Microbial carbon isotope fractionation to produce extraordinarily heavy methane in aging hydrothermal plumes over the southwestern Okinawa Trough

Toshitaka Gamo, Urumu Tsunogai, Shinsuke Ichibayashi, Hitoshi Chiba, Hajime Obata, Tamotsu Oomori, Takuro Noguchi, Edward T. Baker, Takashi Doi, Masahiro Maruo, Yuji Sano

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Within neutrally buoyant hydrothermal plumes derived from the Yonaguni Knoll IV hydrothermal field (24°51' N, 122°42' E, D = 1,370-1,385 m) in the southwestern Okinawa Trough back-arc basin, we obtained profiles of dissolved manganese (Mn), helium isotopes (3He/4He), methane (CH4) and its stable carbon isotope ratio δ13CPDB) in young to old plume waters. We first mapped the spatial distribution of hydrothermal plumes by towing a fixed array of optical sensors (Miniature Autonomous Plume Recorders: MAPRs) above the field. We then made water column observations and samplings using a CTD (Conductivity, Temperature, and Depth sensors)-Carousel package with a transmissometer and Niskin-X bottles at five locations, with distances between 0.6 and 6.1 km from the hydrofhermally active center so far discovered. Vertical profiles of light transmission and chemical tracers indicated triple-layered plumes, the centers of which were at depths of 700-800 m, ∼1,050 m and ∼1,200 m. The CH4 concentrations and δ13C values for the 1,200-m plume ranged between 1,026 and 10 nmol/kg, and between-22.4 and +40.4‰ (the highest δ13C value yet reported for oceanic CH4), respectively, indicating active microbial CH4 oxidation accompanied by the δ13C increase for residual CH 4. The δ13C(CH4) was shown to be useful for tracing such a "microbial plume" whose CH4 concentration has already fallen to almost the background level. By applying the Rayleigh distillation equation for a closed system, we estimated the kinetic isotope fractionation factor of 1.012 for the CH4 oxidation process occurring within the hydrothermal plumes deeper than 1,000 m.

Original languageEnglish
Pages (from-to)477-487
Number of pages11
JournalGeochemical Journal
Volume44
Issue number6
Publication statusPublished - 2010

Fingerprint

Carbon Isotopes
hydrothermal plume
carbon isotopes
Methane
Fractionation
troughs
fractionation
Isotopes
plumes
carbon isotope
trough
methane
plume
Aging of materials
Oxidation
Helium
Water
Optical sensors
Bottles
Manganese

Keywords

  • Carbon isotope fractionation
  • Hydrothermal plume chemistry
  • Microbial methane oxidation
  • Southern Okinawa Trough

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

Cite this

Gamo, T., Tsunogai, U., Ichibayashi, S., Chiba, H., Obata, H., Oomori, T., ... Sano, Y. (2010). Microbial carbon isotope fractionation to produce extraordinarily heavy methane in aging hydrothermal plumes over the southwestern Okinawa Trough. Geochemical Journal, 44(6), 477-487.

Microbial carbon isotope fractionation to produce extraordinarily heavy methane in aging hydrothermal plumes over the southwestern Okinawa Trough. / Gamo, Toshitaka; Tsunogai, Urumu; Ichibayashi, Shinsuke; Chiba, Hitoshi; Obata, Hajime; Oomori, Tamotsu; Noguchi, Takuro; Baker, Edward T.; Doi, Takashi; Maruo, Masahiro; Sano, Yuji.

In: Geochemical Journal, Vol. 44, No. 6, 2010, p. 477-487.

Research output: Contribution to journalArticle

Gamo, T, Tsunogai, U, Ichibayashi, S, Chiba, H, Obata, H, Oomori, T, Noguchi, T, Baker, ET, Doi, T, Maruo, M & Sano, Y 2010, 'Microbial carbon isotope fractionation to produce extraordinarily heavy methane in aging hydrothermal plumes over the southwestern Okinawa Trough', Geochemical Journal, vol. 44, no. 6, pp. 477-487.
Gamo, Toshitaka ; Tsunogai, Urumu ; Ichibayashi, Shinsuke ; Chiba, Hitoshi ; Obata, Hajime ; Oomori, Tamotsu ; Noguchi, Takuro ; Baker, Edward T. ; Doi, Takashi ; Maruo, Masahiro ; Sano, Yuji. / Microbial carbon isotope fractionation to produce extraordinarily heavy methane in aging hydrothermal plumes over the southwestern Okinawa Trough. In: Geochemical Journal. 2010 ; Vol. 44, No. 6. pp. 477-487.
@article{9de3a01ed5164606ba854a9453833e75,
title = "Microbial carbon isotope fractionation to produce extraordinarily heavy methane in aging hydrothermal plumes over the southwestern Okinawa Trough",
abstract = "Within neutrally buoyant hydrothermal plumes derived from the Yonaguni Knoll IV hydrothermal field (24°51' N, 122°42' E, D = 1,370-1,385 m) in the southwestern Okinawa Trough back-arc basin, we obtained profiles of dissolved manganese (Mn), helium isotopes (3He/4He), methane (CH4) and its stable carbon isotope ratio δ13CPDB) in young to old plume waters. We first mapped the spatial distribution of hydrothermal plumes by towing a fixed array of optical sensors (Miniature Autonomous Plume Recorders: MAPRs) above the field. We then made water column observations and samplings using a CTD (Conductivity, Temperature, and Depth sensors)-Carousel package with a transmissometer and Niskin-X bottles at five locations, with distances between 0.6 and 6.1 km from the hydrofhermally active center so far discovered. Vertical profiles of light transmission and chemical tracers indicated triple-layered plumes, the centers of which were at depths of 700-800 m, ∼1,050 m and ∼1,200 m. The CH4 concentrations and δ13C values for the 1,200-m plume ranged between 1,026 and 10 nmol/kg, and between-22.4 and +40.4‰ (the highest δ13C value yet reported for oceanic CH4), respectively, indicating active microbial CH4 oxidation accompanied by the δ13C increase for residual CH 4. The δ13C(CH4) was shown to be useful for tracing such a {"}microbial plume{"} whose CH4 concentration has already fallen to almost the background level. By applying the Rayleigh distillation equation for a closed system, we estimated the kinetic isotope fractionation factor of 1.012 for the CH4 oxidation process occurring within the hydrothermal plumes deeper than 1,000 m.",
keywords = "Carbon isotope fractionation, Hydrothermal plume chemistry, Microbial methane oxidation, Southern Okinawa Trough",
author = "Toshitaka Gamo and Urumu Tsunogai and Shinsuke Ichibayashi and Hitoshi Chiba and Hajime Obata and Tamotsu Oomori and Takuro Noguchi and Baker, {Edward T.} and Takashi Doi and Masahiro Maruo and Yuji Sano",
year = "2010",
language = "English",
volume = "44",
pages = "477--487",
journal = "Geochemical Journal",
issn = "0016-7002",
publisher = "The Physiological Society of Japan",
number = "6",

