Cardiff University | Prifysgol Caerdydd ORCA
Online Research @ Cardiff 
WelshClear Cookie - decide language by browser settings

Shallow microbial recycling of deep-sourced carbon in Gulf of Cadiz mud volcanoes

Nuzzo, M., Hornibrook, E. R. C., Hensen, C., Parkes, Ronald John, Cragg, Barry Andrew, Rinna, J., Von Deimling, J. S., Sommer, S., Magalhaes, V. H., Reitz, A., Bruckmann, W. and Pinheiro, L. M. 2008. Shallow microbial recycling of deep-sourced carbon in Gulf of Cadiz mud volcanoes. Geomicrobiology Journal 25 (6) , pp. 283-295. 10.1080/01490450802258196

Full text not available from this repository.

Abstract

Based upon the molecular and isotopic composition of hydrocarbons it has been proposed that the source of CH4 in Gulf of Cadiz mud volcanoes (MV) is a mixture of deep sourced thermogenic CH4 and shallow biogenic CH4. We directly investigated this possibility by comparing porewater CH4 concentrations and their δ13C values with the potential for Archaeal methanogenesis in Gulf of Cadiz mud volcano (MV) sediments (Captain Arutyunov, Bonjardim, Ginsburg and Porto) using 14C-rate measurements. The CH4 has a deep sourced thermogenic origin (δ13C ∼ -49) but becomes 13C-depleted in and beneath the zone of anaerobic oxidation of methane (AOM) where the rates of hydrogenotrophic methanogenesis increase. Thus we infer that a portion of AOM-produced CO2 is being recycled to CH4 by methanogens yielding further 13C-depleted CH4, which might be misinterpreted as indicative of a fully shallow biogenic origin for this gas. Production of H2 is related to compositional changes in sedimentary organic matter, or to upward flux of substrate-enriched fluids. In contrast to other MVs in the Gulf of Cadiz, Ginsburg MV fluids are enriched in SO42- and contain very high concentrations of acetate (2478 μM below 150 cmbsf); however, the high levels of acetate did not stimulate methanogenesis but instead were oxidized to CO2 coupled to sulphate reduction. Both anaerobic oxidation of thermogenic CH4 linked to shallow methanogenesis and fluid geochemistry control the recycling of deep-sourced carbon at Gulf of Cadiz MVs, impacting near-surface δ13C-CH4 values.

Item Type: Article
Date Type: Publication
Status: Published
Schools: Earth and Ocean Sciences
Subjects: Q Science > QE Geology
Q Science > QR Microbiology
Publisher: Taylor & Francis
ISSN: 0149-0451
Last Modified: 12 Jun 2019 02:18
URI: http://orca-mwe.cf.ac.uk/id/eprint/8640

Citation Data

Cited 12 times in Google Scholar. View in Google Scholar

Cited 11 times in Scopus. View in Scopus. Powered By Scopus® Data

Actions (repository staff only)

Edit Item Edit Item