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Invertebrates

Early animals, arthropods, molluscs, corals and other invertebrate life.

Why are extinct invertebrates central to Earth history?

Invertebrates dominate much of the fossil record and reveal early animal body plans, reefs, oceans and repeated mass-extinction recoveries.

How did this history unfold?

Ediacaran communities precede the Cambrian radiation; later trilobites, molluscs, corals and echinoderms track more than half a billion years of change.

What changed these ecosystems?

Ocean chemistry, oxygen, sea level and mass extinctions repeatedly reorganised marine communities.

Three routes into this topic

Early animals

Ediacaran and Cambrian fossils test how major body plans emerged.

Shells and reefs

Biomineralisation changed predation, habitats and preservation.

Mass extinctions

Invertebrate ranges and abundance make global turnovers measurable.

How do scientists reconstruct this history?

Mineral shells fossilise readily, while exceptional deposits preserve soft tissues that expose anatomy otherwise missing from the record.

Frequently asked questions

Why are extinct invertebrates central to Earth history?

Invertebrates dominate much of the fossil record and reveal early animal body plans, reefs, oceans and repeated mass-extinction recoveries.

How is the fossil record of this group preserved?

Mineral shells fossilise readily, while exceptional deposits preserve soft tissues that expose anatomy otherwise missing from the record.

Why did this group change or disappear?

Ocean chemistry, oxygen, sea level and mass extinctions repeatedly reorganised marine communities.

Check the topic overview

UC Museum of Paleontology · Invertebrates Smithsonian · Ocean fossils
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