Prehistoric Trackways National Monument - Fossils

Fossils

The Prehistoric Trackways National Monument site includes a major deposit of Paleozoic Era fossilized footprints in fossil mega-trackways of land animals, sea creatures, and insects. These are known as trace fossils or ichnofossils. There are also fossilized plants and petrified wood present. Much of the fossilized material originated during the Permian Period and is around 280 million years old.

Some of the animals who may have left tracks in the Robledo mountains include; Dimetrodon, Eryops, Edaphosaurus, and multiple other pelycosaurs. There are at least 13 major trace fossils found at the monument and include Selenichnites (sel-EEN-ick-NIGHT eez) or moon-shaped trace, Kouphichnium (koof-ICK-nee-um) or light trace, Palmichnium (pal-ICK-nee-um) or palm trace, Octopodichnus (oct-toe-pod-ICK-nuss) or eight-footed trace, Lithographus (lith-oh-GRAFF-us) or rock writing, Tonanoxichnus (tong-a-nox-ICK-nuss) or Tonganoxie trace, Augerinoichnus (aw-gurr-EE-no-ICK-nuss) or Augerino trace, Undichna (und-ICK-nuh) or wave-shaped trace, Serpentichnus (serpent-ICK-nuss) or snake-like trace, Batrachichnus (baa-track ICK-nuss) or frog trace, Dromopus (dro-MOE-puss) or running foot, and Dimetropus (die-MEET-row puss) or Dimetrodon foot.

Trackways can be difficult for the general public to find at the monument and few facilities have yet been developed. Many of the slabs pulled out by Jerry MacDonald are housed at the New Mexico Museum of Natural History and Science, although they are not on display at this time. Guided hikes are offered by BLM interpretive staff periodically.

There are plenty of marine invertebrate fossils to be found in the monument, they include Brachiopods, Gastropods, Cephalopods, Bivalves, and Echinoderms.

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