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2.1" Fossil Phyllocarid (Dithyrocaris) - Bear Gulch Limestone, Montana
This is a beautiful fossil phyllocarid of the species Dithyrocaris rolfei that was collected from the Bear Gulch limestone of Fergus County, Montana. The crustacean itself is 2.1" long and preserved with excellent detail. The base of the limestone has been cut flat.
It comes with an acrylic display stand.
It comes with an acrylic display stand.
About Phyllocarids
Phyllocarids are an extinct group of marine arthropods that thrived from the Cambrian to the Devonian period, with some surviving into the Carboniferous. They belong to the subclass Phyllocarida within the class Malacostraca, which includes modern crustaceans like lobsters, shrimp, and crabs. Phyllocarids are characterized by their unique body structure, which includes a bivalve-like carapace that covered the head and thorax, giving them a shrimp-like appearance. This carapace is often smooth but can exhibit ridges or spines, depending on the species.
Their segmented abdomen extends beyond the carapace, ending in a fan-like tail structure called a telson, which is flanked by smaller appendages known as uropods. The carapace helped protect their front limbs, which they used for feeding, while their back limbs were likely adapted for swimming and maneuvering in the water. They are thought to have been filter feeders, scraping detritus or small particles of food from the water column.
Fossils of phyllocarids are relatively rare, but they provide valuable insights into the evolution of crustaceans and other arthropods. Their remains are often found in marine sediments, especially in locations where fine-grained rock has preserved their delicate structures.
Phyllocarids are an extinct group of marine arthropods that thrived from the Cambrian to the Devonian period, with some surviving into the Carboniferous. They belong to the subclass Phyllocarida within the class Malacostraca, which includes modern crustaceans like lobsters, shrimp, and crabs. Phyllocarids are characterized by their unique body structure, which includes a bivalve-like carapace that covered the head and thorax, giving them a shrimp-like appearance. This carapace is often smooth but can exhibit ridges or spines, depending on the species.
Their segmented abdomen extends beyond the carapace, ending in a fan-like tail structure called a telson, which is flanked by smaller appendages known as uropods. The carapace helped protect their front limbs, which they used for feeding, while their back limbs were likely adapted for swimming and maneuvering in the water. They are thought to have been filter feeders, scraping detritus or small particles of food from the water column.
Fossils of phyllocarids are relatively rare, but they provide valuable insights into the evolution of crustaceans and other arthropods. Their remains are often found in marine sediments, especially in locations where fine-grained rock has preserved their delicate structures.
SPECIES
Dithyrocaris rolfei
LOCATION
Fergus County, Montana
FORMATION
Bear Gulch Limestone - Heath Shale Formation
SIZE
2.1” long phyllocarid on a 5 x 4.6" rock
CATEGORY
ITEM
#113196
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