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Trilobite

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Trilobites were a highly successful group of extinct marine arthropods. Their name, meaning "three-lobed entities," refers to the structure of their bodies. These animals belong to the class Trilobita. They are part of a larger group called Artiopoda. This group includes many organisms that look similar to trilobites. However, most other artiopodans were not mineralized. Trilobites were unique because they possessed a heavily mineralized exoskeleton. This hard outer shell was made of calcite.

BLW Trilobite (Paradoxides sp.)
BLW Trilobite (Paradoxides sp.)

The calcite exoskeleton is a major reason we know so much about them. Because calcite fossilizes easily, trilobites left an extensive fossil record. Scientists use these fossils to study many different fields. They contribute to biostratigraphy, which is the study of rock layers. They also help in paleontology, evolutionary biology, and the study of plate tectonics. The fossils allow us to see how life and the Earth changed together.

Fossil Prochuangia from the Cambrian period of Darnjal Formation, Tabas, Iran 02
Fossil Prochuangia from the Cambrian period of Darnjal Formation, Tabas, Iran 02

Trilobites occupied many different ecological niches in the ancient oceans. Some lived on the seabed as predators that hunted other animals. Others acted as scavengers, eating organic bits from the ocean floor. Some species were filter feeders. Other trilobites were capable of swimming to feed on plankton. Some even crawled onto land. Scientists even believe some families, like Olenidae, had symbiotic relationships with sulfur-eating bacteria. In these relationships, the bacteria provided food for the trilobites.

Sidneyia inexpectans
Sidneyia inexpectans

The evolutionary history of trilobites is marked by incredible diversity. They first appeared in the fossil record around 520 million years ago. These earliest known trilobites include groups called redlichiids and ptychopariid bigotinids. They appeared in places like Laurentia, Siberia, and West Gondwana. The group reached its apex of diversity during the late Cambrian and Ordovician periods. During the Ordovician, they were very successful at living in new environments, such as reefs.

Trilobite Ordovicien 8127
Trilobite Ordovicien 8127

Evolution caused trilobites to develop many different physical traits. Some species developed new types of eyes. Others improved their ability to enroll, which is a way of curling up for protection. They also developed different ways to connect their body segments, known as articulation. Some groups grew extreme spines for defense. Others experienced "effacement," which is the loss of surface detail on their shells. This loss of detail might indicate a burrowing or swimming lifestyle.

Trilobite Walliserops trifurcatus
Trilobite Walliserops trifurcatus

Trilobites faced many challenges from mass extinction events. Their diversity began to decline during the mid-to-late Devonian period. They were impacted by the Taghanic event and the Kellwasser event. The Hangenberg event, or the end-Devonian mass extinction, also wiped out most of their diversity. After these events, only one order, Proetida, survived. Diversity recovered slightly during the Early Carboniferous. However, numbers dropped again during the late Carboniferous and Permian periods.

Trilobite diversity EN (cropped)
Trilobite diversity EN (cropped)

The end of the trilobite era came during the end-Permian mass extinction. This event occurred about 251.9 million years ago. By this time, only a handful of species remained. The last trilobites disappeared completely during this period. Despite their extinction, their long existence of almost 270 million years makes them one of the most successful animal groups in Earth's history.

Worlds largest trilobite
Worlds largest trilobite
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