Deep-time library

Browse Fossils by Geologic Age

Connect fossil groups to the periods, environments, and formations in which they occur.

Time narrows the possibilities.

A claimed taxon must fit both the anatomy and the age of the rock. Use these pages as orientation, then consult formation-specific and taxonomic references.

Geologic period

Precambrian Fossils

Before 539 million years ago — Microbial mats, stromatolites, microfossils, and late Precambrian soft-bodied organisms dominate a record that requires exceptional contextual evidence.

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Geologic period

Ediacaran Period Fossils

635–539 million years ago — Soft-bodied organisms, microbial structures, and trace fossils mark a major transition before the Cambrian diversification.

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Geologic period

Cambrian Fossils

539–485 million years ago — Early animal diversification produced trilobites, brachiopods, archaeocyaths, sponges, and unusual soft-bodied assemblages.

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Geologic period

Ordovician Fossils

485–444 million years ago — Marine diversification filled seas with trilobites, brachiopods, bryozoans, crinoids, nautiloids, graptolites, and early vertebrates.

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Geologic period

Silurian Fossils

444–419 million years ago — Reefs expanded, jawed fishes diversified, and terrestrial ecosystems began leaving clearer evidence.

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Geologic period

Devonian Fossils

419–359 million years ago — Often called the Age of Fishes, with placoderms, sharks, ammonoids, corals, trilobites, and early forests.

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Geologic period

Carboniferous Fossils

359–299 million years ago — Coal forests, giant arthropods, crinoid-rich seas, amphibians, and early reptiles characterize many collections.

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Geologic period

Permian Fossils

299–252 million years ago — Synapsids, reptiles, diverse marine invertebrates, and seed plants precede the largest known mass extinction.

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Geologic period

Triassic Fossils

252–201 million years ago — Early dinosaurs, marine reptiles, ammonoids, conifers, and recovering marine communities followed the end-Permian extinction.

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Geologic period

Jurassic Fossils

201–145 million years ago — Ammonites, marine reptiles, dinosaurs, fish, plants, and fine-grained conservation deposits define classic collecting material.

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Geologic period

Cretaceous Fossils

145–66 million years ago — Flowering plants spread while dinosaurs, marine reptiles, ammonites, sharks, fish, and diverse invertebrates flourished.

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Geologic period

Paleogene Fossils

66–23 million years ago — Mammals, birds, sharks, fish, insects, and flowering plants diversified after the end-Cretaceous extinction.

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Geologic period

Neogene Fossils

23–2.58 million years ago — Modern-looking mammal and marine communities include horses, proboscideans, whales, sharks, and abundant mollusks.

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Geologic period

Pleistocene Fossils

2.58 million–11,700 years ago — Ice Age mammals, birds, shells, and plants overlap with human history and frequently require careful age and legal assessment.

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Geologic period

Quaternary Fossils

2.58 million years ago–present — The youngest geologic period includes Pleistocene fossils and Holocene subfossil material, where “fossil” versus recent can be difficult to establish.

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