition of the purified peptidoglycan stimulated the bacterial growth, and after 6 days the cell density in the enriched cultures was 4-fold higher than in the controls. A regrowth of bacteria after addition of L-broth at 105 days caused a 50- to 75-fold increase in dissolved D-AA and GluA. Most of the D-AA and GluA were taken up during the following 10 days, indicating that cell wall constituents are dynamic compounds. Our results show that a variable portion of peptidoglycan in G(-) and G(+) bacteria can be degraded by natural bacteria, and that peptidoglycan in G(-) bacteria is more resistant to bacterial attack than that in G(+) bacteria. Thus, the presence of cell wall constituents in natural DOM may reflect the recalcitrant nature of especially G(-) peptidoglycan. (C) 2003 Federation of European Microbiological Societies. Published by Elsevier B.V. All rights reserved.
Abstract Mechanisms controlling microbial degradation of dissolved organic matter (DOM) in aquatic environments are poorly understood, although microbes are crucial to global nutrient cycling. Bacterial cell wall components may be one of the keys in understanding the presence of slowly degrading DOM in nature. We found that dominant components of bacterial cell walls (d-amino acids (d-AA), glucosamine (GluA) and diaminopimelic acid (DAPA)) comprised up to 11.4% of the dissolved organic nitrogen in 50 diverse rivers entering the Baltic Sea. Occurrence of DAPA, a characteristic component of Gram-negative (G−) bacteria, in the rivers suggests that G− bacteria rather than Gram-positive (G+) were the major source of the cell wall material. In laboratory studies, the degradation of whole bacterial cells, cell wall material and purified peptidoglycan was studied to characterize degradation of cell wall material by natural aquatic bacteria. Addition of whole killed G− and G+ bacteria to cultures of estuarine bacteria demonstrated fragmentation and loss of cell structure of the G+ bacteria, while the G− bacteria maintained an intact cell shape during the entire 69-day period. In another experiment, estuarine bacteria degraded 39–69% of GluA, d-AA and DAPA in added cell wall material of a representative G− bacterial species during 8 days, as compared to a 72–89% degradation of GluA, d-AA and DAPA in cell material of a G+ bacterial species. When cultures of estuarine bacteria were enriched with purified G− and G+ peptidoglycan (1 mg l−1), at least 49% (G−) and 58% (G+) of d-AA in the peptidoglycan was degraded. No major changes in GluA were obvious. Interpretation of the results was difficult as a portion of the purified peptidoglycan was of similar size to the bacteria and could not be differentiated from cells growing in the cultures. Addition of the purified peptidoglycan stimulated the bacterial growth, and after 6 days the cell density in the enriched cultures was 4-fold higher than in the controls. A regrowth of bacteria after addition of L-broth at 105 days caused a 50- to 75-fold increase in dissolved d-AA and GluA. Most of the d-AA and GluA were taken up during the following 10 days, indicating that cell wall constituents are dynamic compounds. Our results show that a variable portion of peptidoglycan in G− and G+ bacteria can be degraded by natural bacteria, and that peptidoglycan in G− bacteria is more resistant to bacterial attack than that in G+ bacteria. Thus, the presence of cell wall constituents in natural DOM may reflect the recalcitrant nature of especially G− peptidoglycan.
Mechanisms controlling microbial degradation of dissolved organic matter (DOM) in aquatic environments are poorly understood, although microbes are crucial to global nutrient cycling. Bacterial cell wall components may be one of the keys in understanding the presence of slowly degrading DOM in nature. We found that dominant components of bacterial cell walls ( D-amino acids ( D-AA), glucosamine (GluA) and diaminopimelic acid (DAPA)) comprised up to 11.4% of the dissolved organic nitrogen in 50 diverse rivers entering the Baltic Sea. Occurrence of DAPA, a characteristic component of Gram-negative (G −) bacteria, in the rivers suggests that G − bacteria rather than Gram-positive (G +) were the major source of the cell wall material. In laboratory studies, the degradation of whole bacterial cells, cell wall material and purified peptidoglycan was studied to characterize degradation of cell wall material by natural aquatic bacteria. Addition of whole killed G − and G + bacteria to cultures of estuarine bacteria demonstrated fragmentation and loss of cell structure of the G + bacteria, while the G − bacteria maintained an intact cell shape during the entire 69-day period. In another experiment, estuarine bacteria degraded 39–69% of GluA, D-AA and DAPA in added cell wall material of a representative G − bacterial species during 8 days, as compared to a 72–89% degradation of GluA, D-AA and DAPA in cell material of a G + bacterial species. When cultures of estuarine bacteria were enriched with purified G − and G + peptidoglycan (1 mg l −1), at least 49% (G −) and 58% (G +) of D-AA in the peptidoglycan was degraded. No major changes in GluA were obvious. Interpretation of the results was difficult as a portion of the purified peptidoglycan was of similar size to the bacteria and could not be differentiated from cells growing in the cultures. Addition of the purified peptidoglycan stimulated the bacterial growth, and after 6 days the cell density in the enriched cultures was 4-fold higher than in the controls. A regrowth of bacteria after addition of L-broth at 105 days caused a 50- to 75-fold increase in dissolved D-AA and GluA. Most of the D-AA and GluA were taken up during the following 10 days, indicating that cell wall constituents are dynamic compounds. Our results show that a variable portion of peptidoglycan in G − and G + bacteria can be degraded by natural bacteria, and that peptidoglycan in G − bacteria is more resistant to bacterial attack than that in G + bacteria. Thus, the presence of cell wall constituents in natural DOM may reflect the recalcitrant nature of especially G − peptidoglycan.
