Acritarch

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Acritarchs are small organic fossils, present from approximately 3,200 million years ago to the present. Their diversity reflects major ecological events such as the appearance of predation and the Cambrian explosion.

Contents

Definition

In general, any small, non-acid soluble (i.e. non-carbonate, non-siliceous) organic structure that can not otherwise be accounted for is classified as an acritarch.

Acritarchs include the remains of a wide range of quite different kinds of organisms - ranging from the egg cases of small metazoans to resting cysts of many different kinds of chlorophyta (green algae). It is likely that some acritarch species represent the resting stages (cysts) of algae that were ancestral to the dinoflagellates. The nature of the organisms associated with older acritarchs is generally not clear, though many are probably related to unicellular marine algae. In theory, when the biological source (taxon) of an acritarch does become known, that particular microfossil is removed from the acritarchs and classified with its proper group.

While the classification of acritarchs into form genera is entirely artificial, it is not without merit, as the form taxa show traits similar to those of genuine taxa - for example an 'explosion' in the Cambrian and a mass extinction at the end of the Permian.

Affinity

Acritarchs may represent the remains of any of the three domains of life, the archaea, the bacteria, and the eukaryotes. Archaea and bacteria usually produce fossils of a very small size, although the sheaths of some bacteria can reach the millimetre scale. Eukaryotes can sometimes be identified by complex traits such as ornamentation or projections, although simple eukaryote acritarchs also exist.[1]

Occurrence

Acritarchs are found in sedimentary rocks from the present back into the Archean.[2] They are typically isolated from siliciclastic sedimentary rocks using hydrofluoric acid but are occasionally extracted from carbonate-rich rocks. They are excellent candidates for index fossils used for dating rock formations in the Paleozoic Era and when other fossils are not available. Because most acritarchs are thought to be marine, they are also useful for palaeoenvironmental interpretation.

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