Fig. 3From: A study on benthic molluscs and stable isotopes from Kutch, western India reveals early Eocene hyperthermals and pronounced transgression during ETM2 and H2 eventsa Amber, plant fossil and glauconite pocket within shale indicated by yellow, blue and green arrows, respectively. b Granular amber within black shale. c Pyroclastics of unit 1. d Grey shale with amber (yellow arrow) and plant fossils (blue arrow) in unit 2. e Black shale with amber (yellow arrow) and plant fossils (blue arrow) in unit 2. f Grey shale with glauconite pocket (green oval) in unit 2. g Grey shale with pyrite (yellow oval) and plant matter (blue arrow) in unit 2. h Green shale in unit 3, glauconite indicated by green arrow; white dots are fragments of fossil molluscs. i Grey shale with pockets of glauconite and mollusc fragments in unit 3. j Green shale with pyrite (yellow arrow) in unit 3. k Shell limestone with mollusc fossils in unit 3; yellow and green arrows indicate Caestocorbula sp. and Claibornicardia sp., respectively. l Mollusc concentration in upper part of unit 3. m Black shale with plant fossil (blue arrow) in unit 4. n Lignite in unit 4. o Ferricrete in unit 4. Scale bars 10Â mmBack to article page