A coralline-like red alga from the lower Ordovician of Wales
The Late Tortonian-Early Messinian Abad Member in the Sorbas Basin, south-east Spain contains abundant foraminifera. Planktonic foraminifera have been used to reconstruct the environmental conditions that developed within the basin. Benthonic foraminifera reveal a detailed picture of the palaeoenvironment. After an initial deepening episode, from upper epibathyal (c. 200m) depths to lower epibathyal (c. 1000m) depths, the basin progressively shallowed to shelf depths (c.