Fig. 4From: On the geophysical processes impacting palaeo-sea-level observationsPhotos showing microfossils used for sea-level reconstructions. a Diatom from coastal sediments in Shimokita plane, Japan (Yokoyama et al. 2012) and b benthic foraminifers in sediment cores obtained from Bonaparte Gulf, Australia (Ishiwa et al. 2016)Back to article page