This article includes a list of general references, but it lacks sufficient corresponding inline citations .(April 2023) |
Established | 1866 |
---|---|
Location | New Haven, Connecticut, US |
Coordinates | 41°19′03″N72°55′12″W / 41.317538°N 72.919863°W |
Type | Natural History |
Director | David Skelly |
Owner | Yale University |
Public transit access | 228, 229 |
Website | peabody |
The Peabody Museum of Natural History at Yale University (also known as the Yale Peabody Museum of Natural History [1] or the Yale Peabody Museum [1] ) is one of the oldest, largest, and most prolific university natural history museums in the world. It was founded by the philanthropist George Peabody in 1866 at the behest of his nephew Othniel Charles Marsh, an early paleontologist. The museum is best known for the Great Hall of Dinosaurs, which includes a mounted juvenile Brontosaurus and the 110-foot-long (34 m) mural The Age of Reptiles . The museum also has permanent exhibits dedicated to human and mammal evolution; wildlife dioramas; Egyptian artifacts; local birds and minerals; and Native Americans of Connecticut.
In 2020, the Peabody Museum closed for its "first comprehensive renovation in 90 years." [2] It reopened, with more than twice the exhibition space, on March 26, 2024. [3] [4]
The Peabody Museum is located at 170 Whitney Avenue in New Haven, Connecticut and is staffed by nearly a hundred staff members. The original building was demolished in 1917; it moved to its current location in 1925, and has since expanded to occupy the Peabody Museum, the attached Kline Geology Laboratory, the Class of 1954 Environmental Sciences Center, parts of three additional buildings, and a field station at Long Island Sound. The museum also owns Horse Island in the Thimble Islands, which is not open to the public; it is used for experiments. The Class of 1954 Environmental Science Center, completed in 2001 and connected to the museum and the adjacent Kline Geology Laboratory, hosts approximately one-half of the museum's 13 million specimens.[ citation needed ]
On August 28, 2018, Yale University announced a contribution of $160 million by Edward P. Bass towards the cost of the renovation of the museum. [5] [6] The landmark commitment ranks among the most generous gifts to Yale and is the largest known gift ever made to a natural history museum in the United States,[ citation needed ] helping to fund the renewal and expansion of the museum. [7]
The galleries were planned to be open through June 30, 2020 (the Great Hall of Dinosaurs was open through January 1, 2020), but had to close in March due to COVID-19 and did not reopen until the conclusion of renovations in 2024. [7] [8] The renovation more than doubled the exhibition space, added 10 classrooms, and included a new education center for K-12 students. [9]
In November 2021, Yale University announced that admission will be free "in perpetuity" once construction is complete. [10]
The Peabody has several world-important collections. Perhaps the most notable are the vertebrate paleontology collections which are among the largest, most extensive, and most historically important fossil collections in the United States (see Othniel Charles Marsh, R.S. Lull, George Gaylord Simpson, John Ostrom, Elisabeth Vrba, and Jacques Gauthier), and the Hiram Bingham Collection of Incan artifacts from Machu Picchu, named for the famous Yale archaeologist who rediscovered the Peruvian ruin. Also notable are the extensive ornithology collection, one of the largest and most taxonomically inclusive in the world,[ citation needed ] and the associated William Robertson Coe Ornithology Library, one of the best in the United States. The collection of marine invertebrates is also extensive, having benefitted from the work of prolific invertebrate zoologists including Addison Emery Verrill. The Yale Herbarium is part of the Peabody Museum. [11]
Faculty curators for the collections are drawn from Yale's departments of Ecology and Evolutionary Biology, Geology and Geophysics, and Anthropology. Because the departments maintain a strong tradition of hiring faculty to perform collections-based research, especially after the renewed support for organismal biology at Yale under President Richard Charles Levin and in particular former provost Alison Richard, nearly all of the collections are under active internal use and enjoy continuous and considerable growth. [ citation needed ]
The museum has erected the first full-scale reproduction of a Torosaurus on Whitney Avenue next to the entrance. The 3 m (9 ft) tall, 7 m (21 ft) long, 3.33 metric ton (7,350 lb) statue was sculpted in clay and cast in bronze, and set on a 4 m (13 ft) tall granite base. The reproduction of T. latus is scientifically faithful of T. latus, and its skin is based on the fossilized skin impressions left by a Chasmosaurus (a closely related ceratopsid). [12]
Permanent exhibits before renovations have included:
As of 2024 [update] , the director of the Peabody Museum is David Skelly, a curator of vertebrate zoology and a professor of ecology in the Department of Ecology & Evolutionary Biology, and the School of Forestry and Environmental Studies. He was named director in 2014. [16]
The Peabody Museum has curators representing anthropology, botany, entomology, invertebrate zoology, invertebrate paleontology, vertebrate zoology (with individual curators for herpetology, ichthyology, mammalogy, and ornithology), paleobotany, vertebrate paleontology; mineralogy and meteoritics; and historical scientific instruments.[ citation needed ]
There are almost 100 full-time and part-time staff, including curators, assistant curators, curators emeriti, curatorial affiliates, and volunteers. Curators and assistant curators are also faculty members in related departments. [17] [18]
Othniel Charles Marsh was an undergraduate and later the Professor of Paleontology at Yale University. His education was paid for by his wealthy uncle George Peabody, who began to donate much of his accumulated wealth to various educational institutions at the end of his life. Marsh and his teams discovered dozens of new genera of dinosaurs and other fossil animals, including Triceratops , Brontosaurus , and Hesperornis . At the request of Marsh and to house some of his discoveries, Peabody founded Yale's Museum of Natural History in 1866 with a gift of $150,000.[ citation needed ]
Yale's collection at the time was mostly minerals, collected by the geologist and mineralogist Benjamin Silliman. Marsh was one of the museum's first three curators and when Peabody died in 1869, he used his inheritance to fund expeditions bringing back specimens which greatly increased the museum's collections. His primary interest was dinosaurs. During the infamous period in paleontological history known as the Bone Wars, he discovered 56 new species of dinosaur and literally shipped tons of fossils back from the American Southwest. His finds also included fossils of vertebrates and invertebrates, trackways of prehistoric animals; and archaeological and ethnological artifacts.
