Acritarchs are tiny, ancient fossils made from organic material. They have been found from very early times, called the Archean eon of the Precambrian, right up to today. The name "acritarch" comes from Greek words meaning "uncertain origin" because these fossils don't fit neatly into other groups. Scientists use the term to describe any small, organic fossils that they can't classify more specifically.
These fossils are important because they show us big changes in the world's ecosystems. For example, the different kinds of acritarchs that appear over time tell us about events like the rise of predators and a big burst of new life called the Cambrian explosion. Many acritarchs are thought to be resting cysts from single-celled marine algae, similar to cysts made today by dinoflagellates. Studying acritarchs helps us understand how life in the oceans has changed over millions of years.
Definition
Acritarchs are tiny, ancient fossils made from organic material that do not dissolve in acid. They have a central space inside and come from many different kinds of tiny sea creatures, such as the egg cases of small animals or resting stages of green algae. Scientists often find them in rocks from long ago, especially from the time before complex animals appeared on Earth.
Even though we do not always know exactly which living things made them, scientists group acritarchs based on their shape. These groups show patterns that match big changes in Earth's history, like the sudden appearance of many new sea creatures during the Cambrian period.
Classification
The group Acritarcha was originally divided into several subgroups, including Acanthomorphitae and Polygonomorphitae, among others.
Scientists believe acritarchs were likely eukaryotes, meaning they had complex cells, unlike simpler bacteria. Some studies show that acritarchs might actually be fossilized microalgae, tiny plants that lived long ago. These fossils often have special features like spines and hairs, which help scientists study their history.
Occurrence
Acritarchs are tiny fossils found in rocks from long ago, all the way back to the Archean. Scientists often find them in certain types of rocks and use them to help figure out how old other rocks are, especially from the Paleozoic Era. Many acritarchs likely came from the ocean.
The oldest known acritarchs that might be from complex cells, called eukaryotes, are from between 1950 and 2150 million years ago. These tiny fossils give us clues about life on Earth in very old times.
Diversity
Around 1 billion years ago, acritarchs became more common, larger, and more complex in shape, especially growing more spines. Their numbers dropped during big ice ages but grew again during the Cambrian explosion, reaching their peak variety in the Paleozoic. The increase in spines about 1,000 million years ago may have been a way to defend against predators.
Evidence suggests that acritarchs faced herbivores around this time. Between 1,700 and 1,400 million years ago, the number of plankton species was limited by nutrients. But about 1,000 million years ago, species longevity dropped, indicating that predation by protist herbivores became important. This pressure may have allowed new species to develop by leaving some nutrients unused.
Etymology
The term Acritarch was created in 1963 using words from ancient Greek. It combines ákritos, which means "confused" or "uncertain," and archē, which means "origin." This name reflects how these tiny fossils were puzzling when they were first discovered.
Selected genera
There are over 900 known types of acritarchs. Acritarchs are tiny, ancient fossils that help scientists understand very old Earth history. This is a small list of some of these types, showing the time periods when they were found:
