Paleontology in Montana facts for kids
Paleontology in Montana refers to paleontological research occurring within or conducted by people from the U.S. state of Montana. The fossil record in Montana stretches all the way back to the Precambrian. During the Late Precambrian, western Montana was covered by a warm, shallow sea where local bacteria formed stromatolites and bottom-dwelling marine life left tracks on the sediment that would later fossilize. This sea remained in place during the early Paleozoic, although withdrew during the Silurian and Early Devonian, leaving a gap in the local rock record until its return. This sea was home to creatures including brachiopods, conodonts, crinoids, fish, and trilobites. During the Carboniferous the state was home to an unusual cartilaginous fish fauna. Later in the Paleozoic the sea began to withdraw, but with a brief return during the Permian.
During the Triassic Montana was again covered in a sea whose inhabitants are the state's only known fossils from this time. Much of Montana remained covered by seawater into the Late Jurassic, but exposed areas were greened by a flora of conifers, cycads, ferns, and ginkgoes. This coastal plain was home to dinosaurs including the ornithopod Camptosaurus, the sauropods Apatosaurus and Diplodocus, and the theropod Allosaurus. During the early Cretaceous the state was home to its first flowering plants as well as predators such as Deinonychus. Later the Western Interior Seaway, home to creatures such as mosasaurs and plesiosaurs, came to cover the state. On land, the duckbilled Maiasaura formed vast nesting colonies. By the end of the Cretaceous Montana was home to some of the most famous dinosaurs; creatures such as Edmontosaurus, Triceratops, and Tyrannosaurus.
During the early Cenozoic the sea began to withdraw from the state. Plants, insects, and titanotheres are preserved from this time. Later inhabitants would include arctocyonids, insectivores, multituberculates, pantodonts, primates, and taeniodonts. As the Cenozoic proceeded the climate cooled until the Ice Age started and glaciers entered the state. At this time mammoths, musk oxen, and dire wolves lived in the areas of the state not covered by glaciers. Local Native Americans have been devising mythical explanations for fossils and also repurposing them for practical uses for thousands of years. The first scientific collection of local fossils began in the mid 19th century. Other important discoveries include the plant and insect fossils of Ruby Valley and Deinonychus, which triggered the Dinosaur Renaissance. The Cretaceous Duck-billed dinosaur Maiasaura peeblesorum is the Montana state fossil.
Prehistory
The fossil record in Montana stretches all the way back to the Precambrian. During the Late Precambrian, western Montana was covered by a warm, shallow sea. This sea was home to stromatolites and to bottom-dwelling marine life whose tracks on the benthic sediment would later fossilize. Montanan life of the time included arthropods, blue-green algae, conularians, fungi, and worms. Their fossils were preserved in what are now known as Glacier National Park. The worms left trace fossils such as burrow fillings and trails through the sediment. During the ensuing Cambrian period the state was still largely covered by sea water. Montana's Cambrian sea was home to algae, invertebrates, and even some of the first known vertebrates. Later, Cambrian trilobites left behind remains in Nixon Gulch, Horseshoe Hills north of Manhattan, Sawtooth-Lewis and Clark ranges west of Augusta, and the Bridger Range north of Bozeman. The sea eventually withdrew from the state and most of Montana's Silurian and Early Devonian sediments were lost to erosion. During the Late Devonian nearly the entire state was again inundated by the sea. Montana's Late Devonian sea was home to brachiopods, conodonts, crinoids, fish, molluscs, and sponges. Seas continued to cover the state into the Carboniferous period. At that time, the state was home to a bewildering array of cartilaginous fishes. Further into the Paleozoic, Mississippian brachiopods, bryozoans, and corals left behind fossils in the Bridger Range and at Shell Mountain south of Big Timber. Later in the Carboniferous, during the Pennsylvanian epoch, the sea began to retreat. Geological uplift was raising the elevation of the northern and northwestern regions of the state. Montana was covered by the sea again for a short interval of the Permian period.
