Carbon isotope trends in north-west European mosasaurs (Squamata; Late Cretaceous)

Author:

Giltaij Tom J.1,Jeroen van der Lubbe1,Lindow Bent2,Schulp Anne S.3,Jagt John W.M.4

Affiliation:

1. Vrije Universiteit Amsterdam

2. Statens Naturhistoriske Museum, Copenhagen

3. Naturalis Biodiversity Center, Leiden

4. Natuurhistorisch Museum Maastricht

Abstract

The carbon stable isotope composition (δ13C) of tooth enamel in mosasaurid squa-mates reflects aspects of their diet and diving behaviour. Here we present new δ13C data for such marine squamates from the Maastrichtian of Denmark and compare these with results obtained in previous studies from the lower-latitude type area of the Maastrichtian Stage (latest Cretaceous; 72.1–66.0 Ma) in the south-east Nether-lands and north-east Belgium. For the Danish samples, there is a weak correlation between mosasaur body size and δ13C values, with larger-sized taxa having lower δ13C values, comparable to what has previously been observed for mosasaurs from the Maastrichtian type area.

Publisher

Geological Society of Denmark

Subject

Geology

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