- Acanthodiacrodium (Ordovician)
- Acrosphaeridium (Ordovician)
- Actipillion (Ordovician)
- Akomachra (Ordovician)
- Ammonidium (Silurian)
- Aranidium (Cambrian)
- Arbusculidium (Cambrian-Ordovician)
- Archaeodiscina (Cambrian)
- Arcosphaeridium (Ordovician)
- Aremoricanium (Ordovician)
- Arkonia (Ordovician)
- Asteridium (Cambrian)
- Athabascaella (Tremadocian, Early Ordovician)
- Axisphaeridium (Ordovician)
- Bacisphaeridium (Ordovician)
- Baltisphaeridium (Cambrian-Silurian)
- Buedingiisphaeridium (Ordovician)
- Caldariola (Cambrian)
- Calyxiella
- Celtiberium
- Cephalonyx
- Ceratophyton (Cambrian)
- Cheleutochroa (Ordovician)
- Chlamydosphaeridia (Ordovician)
- Comasphaeridium (Ordovician)
- Coronitesta (Ordovician)
- Coryphidium (Ordovician)
- Costatilobus (Ordovician)
- Cristallinium (Cambrian)
- Cycloposphaeridium (Ordovician)
- Cymatiogalea (Cambrian)
- Cymatiosphaera (Cambrian-Ordovician)
- Dactylofusa (Ordovician)
- Dasydiacrodium (Cambrian)
- Dicommopalla (Ordovician)
- Dictyosphaera (Statherian-Paleozoic)
- Dictyosphaeridium (Ordovician)
- Diexallophasis (Silurian)
- Dilatisphaera (Ordovician)
- Domasia (Ordovician-Silurian)
- Dongyesphaera (Paleozoic)
- Elektroriskos (Cambrian)
- Elenia
- Eliasum
- Estiastra (Ordovician)
- Excultibrachium (Ordovician)
- Fimbriaglomerella
- Florisphaeridium (Ordovician)
- Globosphaeridium (Cambrian)
- Goniosphaeridium (Cambrian-Ordovician)
- Gorgonisphaeridium (Ordovician)
- Granomarginata (Cambrian)
- Gyalorhethium (Ordovician)
- Hapsidopalla (Ordovician)
- Helosphaeridium (Ordovician)
- Impluviculus (Cambrian)
- Introvertocystis (Late Cretaceous)
- Izhoria
- Joehvisphaera (Ordovician)
- Korilophyton (Cambrian)
- Kundasphaera (Ordovician)
- Labyrinthosphaeridium (Ordovician)
- Lacunosphaeridium (Ordovician)
- Ladogella
- Leiofusa (Cambrian-Silurian)
- Leiosphaeridia (Statherian-Present)
- Leiovalia (Ordovician)
- Liepaina (Cambrian)
- Liliosphaeridium (Ordovician)
- Lophosphaeridium (Ordovician-Silurian)
- Lunulidia
- Micrhystridium (Ordovician-Silurian)
- Multiplicisphaeridium (Cambrian-Silurian)
- Nanocyclopia (Ordovician)
- Nodosus
- Oppilatala (Silurian)
- Ordovicidium (Ordovician)
- Orthosphaeridium (Ordovician)
- Ovulum (Cambrian)
- Palaeocladophora (Cambrian)
- Palaeomonostroma (Cambrian)
- Peteinosphaeridium (Ordovician)
- Pheoclosterium (Ordovician)
- Pirea (Cambrian)
- Poikilofusa
- Polyancistrodorus (Ordovician)
- Polyedryxium (Ordovician)
- Polygonium (Cambrian-Ordovician)
- Portalites (Permian)
- Priscogaleata (Ordovician)
- Priscotheca
- Protosphaeridium (Silurian)
- Pterospermella
- Pterospermopsis (Ordovician)
- Pulvinosphaeridium (Ordovician)
- Quadrisporites (Permian)
- Raplasphaera (Ordovician)
- Revinotesta (Ordovician)
- Rhopaliophora (Ordovician)
- Saharidia (Ordovician)
- Salopidium (Silurian)
- Satka (Paleozoic)
- Shuiyousphaeridium (Orosirian-Ediacaran)
- Skiagia (Cambrian)
- Solisphaeridium (Ordovician)
- Stellechinatum (Ordovician)
- Stelliferidium (Cambrian)
- Taeniosphaeridium (Ordovician)
- Tasmanites (Ordovician-Silurian)
- Tetraporina (Permian)
- Timofeevia (Cambrian-Ordovician)
- Tranvikium (Ordovician)
- Trichosphaeridium
- Tunisphaeridium (Ordovician-Silurian)
- Tylotopalla (Ordovician)
- Vernanimalcula (Ediacaran)
- Veryhachium (Cambrian-Silurian)
- Villosacapsula (Ordovician)
- Visbysphaera (Silurian)
- Volkovia
- Vulcanisphaera (Cambrian-Ordovician)
- Winwaloeusia (Ordovician)
This article is a child-friendly adaptation of the Wikipedia article on Acritarch, available under CC BY-SA 4.0.
Images from Wikimedia Commons. Tap any image to view credits and license.
Safekipedia