Belinuropsis

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Belinuropsis
Temporal range: Carboniferous
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Scientific classification
Kingdom:
Phylum:
Genus:
Belinuropsis

Matthew, 1910
Type species
Belinuropsis wigudensis
Matthew, 1910

Belinuropsis is a dubious genus of prehistoric arthropod which contains one species, B. wigudensis, from the Silurian period of New Brunswick, Canada. Matthew tried to describe Belinuropsis originally as a species of Belinurus . Two specimens that match the Matthew's illustration of B. wigudensis have been located in the New Brunswick Museum paleontology collection and assigned catalogue numbers NBMG 3307 and NBMG 3308 (Miller, 1988). Examination of the specimens casts doubt on validity of the genus erected by Matthew. The material is poorly preserved and difficult to interpret, so, after examinations of the specimens, Belinuropsis has been considered as nomen dubium . [1]

A genus is a taxonomic rank used in the biological classification of living and fossil organisms, as well as viruses, in biology. In the hierarchy of biological classification, genus comes above species and below family. In binomial nomenclature, the genus name forms the first part of the binomial species name for each species within the genus.

Arthropod Phylum of invertebrates

An arthropod is an invertebrate animal having an exoskeleton, a segmented body, and paired jointed appendages. Arthropods form the phylum Euarthropoda, which includes insects, arachnids, myriapods, and crustaceans. The term Arthropoda as originally proposed refers to a proposed grouping of Euarthropods and the phylum Onychophora. Arthropods are characterized by their jointed limbs and cuticle made of chitin, often mineralised with calcium carbonate. The arthropod body plan consists of segments, each with a pair of appendages. The rigid cuticle inhibits growth, so arthropods replace it periodically by moulting. Arthopods are bilaterally symmetrical and their body possesses an external skeleton. Some species have wings.

The Silurian is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at 443.8 million years ago (Mya), to the beginning of the Devonian Period, 419.2 Mya. The Silurian is the shortest period of the Paleozoic Era. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by several million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera were wiped out.

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References

  1. Miller, Randall F. (1995-08-01). "The status of Belinuropsis wigudensis Matthew, 1910, a Pennsylvanian merostome from New Brunswick, Canada". Atlantic Geology. 31 (2). ISSN   1718-7885.