During the Early Triassic, Montana was located about thirty degrees of latitude north of the equator. The sea returned twice to cover significant areas of Montana during the ensuing Triassic period. The state's only known contemporary fossils are the remains of this sea's inhabitants. On land Montana was hot and dry. At the time, the far southwesternmost corner of Montana was covered by a small extension of the shallow sea that covered the western coast of North America and stretched into northern Canada. South central Montana, by contrast, was a desert divided by streams. Outside of these regions little is known because sediments were being eroded rather than deposited. During the Jurassic, the sea returned to cover the state. The sea was gradually filled in by sediments eroded away from areas of higher elevation in the western region of the state. During the Late Jurassic, most of Montana was covered in seawater, similar to that which covered the southwestern corner during the Triassic. Ironically, at this point in time the southwestern area of the state contained an island. This sea would have been home to cephalopods, crinoids, ichthyosaurs, and pelecypods. At the time, Montana was located at about 40 degrees Latitude. The state's flora consisted of conifers, cycads, ferns, and ginkgoes. South of Montana's sea was a coastal plain split by streams flowing west from areas of higher elevation to the east. This coastal plain was home to dinosaurs including the ornithopod Camptosaurus, the sauropods Apatosaurus and Diplodocus, and the theropod Allosaurus. These sediments deposited what is now known as the Morrison Formation.
For thirty million years following the deposition of the Morrison Formation sediments in Montana were being eroded rather than deposited. Seawater was still present in Montana, now extending as an embayment down from the Arctic Circle. Rivers were still flowing into the local sea, but the local dinosaur fauna was very different. Carnivores living here included Deinonychus and Microvenator. Herbivores included Sauropelta and Tenontosaurus. Around this time flowering plants would make their first appearance in the state. During the middle part of the Cretaceous Montana was partially covered by the Western Interior Seaway. Significant volcanic eruptions occurred in Montana during the time of the Western Interior Seaway. This sea was home to cephalopods, clams, and plesiosaurs. The sediments deposited by this sea compose what is now called the Colorado Group. No dinosaur fossils are known to have been preserved in the Colorado group in Montana, but outside the state occasional discoveries have been made. Southwestern Montana was dry land, but none of those deposits have yielded dinosaur fossils yet. 85 million years ago the Western Interior Seaway withdrew slightly leaving western Montana as a coastal plain. Dinosaurs were present but rarely left fossilized remains. The sea was home to animals such as cephalopods, gastropods, mosasaurs, pelecypods, and plesiosaurs.
During the Campanian Stage of the Late Cretaceous the coastal plain bordering the Western Interior Seaway was lined with rivers and dotted with a few lakes. These bodies of water deposited the sediments that later became the Two Medicine Formation. Nearby volcanoes were erupting, depositing ash that would later become bentonite. The climate was semiarid. The flora of the coastal plain included conifer forests, deciduous trees, and ferns. A diverse array of dinosaurs lived in Montana at this time. Duckbilled hadrosaurs were common inhabitants of Montana's Campanian coastal plains. Maiasaura is one example. Montana has an especially good fossil record of ceratopsid dinosaurs. Examples of contemporary local ceratopsians include Einiosaurus. The theropods Daspletosaurus and Troodon were also present. Both Maiasaura and Troodon are known to have formed nesting colonies in the area. Late Cretaceous fossil dinosaur footprints are surprisingly rare in Montana compared to other western states with contemporary deposits. This might be due to the local ancient environments not being well suited for track preservation or merely because scientists have not yet looked in the right places.
