Bacterial degradation of large particles in the southern Indian Ocean using in vitro incubation experiments

International audience Large particles (> 60 mm) were collected at 30 and 200 m water depth by in situ pumps in the southern Indian Ocean in January–February 1999. The samples were incubated under laboratory conditions with their own bacterial assemblages for 7–17 days in batches under oxic condi...

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Published in:Organic Geochemistry
Main Authors: Panagiotopoulos, Christos, Sempere, Richard, Obernosterer, Ingrid, Striby, Laurent, Goutx, Madeleine, van Wambeke, France, Gautier, Sophie, Lafont, Raymond
Other Authors: Institut méditerranéen d'océanologie (MIO), Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de MicrobiologiE de Géochimie et d'Ecologie Marines (LMGEM), Université de la Méditerranée - Aix-Marseille 2-Centre National de la Recherche Scientifique (CNRS), Laboratoire d'Océanographie Microbienne (LOMIC), Observatoire océanologique de Banyuls (OOB), Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Equipe 2, Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2002
Subjects:
Online Access:https://hal.science/hal-01831214
https://hal.science/hal-01831214/document
https://hal.science/hal-01831214/file/Panagiot%20et%20al%202002.pdf
https://doi.org/10.1016/S0146-6380(02)00057-8
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record_format openpolar
institution Open Polar
collection Université de Toulon: HAL
op_collection_id ftunivtoulon
language English
topic Marine particles
Organic carbon
Carbohydrates
Amino-acids
Lipids
Bacterial decomposition
Southern Indian Ocean
Polar Front Zone (PFZ)
Sub-Antarctic area (SAr)
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDV.MP.BAC]Life Sciences [q-bio]/Microbiology and Parasitology/Bacteriology
spellingShingle Marine particles
Organic carbon
Carbohydrates
Amino-acids
Lipids
Bacterial decomposition
Southern Indian Ocean
Polar Front Zone (PFZ)
Sub-Antarctic area (SAr)
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDV.MP.BAC]Life Sciences [q-bio]/Microbiology and Parasitology/Bacteriology
Panagiotopoulos, Christos
Sempere, Richard
Obernosterer, Ingrid
Striby, Laurent
Goutx, Madeleine
van Wambeke, France
Gautier, Sophie
Lafont, Raymond
Bacterial degradation of large particles in the southern Indian Ocean using in vitro incubation experiments
topic_facet Marine particles
Organic carbon
Carbohydrates
Amino-acids
Lipids
Bacterial decomposition
Southern Indian Ocean
Polar Front Zone (PFZ)
Sub-Antarctic area (SAr)
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDV.MP.BAC]Life Sciences [q-bio]/Microbiology and Parasitology/Bacteriology
description International audience Large particles (> 60 mm) were collected at 30 and 200 m water depth by in situ pumps in the southern Indian Ocean in January–February 1999. The samples were incubated under laboratory conditions with their own bacterial assemblages for 7–17 days in batches under oxic conditions in the dark. Particulate and dissolved fractions of organic carbon , amino acids, sugars and lipids, as well as bacterial production were quantified over time. During the experiments, 32–38% and 43–50% of total organic carbon (TOC) was mineralized and considered as labile material in the Polar Front Zone (PFZ) and Sub-Antarctic region (SAr), respectively. This material was utilized with a bacterial growth efficiency (BGE) of 10–21% (PFZ) and 12–17% (SAr), with the lower values being observed for surface samples (30 m). These results imply that most (79–90%) of the incorporated carbon from large particles was respired as CO 2. The study revealed that the initial relative abundance of the three main classes of organic matter, including sugars, amino acids and lipids, varied greatly between SAr and PFZ, with sugars being more abundant in SAr (15–19% of TOC) than in PFZ (8–9% of TOC). In the PFZ, mineralization rates of amino acids and lipids were two to ten fold higher than those of sugars, whereas the opposite was observed in SAr biodegradation experiments. Moreover, our results suggested that organic carbon is mineralized by bacteria more rapidly in the euphotic zone of the SAr than the PFZ. The differences observed between the two sites may be related to the more rapid dissolution of silica as well as the higher temperatures and bacterial production encountered in SAr waters. The bacterial processes apparently affect the composition of material sinking to the ocean interior. #
author2 Institut méditerranéen d'océanologie (MIO)
Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire de MicrobiologiE de Géochimie et d'Ecologie Marines (LMGEM)
Université de la Méditerranée - Aix-Marseille 2-Centre National de la Recherche Scientifique (CNRS)
Laboratoire d'Océanographie Microbienne (LOMIC)
Observatoire océanologique de Banyuls (OOB)
Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)
Equipe 2
Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Panagiotopoulos, Christos
Sempere, Richard
Obernosterer, Ingrid
Striby, Laurent
Goutx, Madeleine
van Wambeke, France
Gautier, Sophie
Lafont, Raymond
author_facet Panagiotopoulos, Christos
Sempere, Richard
Obernosterer, Ingrid
Striby, Laurent
Goutx, Madeleine
van Wambeke, France
Gautier, Sophie
Lafont, Raymond
author_sort Panagiotopoulos, Christos
