Portal:Paleontology

The Palaeontology Portal

Introduction

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...)

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The small shelly fauna or small shelly fossils, abbreviated to SSF, are mineralized fossils, many only a few millimetres long, with a nearly continuous record from the latest stages of the Ediacaran to the end of the Early Cambrian period. They are very diverse, and there is no formal definition of "small shelly fauna" or "small shelly fossils". Almost all are from earlier rocks than more familiar fossils such as trilobites. Since most SSFs were preserved by being covered quickly with phosphate and this method of preservation is mainly limited to the Late Ediacaran and Early Cambrian periods, the animals that made them may actually have arisen earlier and persisted after this time span.

The bulk of the fossils are fragments or disarticulated remains of larger organisms, including sponges, molluscs, slug-like halkieriids, brachiopods, echinoderms, and onychophoran-like organisms that may have been close to the ancestors of arthropods. Although the small size and often fragmentary nature of SSFs makes it difficult to identify and classify them, they provide very important evidence for how the main groups of marine invertebrates evolved, and particularly for the pace and pattern of evolution in the Cambrian explosion. Besides including the earliest known representatives of some modern phyla, they have the great advantage of presenting a nearly continuous record of Early Cambrian organisms whose bodies include hard parts. (see more...)

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Stephen Jay Gould (September 10, 1941 – May 20, 2002) was an American paleontologist, evolutionary biologist, and historian of science. He was also one of the most influential and widely read writers of popular science of his generation. Gould spent most of his career teaching at Harvard University and working at the American Museum of Natural History in New York. In the later years of his life, Gould also taught biology and evolution at New York University.

Gould's most significant contribution to evolutionary biology was the theory of punctuated equilibrium, which he developed with Niles Eldredge in 1972. The theory proposes that most evolution is marked by long periods of evolutionary stability, which is punctuated by rare instances of branching evolution. The theory was contrasted against phyletic gradualism, the popular idea that evolutionary change is marked by a pattern of smooth and continuous change in the fossil record.

Most of Gould's research was based on the land snail genera Poecilozonites and Cerion. He also contributed to evolutionary developmental biology, and has received wide praise for his book Ontogeny and Phylogeny. In evolutionary theory he opposed strict selectionism, sociobiology as applied to humans, and evolutionary psychology. Gould was known by the general public mainly from his 300 popular essays in the magazine Natural History, and his books written for a non-specialist audience. In April 2000, the US Library of Congress named him a "Living Legend". (see more...)

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An extremely well preserved specimen of the Late Jurassic ichthyodectid fish genus Thrissops, similar to the species T. formosus. The specimen was discovered near Ettling, Bavaria, Germany and still preserves remains of the animal's soft tissue like musculature and the gastrointestinal tract. Even the color pattern it exhibited in life is preserved as spots by the melanin in its scales.
Photo credit: H. Zell

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Topics

General - Paleontology - Fossil - Evolution - Extinction
History - History of paleontology - Bone Wars - List of years in paleontology2026 in paleontology2026 in paleoanthropology
Locations - List of dinosaur-bearing rock formations - List of fossil sites - Como Bluff - Coon Creek Formation - Dinosaur Cove - Dinosaur National Monument - Dinosaur Park Formation - Dinosaur State Park and Arboretum - Glen Rose Formation - Hell Creek Formation - Lance Formation - Morrison Formation - Red Gulch Dinosaur Tracksite - Two Medicine Formation
Paleontologists - Mary Anning - Robert T. Bakker - Barnum Brown - William Buckland - Edward Drinker Cope - Jack Horner - Gideon Mantell - Othniel Charles Marsh - John Ostrom - Dong Zhiming
Geologic Time - Paleozoic Era - Cambrian (Early Cambrian - Middle Cambrian - Furongian) - Ordovician (Early Ordovician - Middle Ordovician - Late Ordovician) - Silurian (Llandovery - Wenlock - Ludlow - Pridoli) - Devonian (Early Devonian - Middle Devonian - Late Devonian) - Carboniferous (Mississippian - Pennsylvanian) - Permian (Cisuralian - Guadalupian - Lopingian) - Mesozoic Era - Triassic (Early Triassic - Middle Triassic - Late Triassic) - Jurassic (Early Jurassic - Middle Jurassic - Late Jurassic) - Cretaceous (Early Cretaceous - Late Cretaceous) - Cenozoic Era - Paleogene (Paleocene - Eocene - Oligocene) - Neogene (Miocene - Pliocene) - Quaternary (Pleistocene - Holocene)
Fringe and Pseudoscience - Creationist perspectives on dinosaurs - Living dinosaurs
Popular Culture - Cultural depictions of dinosaurs - Jurassic Park (novel) - Jurassic Park (film) - Stegosaurus in popular culture -Tyrannosaurus in popular culture - Walking with...

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