The museum officially opened to the public in 1876. In 1917, it was demolished and replaced by the Harkness Memorial Quadrangle dormitory.[ citation needed ] When World War I began most of the collections were put in storage until December 1925, when the current building was dedicated.[ citation needed ] The new building had a great, 2-story hall designed specifically to hold Marsh's dinosaurs.
Some other significant events include:
Apatosaurus is a genus of herbivorous sauropod dinosaur that lived in North America during the Late Jurassic period. Othniel Charles Marsh described and named the first-known species, A. ajax, in 1877, and a second species, A. louisae, was discovered and named by William H. Holland in 1916. Apatosaurus lived about 152 to 151 million years ago (mya), during the late Kimmeridgian to early Tithonian age, and are now known from fossils in the Morrison Formation of modern-day Colorado, Oklahoma, New Mexico, Wyoming, and Utah in the United States. Apatosaurus had an average length of 21–23 m (69–75 ft), and an average mass of 16.4–22.4 t. A few specimens indicate a maximum length of 11–30% greater than average and a mass of approximately 33 t.
John Bell Hatcher was an American paleontologist and fossil hunter known as the "king of collectors" and best known for discovering Torosaurus and Triceratops, two genera of dinosaurs described by Othniel Charles Marsh. He was part of a new, professional middle class in American science, having financed his education with his labor while also being more educated than older fossil collectors. As such, he faced unique challenges throughout his long and productive career.
Othniel Charles Marsh was an American professor of Paleontology in Yale College and President of the National Academy of Sciences. He was one of the preeminent scientists in the field of paleontology. Among his legacies are the discovery or description of dozens of new species and theories on the origins of birds.
The Carnegie Museum of Natural History is a natural history museum in the Oakland neighborhood of Pittsburgh, Pennsylvania. It was founded by Pittsburgh-based industrialist Andrew Carnegie in 1896. Housing some 22 million specimens, the museum features one of the finest paleontological and entomological collections in the world.
The Sam Noble Oklahoma Museum of Natural History is the officially designated natural history museum for the State of Oklahoma, located on the campus of the University of Oklahoma. The museum was founded in 1899 by an act of the Oklahoma Territorial Legislature. Its current building was completed in 1999 under the leadership of Michael A. Mares, who was director from 1983-2003 and from 2008-2018. The museum contains more than 10 million objects and specimens in 12 collections. The current building is a 198,000-square-foot facility with almost 50,000 square feet of public space, with five permanent and two temporary galleries and exhibits that provide an in-depth tour of Oklahoma's natural and cultural history. The remainder of the facility is dedicated to housing museum collections, laboratories, libraries, and offices. It is one of the world's largest university-based natural history museums.
Addison Emery Verrill was an American invertebrate zoologist, museum curator and university professor.
Como Bluff is a long ridge extending east–west, located between the towns of Rock River and Medicine Bow, Wyoming. The ridge is an anticline, formed as a result of compressional geological folding. Three geological formations, the Sundance, the Morrison, and the Cloverly Formations, containing fossil remains from the Late Jurassic of the Mesozoic Era are exposed.
Brontosaurus is a genus of herbivorous sauropod dinosaur that lived in present-day United States during the Late Jurassic period. It was described by American paleontologist Othniel Charles Marsh in 1879, the type species being dubbed B. excelsus, based on a partial skeleton lacking a skull found in Como Bluff, Wyoming. In subsequent years, two more species of Brontosaurus were named: B. parvus in 1902 and B. yahnahpin in 1994. Brontosaurus lived about 156 to 146 million years ago (mya) during the Kimmeridgian and Tithonian ages in the Morrison Formation of what is now Utah and Wyoming. For decades, the animal was thought to have been a taxonomic synonym of its close relative Apatosaurus, but a 2015 study by Emmanuel Tschopp and colleagues found it to be distinct. It has seen widespread representation in popular culture, being the archetypal "long-necked" dinosaur in general media.
