Fig. 7From: Is the relative thickness of ammonoid septa influenced by ocean acidification, phylogenetic relationships and palaeogeographic position?Examples of different septal thickness ranges corresponding to their time period. The figure shows mainly two different septal thicknesses. Ammonoids from the Late Triassic and the Early Cretaceous show a greater septal thickness than those from the Early and Middle Jurassic. A Rhacophyllites neojurensis (Phylloceratidae); B Arietites sp. (Arietitidae); C Ludwigia bradfordensis (Graphoceratidae); D Argonauticeras besairei (Lytoceratidae). Well discernible examples of septa are indicated by red arrowsBack to article page