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Paleontology in New Mexico refers to paleontological research occurring within or conducted by people from the U.S. state of New Mexico. The fossil record of New Mexico is exceptionally complete and spans almost the entire stratigraphic column. [1] More than 3,300 different kinds of fossil organisms have been found in the state.
Prehistoric Trackways National Monument is a national monument in the Robledo Mountains of Doña Ana County, New Mexico, United States, near the city of Las Cruces.The monument's Paleozoic Era fossils are on 5,255 acres (2,127 ha) [1] of land administered by the Bureau of Land Management. [2]
Folsom site or Wild Horse Arroyo, designated by the Smithsonian trinomial 29CX1, is a major archaeological site about 8 miles (13 km) west of Folsom, New Mexico. It is the type site for the Folsom tradition , a Paleo-Indian cultural sequence dating to between 11000 BC and 10000 BC .
The fossils were given to the New Mexico Museum of Natural History and Science in 1980, and it was designated the state fossil in 1981 under former-Gov. Bill Richardson.
The Hartley Mammoth Site is a pre-Clovis archaeological and paleontological site in New Mexico.Preserving the butchered remains of two Columbian mammoths, small mammals and fish, the site is notable due to its age (~37,500 BP), which is significantly older than the currently accepted dates for the settlement of the Americas.
Fossil of the Carboniferous horsetail relative Annularia †Annularia †Annularia radiata †Annularia sphenophylloides †Anomphalus †Aphlebia †Archaeocidaris; Archaeolithophyllum †Archeria †Armenoceras †Aspidosaurus †Athyris †Athyris lamellosa; Mold fossil of a shell of the Early Devonian-Late Triassic bivalve Aviculopecten ...
Fossil collecting here without a permit is prohibited by law. The John D. Dingell, Jr. Conservation, Management, and Recreation Act , signed March 12, 2019, authorizes the establishment of the Ah-Shi-Sle-Pah Wilderness as a component of the National Wilderness Preservation System , protecting approximately 7,242 acres.
New Mexico at the start of the Paleozoic was dominated by the Transcontinental Arch, an elevated region from Minnesota to northern New Mexico. [23] Small quantities of alkaline magma were intruded in the early Cambrian along north–south faults, which may indicate incipient rifting of the New Mexico aulacogen . [ 24 ]