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The ichnogenus Thalassinoides: burrow fossil produced by crustaceans from the Middle Jurassic, Makhtesh Qatan, southern Israel. An ichnotaxon (plural ichnotaxa) is "a taxon based on the fossilized work of an organism", i.e. the non-human equivalent of an artifact.
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Grallator ["GRA-luh-tor"] is an ichnogenus (form taxon based on footprints) which covers a common type of small, three-toed print made by a variety of bipedal theropod dinosaurs. Grallator-type footprints have been found in formations dating from the Early Triassic through to the early Cretaceous periods.
Anomoepus is the name assigned to several fossil footprints first reported from Early Jurassic beds of the Connecticut River Valley, Massachusetts, US in 1802. Map showing tracks of Anomoepus (green) and Grallator (blue) in Moyeni. All four feet have left impressions. The smaller forefeet have five toes, whereas the larger hind feet have three ...
Anatrisauropus is an ichnogenus of dinosaur footprint, possibly belonging to a saurischian. [2] It has only been discovered in Lesotho ( Molteno Formation and Karoo Basin ). Three ichnospecies are known: A. camisardi , A. ginsburgi [ 1 ] and A. hereroensis ; all of which were named by Paul Ellenberger between 1965 and 1972.
Name of the Footprint The name Megalosauripus means large saurian footprints and derives historically from an archaic and generalized concept of megalosaurid dinosaurs. The name may coincidentally, but by no means certainly, imply a relationship to dinosaurs like Megalosaurus and its relatives.
Xiuningpus Temporal range: 99.7–66.043 Ma Pre๊ ๊ O S D C P T J K Pg N Trace fossil classification Domain: Eukaryota Kingdom: Animalia Phylum: Chordata Clade: Dinosauria (?) Ichnogenus: † Xiuningpus Yu, 1988 Type ichnospecies † Xiuningpus xintanensis Yu, 1988 Other ichnospecies † Xiuningpus qukouensis Yu, 1988 Xiuninggpus is an extinct ichnogenus of dinosaur footprint. There are two ...
Argoides is an ichnogenus of dinosaur footprint, originally named as an ichnospecies of Ornithichnites, [1] [2] left by what was possibly an ornithopod, although due to the age of the tracks (some of which predate the oldest known ornithopod fossils), they were probably instead made by theropods. [3]
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