Da. Pearson et al., Palynologically calibrated vertebrate record from North Dakota consistent with abrupt dinosaur extinction at the Cretaceous-Tertiary boundary, GEOLOGY, 29(1), 2001, pp. 39-42
New data from 17 Cretaceous-Tertiary (K-T) boundary sections and 53 vertebr
ate sites in the Hell Creek and Fort Union Formations in southwestern North
Dakota document a 1.76 m barren interval between the highest Cretaceous ve
rtebrate fossils and the palynologically recognized K-T boundary. The bound
ary is above the formational contact at 15 localities and coincident with i
t at two, demonstrating that the formational contact is diachronous. Dinosa
urs are common in the highest Cretaceous vertebrate samples and a partial d
inosaur skeleton in the Port Union Formation is the highest recorded Cretac
eous vertebrate fossil in this area.