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Keystone Gallery is a fossil museum north of Scott City, Kansas, that was established in 1991 in a former church building by Chuck Bonner and Barbara Shelton to display the region's fossils. [1] [2] Chuck Bonner is the son of the paleontologist Marion Charles Bonner, and the family's fossils are found in museums across the country. [2]
After 1.5 million years ago (extinction of Paranthropus), all fossils shown are human (genus Homo). After 11,500 years ago (11.5 ka, beginning of the Holocene), all fossils shown are Homo sapiens (anatomically modern humans), illustrating recent divergence in the formation of modern human sub-populations.
The Boskop Man is an anatomically modern human fossil of the Middle Stone Age (Late Pleistocene) discovered in 1913 in South Africa. [1] The fossil was at first described as Homo capensis and considered a separate human species by Broom (1918), [2] but by the 1970s this "Boskopoid" type was widely recognized as representative of the modern Khoisan populations.
Fossils — of prehistoric plants, animals, fungi, and algae. As well as some genera/species that are still extant, yet have an extensive fossil record. Subcategories.
Small tar pit. La Brea Tar Pits is an active paleontological research site in urban Los Angeles. Hancock Park was formed around a group of tar pits where natural asphalt (also called asphaltum, bitumen, or pitch; brea in Spanish) has seeped up from the ground for tens of thousands of years.
Dasypus bellus fossil occurrence in Florida. The earliest fossils are found in early Pleistocene South America, and would emigrate into southern North America. They have been found at many sites in Florida, including caves, sinkholes, river sites, coastal, and lake deposits. By the late Pleistocene, D. bellus spread into the American Southwest ...
Millions of prehistoric marine fossils were discovered beneath a California high school over the course of a multi-year construction project. The relics recovered at San Pedro High School included ...
The trackway Protichnites from the Cambrian, Blackberry Hill, central Wisconsin. A trace fossil, also known as an ichnofossil (/ ˈ ɪ k n oʊ f ɒ s ɪ l /; from Greek: ἴχνος ikhnos "trace, track"), is a fossil record of biological activity by lifeforms but not the preserved remains of the organism itself. [1]