During the Campaninn-Maastrichtian, Patagonia was hooded by the Atlantic an
d reduced to an archipelago. Several localities of northern Patagonia have
yielded marine reptiles. Analysis of several assemblages suggests that the
diversity and abundance of pelagic marine reptiles in northern Patagonia wa
s higher by the end of the Cretaceous than previously thought. Several ples
iosaurids, including Aristonectes parvidens and the polycotylid Sulcusuchus
, and the first remains of mosasaurinae have been found. The Cretaceous mar
ine reptile record from South America is scanty. Nevertheless, materials de
scribed here suggest that Tethyan and Weddelian forms converged in northern
Patagonia, as seen with invertebrates. (C) 2001 Elsevier Science Ltd. All
rights reserved.