from the Upper Cretaceous of Antarctica, skull material is extremely rare. Here, new elasmosaurid cranial material from the lower Maastrichtian levels of the Cape Lamb Member (Snow Hill Island Formation) on Vega Island, Antarctica is described. The studied specimen (MLP 15-I-7-6) is a non-aristonectine elasmosaurid but shows a palate morphology characterized by the absence of a posterior interpterygoid symphysis and a posterior plate-like extension of the pterygoids, features previously associated with the aristonectine palatal structure. The specimen MLP 15-I-7-6 thus provides an indication that these palatal features are also present in non-aristonectine Weddellian elasmosaurids, and makes available additional evidence of the close phylogenetical relationship between the aristonectines and some Weddellian non-aristonectine elasmosaurids. 1. Introduction Elasmosaurids are a monophyletic group of plesiosaurs with extremely long necks. The biochron of this clade extends from the Early Cretaceous up to the Maastrichtian/Danian boundary (Ketchum and Benson, 2010, 2011; Benson and Druckenmiller, 2014). With a cosmopolitan distribution, it is one of the most frequently recorded groups of marine reptiles in the Late Cretaceous (Welles, 1962; Brown, 1981; Carpenter, 1999). Remains of Antarctic Cretaceous elasmosaurids comprise tens of specimens spanning between the lower Campanian and the K/T limit (O'Gorman, 2012). With the remarkable exception of the holotype of Morturneria seymouriensis, the Antarctic plesiosaur specimens collected so far have not preserved any informative cranial