Mechanisms controlling microbial degradation of dissolved organic matter (DOM) in aquatic environments are poorly understood, although microbes are crucial to global nutrient cycling. Bacterial cell wall components may be one of the keys in understanding the presence of slowly degrading DOM in nature. We found that dominant components of bacterial cell walls (D-amino acids (D-AA), glucosamine (GluA) and diaminopimelic acid (DAPA)) comprised up to 11.4% of the dissolved organic nitrogen in 50 diverse rivers entering the Baltic Sea. Occurrence of DAPA, a characteristic component of Gram-negative (G(-)) bacteria, in the rivers suggests that G(-) bacteria rather than Gram-positive (G(+)) were the major source of the cell wall material. In laboratory studies, the degradation of whole bacterial cells, cell wall material and purified peptidoglycan was studied to characterize degradation of cell wall material by natural aquatic bacteria. Addition of whole killed G(-) and G(+) bacteria to cultures of estuarine bacteria demonstrated fragmentation and loss of cell structure of the G(+) bacteria, while the G(-) bacteria maintained an intact cell shape during the entire 69-day period. In another experiment, estuarine bacteria degraded 39-69% of GluA, D-AA and DAPA in added cell wall material of a representative G(-) bacterial species during 8 days, as compared to a 72-89% degradation of GluA, D-AA and DAPA in cell material of a G(+) bacterial species. When cultures of estuarine bacteria were enriched with purified G(-) and G(+) peptidoglycan (1 mg l(-1)), at least 49% (G(-)) and 58% (G(+)) of D-AA in the peptidoglycan was degraded. No major changes in GluA were obvious. Interpretation of the results was difficult as a portion of the purified peptidoglycan was of similar size to the bacteria and could not be differentiated from cells growing in the cultures. Addition of the purified peptidoglycan stimulated the bacterial growth, and after 6 days the cell density in the enriched cultures was 4-fold higher than in the controls. A regrowth of bacteria after addition of L-broth at 105 days caused a 50- to 75-fold increase in dissolved D-AA and GluA. Most of the D-AA and GluA were taken up during the following 10 days, indicating that cell wall constituents are dynamic compounds. Our results show that a variable portion of peptidoglycan in G(-) and G(+) bacteria can be degraded by natural bacteria, and that peptidoglycan in G(-) bacteria is more resistant to bacterial attack than that in G(+) bacteria. Thus, the presence of cell wall constituents in natural DOM may reflect the recalcitrant nature of especially G(-) peptidoglycan.
