1. Preserved appendages in a Silurian binodicope: implications for the evolutionary history of ostracod crustaceans.
- Author
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Siveter DJ, Briggs DEG, Siveter DJ, and Sutton MD
- Subjects
- Animals, Male, Extremities anatomy & histology, Animal Shells anatomy & histology, Crustacea anatomy & histology, Crustacea classification, Fossils anatomy & histology, Biological Evolution
- Abstract
Ostracod crustaceans originated at least 500 Ma ago. Their tiny bivalved shells represent the most species-abundant fossil arthropods, and ostracods are omnipresent in a wide array of freshwater and marine environments today and in the past. Derima paparme gen. et sp. nov. from the Herefordshire Silurian Lagerstätte (~430 Ma) in the Welsh Borderland, UK, is one of only a handful of exceptionally preserved ostracods (with soft parts as well as the shell) known from the Palaeozoic. A male specimen provides the first evidence of the appendages of Binodicopina, a major group of Palaeozoic ostracods comprising some 135 Ordovician to Permian genera. The appendage morphology of D. paparme , but not its shell, indicates that binodicopes belong to Podocopa. The discovery that the soft-part morphology of binodicopes allies them with podocopes affirms that using the shell alone is an unreliable basis for classifying certain fossil ostracods, and knowledge of soft-part morphology is critical for the task. Current assignment of many fossil ostracods to higher taxa, and therefore the evolutionary history of the group, may require reconsideration.
- Published
- 2024
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