Buenellus

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Buenellus higginsi
Temporal range: Atdabanian
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Buenellus.jpg
Buenellus higginsi fossils at the Geological Museum, Copenhagen
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Arthropoda
Class: Trilobita
Order: Redlichiida
Family: Nevadiidae
Genus: Buenellus
Blaker, 1988
Species:
B. higginsi
Binomial name
Buenellus higginsi
Blaker, 1988

Buenellus higginsi is an average size (about 5 centimetres or 2.0 inches) trilobite, which lived during the Lower Cambrian period, in what is now North-West Greenland. It is a prominent member of the Sirius Passet fauna. Buenellus higginsi is the only known species in the genus Buenellus (i.e., the genus is monotypic).

Contents

Etymology

The genus name is a contraction of Buen, from the formation in which it was first collected, and Olenellus , a somewhat related trilobite genus. The species specific epithet honors A. Higgins, who discovered the Sirius Passet Lagerstätte in 1984 during the Geological Survey of Greenland.

Description

The general outline of the body is rounded n the front third, parallel sided in the middle third, and progressively tapering backwards in the back third, ending at an angle of approximately 45° with the midline. The headshield (or cephalon is approximately 58× as long as it is wide. The (in this case only slightly) vaulted central axis of the head or glabella tapers gently forward and does not reach the anterior margin. The outer backside of the cephalon (or genal angle) has short genal spines. The thorax has 17 or 18 articulating segments, maintaining width or widening slightly backwards up to the 8th segment, then tapering posteriorly. The posterior segment may be fused with the anterior part of a simple and small pygidium. Pleural spines are short, and the pleural regions are only slightly wider than the axis. [1] [2]

Differences with other Nevadiidae

The general shape of the body of other species in the Nevadid family (like Nevadia and Nevadella ) is shorter, with the greatest width across the back of the cephalon, and the entire thorax tapering backwards.

Distribution

Buenellus higginsi has been collected from early to middle Atdabanian deposits at the lower Buen Formation (“Nevadella” Zone), Sirius Passet lagerstätte at its junction with the J. P. Koch Fjord, Peary Land, Greenland 82°47.6′N42°13.7′W / 82.7933°N 42.2283°W / 82.7933; -42.2283 . It has also been reported from Novaya Zemlya, Russian Republic.

Ecology

Mineral-filled gut tracts in B. higginsi suggest they were not filled with sediment at the time of burial, and that the species was a predator of soft prey.

Healed injuries, some of which are the result of unsuccessful predaceous attacks, are not uncommon in B. higginsi. Carnivory on B. higginsi is also implied by the remains of anomalocaridids and other potential predators. [3]

Other exoskeletons show evidence of post-mortem disruption, perhaps because of scavenging. Buenellus higginsi, one of the earliest known trilobites from Laurentia, seems to have played an important role in the Sirius Passet ecosystem, serving both as predator on, and prey for, contemporary animals. [4]

Habitat

Buenellus higginsi was probably a marine bottom dweller, that lived in deeper water. This may be deduced from the dominance of eyeless forms and the absence of seaweeds at the collection site. [5]

Soft tissue preservation

Many specimens of B. higginsi show some form of exceptionally preserved, non-biomineralised tissue. Structures interpreted as alimentary tracts and probable digestive glands are commonly preserved. The slender antennas are rarely preserved. [4]

Related Research Articles

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<span class="mw-page-title-main">Sirius Passet</span> Cambrian Lagerstätte in Greenland

Sirius Passet is a Cambrian Lagerstätte in Peary Land, Greenland. The Sirius Passet Lagerstätte was named after the Sirius sledge patrol that operates in North Greenland. It comprises six places in Nansen Land, on the east shore of J.P. Koch Fjord in the far north of Greenland. It was discovered in 1984 by A. Higgins of the Geological Survey of Greenland. A preliminary account was published by Simon Conway Morris and others in 1987 and expeditions led by J. S. Peel and Conway Morris have returned to the site several times between 1989 and the present. A field collection of perhaps 10,000 fossil specimens has been amassed. It is a part of the Buen Formation.

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<i>Phragmochaeta</i> Extinct annelid

Phragmochaeta canicularis is an extinct animal belonging to the annelids and lived in the Early Cambrian. Fossils have only been found in the Buen Formation at the Sirius Passet Lagerstätte, Greenland and the animal is probably the first polychaete.

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References

  1. Mark R. Blaker & John S. Peel (1997). Lower Cambrian trilobites from North Greenland. Meddelelser om Grønland. Geoscience. Vol. 35. ISBN   978-87-635-1241-1.
  2. H. B. Whittington; et al. (1997). "Introduction, Order Agnostida, Order Redlichiida". Treatise on Invertebrate Paleontology. Part O, Revised. Trilobita.
  3. Loren E. Babcock (2002). Anatomy, paleoecology, and taphonomy of the trilobite Buenellus from the Sirius Passet biota (Cambrian), North Greenland. Geological Society of America Annual Meeting. Denver, Colorado. paper no. 75-8.
  4. 1 2 Loren E. Babcock & John S. Peel (2003). "Palaeobiology, taphonomy and stratigraphic significance of the trilobite Buenellus from the Sirius Passet biota, Cambrian of North Greenland". Memoirs of the Association of Australasian Palaeontologists. 34: 401–418.
  5. John S. Peel & Martin Stein (2009). "A new arthropod from the Lower Cambrian Sirius Passet fossil-Lagerstätten of North Greenland" (PDF). Bulletin of Geosciences . 84 (4): 625–630. doi: 10.3140/bull.geosci.1158 .