Annamitella liexiensis Trilobite Pair

Travel back approximately 480 million years with this remarkable pair of Annamitella liexiensis trilobite fossils from the Early Ordovician Period. Discovered in Hunan Province, China, these fascinating specimens offer a glimpse into the ancient marine environments that existed long before dinosaurs appeared on Earth.

Annamitella liexiensis is a species of trilobite known for its distinctive segmented exoskeleton, broad head shield, and elongated body shape. Like other trilobites, these prehistoric marine arthropods possessed a hard outer shell that provided protection as they moved along the ancient seafloor. Trilobites were among the most successful groups of early marine animals, surviving for nearly 270 million years before becoming extinct approximately 252 million years ago.

This impressive fossil plate features two Annamitella liexiensis trilobites preserved together on a single natural stone matrix. The larger specimen measures approximately 3 inches, while the smaller measures approximately 1.75 inches. Both fossils display distinctive head shields, clearly defined thoracic segments, and rounded tail sections. Their deep black coloration contrasts subtly with the dark charcoal-gray matrix, highlighting the intricate details of their ancient exoskeletons. The naturally shaped stone features fine mineral veins and surface textures that add character to this unique display piece.

Featuring two trilobites of different sizes on a substantial matrix, this fascinating fossil plate makes an excellent addition to any trilobite collection or natural history display.

Specimen Details

Species: Annamitella liexiensis
Geological Period: Early Ordovician
Approximate Age: 486–477 million years
Formation: Nantsinkwan Formation
Locality: Yongshun County, Hunan Province, China
Number of Trilobites: 2
Trilobite Sizes: Approximately 3 inches and 1.75 inches
Matrix Size: Approximately 10 x 7.5 inches
Certificate of Authenticity: Included

You will receive the exact specimen pictured.

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