Greinert, Jens; Bollwerk, S; Derkachev, A N; Bohrmann, Gerhard; Suess, Erwin (2002): AMS 14C ages and isotopic compositions of samples from the Derugin Basin, Sea of Okhotsk. PANGAEA, https://doi.org/10.1594/PANGAEA.769675, Supplement to: Greinert, J et al. (2002): Massive barite deposits and carbonate mineralization in the Derugin Basin, Sea of Okhotsk: Precipitation process at cold vent sites. Earth and Planetary Science Letters, 203, 165-180, https://doi.org/10.1016/S0012-821X(02)00830-0
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An area of massive barite precipitations was studied at a tectonic horst in 1500 m water depth in the Derugin Basin, Sea of Okhotsk. Seafloor observations and dredge samples showed irregular, block- to column-shaped barite build-ups up to 10 m high which were scattered over the seafloor along an observation track 3.5 km long. High methane concentrations in the water column show that methane expulsion and probably carbonate precipitation is a recently active process. Small fields of chemoautotrophic clams (Calyptogena sp., Acharax sp.) at the seafloor provide additional evidence for active fluid venting. The white to yellow barites show a very porous and often layered internal fabric, and are typically covered by dark-brown Mn-rich sediment; electron microprobe spectroscopy measurements of barite sub-samples show a Ba substitution of up to 10.5 mol% of Sr. Rare idiomorphic pyrite crystals (~1%) in the barite fabric imply the presence of H2S. This was confirmed by clusters of living chemoautotrophic tube worms (1 mm in diameter) found in pores and channels within the barite. Microscopic examination showed that micritic aragonite and Mg-calcite aggregates or crusts are common authigenic precipitations within the barite fabric. Equivalent micritic carbonates and barite carbonate cemented worm tubes were recovered from sediment cores taken in the vicinity of the barite build-up area. Negative d13C values of these carbonates (>-43.5 per mill PDB) indicate methane as major carbon source; d18O values between 4.04 and 5.88 per mill PDB correspond to formation temperatures, which are certainly below 5°C. One core also contained shells of Calyptogena sp. at different core depths with 14C-ages ranging from 20 680 to >49 080 yr. Pore water analyses revealed that fluids also contain high amounts of Ba; they also show decreasing SO4**2- concentrations and a parallel increase of H2S with depth. Additionally, S and O isotope data of barite sulfate (d34S: 21.0-38.6 per mill CDT; d18O: 9.0-17.6 per mill SMOW) strongly point to biological sulfate reduction processes. The isotope ranges of both S and O can be exclusively explained as the result of a mixture of residual sulfate after a biological sulfate reduction and isotopic fractionation with 'normal' seawater sulfate. While massive barite deposits are commonly assumed to be of hydrothermal origin, the assemblage of cheomautotrophic clams, methane-derived carbonates, and non-thermally equilibrated barite sulfate strongly implies that these barites have formed at ambient bottom water temperatures and form the features of a Giant Cold Seep setting that has been active for at least 49 000 yr.
Median Latitude: 54.003079 * Median Longitude: 146.287444 * South-bound Latitude: 53.996600 * West-bound Longitude: 146.261433 * North-bound Latitude: 54.020267 * East-bound Longitude: 146.297167
Date/Time Start: 1998-08-17T00:21:00 * Date/Time End: 1998-08-20T07:15:00
LV28-25-1 * Latitude: 54.014067 * Longitude: 146.277433 * Date/Time: 1998-08-17T00:21:00 * Elevation: -1491.0 m * Recovery: 1.48 m * Location: Sea of Okhotsk * Campaign: LV28 (KOMEX I) * Basis: Akademik M.A. Lavrentiev * Method/Device: Hydro corer (HYC) * Comment: Derugin Basin/148 cm/carbonate and barite concretions
LV28-35-1 * Latitude: 54.006883 * Longitude: 146.275567 * Date/Time: 1998-08-20T02:27:00 * Elevation: -1515.0 m * Location: Sea of Okhotsk * Campaign: LV28 (KOMEX I) * Basis: Akademik M.A. Lavrentiev * Method/Device: Dredge (DRG) * Comment: Derugin Basin cont./full/sediment, barite & calc. burrows, extinct, vent fauna, barite chimney fragments
LV28-36-1 * Latitude: 54.020267 * Longitude: 146.261433 * Date/Time: 1998-08-20T05:20:00 * Elevation: -1490.0 m * Location: Sea of Okhotsk * Campaign: LV28 (KOMEX I) * Basis: Akademik M.A. Lavrentiev * Method/Device: Dredge (DRG) * Comment: Derugin Basin cont./full/100s kg big chimney fragments, all barite; track from 54°01.297/146°15.875 to 54°00.940/146°16.323
Datasets listed in this publication series
- Greinert, J; Bollwerk, S; Derkachev, AN et al. (2002): (Table 1) AMS 14C ages of clam shells found in Core SLR 37-1. https://doi.org/10.1594/PANGAEA.769668
- Greinert, J; Bollwerk, S; Derkachev, AN et al. (2002): (Table 2) S, O and Sr isotopic data from barite build-ups (DR samples) and small barite cemented worm burrows found in the sediment of Core SLR 37-1 and HYC 25-1. https://doi.org/10.1594/PANGAEA.769669
- Greinert, J; Bollwerk, S; Derkachev, AN et al. (2002): (Table 3) Carbon and oxygen isotopic data of carbonates from Core SLR 37-1, HYC 25-1 and an aragonite crust from station DR 35-1. https://doi.org/10.1594/PANGAEA.769673