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Reduviasporonites, the Glossary

Index Reduviasporonites

Reduviasporonites or Tympanicysta are palynomorphs — microfossils which appear to be fungal or algal cells or spores.[1]

Table of Contents

  1. 6 relations: Algae, Flowerpot Formation, Microfossil, Palynology, Penicillium, Permian–Triassic extinction event.

  2. Fossil taxa described in 1962

Algae

Algae (alga) are any of a large and diverse group of photosynthetic, eukaryotic organisms.

See Reduviasporonites and Algae

Flowerpot Formation

The Flowerpot Formation is a geologic formation in Oklahoma.

See Reduviasporonites and Flowerpot Formation

Microfossil

A microfossil is a fossil that is generally between 0.001 mm and 1 mm in size, the visual study of which requires the use of light or electron microscopy.

See Reduviasporonites and Microfossil

Palynology

Palynology is the study of microorganisms and microscopic fragments of mega-organisms that are composed of acid-resistant organic material and occur in sediments, sedimentary rocks, and even some metasedimentary rocks.

See Reduviasporonites and Palynology

Penicillium

Penicillium is a genus of ascomycetous fungi that is part of the mycobiome of many species and is of major importance in the natural environment, in food spoilage, and in food and drug production.

See Reduviasporonites and Penicillium

Permian–Triassic extinction event

Approximately 251.9 million years ago, the Permian–Triassic (P–T, P–Tr) extinction event (PTME; also known as the Late Permian extinction event, the Latest Permian extinction event, the End-Permian extinction event, and colloquially as the Great Dying) forms the boundary between the Permian and Triassic geologic periods, and with them the Paleozoic and Mesozoic eras.

See Reduviasporonites and Permian–Triassic extinction event

See also

Fossil taxa described in 1962

References

[1] https://en.wikipedia.org/wiki/Reduviasporonites

Also known as Tympanicysta.