Echinoid Fossil Peronella ricta Nanga Western Australia (EA9341) Shark bay

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Location: Mt Evelyn, Victoria
Ships to: US,
Item: 156501112829

Restocking fee:No
Return shipping will be paid by:Buyer
Returns Accepted:Returns Accepted
Item must be returned within:60 Days
Specimen size:6.0 x 5.1 x 1.1 cm
Geological Age:Middle Pleistocene 1.4 million years Old
Product Type:Fossils
Era:Unknown
Described by:Gregory in 1892
Region:Australia
Material:Fossil Echinoid
Formation Collected from ::Carbla Oolite, Gladstone Formation
Species:Peronella ricta
Location collected from:Near Nanga, Shark Bay, Western Australia. Australia

Peronella ricta is a species of echinoid that thrived during the Middle Pleistocene, approximately 1.4 million years ago. This particular specimen was discovered near Nanga, in the Shark Bay region of Western Australia, a locale known for its significant paleontological sites. The fossil was embedded within the Carbla Oolite, part of the Gladstone Formation, a geological layer that has yielded numerous marine fossils from this period. The environmental conditions during the Pleistocene would have supported a diverse marine ecosystem, providing a rich context for the life of Peronella ricta. The specimen measures 6.0 x 5.1 x 1.1 cm cm, making it a relatively delicate and compact example of its species. Despite its small size, the fossil is well-preserved, displaying the characteristic features of Peronella ricta. The fine details of the test, or external skeleton, such as the arrangement of the tubercles and the ambulacral areas, offer valuable information on the species’ morphology and the evolutionary adaptations that occurred in response to the Pleistocene marine environment. This level of preservation is crucial for paleontologists studying the biodiversity and ecological dynamics of ancient marine systems. Peronella ricta was first described by Gregory in 1892, and since then, it has played an important role in the understanding of Pleistocene echinoids. The study of such fossils allows scientists to reconstruct the past environments of Western Australia and to gain insights into the climatic changes that have shaped the region’s geological history. This specimen not only contributes to the broader understanding of Pleistocene marine life but also serves as a testament to the intricate and diverse nature of echinoid evolution.

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