Jean Léopold Nicolas Frédéric, Baron Cuvier, known as Georges Cuvier, was a French naturalist and zoologist, sometimes referred to as the "founding father of paleontology". Cuvier was a major figure in natural sciences research in the early 19th century and was instrumental in establishing the fields of comparative anatomy and paleontology through his work in comparing living animals with fossils.
Timeline of paleontology
William Buckland DD, FRS was an English theologian who became Dean of Westminster. He was also a geologist and palaeontologist.
A coprolite is fossilized feces. Coprolites are classified as trace fossils as opposed to body fossils, as they give evidence for the animal's behaviour rather than morphology. The name is derived from the Greek words κόπρος and λίθος. They were first described by William Buckland in 1829. Before this, they were known as "fossil fir cones" and "bezoar stones". They serve a valuable purpose in paleontology because they provide direct evidence of the predation and diet of extinct organisms. Coprolites may range in size from a few millimetres to over 60 centimetres.
The Last Interglacial, also known as the Eemian among other names, was the interglacial period which began about 130,000 years ago at the end of the Penultimate Glacial Period and ended about 115,000 years ago at the beginning of the Last Glacial Period. It corresponds to Marine Isotope Stage 5e. It was the second-to-latest interglacial period of the current Ice Age, the most recent being the Holocene which extends to the present day. During the Last Interglacial, the proportion of CO2 in the atmosphere was about 280 parts per million. The Last Interglacial was one of the warmest periods of the last 800,000 years, with temperatures comparable to and at times warmer than the contemporary Holocene interglacial, with the maximum sea level being up to 6 to 9 metres higher than at present, with global ice volume likely also being smaller than the Holocene interglacial.
The straight-tusked elephant is an extinct species of elephant that inhabited Europe and Western Asia during the Middle and Late Pleistocene. One of the largest known elephant species, mature fully grown bulls on average had a shoulder height of 4 metres (13 ft) and a weight of 13 tonnes (29,000 lb). Straight-tusked elephants likely lived very similarly to modern elephants, with herds of adult females and juveniles and solitary adult males. The species was primarily associated with temperate and Mediterranean woodland and forest habitats, flourishing during interglacial periods, when its range would extend across Europe as far north as Great Britain and eastwards into Russia. Skeletons found in association with stone tools and wooden spears suggest they were scavenged and hunted by early humans, including Neanderthals. It is the ancestor of most dwarf elephants that inhabited islands in the Mediterranean.
The history of paleontology traces the history of the effort to understand the history of life on Earth by studying the fossil record left behind by living organisms. Since it is concerned with understanding living organisms of the past, paleontology can be considered to be a field of biology, but its historical development has been closely tied to geology and the effort to understand the history of Earth itself.
The cave hyena, also known as the Ice Age spotted hyena, are paleosubspecies of spotted hyena known from Eurasia, which ranged from the Iberian Peninsula to eastern Siberia. It is one of the best known mammals of the Ice Age and is well represented in many European bone caves. It preyed on large mammals, and was responsible for the accumulation of hundreds of large Pleistocene mammal bones in areas including horizontal caves, sinkholes, mud pits, and muddy areas along rivers.
The Adams mammoth is the first woolly mammoth skeleton with skin and flesh still attached to be recovered by scientists. The mostly complete skeleton and flesh were discovered in 1799 in northeastern Siberia by Ossip Shumachov, an Evenki hunter and subsequently recovered in 1806 when Russian botanist Mikhail Adams journeyed to the location and collected the remains.
Duria Antiquior, a more ancient Dorset, was the first pictorial representation of a scene of prehistoric life based on evidence from fossil reconstructions, a genre now known as paleoart.
The Allenton Hippo is a hippopotamus skeleton that was found in Allenton, Derby, England, in 1895. The skeleton is exhibited in Derby Museum and Art Gallery and is 3 metres (9.8 ft) in length. It is celebrated today in a sculpture near to where the skeleton was discovered.
The narrow-nosed rhinoceros, also known as the steppe rhinoceros is an extinct species of rhinoceros belonging to the genus Stephanorhinus that lived in western Eurasia, including Europe, as well as North Africa during the Pleistocene. It first appeared in Europe around 500,000 years ago during the Middle Pleistocene and survived there until at least 34,000 years Before Present. It was native to temperate and Mediterranean environments, where it fed on low growing plants and to a lesser extent woody plants. Evidence has been found that it was exploited for food by archaic humans, including Neanderthals.
The Mammutmuseum Niederweningen is a paleontological and geological museum in the municipality of Niederweningen in the Wehntal valley, Canton of Zürich, Switzerland, and one of the few mammoth museums in Europe.
Bubalus murrensis, also known as European water buffalo, is an extinct water buffalo species native to Europe during the Pleistocene epoch, possibly persisting into the Holocene.
Betal Rock Shelter, a karst cave located on the south-eastern edge of the Lower Pivka river valley on a slope just above the road from Postojna to Bukovje is a site where rich cultural sediment layers with remains of stone tools, artifacts, and numerous fossilized bones of contemporary animals were found. Its entrance was formed by the collapse of the 174 m (571 ft) long cave's ceiling, carved out by the waters of the Pivka River.
Phascolotherium is a genus of extinct eutriconodont mammal from the Middle Jurassic of the United Kingdom. Found in the Stonesfield Slate, it was one of the first Mesozoic mammals ever found and described, although like the other mammal jaws found at the same time, it was mistakenly thought at first to be a marsupial.
The Cave of Aurignac is an archaeological site in the commune of Aurignac, Haute-Garonne department in southwestern France. Sediment excavation and artefact documentation since 1860 confirm the idea of the arrival and permanent presence of European early modern humans during the Upper Palaeolithic. The eponymous location represents the type site of the Aurignacian, the earliest known culture attributed to modern humans in western Eurasia. Assemblages of Aurignacian tool making tradition can be found in the cultural sediments of numerous sites from around 45,000 years BP to around 26,000 years BP. In recognition of its significance for various scientific fields and the 19th-century pioneering work of Édouard Lartet the Cave of Aurignac was officially declared a national Historic Monument of France by order of May 26, 1921.
Dream Cave is a natural limestone cavern located near Wirksworth in Derbyshire, England. It was discovered by lead miners in 1822 and was found to contain the almost complete skeletal remains of a woolly rhinoceros and other large mammal bones. These remains were acquired by the geologist William Buckland and are now housed in Oxford Museum.
Jules de Christol was a French paleontologist and geologist who identified the fossil horse ancestor Hipparion. He was among the first French zoologists to suggest the existence of human remains that were "antediluvian", older than the supposed Biblical flood, contrary to the dominant view of Earth history at the time.
The Armley Hippo, previously known as the Leeds Hippopotamus, is a partial skeleton of a common hippopotamus consisting of 122 bones, of which 25 were taxidermy-mounted in 2008 by James Dickinson for display at Leeds City Museum in Leeds, West Yorkshire, England. The skeleton dates to the last interglacial (Eemian) around 130,000 to 115,000 years ago.
