Methane-derived authigenic carbonates from the Ulleung basin sediments, East Sea of Korea

• Published in: Continental shelf research Vol. 29; no. 13; pp. 1588 - 1596
• Main Authors: Lim, Dhongil, Choi, Jinyong, Xu, Zhaokai, Kim, Moonkoo, Choi, Donglim, Jung, Hoisoo, Lee, Panmook
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 30-06-2009
• Subjects: Authigenic carbonates; East Sea (Japan Sea); Gas hydrate; Marine; Methane seep environments; INW, Korea, Rep; INW, Japan Sea, Ulleung Basin; Gas hydrate; East Sea (Japan Sea); Authigenic carbonates; Methane seep environments
• ISSN: 0278-4343; 1873-6955
• DOI: 10.1016/j.csr.2009.04.013

Authigenic carbonates were sampled in methane-enriched piston core sediments collected from gas venting sites on the western continental slope of the Ulleung Basin, East Sea of Korea. Multidisciplinary investigations on these carbonates, including the scanning electronic microscope (SEM) observations and mineralogical-geochemical compositions, were carried out to identify the carbon and oxygen sources and the forming mechanism of these carbonates. The authigenic carbonates from the study area correspond to semi-consolidated, compact concretions or nodules ranging from 2 to 9
cm in size. X-ray diffraction and electron microprobe analyses showed that most of the sampled carbonate concretions were composed of almost purely authigenic high-Mg calcite (10.7–14.3
mol% MgCO
3). Characteristically, microbial structures such as filaments and rods, which were probably associated with the authigenic minerals, were abundantly observed within the carbonate matrix. The carbonates were strongly depleted in
δ
13C (−33.85‰ to −39.53‰ Peedee Belemnite (PDB)) and were enriched in
δ
18O (5.16–5.60‰ PDB), indicating that the primary source of carbon is mainly derived from the anaerobic oxidation of methane. Such methane probably originated from the destabilization of the underlying gas hydrates as strongly supporting from the enriched
18O levels. Furthermore, the strongly depleted
δ
13C values (−60.7‰ to −61.6‰ PDB) of the sediment void gases demonstrate that the majority of the gas venting at the Ulleung Basin is microbial methane by CO
2 reduction. This study provides another example for the formation mechanism of methane-derived authigenic carbonates associated with gas-hydrate decomposition in gas-seeping pockmark environments.