Microvenator is a genus of dinosaur from the Early Cretaceous Cloverly Formation in what is now south central Montana. Microvenator was an oviraptorosaurian theropod. The holotype fossil is an incomplete skeleton, most likely a juvenile with a length of 1.3 m (4.3 ft), and consequently, the adult size remains uncertain. Microvenator celer is primitive and may be the "sister taxon to all other oviraptorosaurs."
Charles Robert Knight was an American wildlife and paleoartist best known for his detailed paintings of dinosaurs and other prehistoric animals. His works have been reproduced in many books and are currently on display at several major museums in the United States. One of his most famous works is a mural of Tyrannosaurus and Triceratops, which helped establish the two dinosaurs as "mortal enemies" in popular culture. Working at a time when many fossil discoveries were fragmentary and dinosaur anatomy was not well understood, many of his illustrations have later been shown to be incorrect representations. Nevertheless, he has been hailed as "one of the great popularizers of the prehistoric past".
Charles Whitney Gilmore was an American paleontologist who gained renown in the early 20th century for his work on vertebrate fossils during his career at the United States National Museum. Gilmore named many dinosaurs in North America and Mongolia, including the Cretaceous sauropod Alamosaurus, Alectrosaurus, Archaeornithomimus, Bactrosaurus, Brachyceratops, Chirostenotes, Mongolosaurus, Parrosaurus, Pinacosaurus, Styracosaurus ovatus and Thescelosaurus.
Dermodactylus was a genus of pterodactyloid pterosaur from the Kimmeridgian-Tithonian-age Upper Jurassic Morrison Formation of Wyoming, United States. It is based on a single partial bone, from the hand.
Rudolph Franz Zallinger was an American-based Austrian-Russian artist. His most notable works include his mural The Age of Reptiles (1947) at Yale University's Peabody Museum of Natural History, and the March of Progress (1965) with numerous parodies and versions. His painting of a Tyrannosaurus heavily influenced the creature design of Toho Studios' Godzilla (1954). Two of Zallinger's dinosaurs—the T. rex and Brontosaurus—are seen in that film as part of a slide demonstration during a lecture in the National Diet Building.
Garden Park is a paleontological site in Fremont County, Colorado, known for its Jurassic dinosaurs and the role the specimens played in the infamous Bone Wars of the late 19th century. Located 10 km (6.2 mi) north of Cañon City, the name originates from the area providing vegetables to the miners at nearby Cripple Creek in the 19th century. Garden Park proper is a triangular valley surrounded by cliffs on the southeast and southwest and by mountains to the north; however, the name is also refers to the dinosaur sites on top and along the cliffs. The dinosaur sites now form the Garden Park Paleontological Resource Area, which is overseen by the Bureau of Land Management.
Apatosaurinae is a subfamily of diplodocid sauropods, an extinct group of large, quadrupedal dinosaurs, the other subfamily in Diplodocidae being Diplodocinae. Apatosaurines are distinguished by their more robust, stocky builds and shorter necks proportionally to the rest of their bodies. Several fairly complete specimens are known, giving a comprehensive view of apatosaurine anatomy.
The Age of Reptiles is a 110-foot (34 m) mural depicting the period of ancient history when reptiles were the dominant creatures on the earth, painted by Rudolph Zallinger. The fresco sits in the Yale Peabody Museum in New Haven, Connecticut, and was completed in 1947 after five years of work. The Age of Reptiles was at one time the largest painting in the world, and depicts a span of nearly 350 million years in Earth's history.
Paleoart is any original artistic work that attempts to depict prehistoric life according to scientific evidence. Works of paleoart may be representations of fossil remains or imagined depictions of the living creatures and their ecosystems. While paleoart is typically defined as being scientifically informed, it is often the basis of depictions of prehistoric animals in popular culture, which in turn influences public perception of and fuels interest in these organisms. The word paleoart is also used in an informal sense, as a name for prehistoric art, most often cave paintings.
Charles Emerson Beecher was an American paleontologist most famous for the thorough excavation, preparation and study of trilobite ventral anatomy from specimens collected at Beecher's Trilobite Bed. Beecher was rapidly promoted at Yale Peabody Museum, eventually rising to head that institution.
Paleontology in Connecticut refers to paleontological research occurring within or conducted by people from the U.S. state of Connecticut. Apart from its famous dinosaur tracks, the fossil record in Connecticut is relatively sparse. The oldest known fossils in Connecticut date back to the Triassic period. At the time, Pangaea was beginning to divide and local rift valleys became massive lakes. A wide variety of vegetation, invertebrates and reptiles are known from Triassic Connecticut. During the Early Jurassic local dinosaurs left behind an abundance of footprints that would later fossilize.
The Raymond M. Alf Museum of Paleontology is a paleontology museum in Claremont, California, that is part of The Webb Schools. It is the only nationally accredited museum on a secondary school campus in the United States. The museum has two circular 4,000 sq. ft. exhibition halls and 20,000 unique annual visitors. The collections number about 140,000 specimens, 95% of which were found by Webb students on fossil-collecting trips called “Peccary Trips,” expeditions usually centered in California, Utah, and Montana. The collections consist primarily of vertebrate, invertebrate, and track fossils and the museum's large track collection is widely recognized as one of the most diverse in the world.