Relating sulfate and methane dynamics to geology: Accretionary prism offshore SW Taiwan.

Chuang, Pei-Chuan, Dale, Andrew W., Wallmann, Klaus, Haeckel, Matthias, Yang, Tsanyao Frank, Chen, Nai-Chen, Chen, Hsiao-Chi, Chen, Hsuan-Wen, Lin, Saulwood, Sun, Chih-Hsien, You, Chen-Feng, Horng, Chorng-Shern, Wang, Yunshuen and Chung, San-Hsiung (2013) Relating sulfate and methane dynamics to geology: Accretionary prism offshore SW Taiwan. Geochemistry, Geophysics, Geosystems, 14 (7). pp. 2523-2545. DOI 10.1002/ggge.20168.

[img]
Preview
Text
Chuang.pdf - Published Version

Download (5Mb) | Preview

Supplementary data:

Abstract

Geochemical data (CH4, SO42−, I−, Cl−, particulate organic carbon (POC), δ13C-CH4, and δ13C-CO2) are presented from the upper 30 m of marine sediment on a tectonic submarine accretionary wedge offshore southwest Taiwan. The sampling stations covered three ridges (Tai-Nan, Yung-An, and Good Weather), each characterized by bottom simulating reflectors, acoustic turbidity, and different types of faulting and anticlines. Sulfate and iodide concentrations varied little from seawater-like values in the upper 1–3 m of sediment at all stations; a feature that is consistent with irrigation of seawater by gas bubbles rising through the soft surface sediments. Below this depth, sulfate was rapidly consumed within 5–10 m by anaerobic oxidation of methane (AOM) at the sulfate-methane transition. Carbon isotopic data imply a mainly biogenic methane source. A numerical transport-reaction model was used to identify the supply pathways of methane and estimate depth-integrated turnover rates at the three ridges. Methane gas ascending from deep layers, facilitated by thrusts and faults, was by far the dominant term in the methane budget at all sites. Differences in the proximity of the sampling sites to the faults and anticlines mainly accounted for the variability in gas fluxes and depth-integrated AOM rates. By comparison, methane produced in situ by POC degradation within the modeled sediment column was unimportant. This study demonstrates that the geochemical trends in the continental margins offshore SW Taiwan are closely related to the different geological settings.

Document Type: Article
Additional Information: WOS:000323828800025
Keywords: gas hydrate; methane flux; bubble irrigation; anaerobic oxidation of methane; POC degradation; accretionary wedge; Taiwan
Research affiliation: OceanRep > The Future Ocean - Cluster of Excellence > FO-R05
OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems
OceanRep > The Future Ocean - Cluster of Excellence
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1002/ggge.20168
ISSN: 1525-2027
Projects: Future Ocean
Date Deposited: 30 Sep 2013 12:48
Last Modified: 13 Mar 2017 09:50
URI: http://oceanrep.geomar.de/id/eprint/22043

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...