The fossils and geologic features at Tule Springs represent resources that Nuwu/Nuwuvi ancestors interacted with thousands of years ago that continue into the present and How old are the fossils at Tule Springs?Although the rock record of Tule Springs dates to over 570,000 years ago, fossils are found in sediments that are 100,000-12,500 years old. These plants and animals lived and died during a time called the Pleistocene Epoch (ply-stuh-seen eh-puhk). During the Pleistocene, or the last Ice Age, the world was cooler. Large ice sheets formed high in North America, expanding during glacial periods, and shrinking during interglacial periods. Although there were no large glaciers or ice sheets at Tule Springs at that time, it was much cooler and wetter than it is today. What kinds of fossils are there?From wetland snails the size of a sesame seed, to 12-foot-long Columbian mammoth tusks, there are many different kinds of fossils found at Tule Springs. Vertebrate FossilsVertebrate fossils, or remains of animals with a backbone, include both extinct and extant (still living) species. Fossils belonging to extinct species are mostly from very large mammals and were part of the Pleistocene megafauna. They include the Columbian mammoth, ancient camel, ancient horses, ancient bison, giant ground sloths, saber-toothed cat, dire wolf, and the American lion. The vertebrate fossil record of Tule Springs also includes species who no longer live at Tule Springs, but remain in other parts of North America. They include fish, pronghorn, deer, and the yellow-bellied marmot. Many animals and plants that live at Tule Springs today are also found in the fossil record. They include coyote, mountain lion, jackrabbit, birds of prey, small rodents, badger, lizards and snakes. Invertebrate FossilsInvertebrate fossils, or the remains of animals without backbones, include mostly extant (still living) genera. They belong to mollusks like gastropods (snails) and bivalves (clams), and crustaceans like ostracods. It is difficult to identify mollusk fossils to species because the soft tissue of their bodies have decayed long ago. These shelled organisms lived within ancient wetlands or wet meadows. Often, invertebrate fossils can give valuable clues to interpret past environments because these animals prefer specific water conditions and habitat types. Plant FossilsWhile rare, there are plant fossils documented in the Tule Springs fossil record. Paleontologists have found impressions of plant leaves, stems, and bark within the Las Vegas Formation. Additionally, fossil pollen has been recovered from Tule Springs. The plant fossils of Tule Springs belong to water-loving species, like cattails, cottonwood trees, and ash trees. Desert plants are also documented, such as globemallow, saltbush, and sagebrush. Fossil pollen is also commonly found from juniper and pine trees. Today, these species are found high into the mountain foothills, where it is cooler and wetter than in the valley. What happened to Ice Age plants and animals?Over 30 types of large mammals went extinct in North America toward the end of the Pleistocene Epoch about 12,000-10,000 years ago. The cause of this extinction is still under investigation. The most strongly-supported hypotheses include a changing climate, human hunting, or a combination of those factors. Where can I see fossils?There are thousands of fossils beneath your feet at Tule Springs Fossil Beds! They are often hard to spot without a trained eye because they blend into the surrounding sediment.
Can I collect or dig for fossils?The fossils at Tule Springs Fossil Beds are protected under Federal Laws and Regulations. You may only dig or collect fossils with an approved National Park Service Scientific Research and Collection Permit. Leave fossils where they are found. |
Last updated: January 13, 2025