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Early in the Maastrichtian the Western Interior Seaway expanded its boundaries somewhat. It was home to cephalopods, clams, crustaceans, fishes, gastropods, mosasaurs, and plesiosaurs. Later in the Maastrichtian stage, volcanic activity was still ongoing in the Elkhorn region and the Western Interior Seaway began to withdraw. This regression would end up resulting in both halves of North America reuniting. As the seaway withdrew the area closest to the Rocky Mountains became an expanding desert. Eastern Montana was hot and humid, by contrast, as the coastal plain was also expanding as a result of the marine regression. By the late Maastrichtian stage large rivers flowed across the eastern part of the state, depositing the sediments that would one day become the Hell Creek Formation. At the time, Montana was home to some of the most famous dinosaurs; creatures including Edmontosaurus, Pachycephalosaurus, Triceratops, and Tyrannosaurus.
History
Scientific research
In 1855, United States Geological Survey geologist Ferdinand Vandiveer Hayden was exploring a region of what was then called Nebraska Territory, but which is located what is now central Montana. Not far from the mouth of the Judith River he discovered fossils of bones, shells, and teeth. After returning from his expedition he gave the fossils to Joseph Leidy in Philadelphia. Leidy could tell that these teeth were different than those of any known animal, yet were recognizably dinosaurian based on their similarities to previously discovered dinosaur fossils in England. Leidy had made the first scientific identification of dinosaur fossils from Montana. As the remains were distinct from any previously described dinosaur taxa, Leidy erected three new genera and species for them; Deinodon horridus, Trachodon mirabilis, and Troodon formosus.
In 1901, Dr. Earl Douglass discovered fossil plants, mollusks, and vertebrae at Bear Butte, northwest of Melville in Sweet Grass County's Fort Union Beds. In 1933, another fossil site called the Scarritt site opened in the Fort Union beds. By the publication of a 1937 paper on the Fort Union beds by George Gaylord Simpson, 57 different fossil sites were known from the beds and 25 were of significant quality. Among the finds were arctocyonids, insectivores, multituberculates, pantodonts, primates, and taeniodonts.
Montanan Tertiary deposits in the Ruby Valley basin were first studied in 1947 by Dr. Herman F. Becker on behalf of the New York Botanical Garden. These deposits from the southwestern part of the state are one of the best sources of plant and insect fossils in North America. In 1959 Becker's Ruby Valley excavations uncovered about 5,000 specimens of more than two hundred species of plants, insects, and fishes. Invertebrate finds included ants, bees, beetles, earwigs, caddis flies, crane flies, damsel flies, lantern flies, may flies, grasshoppers, leaf hoppers, mosquitoes, snails, and wasps. Vertebrate remains included feathers, and, once in a while, a bird. In 1961 a new flora was found nearby in a badger burrow. The flora is called the Badger Flora. Among the different kinds of plants were water lilies and lotuses.
In 1964, John Ostrom led an expedition that included his student Robert T. Bakker into the south-central part of the state. The rocks they prospected were of the Cloverly Formation, dating back to the Early Cretaceous. Among their finds were the first documented remains of a small carnivorous dinosaur that would be named Deinonychus antirrhopus. This discovery helped ignite the Dinosaur Renaissance. It exhibited important anatomical similarities to birds that helped scientists shed antiquated ideas interpreting dinosaurs as "overgrown lizards".
In 1978, paleontologist Bill Clemens alerted Jack Horner and Bob Makela to the presence of unidentified dinosaur fossils in Bynum. Horner visited the town and recognized the remains as belonging to a duck-billed dinosaur. While in town the owner of a local rock shop, Marion Brandvold, showed him some tiny bones. Horner identified them as baby duck-bill bones. Horner also knew that this was an important find and convinced Brandvold to donate her fossils to a museum. She obliged and gave them to Princeton University. Horner's team prospected in the area where Brandvold found the baby hadrosaur fossils. Their effort paid off with the discovery of the first scientifically documented dinosaur eggs of the Western Hemisphere and a new kind of duck-bill, Maiasaura peeblesorum.
People
Gloria Jean Siebrecht was born in Kallispell in 1940.
John R. Horner was born in Shelby on June 15, 1946.
Natural history museums
