(Table 2) Bottom ages of loess sequence units in China determined by comparison to the lithological section of Hutouliang dated by the lightness timescale
We have analyzed inorganic and organic carbons and determined the isotopic composition of both sedimentary organic carbon and inorganic carbon in carbonates contained in sediments recovered from Holes
ROV (sprint 103) equiped with 36mm still camera; Kodak Ektachrome 100; Nikon super coolscan 4000ED; JPEG compression. Along the same transect sea-bed was videotaped in betacam format using same lense