Tetragraptus approximatus
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| Tetragraptus approximatus Temporal range: | |
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| Illustration of Tetragraptus approximatus | |
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| Original illustrations of Tetragraptus approximatus by Nicholson (1873). At the top is a magnified section of the stipes. A complete specimen is illustrated below. | |
Scientific classification  | |
| Kingdom: | Animalia |
| Phylum: | Hemichordata |
| Class: | Pterobranchia |
| Subclass: | Graptolithina |
| Order: | †Graptoloidea |
| Family: | †Tetragraptidae |
| Genus: | †Tetragraptus |
| Species: | †T. approximatus |
| Binomial name | |
| †Tetragraptus approximatus Nicholson, 1873 | |
Tetragraptus approximatus is a species of dichograptid graptolite belonging to the genus Tetragraptus. It existed during the Floian Age (477.1 million years ago) of the Ordovician. It is an important index fossil in biostratigraphy.
The general outline of each Tetragraptus approximatus colony (rhabdosome) is highly distinctive. It resembles a long narrow letter H or X. The central process (the funicle) is about 2.5 mm (0.098 in) long, each end bifurcating at right angles with each other. Each pair of branches (stipes) curve away sharply from the ends of the funicle then run more or less parallel with each other at a distance of 5 to 8 mm (0.20 to 0.31 in) apart. Each of the stipes can reach more than 45 mm (1.8 in) in length, with approximately ten cup-like structures (thecae) for every 10 mm (0.39 in) of the stipes. The thecae are tilted at a 45° angle to the axis.[1][2]
Taxonomy
Tetragraptus approximatus is classified under the genus Tetragraptus of the family Tetragraptidae.[3] It was first described by the British paleontologist Henry Alleyne Nicholson in 1873 from specimens recovered from Lévis, Quebec, Canada.[2]