Fig. 1: Examples of macroscopic dissolution structures in outcrop.
From: Micro-scale dissolution seams mobilise carbon in deep-sea limestones
a Outcrop of the Kaiwhata limestones with flat-lying beds. White arrows mark large bedding-parallel diagenetic wave-like stylolites. b Close-up cross-sectional view of a horizontal wackestone bed. Dark-grey speckles are detrital grains. The yellow and white arrows mark bedding-internal diagenetic stylolites filled with siltstone. The yellow arrow marks a tell-tale stylolite “tooth”.
