2026-06-28T15:21:35Zhttp://doidb.wdc-terra.org/oaip/oai

oai:doidb.wdc-terra.org:1372026-06-10T10:05:57ZDOIDBDOIDB.SDDB

false4DOIDB.SDDB 10.1594/GFZ.SDDB.1076 Martin, Patrick Boes, Xavier Goddeeris, Boudewijn Fagel, Natalie Deutsches GeoForschungsZentrum GFZ 2006 2006-11-16 Dataset 10.1016/j.gloplacha.2004.11.012 In all abyssal stations, densities are never over an average of c. 3100 individuals m−2 (Fig. 3, Table 1). In contrast, the shallow station (CON01-427, Posolskoe Bank) harbours the highest observed densities (oligochaetes reach densities as high as 13573 individuals m−2 on average). Gammarids are present in this latter station at 128 m deep, while they are absent from all deep stations. The presence of some groups is anecdotal, such as Hydrachnidia (one specimen in a core at 388 m and two specimens in a core at 625 m) and chironomid larvae (two larvae in a core at 625 m). Interestingly, the two deepest Vydrino cores (CON01-105-7, 600 m, and CON01-106-3, 700 m) are virtually free from animals, suggesting that these stations are perhaps the best choice for the study of stratigraphy and climate proxies.
51.5999 108.913 51.568 53.955