Portal:Paleontology

The Palaeontology Portal

Introduction

Bust of the paleontologist Georges Cuvier (left) and a cast skeleton of *Palaeotherium magnum* (named by Cuvier in 1804, right), Cuvier Museum of Montbéliard

Paleontology or palaeontology is the scientific study of the life of the past, mainly but not exclusively through the study of fossils. Paleontologists use fossils as a means to classify organisms, measure geologic time, and assess the interactions between prehistoric organisms and their natural environment. While paleontological observations are known from at least the 6th century BC, the foundation of paleontology as a science dates back to the work of Georges Cuvier in 1796. Cuvier demonstrated evidence for the concept of extinction and how the life of the past was not necessarily the same as that of the present. The field developed rapidly over the course of the following decades, and the French word paléontologie was introduced for the study in 1822, which was derived from the Ancient Greek word for 'ancient' and words describing relatedness and a field of study. Further advances in the field accompanied the work of Charles Darwin who popularized the concept of evolution. Together, evolution and extinction can be understood as complementary processes that shaped the history of life.

Paleontology overlaps the most with the fields of geology and biology. It draws on technology and analysis of a wide range of sciences to apply them to the study of life and environments of the past, particularly for the subdisciplines of paleobiology and paleoecology that are analogous to biology and ecology. Paleontology also contributes to other sciences, being utilized for biostratigraphy to reconstruct the geologic time scale of Earth, or in studies on extinction to establish both external and internal factors that can lead to the disappearance of a species. Much of the history of life is now better understood because of advances in paleontology and the increase in interdisciplinary studies. Several improvements in understanding have occurred from the introduction of theoretical analysis to paleontology in the 1950s and 1960s which led to the rise of more focused fields of paleontology that assess the changing geography and climate of Earth, the phylogenetic relationships between different species, and the analysis of how fossilization occurs and what biases can impact the quality of the fossil record. (Full article...)

Selected article on the prehistoric world and its legacies

Artist's restoration of Nigersaurus taqueti. — Artist's restoration of *Nigersaurus taqueti*.

Nigersaurus (meaning "Niger reptile") is a genus of rebbachisaurid sauropod dinosaur that lived during the middle Cretaceous period, about 115 to 105 million years ago. It was discovered in the Elrhaz Formation in an area called Gadoufaoua, in the Republic of Niger. Fossils of this dinosaur were first described in 1976, but it was only named in 1999 after further and more complete remains were found and described. The genus contains a single species, Nigersaurus taqueti.

Nigersaurus was 9 m (30 ft) long, which is small for a sauropod, and had a short neck. It weighed around four tonnes, comparable to a modern elephant. Its skeleton was filled with air spaces connected to air sacs, but the limbs were robustly built. Its skull was very specialised for feeding, with a wide muzzle filled with more than 500 teeth. The jaws may have borne a keratinous sheath. Unlike other tetrapods, the tooth-bearing bones of its jaws were rotated transversely relative to the rest of the skull, so that all of its teeth were located far to the front.

Nigersaurus was probably a browser, and fed with its head close to the ground. It lived in a riparian habitat, and its diet probably consisted of soft plants, such as ferns, horsetails, and angiosperms. It is one of the most common fossil vertebrates found in the area, and shared its habitat with other dinosaurian megaherbivores, as well as large theropods and crocodylomorphs. (see more...)

Did you know?

The holotype fossil of Allorapisma chuorum

... that wings of the extinct moth lacewing Allorapisma are most similar to a Cretaceous genus from Brazil?
... that the rauisuchian Tsylmosuchus is known from strata in Russia that are early Olenekian in age, making it one of the earliest archosaurs?
... that malacologist Myra Keen was called the "First Lady of Malacology"?
... that the nearest living relatives of Eosacantha, a fossil tortoise beetle from Colorado, are found in Africa, tropical Asia, and Australia?
... that when the extinct forester moth Neurosymploca? oligocenica was described, a second fossil was known but unavailable for study?