Mechanisms controlling microbial degradation of dissolved organic matter (DOM) in aquatic environments are poorly understood, although microbes are crucial to global nutrient cycling. Bacterial cell wall components may be one of the keys in understanding the presence of slowly degrading DOM in nature. We found that dominant components of bacterial cell walls (D‐amino acids (D‐AA), glucosamine (GluA) and diaminopimelic acid (DAPA)) comprised up to 11.4% of the dissolved organic nitrogen in 50 diverse rivers entering the Baltic Sea. Occurrence of DAPA, a characteristic component of Gram‐negative (G−) bacteria, in the rivers suggests that G− bacteria rather than Gram‐positive (G+) were the major source of the cell wall material. In laboratory studies, the degradation of whole bacterial cells, cell wall material and purified peptidoglycan was studied to characterize degradation of cell wall material by natural aquatic bacteria. Addition of whole killed G− and G+ bacteria to cultures of estuarine bacteria demonstrated fragmentation and loss of cell structure of the G+ bacteria, while the G− bacteria maintained an intact cell shape during the entire 69‐day period. In another experiment, estuarine bacteria degraded 39–69% of GluA, D‐AA and DAPA in added cell wall material of a representative G− bacterial species during 8 days, as compared to a 72–89% degradation of GluA, D‐AA and DAPA in cell material of a G+ bacterial species. When cultures of estuarine bacteria were enriched with purified G− and G+ peptidoglycan (1 mg l−1), at least 49% (G−) and 58% (G+) of D‐AA in the peptidoglycan was degraded. No major changes in GluA were obvious. Interpretation of the results was difficult as a portion of the purified peptidoglycan was of similar size to the bacteria and could not be differentiated from cells growing in the cultures. Addition of the purified peptidoglycan stimulated the bacterial growth, and after 6 days the cell density in the enriched cultures was 4‐fold higher than in the controls. A regrowth of bacteria after addition of L‐broth at 105 days caused a 50‐ to 75‐fold increase in dissolved D‐AA and GluA. Most of the D‐AA and GluA were taken up during the following 10 days, indicating that cell wall constituents are dynamic compounds. Our results show that a variable portion of peptidoglycan in G− and G+ bacteria can be degraded by natural bacteria, and that peptidoglycan in G− bacteria is more resistant to bacterial attack than that in G+ bacteria. Thus, the presence of cell wall constituents in natural DOM may reflect the recalcitrant nature of especially G− peptidoglycan.
Author Pedersen, Anne-Grethe U
Stepanaukas, Ramunas
Jørgensen, Niels O.G
Nybroe, Ole
Hansen, Michael
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1574-6941
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Fri Aug 16 21:35:24 EDT 2024
Fri Aug 23 03:23:31 EDT 2024
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Wed Sep 11 04:52:19 EDT 2024
Fri Feb 23 02:29:14 EST 2024
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Issue 3
Keywords Degradation
Peptidoglycan
Bacterial cell wall
Glucosamine
Diaminopimelic acid
Baltic river
D-amino acid
amino acid
Biotope
Organic matter
Rivers
Nitrogen
Cell wall
Marine environment
Ecological damage
Aquatic environment
Environment
Nutrient
Gram negative bacteria
Language English
License CC BY 4.0
LinkModel DirectLink
MeetingName Aquatic Microbial Ecology
MergedId FETCHMERGED-LOGICAL-c5999-a3e6c2068dd0d6863aea7c11a7d77d09137ace383bf98284dea54206e66c5ed3
Notes Savannah River Ecology Laboratory, Aiken, SC 29803, USA.
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OpenAccessLink https://academic.oup.com/femsec/article-pdf/46/3/269/18091913/46-3-269.pdf
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  contributor:
    fullname: Mopper
– volume: 38
  start-page: 1282
  year: 1993
  ident: 10.1016/S0168-6496(03)00194-6-BIB20|cit20
  article-title: Bacterial growth efficiency on natural dissolved organic matter
  publication-title: Limnol. Oceanogr.
  doi: 10.4319/lo.1993.38.6.1282
  contributor:
    fullname: Kroer
– ident: 10.1016/S0168-6496(03)00194-6-BIB35|cit35
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Snippet Mechanisms controlling microbial degradation of dissolved organic matter (DOM) in aquatic environments are poorly understood, although microbes are crucial to...
Abstract Mechanisms controlling microbial degradation of dissolved organic matter (DOM) in aquatic environments are poorly understood, although microbes are...
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StartPage 269
SubjectTerms acid
Animal, plant and microbial ecology
Bacterial cell wall
Baltic river
Biodegradation of pollutants
Biologi
Biological and medical sciences
Biological Sciences
Biotechnology
D-amino
D-amino acid
Degradation
Diaminopimelic acid
Earth and Related Environmental Sciences
Ecology
Ekologi
Environment and pollution
Environmental Sciences
Fundamental and applied biological sciences. Psychology
Geovetenskap och miljövetenskap
Glucosamine
Industrial applications and implications. Economical aspects
Microbial ecology
Miljövetenskap
Natural Sciences
Naturvetenskap
Peptidoglycan
Various environments (extraatmospheric space, air, water)
Title Occurrence and degradation of peptidoglycan in aquatic environments
URI https://dx.doi.org/10.1016/S0168-6496(03)00194-6
https://onlinelibrary.wiley.com/doi/abs/10.1016%2FS0168-6496%2803%2900194-6
https://www.ncbi.nlm.nih.gov/pubmed/19719558
https://search.proquest.com/docview/734022329
https://lup.lub.lu.se/record/292448
Volume 46
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