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The Smoky Hill Chalk Member of the Niobrara Chalk formation is a Cretaceous conservation Lagerstätte, or fossil rich geological formation, known primarily for its exceptionally well-preserved marine reptiles. [2] Named for the Smoky Hill River, [1] the Smoky Hill Chalk Member is the uppermost of the two structural units of the Niobrara Chalk. [2]
Groenlandaspis is unusual among placoderms in that it is known what color it was; preserved pigment cells in its fossils indicate that its posterior was red and its anterior was silvery-white in a countershaded pattern, camouflaging it in the murky, silty waters of the rivers in which it dwelled. [11]
The animal had apparently been washed out to sea after death. [3] After three days of mine safety training, museum staff and Suncor employees began working to recover all pieces of the fossil. Aside from the several pieces broken free, the bulk of the specimen was still embedded 8 metres (26 ft) up a cliff that was 12 metres (39 ft) high.
Print/export Download as PDF; Printable version; ... Pages in category "Fossil record of animals" The following 11 pages are in this category, out of 11 total.
Astraspis desiderata. Nearly complete fossils suggest the living animals were about 200 mm (7.9 in) in length. The body had a mobile tail covered with small protective plate-like scales of less than 1 mm (0.039 in) and a forebody covered with plate-like scales larger than 2 mm (0.079 in).
The Painted Hills is a geologic site in Wheeler County, Oregon that is one of the three units of the John Day Fossil Beds National Monument along with Sheep Rock and Clarno. It totals 3,132 acres (12.67 km 2 ) and is located 9 miles (14 km) northwest of Mitchell, Oregon .
Print/export Download as PDF; Printable version; In other projects ... The fossil was 3 cm wide, and the animal was likely the size of a large spider, ...
Range of Cynarctoides based on fossil record Cynarctoides is an extinct genus of the Borophaginae subfamily of canids native to North America . It lived from the Early Oligocene to the Middle Miocene , 33.3—13.6 Mya , existing for approximately 19.7 million years .
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