Marine reptile occurrences are rare in the Lower Jurassic Series outside of Europe. Here we
describe diverse marine reptile faunas from the Lower Jurassic Series (Pliensbachian and …

Abstract During the Cenomanian–Turonian transition (∼ 94 Ma), what is today Central
Russia formed part of the northern epicontinental margin of the Tethys Ocean. Diverse …

Marine repile remains have often been found in the extensive Mesozoic epícontinental
marine units of the former Soviet Union, and in particular, the Russian Platform of the …

Even though a handful of long-lived reptilian clades dominated Mesozoic marine
ecosystems, several biotic turnovers drastically changed the taxonomic composition of these …

Marine reptile remains from the Jurassic of Moscow area were at first described in the year
1845, since then considerable materials from the Callovian, Oxfordian and Volgian …

Our knowledge of marine reptiles of the Callovian age (Middle Jurassic) is majorly based on
the collections from the Oxford Clay Formation of England, which yielded a diverse marine …

All current data on the Jurassic and Cretaceous climates of Siberia based on isotope,
paleontological, and lithological proxies are summarized. The late Pliensbachian cooling …

The Vocontian Basin (SE France) was formed along the northwestern border of Tethys
during Mesozoic times. Mainly known for its rich ammonite fauna, this basin has also yielded …

Here we describe the first findings of reptile remains in the Upper Cretaceous marine strata
of Siberia, which represent the northernmost occurrences of plesiosaurians,? mosasaurids …

A new marine vertebrate assemblage from the Late Jurassic (late Kimmeridgian) at
Krzyżanowice near Iłża in the NE margin of the Holy Cross Mountains in Poland is …