Abstract
Dinosaur footprints occur in fluvial and deltaic Rhaetian and Hettangian strata of the Hoganas Formation in Skane (Scania), southern Sweden. The Rhaetian tracks are assigned to Grallator (Eubrontes) cf. giganteus while the Hettangian ones are assigned to Grallator (Eubrontes) soltykovensis. The tracks were left by large theropods crossing deltaic and alluvial plains.
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