“…Above the previous sediments (only visible in log 3), and bounded by two faint erosive surfaces of minor importance, a thin layer ( ca 0·5 m thick, henceforth called ‘Unit 4b’) of fossil‐rich, medium to coarse‐grained sandstone, with no apparent bedding structures occurs. This layer is very rich in microgastropods, bivalves, fragments of Zullobalanus santamariaensis Buckeridge & Winkelmann, 2010 (Winkelmann et al ., ), several bryozoan species, echinoids and rhodoliths. Shell debris is randomly/chaotically distributed within this layer, with no preferential geometric arrangement.…”