Trilobite

Trilobita Diversity

BLW Trilobite (Paradoxides sp.)

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

Scutelluid trilobite

Trilobite Walliserops trifurcatus

Cambrian Trilobite Olenoides Mt. Stephen

Trilobites are an extinct group of marine arthropods that belong to the class Trilobita. They appeared in the Cambrian period about 521 million years ago and flourished throughout the lower Paleozoic era before beginning a drawn-out decline to extinction when the last of the trilobites disappeared in the mass extinction at the end of the Permian period, about 252 million years ago. The trilobites were among the most successful of all early animals, roaming the oceans for over 270 million years.

Morphology

Trilobites are easily recognized by their distinctive three-lobed, three-segmented form. Their bodies are divided into three sections: the cephalon (head), the thorax (body), and the pygidium (tail). The name "trilobite" (meaning "three lobes") is derived from the longitudinal division of the body into these three sections. Trilobites vary in size from a few millimeters to over 70 centimeters in length.

Ecology

Trilobites were benthic creatures, living primarily on the sea floor. Some were scavengers, while others were predators. Their diets likely included small microorganisms and detritus. Trilobites had a wide range of adaptations, including spines and enrollment capabilities, which may have been used for defense against predators.

Classification

Trilobites are divided into several orders and families, reflecting a wide diversity of forms. Some of the major orders include Redlichiida, Ptychopariida, Phacopida, and Proetida. These classifications are based on differences in the cephalon, thorax, and pygidium, as well as other morphological features.

Fossil Record

Trilobites are known primarily through their well-preserved fossils, which have been found on every continent. The fossil record of trilobites includes not only their calcified exoskeletons but also rare instances of soft-body preservation. Trilobite fossils are highly sought after by collectors and are used by scientists to understand more about the Paleozoic marine environments.

Extinction

The decline and eventual extinction of trilobites at the end of the Permian period were likely caused by a combination of environmental changes, including drastic changes in sea level, temperature, and chemistry of the oceans. The end-Permian mass extinction was the largest extinction event in Earth's history, affecting many marine communities.

Legacy

Today, trilobites are of great interest to paleontologists, not only for their intrinsic scientific value but also for their use in biostratigraphy, where they help to date the rock layers in which they are found. Their diverse and well-preserved fossils make them important indicators of the evolutionary history of life on Earth.

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