2026-06-26T02:22:04Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:562026-06-10T10:05:33ZDOIDBDOIDB.SDDBfalse4DOIDB.SDDB
10.1594/GFZ.SDDB.1040
Demory, Francois
OberhÀnsli, Hedi
Nowaczyk, Norbert
Gottschalk, Matthias
Wirth, Richard
Naumann, Rudolf
Downcore variations of the SIRM/ÎșLF for CON01-603-2, CON01-604-2, CON01-605-3, VER98-1-1, VER98
Deutsches GeoForschungsZentrum GFZ
2006
2006-09-15
Dataset
10.1016/j.gloplacha.2004.11.010
Greigite levels in glacial sediments cannot be correlated between cores (Fig. 12), which suggests that greigite concentrations are driven by local processes. We suggest that faecal pellets could be a suitable microenvironment for sulphate reduction. And while greigite could potentially act as proxy for faecal pellets in glacial sediments, unfortunately, we cannot rely on this possible indicator since the greigite is very sensitive to onshore alterations after sampling (Snowball and Thompson, 1990).
104.851
108.914
51.5831
53.9632