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Paleontology and Fossils

Paleontology is the scientific study of life that existed before the start of recorded history, based on the fossil record. A fossil is the preserved remains, impression, or trace of a once-living organism. Most fossils form when an organism is buried in sediment soon after death and its hard parts — shells, bones, teeth, or woody tissue — are gradually replaced or infilled by minerals over long periods. Soft tissues rarely survive, so the record is biased toward organisms with durable skeletons.

Fossils are commonly divided into body fossils and trace fossils. Body fossils preserve part of the organism itself, while trace fossils, or ichnofossils, record activity such as burrows, tracks, and footprints. Among invertebrates, ammonites and trilobites are widely studied because they are abundant, distinctive, and changed quickly through time, making them useful for dating rock layers. Crinoids, brachiopods, and corals are other common marine fossils. Insects such as beetles (Coleoptera) and flies (Diptera) are sometimes preserved in amber, hardened tree resin that can trap small organisms in fine detail.

Because layered sedimentary rocks form in sequence, fossils help geologists correlate strata and reconstruct ancient environments. Fossils of plants, marine animals, and land vertebrates indicate past climates, sea levels, and the positions of continents. Paleomaps, which show how landmasses were arranged in earlier geological periods, draw on this evidence together with the study of plate movement.

Frequently asked questions

What is the difference between a body fossil and a trace fossil?
A body fossil preserves part of the organism, such as a bone or shell. A trace fossil records behavior, such as a footprint, burrow, or track.
Why are trilobites and ammonites useful to geologists?
They were widespread, evolved rapidly, and have recognizable forms, so particular species occur in narrow time ranges and help date the rock layers that contain them.
How are insects preserved in amber?
Sticky tree resin can trap small organisms, then harden and fossilize over millions of years, sometimes preserving fine anatomical detail.




Paleontology and fossiles: General overview, Fossils

Amber  see also Dinosaur fossils
Amber Baltic amber, insects, fossils spider, acarina, fossils insects, rav, harpaks, retinite, succinite, kohaku, glessum, fung chi, fossil resin, fuling, fehg, bernstein, elektron, ambra, ambre, agdsten, inclusions, palaeoentomology, fossil fishes, ammonites, trilobites, brachiopods, mollusks, echinoderm, belemnites, sponge, shark teeth, corals, bivalvia, gastropoda, shells, paleontology
Amber web site dedicated to amber fossil resin and copal. Its paleontological significance is explored in detail. There are numerous original photographs of amber and inclusions with sections on its formation and role in human history, a tip
Amber neotropical amber
Amber
Amber amber is a semi-precious gem formed out of the fossilized resin of ancient trees. Age varies from 20 million years up to 245 million years. Dominican amber ranges from 25-40 millions years (tertiary period)
Amber gallery
Amber photos part of Fossils
Amber: window to the past
Amberized fossil leaf amber is the fossilized resin of ancient trees and often, along with insects, plant material is trapped by dripping resin and thereby preserved intact over millenia by the gradual process of amberization
Blue Amber The purpose of this site is to act as an information portal for Dominican Blue Amber. Amber is supposed to be amber color, right? Wrong. There is the original color of amber, yellow, orange, honey, cognac or the kind. But there also is cream, cherry, red, green and even blue as the rarest of all
Fossils  see also Dinosaur fossils
British chalk fossils chalks are found the world over in rock successions dating from the Late Cretaceous (98-65 million years ago). They record a period of extreme warming and unusually high sea-levels, when much of the world's  continental platforms were flooded by marine water
Crinoids Crinoids explained
Crinoids a tip
Detrich fossil company photos of spectacular fossil discoveries and details of global expeditions
Dinosaur tracking fossilized dinosaur tracks are forms of trace fossils, also known as ichnites or ichnofossils. Unlike body fossils, which are the remains of dead bodies, trace fossils record the active movements and behaviors of ancient organisms
Echinodermata
Echinologia en Français
Eocene and Oligocene Fossils A Collection of Eocene and Oligocene Fossils
Eocene fossils
Introduction to ichnology ichnology: study of plant and animal traces
Jurassic ammonites and fossil brachiopoda
Fossiele planten in Dutch
Fossielen in België
Fossil hominids to provide an overview of the study of human evolution, and of the currently accepted fossil evidence
Fossils of the Gault clay dedicated to the fossils of the lower cretaceous Albian (Gault Clay and Folkestone Beds) in the county of Kent, south-east England
Fossils, rocks, and time the diversity and evolution of life on Earth through the last 600 million years
Fossil sharks from Transylvania
Fossil shark teeth
Ginkgo a living fossil The genus Ginkgo is one of the major groups in the phylum Ginkgophytes. Fossils of Ginkgo are recognized by its leaves, reproductive organs and wood. Its leaf remains are the most often found, ...
Miocene fossils Miocene fossils
Photographs and descriptions of fossils
Pictures of fossils
Plant fossils of West Virginia
Shark teeth
Shark teeth
Shark teeth dedicated to the fossil sharks and rays from the Cretaceous of the Netherlands. Objective is to give a brief overview of the most common species which can be found in the cretaceous sediments of the SE part of The Netherlands and the adjoining area in Belgium
Sheppey Fossils
Stromatolite fossils in the Hakatai shale
Invertebrates  see also Dinosaur fossils
Brachiopoda
Bryozoa: fossil record
Crinoid education project
Hidden world of the conodonta the Conodonta are an extinct phylum (Sweet, 1988) of small, bilaterally symmetrical vermiform (worm-like) animals
Neogene marine invertebrates an online biotic database containing images and data for taxa used in analyses of Tropical American biodiversity over the past 25 million years
Orders of trilobites Orders of trilobites
Ordovician conodonts Conodonts in Vertebrate Evolution, Conodont Element Types, Species Identified, Scolocodonts, What are Conodonts?
The semi compleat trilobite presentation of trilobite images
Trilobite Trilobites are hard shelled, segmented creatures that existed over 300 million years ago
Trilobite gallery trilobites are an extinct group of marine arthropods which existed during the Paleozoic era, from the Cambrian to the Permian period about 540-245 million years ago
Trilobites Trilobites are ancient arthropods that lived in the oceans of the world during the Paleozoic Era (545-253 MYA). Today, trilobites are found throughout the world, with representatives on every continent

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