(Table 3) Stable isotope composition of sof t tissues of specimens from the Sea of Okhotsk

• Main Authors: Sahling, Heiko, Galkin, Sergey V, Salyuk, Anatoly, Greinert, Jens, Foerstel, Hilmar, Piepenburg, Dieter, Suess, Erwin
• Format: Dataset
• Language: English
• Published: PANGAEA 2003
• Subjects: Akademik M.A. Lavrentiev; Area/locality; Dredge; DRG; Event label; GE99/KOMEX_VI; GE99-25-1; GE99-28-1; KOMEX; KOMEX I; Kurile-Okhotsk Sea Marine Experiment; LV28; LV28-16-2; LV28-30-2; LV28-30-3; LV28-30-4; LV28-30-5; LV28-36-1; LV28-38-1; LV28-47-1; Marshal Gelovany; Mass spectrometry; Material; MUC; MultiCorer; Obzhirov flare; Sea of Okhotsk; Species; Taxon/taxa; TRAWL; Trawl net; δ13C; organic carbon; δ15N; gas; Okhotsk; okhotsk sea; Sakhalin
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.769751; https://doi.org/10.1594/PANGAEA.769751

We discovered and investigated several cold-seep sites in four depth zones of the Sea of Okhotsk off Northeast Sakhalin: outer shelf (160–250 m), upper slope (250–450 m), intermediate slope (450–800 m), and Derugin Basin (1450–1600 m). Active seepage of free methane or methane-rich fluids was detected in each zone. However, seabed photography and sampling revealed that the number of chemoautotrophic species decreases dramatically with decreasing water depth. At greatest depths in the Derugin Basin, the seeps were inhabited by bacterial mats and bivalves of the families Vesicomyidae (Calyptogena aff. pacifica, C. rectimargo, Archivesica sp.), Solemyidae (Acharax sp.) and Thyasiridae (Conchocele bisecta). In addition, pogonophoran tubeworms of the family Sclerolinidae were found in barite edifices. At the shallowest sites, on the shelf at 160 m, the seeps lack chemoautotrophic macrofauna; their locations were indicated only by the patchy occurrence of bacterial mats. Typical seep-endemic metazoans with chemosynthetic symbionts were confined to seep sites at depths below 370 m. A comparative analysis of the structure of seep and background communities suggests that differences in predation pressure may be an important determinant of this pattern. The abundance of predators such as carnivorous brachyurans and asteroids, which can invade seeps from adjacent habitats and efficiently prey on sessile seep bivalves, decreased very pronouncedly with depth. We conclude from the obvious correlation with the conspicuous pattern in the distribution of seep assemblages that, on the shelf and at the upper slope, predator pressure may be high enough to effectively impede any successful settlement of viable populations of seep-endemic metazoans. However, there was also evidence that other depth-related factors, such as bottom-water current, sedimentary regimes, oxygen concentrations and the supply of suitable settling substrates, may additionally regulate the distribution of seep fauna in the area. As a consequence of the ...