Fig. 4From: Sedimentary organic matter from a cored Early Triassic succession, Georgetown (Idaho, USA)Different particulate organic matter compositions in the Georgetown core succession: 1 Kerogen GTB 001 K a 12.2/123.3; 2 Kerogen GTB 004 K a 10.5/126.3; 3 Kerogen GTB 020 K a 20.7/128.3; 4 Kerogen GTB 036 K a 6.7/135.1; 5 Kerogen GTB 048 K a 9.4/141.5; 6 Kerogen GTB 052 K a 19.0/129.5Back to article page