Preliminary Report on a Late Cretaceous Vertebrate Fossil Assemblage in Northwestern Coahuila, Mexico

Building off the first part of the series (Löser, 2011), which introduced the Early Cretaceous (Late Barremian to Albian) coral fauna from the Bisbee Basin, this third part

two fossil sections (late Quaternary), and a group of modern samples analyzed through pollen and non-pollen palynomorphs, enabled the reconstruction of the palaeoclimatic

Figure 1. Location of the outcrops of the Mesozoic peri-Adriatic carbonate platforms with terrestrial vertebrate evidence. Pelmetto, etc.), early Norian footprints, 5) W

Geographic distributions indica te a late Early Cretaceous dispersal of Eolambia into North America, with subsequent divergence of Protohadros and Claosaurus, and a second

One exception is a preliminary report (Melchor, 1998) on invertebrate and vertebrate ich- nocoenoses from the Ischichuca Formation (Middle to Late Triassic of Ischigualasto- Villa

a recently discovered site near Sucre (Maragua syn- cline) reporting for the first time gregarious behav- iour in Late Cretaceous sauropods (Lockley et al., in press); the other

Peculiar theropod pedal unguals from the Lameta Formation are different from those of other theropods (e.g., Allosaurus, Sin raptor, Tyranno- sauridae, Ornithomimidae,

The recent record of Patagonian Late Cretaceous land mammals (Bonaparte, 1990, 1996, and literature therein), although not of latest Cretaceous age (see Pascual et al., 2000),