... that the 150-million-year-old ink of the extinct, squid-like Belemnotheutis (artist's rendition pictured) was used to draw a picture that paleontologists called "the ultimate self portrait"?
... that Archaeomarasmius, Aureofungus, Coprinites, and Protomycena are the only four genera of agaric mushrooms known from the fossil record?
... that although the first two fossils of Indraloris to be found were misidentified as a carnivoran and a loris, it is in fact a member of the extinct adapiform primates?
... that the extinct Itilochelys is one of only three known fossil cheloniid sea turtle taxa found in the Volgograd Region?
... that fossils of Eucommia constans are the youngest and most southerly examples of Eucommia in North America?

General images -

The following are images from various paleontology-related articles on Wikipedia.

Image 1Philippe-Charles Schmerling (from List of paleontologists)
Image 2Elmer Riggs and H.W. Menke in Field Columbian Museum's paleontology lab, 1899 (from History of paleontology)
Image 3Photograph of the second Archaeopteryx skeleton to be found, taken in 1881 at the Natural History Museum, Berlin (from History of paleontology)
Image 4Johann Jakob Scheuchzer tried to explain fossils using Biblical floods in his Herbarium of the Deluge (1709). (from History of paleontology)
Image 5A complete Anomalocaris fossil from the Burgess Shale (from History of paleontology)
Image 6Illustration of fossil Iguanodon teeth with a modern iguana jaw for comparison from Mantell's 1825 paper describing Iguanodon (from History of paleontology)
Image 7Duria Antiquior – A more Ancient Dorset is a watercolor painted in 1830 by the geologist Henry De la Beche based on fossils found by Mary Anning. The late 18th and early 19th century was a time of rapid and dramatic changes in ideas about the history of life on Earth. (from History of paleontology)
Image 8Illustration from Steno's 1667 paper shows a shark head and its teeth along with a fossil tooth for comparison. (from History of paleontology)
Image 9A Spriggina fossil from the Ediacaran (from History of paleontology)
Image 10Illustration of the fossil jaw of the Stonesfield mammal from Gideon Mantell's 1848 Wonders of Geology (from History of paleontology)
Image 11Illustration from William Smith's Strata by Organized Fossils (1817) (from History of paleontology)
Image 12A drawing comparing jaws was added in 1799 when Cuvier's 1796 presentation on living and fossil elephants was published. (from History of paleontology)
Image 13First mention of the word palæontologie, as coined in January 1822 by Henri Marie Ducrotay de Blainville in his Journal de physique (from History of paleontology)
Image 14Fossil of the Taung child discovered in South Africa in 1924 (from History of paleontology)
Image 15Stephan Endlicher (from List of paleontologists)
Image 16Diagram by O.C. Marsh of the evolution of horse feet and teeth, reproduced in T. H. Huxley's 1876 book, Professor Huxley in America (from History of paleontology)
Image 17Geologic time scale from an 1861 book by Richard Owen shows the appearance of major animal types. (from History of paleontology)

Selected article on paleontology in human science, culture and economics

Paleontology or palaeontology (/ˌpeɪliɒnˈtɒlədʒi, ˌpæli-, -ən-/) is the scientific study of prehistoric life. It includes the study of fossils to determine organisms' evolution and interactions with each other and their environments (their paleoecology). As a "historical science" it attempts to explain causes rather than conduct experiments to observe effects. Paleontological observations have been documented as far back as the 5th century BC. The science became established in the 18th century as a result of Georges Cuvier's work on comparative anatomy, and developed rapidly in the 19th century. The term itself originates from Greek: παλαιός (palaios) meaning "old, ancient," ὄν, ὀντ- (on, ont-), meaning "being, creature" and λόγος (logos), meaning "speech, thought, study".

Paleontology lies on the border between biology and geology. It now uses techniques drawn from a wide range of sciences, including biochemistry, mathematics and engineering. Use of all these techniques has enabled paleontologists to discover much of the evolutionary history of life, almost all the way back to when Earth became capable of supporting life, about 3,800 million years ago. As knowledge has increased, paleontology has developed specialized sub-divisions, some of which focus on different types of fossil organisms while others study ecology and environmental history, such as ancient climates. Body fossils and trace fossils are the principal types of evidence about ancient life, and geochemical evidence has helped to decipher the evolution of life before there were organisms large enough to leave fossils. (see more...)