Colombié, C.; Giraud, F.; Schnyder, J.; Goetz, A.E. (Annette); Boussaha, M.; Aurell, M.; Badenas, B.
(Elsevier, 2014-10)
The middle Oxfordian warming climate and sea-level rise initiated the development of vast carbonate platforms
in some western European basins. At the same time, however, siliciclastics and siliceous sponges dominated
certain ...