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...)

Selected article on the prehistoric world and its legacies

Chitinozoa (singular: chitinozoan, plural: chitinozoans) are a taxon of flask-shaped, organic walled marine microfossils produced by an as yet unknown animal. Common from the Ordovician to Devonian periods (i.e. the mid-Paleozoic), the millimetre-scale organisms are abundant in almost all types of marine sediment across the globe. This wide distribution, and their rapid pace of evolution, makes them valuable biostratigraphic markers.

Their bizarre form has made classification and ecological reconstruction difficult. Since their discovery in 1931, suggestions of protist, plant, and fungalaffinities have all been entertained. The organisms have been better understood as improvements in microscopy facilitated the study of their fine structure, and there is mounting evidence to suggest that they represent either the eggs or juvenile stage of a marine animal.

The ecology of chitinozoa is also open to speculation; some may have floated in the water column, where others may have attached themselves to other organisms. Most species were particular about their living conditions, and tend to be most common in specific paleoenvironments. Their abundance also varied with the seasons.(see more...)

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

Selected article on paleontology in human science, culture and economics

The history of paleontology traces the history of the effort to study the fossil record left behind by ancient life forms. Although fossils had been studied by scholars since ancient times, the nature of fossils and their relationship to life in the past became better understood during the 17th and 18th centuries. At the end of the 18th century the work of Georges Cuvier ended a long running debate about the reality of extinction and led to the emergence of paleontology as a scientific discipline.

The first half of the 19th century saw paleontological activity become increasingly well organized. This contributed to a rapid increase in knowledge about the history of life on Earth, and progress towards definition of the geologic time scale. As knowledge of life's history continued to improve, it became increasingly obvious that there had been some kind of successive order to the development of life. After Charles Darwin published Origin of Species in 1859, much of the focus of paleontology shifted to understanding evolutionary paths.

The last half of the 19th century saw a tremendous expansion in paleontological activity, especially in North America. The trend continued in the 20th century with additional regions of the Earth being opened to systematic fossil collection, as demonstrated by a series of important discoveries in China near the end of the 20th century. There was also a renewed interest in the Cambrian explosion that saw the development of the body plans of most animal phyla. (see more...)

On this day...

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Fossil remains of various horse genera, showing the evolution of their skeletons, skulls and limb bones over time. The uppermost and most recent genus is that of the modern horse, Equus. Below that is Pliohippus, dating back to the late Miocene. Below that and older still is Merychippus of the middle Miocene. The bottom and oldest horse genus is Mesohippus from the late Eocene.
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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