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Stromatolite

Adapted from Wikipedia · Adventurer experience

A close-up of stromatolites, layered structures formed by ancient microorganisms, on Highborne Cay in the Bahamas.

Stromatolites, also known as stromatoliths, are special layered rocks made by tiny living things called microorganisms. These tiny organisms, especially a type called cyanobacteria, live in water and use sunlight to make their own food. As they grow, they create sticky material that holds together sand and tiny particles, forming layers that build up over time.

Fossilized stromatolite in Strelley Pool chert, about 3.4 billion years old, from Pilbara Craton, Western Australia

Because of this way of growing, layer by layer, stromatolites have a very clear pattern called lamination. Scientists look at these patterns to learn about the conditions when the stromatolites were formed and to understand very old environments on Earth. Some stromatolites can grow quite big, reaching a meter or more in height.

Fossilized stromatolites are some of the oldest proof of life on our planet. They help scientists learn about the early world and the first living things. Today, living stromatolites are rare, found only in a few special places, but they are still important for understanding both the past and present of life on Earth.

Definition

Paleoproterozoic oncoids from the Franceville Basin, Gabon, Central Africa. Oncoids are unfixed stromatolites ranging in size from a few millimeters to a few centimeters

Stromatolites are layered structures made in shallow water by tiny living things, especially cyanobacteria. These living things make sticky substances that catch and hold bits of sand and other materials, creating layers over time.

The layers in stromatolites make them different from thrombolites, which have a clotted, non-layered texture. Sometimes people confuse "stromatolite" with "strombolite," but they are quite different.

Ancient stromatolites

Fossilized stromatolites, about 425 million years old, in the Soeginina Beds (Paadla Formation, Ludlow, Silurian) near Kübassaare, Estonia

Fossilized stromatolites come in many shapes, such as cone-like, flat, dome-shaped, column-shaped, and branching forms. They are very common in very old rocks from the Precambrian but are rare today. Scientists study them to learn about life on Earth long ago.

Stromatolites are important because they may be some of the earliest signs of life. They were most common about 1.25 billion years ago but became less common as other animals evolved. Stromatolites helped change Earth’s atmosphere by adding oxygen, which made it possible for more complex life to develop.

Modern occurrence

Stromatolites at Lake Thetis, Western Australia

Stromatolites are made by tiny, simple life forms called cyanobacteria and other bacteria. They build layers of rock. These tiny life forms live in places where few animals can survive, like very salty water or places without much light. They stick together and build up layers over time, creating structures we can see today.

You can find modern stromatolites in many parts of the world. One famous spot is Shark Bay in Western Australia, where scientists found a special kind of chlorophyll in these rocks. Other places include Brazil, Chile, and even lakes in Canada. These structures help scientists learn how life might exist on other planets.

Images

Ancient rock structures called stromatolites growing in the ocean off the coast of Western Australia.
Ancient layered rocks formed by tiny ocean microbes, found in New York state.
Ancient layered rocks formed by tiny sea microbes in Canada.
A natural stromatolite formation found in Nettle Cave, Jenolan Caves, Australia. Stromatolites are layered structures created by ancient microorganisms.
Ancient layered rocks formed by tiny sea creatures over a billion years ago in Glacier National Park.
Natural rock formations called microbialite towers growing in Pavilion Lake, showing layers built by tiny organisms over time.

This article is a child-friendly adaptation of the Wikipedia article on Stromatolite, available under CC BY-SA 4.0.

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