Production of Labile Protein-Like Dissolved Organic Carbon Associated With Anaerobic Methane Oxidization in the Haima Cold Seeps, South China Sea

Cold seeps where methane-rich fluids escape from the seafloor generally support enormous biomass of chemosynthetic organisms and associated fauna. In addition to transporting a great amount of methane toward the seafloor, cold seeps also contribute to the aged, dissolved organic carbon (DOC) pool in...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Tingcang Hu, Min Luo, Yunping Xu, Shanggui Gong, Duofu Chen
Formato: article
Lenguaje:EN
Publicado: Frontiers Media S.A. 2021
Materias:
AOM
Q
Acceso en línea:https://doaj.org/article/599e57b1b90b44e2ad2037dbd686d3eb
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:599e57b1b90b44e2ad2037dbd686d3eb
record_format dspace
spelling oai:doaj.org-article:599e57b1b90b44e2ad2037dbd686d3eb2021-12-02T09:37:06ZProduction of Labile Protein-Like Dissolved Organic Carbon Associated With Anaerobic Methane Oxidization in the Haima Cold Seeps, South China Sea2296-774510.3389/fmars.2021.797084https://doaj.org/article/599e57b1b90b44e2ad2037dbd686d3eb2021-12-01T00:00:00Zhttps://www.frontiersin.org/articles/10.3389/fmars.2021.797084/fullhttps://doaj.org/toc/2296-7745Cold seeps where methane-rich fluids escape from the seafloor generally support enormous biomass of chemosynthetic organisms and associated fauna. In addition to transporting a great amount of methane toward the seafloor, cold seeps also contribute to the aged, dissolved organic carbon (DOC) pool in the deep ocean. Here, two sediment cores from the “Haima cold seeps,” northern South China Sea and a nearby reference core were analyzed for pore-water sulfate and DOC concentrations, δ13C of DOC, and optical properties of dissolved organic matter (DOM). High DOC concentrations (0.9–3.7 mM) accompanied by extremely low δ13C values (−43.9 to −76.2‰) suggest the conversion of methane into sedimentary DOC pool in the seep sediments. Parallel factor analysis (PARAFAC) of the fluorescence excitation-emission matrices shows higher fluorescent intensities of labile protein-like components (C2 and C4) and lower fluorescent intensities of refractory humic-like components (C1 and C3) in the seep cores compared to the reference core. The intensity of C2 is positively correlated with DOC concentrations and δ13C-DOC in the seep sediments, suggesting that the labile protein-like DOM was produced by the anaerobic oxidation of methane (AOM). Moreover, low humification index (HIX) and high biological index (BIX) values also indicate intensified production of relatively labile DOM with lower degradation degree in the seep cores compared to the reference core. Hence, we highlight that methane-derived DOC may serve as important carbon and energy sources for heterotrophic microbial communities due to its relatively labile nature.Tingcang HuMin LuoMin LuoYunping XuShanggui GongDuofu ChenFrontiers Media S.A.articlecold seepsdissolved organic carbonfluorescence spectrumprotein-likeAOMScienceQGeneral. Including nature conservation, geographical distributionQH1-199.5ENFrontiers in Marine Science, Vol 8 (2021)
institution DOAJ
collection DOAJ
language EN
topic cold seeps
dissolved organic carbon
fluorescence spectrum
protein-like
AOM
Science
Q
General. Including nature conservation, geographical distribution
QH1-199.5
spellingShingle cold seeps
dissolved organic carbon
fluorescence spectrum
protein-like
AOM
Science
Q
General. Including nature conservation, geographical distribution
QH1-199.5
Tingcang Hu
Min Luo
Min Luo
Yunping Xu
Shanggui Gong
Duofu Chen
Production of Labile Protein-Like Dissolved Organic Carbon Associated With Anaerobic Methane Oxidization in the Haima Cold Seeps, South China Sea
