A unique Fe-rich carbonate chimney associated with cold seeps in the Northern Okinawa Trough, East China Sea

The East China Sea is an important marginal sea of the Western Pacific Ocean, from which natural gas hydrate sample has not been acquired so far. Recently, copious carbonate chimneys have been discovered in turbidite deposits in the olistostrome zone located on the west slope of the northern section of Okinawa Trough. Here, the petrology, geochemistry and chronology of an iron-rich carbonate chimney were characterized, confirming a close relationship between its formation and the dissociation of natural gas hydrate beneath the chimney in OT. A distinctive relationship has been observed between goethite and total carbonate contents along with a negative correlation between Fe and Ca contents. Conversely, abundant Fe accumulated on carbonate substrate by mineralized microorganisms. The delta C-13 values of the chimney wall were from -27.56 to -43.66 parts per thousand (average: -37.18 parts per thousand, V-PDB), implying anaerobic oxidation of methane (AOM) as a predominant controlling factor on carbonate precipitation. As no pyrite and organic residues were identified in the iron-rich chimney, it was assumed that AOM was coupled to the iron reduction reaction at least to some extent during the chimney growth owing to the local deficiency of sulfate supply. The delta Fe-56 values of bulk chimney wall (ranging from -0.316 parts per thousand to -0.023 parts per thousand, average -0.134 parts per thousand) suggest mass and isotope exchanges between the chimney and ambient environment during its growth history, whereas the enrichment of delta O-18 of the carbonate implies these carbonate sourcing from hydrate dissociation underlying our sampling site. This assumption has been supported by a distinct bottom simulation reflector (BSR) and a well-developed fault system beneath the sampling site. This is the first report of cold seepage inside the OT and the identified iron-dependent AOM has shed a new light to the Carbon cycle related to the marine methane oxidation, particularly before the Great Oxidation Event similar to 2.45 Ga ago. (C) 2014 Elsevier Ltd. All rights reserved.