title Bacterial degradation of large particles in the southern Indian Ocean using in vitro incubation experiments
title_short Bacterial degradation of large particles in the southern Indian Ocean using in vitro incubation experiments
title_full Bacterial degradation of large particles in the southern Indian Ocean using in vitro incubation experiments
title_fullStr Bacterial degradation of large particles in the southern Indian Ocean using in vitro incubation experiments
title_full_unstemmed Bacterial degradation of large particles in the southern Indian Ocean using in vitro incubation experiments
title_sort bacterial degradation of large particles in the southern indian ocean using in vitro incubation experiments
publisher HAL CCSD
publishDate 2002
url https://hal.science/hal-01831214
https://hal.science/hal-01831214/document
https://hal.science/hal-01831214/file/Panagiot%20et%20al%202002.pdf
https://doi.org/10.1016/S0146-6380(02)00057-8
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source ISSN: 0146-6380
Organic Geochemistry
https://hal.science/hal-01831214
Organic Geochemistry, 2002, 33 (8), pp.985-1000. ⟨10.1016/S0146-6380(02)00057-8⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/S0146-6380(02)00057-8
hal-01831214
https://hal.science/hal-01831214
https://hal.science/hal-01831214/document
https://hal.science/hal-01831214/file/Panagiot%20et%20al%202002.pdf
doi:10.1016/S0146-6380(02)00057-8
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1016/S0146-6380(02)00057-8
container_title Organic Geochemistry
container_volume 33
container_issue 8
container_start_page 985
op_container_end_page 1000
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spelling ftunivtoulon:oai:HAL:hal-01831214v1 2024-09-15T17:42:17+00:00 Bacterial degradation of large particles in the southern Indian Ocean using in vitro incubation experiments Panagiotopoulos, Christos Sempere, Richard Obernosterer, Ingrid Striby, Laurent Goutx, Madeleine van Wambeke, France Gautier, Sophie Lafont, Raymond Institut méditerranéen d'océanologie (MIO) Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de MicrobiologiE de Géochimie et d'Ecologie Marines (LMGEM) Université de la Méditerranée - Aix-Marseille 2-Centre National de la Recherche Scientifique (CNRS) Laboratoire d'Océanographie Microbienne (LOMIC) Observatoire océanologique de Banyuls (OOB) Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Equipe 2 Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS) 2002 https://hal.science/hal-01831214 https://hal.science/hal-01831214/document https://hal.science/hal-01831214/file/Panagiot%20et%20al%202002.pdf https://doi.org/10.1016/S0146-6380(02)00057-8 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/S0146-6380(02)00057-8 hal-01831214 https://hal.science/hal-01831214 https://hal.science/hal-01831214/document https://hal.science/hal-01831214/file/Panagiot%20et%20al%202002.pdf doi:10.1016/S0146-6380(02)00057-8 info:eu-repo/semantics/OpenAccess ISSN: 0146-6380 Organic Geochemistry https://hal.science/hal-01831214 Organic Geochemistry, 2002, 33 (8), pp.985-1000. ⟨10.1016/S0146-6380(02)00057-8⟩ Marine particles Organic carbon Carbohydrates Amino-acids Lipids Bacterial decomposition Southern Indian Ocean Polar Front Zone (PFZ) Sub-Antarctic area (SAr) [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDV.MP.BAC]Life Sciences [q-bio]/Microbiology and Parasitology/Bacteriology info:eu-repo/semantics/article Journal articles 2002 ftunivtoulon https://doi.org/10.1016/S0146-6380(02)00057-8 2024-07-15T23:39:38Z International audience Large particles (> 60 mm) were collected at 30 and 200 m water depth by in situ pumps in the southern Indian Ocean in January–February 1999. The samples were incubated under laboratory conditions with their own bacterial assemblages for 7–17 days in batches under oxic conditions in the dark. Particulate and dissolved fractions of organic carbon , amino acids, sugars and lipids, as well as bacterial production were quantified over time. During the experiments, 32–38% and 43–50% of total organic carbon (TOC) was mineralized and considered as labile material in the Polar Front Zone (PFZ) and Sub-Antarctic region (SAr), respectively. This material was utilized with a bacterial growth efficiency (BGE) of 10–21% (PFZ) and 12–17% (SAr), with the lower values being observed for surface samples (30 m). These results imply that most (79–90%) of the incorporated carbon from large particles was respired as CO 2. The study revealed that the initial relative abundance of the three main classes of organic matter, including sugars, amino acids and lipids, varied greatly between SAr and PFZ, with sugars being more abundant in SAr (15–19% of TOC) than in PFZ (8–9% of TOC). In the PFZ, mineralization rates of amino acids and lipids were two to ten fold higher than those of sugars, whereas the opposite was observed in SAr biodegradation experiments. Moreover, our results suggested that organic carbon is mineralized by bacteria more rapidly in the euphotic zone of the SAr than the PFZ. The differences observed between the two sites may be related to the more rapid dissolution of silica as well as the higher temperatures and bacterial production encountered in SAr waters. The bacterial processes apparently affect the composition of material sinking to the ocean interior. # Article in Journal/Newspaper Antarc* Antarctic Université de Toulon: HAL Organic Geochemistry 33 8 985 1000