description Cold seeps where methane-rich fluids escape from the seafloor generally support enormous biomass of chemosynthetic organisms and associated fauna. In addition to transporting a great amount of methane toward the seafloor, cold seeps also contribute to the aged, dissolved organic carbon (DOC) pool in the deep ocean. Here, two sediment cores from the “Haima cold seeps,” northern South China Sea and a nearby reference core were analyzed for pore-water sulfate and DOC concentrations, δ13C of DOC, and optical properties of dissolved organic matter (DOM). High DOC concentrations (0.9–3.7 mM) accompanied by extremely low δ13C values (−43.9 to −76.2‰) suggest the conversion of methane into sedimentary DOC pool in the seep sediments. Parallel factor analysis (PARAFAC) of the fluorescence excitation-emission matrices shows higher fluorescent intensities of labile protein-like components (C2 and C4) and lower fluorescent intensities of refractory humic-like components (C1 and C3) in the seep cores compared to the reference core. The intensity of C2 is positively correlated with DOC concentrations and δ13C-DOC in the seep sediments, suggesting that the labile protein-like DOM was produced by the anaerobic oxidation of methane (AOM). Moreover, low humification index (HIX) and high biological index (BIX) values also indicate intensified production of relatively labile DOM with lower degradation degree in the seep cores compared to the reference core. Hence, we highlight that methane-derived DOC may serve as important carbon and energy sources for heterotrophic microbial communities due to its relatively labile nature.
format article
author Tingcang Hu
Min Luo
Min Luo
Yunping Xu
Shanggui Gong
Duofu Chen
author_facet Tingcang Hu
Min Luo
Min Luo
Yunping Xu
Shanggui Gong
Duofu Chen
author_sort Tingcang Hu
title Production of Labile Protein-Like Dissolved Organic Carbon Associated With Anaerobic Methane Oxidization in the Haima Cold Seeps, South China Sea
title_short Production of Labile Protein-Like Dissolved Organic Carbon Associated With Anaerobic Methane Oxidization in the Haima Cold Seeps, South China Sea
title_full Production of Labile Protein-Like Dissolved Organic Carbon Associated With Anaerobic Methane Oxidization in the Haima Cold Seeps, South China Sea
title_fullStr Production of Labile Protein-Like Dissolved Organic Carbon Associated With Anaerobic Methane Oxidization in the Haima Cold Seeps, South China Sea
title_full_unstemmed Production of Labile Protein-Like Dissolved Organic Carbon Associated With Anaerobic Methane Oxidization in the Haima Cold Seeps, South China Sea
title_sort production of labile protein-like dissolved organic carbon associated with anaerobic methane oxidization in the haima cold seeps, south china sea
publisher Frontiers Media S.A.
publishDate 2021
url https://doaj.org/article/599e57b1b90b44e2ad2037dbd686d3eb
work_keys_str_mv AT tingcanghu productionoflabileproteinlikedissolvedorganiccarbonassociatedwithanaerobicmethaneoxidizationinthehaimacoldseepssouthchinasea
AT minluo productionoflabileproteinlikedissolvedorganiccarbonassociatedwithanaerobicmethaneoxidizationinthehaimacoldseepssouthchinasea
AT minluo productionoflabileproteinlikedissolvedorganiccarbonassociatedwithanaerobicmethaneoxidizationinthehaimacoldseepssouthchinasea
AT yunpingxu productionoflabileproteinlikedissolvedorganiccarbonassociatedwithanaerobicmethaneoxidizationinthehaimacoldseepssouthchinasea
AT shangguigong productionoflabileproteinlikedissolvedorganiccarbonassociatedwithanaerobicmethaneoxidizationinthehaimacoldseepssouthchinasea
AT duofuchen productionoflabileproteinlikedissolvedorganiccarbonassociatedwithanaerobicmethaneoxidizationinthehaimacoldseepssouthchinasea
_version_ 1718398067355418624