( Mateus et al. 1997 ), as well as the LateCretaceous oospecies Triprismatoolithus stephensi attributed to a theropod dinosaur ( Jackson and Varricchio 2010 ), and even in the extant ratite bird Struthio ( Zelenitsky and Modesto 2003 ). The overall
Fishes are important faunal elements of LateCretaceous non-marine paleocommunities. Studies on the diversity and distribution of fish in the LateCretaceous could provide conclusive informations on understanding
of the Žukova Cove, from where Mezga et al. (2006b) described the first dinosaur footprints of the island. Fig. 1. Location of the new LateCretaceous track site on Hvar Island, Croatia. A, Position of Hvar Island in Croatia. B, The position of the
Late Jurassic ages (176–144 Ma) in the SSMB and granodiorite–diorite of Middle Jurassic age (166–167 Ma) in the UDMB.
In the ZOB, the Neyriz, Kermanshah, and Haji-Abad Ophiolites are unconformably covered by LateCretaceous limestone and
niobian rutile was described from the LateCretaceous beforsite dykes of the Velence Mts. ( Szakáll et al., 2014b ).
Rhyolite bodies may also contain postmagmatic hydrothermal HFSE mineralization, when the magma was enriched in HFSE (e