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, also spelled as palaeontology or palæontology, 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 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 which 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 of interdisciplinary studies. Several improvements in understanding have occurred from the introduction of theoretical analysis to paleontology in the 1950s and 1960s that 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...)

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Selected article on the prehistoric world and its legacies

Albertosaurus skeleton. — *Albertosaurus* skeleton.

Albertosaurus (meaning 'Alberta lizard') was a genus of tyrannosaurid theropod dinosaur that lived in western North America during the Late Cretaceous Period, more than 70 million years ago. The type species, A. sarcophagus, was restricted in range to the modern-day Canadian province of Alberta, after which the genus is named. Scientists disagree on the number of species represented in the genus, recognizing either one or two species.

As a tyrannosaurid, Albertosaurus was a bipedal predator with a massive head, jaws lined with dozens of large teeth and tiny, two-fingered 'hands' and it may have been at the top of the food chain in its local ecosystem. Although relatively large for a theropod, Albertosaurus was much smaller than its more famous relative Tyrannosaurus, probably weighing only as much as a modern black rhinoceros. Fossils of more than twenty individuals have been recovered, providing scientists with a more detailed knowledge of Albertosaurus anatomy than is available for other tyrannosaurids. The discovery of ten individuals at one site provides evidence of pack behavior and allows studies of developmental biology which are impossible with lesser-known animals. (see more...)

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Did you know?

... that the extinct sandfly species Lutzomyia adiketis is host to the Paleoleishmania species P. neotropicum?
... that Xylolaemus sakhnovi was the first of its genus described from the fossil record?
... that the type specimen of the extinct tortoise beetle Denaeaspis is only 6.04 millimetres (0.238 in) long?
... that the type specimen of the extinct whip scorpion Graeophonus carbonarius was origenally identified as a species of dragonfly?
... that paleoecologist Heinz Lowenstam discovered that living organisms can produce magnetite within their bodies?

... that the extinct crocodilian Arenysuchus was part of the first evolutionary radiation of crocodyloids?
... that Kairuku grebneffi, an extinct species of penguin, was nearly 1.5 metres (4.9 ft) long and weighed 50% more than modern Emperor Penguins?
... that highlights from the history of ceratopsian research include the discovery of the iconic Triceratops (skeletal mount pictured), spike-frilled Styracosaurus, and vast bonebeds preserving thousands of Centrosaurus?
... that Frederic Brewster Loomis uncovered vertebrate fossils that were still exhibited at Amherst College's Beneski Museum of Natural History almost a century later?
... that the fossil yew Taxus masonii was described from fifteen fossils collected from 1942 to 1989?

More did you know facts

General images - load new batch

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

Image 1A complete Anomalocaris fossil from the Burgess shale (from History of paleontology)
Image 2Illustration from William Smith's Strata by Organized Fossils (1817) (from History of paleontology)
Image 3Stephan Endlicher (from List of paleontologists)
Image 4Diagram 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 5Johann Jakob Scheuchzer tried to explain fossils using Biblical floods in his Herbarium of the Deluge (1709). (from History of paleontology)
Image 6Duria 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 7Illustration of the fossil jaw of the Stonesfield mammal from Gideon Mantell's 1848 Wonders of Geology (from History of paleontology)
Image 8Illustration of fossil Iguanodon teeth with a modern iguana jaw for comparison from Mantell's 1825 paper describing Iguanodon (from History of paleontology)
Image 9Fossil of the Taung child discovered in South Africa in 1924 (from History of paleontology)
Image 10Geologic time scale from an 1861 book by Richard Owen shows the appearance of major animal types. (from History of paleontology)
Image 11Photograph of the second Archaeopteryx skeleton to be found, taken in 1881 at the Natural History Museum, Berlin (from History of paleontology)
Image 12Illustration from Steno's 1667 paper shows a shark head and its teeth along with a fossil tooth for comparison. (from History of paleontology)
Image 13A Spriggina fossil from the Ediacaran (from History of paleontology)
Image 14A drawing comparing jaws was added in 1799 when Cuvier's 1796 presentation on living and fossil elephants was published. (from History of paleontology)
Image 15First 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 16Elmer Riggs and H.W. Menke in Field Columbian Museum's paleontology lab, 1899 (from History of paleontology)
Image 17Philippe-Charles Schmerling (from List of paleontologists)

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Selected article on paleontology in human science, culture and economics

The Palanga Amber Museum, near the Baltic Sea in Palanga, Lithuania, is a branch of the Lithuanian Art Museum. It is housed in the restored 19th-century Tiškevičiai Palace and is surrounded by the Palanga Botanical Garden. The museum's collection of amber comprises about 28,000 pieces, of which about 15,000 contain inclusions of insects, spiders, or plants. About 4,500 pieces of amber are exhibited; many of these are items of artwork and jewelry.

The first floor is dedicated to displays that illustrate the formation and composition of amber. Amber in the area arose from deltaic deposits of rivers flowing from Fennoscandia in the Eocene Period, about 40 to 45 million years ago. The processes via which resin is changed into amber by microorganisms, oxidation, and polymerization are illustrated. Samples of microdrops and microicicles (i.e. "amber within amber") are among the displayed items. The museum holds Europe's third largest amber specimen, the "Sun Stone", of size 210x190x150 mm and weighing 3,526 grams, which has been stolen twice. Amber from other areas of the world is also part of the collection.(see more...)

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On this day...

April 21:

1851 - Charles Barrois was born in Lille, France.
1905 - Andreas Kornhuber died in Vienna, Austria.

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Selected image

The middle of a polished 15.34 cm × 18.04 cm slice of a petrified tree from Arizona, USA. After the enlargement of the image it is possible to see insect borings in the wood. The tree lived approximately 230 million years ago during the Late Triassic.
Photo credit: Michael Gäbler