}

TY - JOUR

T1 - Microbial carbon isotope fractionation to produce extraordinarily heavy methane in aging hydrothermal plumes over the southwestern Okinawa Trough

AU - Gamo, Toshitaka

AU - Tsunogai, Urumu

AU - Ichibayashi, Shinsuke

AU - Chiba, Hitoshi

AU - Obata, Hajime

AU - Oomori, Tamotsu

AU - Noguchi, Takuro

AU - Baker, Edward T.

AU - Doi, Takashi

AU - Maruo, Masahiro

AU - Sano, Yuji

PY - 2010

Y1 - 2010

N2 - Within neutrally buoyant hydrothermal plumes derived from the Yonaguni Knoll IV hydrothermal field (24°51' N, 122°42' E, D = 1,370-1,385 m) in the southwestern Okinawa Trough back-arc basin, we obtained profiles of dissolved manganese (Mn), helium isotopes (3He/4He), methane (CH4) and its stable carbon isotope ratio δ13CPDB) in young to old plume waters. We first mapped the spatial distribution of hydrothermal plumes by towing a fixed array of optical sensors (Miniature Autonomous Plume Recorders: MAPRs) above the field. We then made water column observations and samplings using a CTD (Conductivity, Temperature, and Depth sensors)-Carousel package with a transmissometer and Niskin-X bottles at five locations, with distances between 0.6 and 6.1 km from the hydrofhermally active center so far discovered. Vertical profiles of light transmission and chemical tracers indicated triple-layered plumes, the centers of which were at depths of 700-800 m, ∼1,050 m and ∼1,200 m. The CH4 concentrations and δ13C values for the 1,200-m plume ranged between 1,026 and 10 nmol/kg, and between-22.4 and +40.4‰ (the highest δ13C value yet reported for oceanic CH4), respectively, indicating active microbial CH4 oxidation accompanied by the δ13C increase for residual CH 4. The δ13C(CH4) was shown to be useful for tracing such a "microbial plume" whose CH4 concentration has already fallen to almost the background level. By applying the Rayleigh distillation equation for a closed system, we estimated the kinetic isotope fractionation factor of 1.012 for the CH4 oxidation process occurring within the hydrothermal plumes deeper than 1,000 m.

AB - Within neutrally buoyant hydrothermal plumes derived from the Yonaguni Knoll IV hydrothermal field (24°51' N, 122°42' E, D = 1,370-1,385 m) in the southwestern Okinawa Trough back-arc basin, we obtained profiles of dissolved manganese (Mn), helium isotopes (3He/4He), methane (CH4) and its stable carbon isotope ratio δ13CPDB) in young to old plume waters. We first mapped the spatial distribution of hydrothermal plumes by towing a fixed array of optical sensors (Miniature Autonomous Plume Recorders: MAPRs) above the field. We then made water column observations and samplings using a CTD (Conductivity, Temperature, and Depth sensors)-Carousel package with a transmissometer and Niskin-X bottles at five locations, with distances between 0.6 and 6.1 km from the hydrofhermally active center so far discovered. Vertical profiles of light transmission and chemical tracers indicated triple-layered plumes, the centers of which were at depths of 700-800 m, ∼1,050 m and ∼1,200 m. The CH4 concentrations and δ13C values for the 1,200-m plume ranged between 1,026 and 10 nmol/kg, and between-22.4 and +40.4‰ (the highest δ13C value yet reported for oceanic CH4), respectively, indicating active microbial CH4 oxidation accompanied by the δ13C increase for residual CH 4. The δ13C(CH4) was shown to be useful for tracing such a "microbial plume" whose CH4 concentration has already fallen to almost the background level. By applying the Rayleigh distillation equation for a closed system, we estimated the kinetic isotope fractionation factor of 1.012 for the CH4 oxidation process occurring within the hydrothermal plumes deeper than 1,000 m.

KW - Carbon isotope fractionation

KW - Hydrothermal plume chemistry

KW - Microbial methane oxidation

KW - Southern Okinawa Trough

UR - http://www.scopus.com/inward/record.url?scp=79957938848&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=79957938848&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:79957938848

VL - 44

SP - 477

EP - 487

JO - Geochemical Journal

JF - Geochemical Journal

SN - 0016-7002

IS - 6

ER -