Fig. 27. A. Early Triassic reconstruction of Pangaea showing Cimmerian superterrane and Neotethys opening. B. Late Triassic paleogeography of Corsica (C), Sardinia (S), Maures, Estérel (M-E), and the Ebro Block (E) in western Neotethys. C. Cretaceous Western Neotethys realm with Adria continental crust stretching from North Gondwana and inserting between westernmost parts of Cimmerian superterrane. (A, C from Dilek & Furnes 2019; B from Edel et al. 2015, modified). ADR = Adria; AT = Alpine Tethys; ATB = Anatolide-Tauride Block; B = Briançonnais; BSB = Black Sea Basin; ECS = Ebro–Corso–Sardinian Blocks; MP = Menderes Platform; NNT = Northern Neotethys; PL = Pelagonia; SAP = South Armenian Platform; TP = Tauride Platform; VO = Vardar Ocean.

Published as part of Karaman, Ivo M., Mitov, Plamen G. & Snegovaya, Nataly, 2024, Parasironidae fam. nov., a Cimmerian lineage of Mediterranean Cyphophthalmi (Opiliones), with the description of three new genera and four new species, pp. 173-209 in European Journal of Taxonomy 921 (1) on page 204, DOI: 10.5852/ejt.2024.921.2427, http://zenodo.org/record/10656519