Liobole

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Liobole
Temporal range: 360–341  Ma
Liobole.jpg
Liobole Glabra
Scientific classification Red Pencil Icon.png
Kingdom: Animalia
Phylum: Arthropoda
Class: Trilobita
Order: Proetida
Family: Proetidae
Genus: Liobole
Richter and Richter, 1949
Species and subspecies
  • LioboleOwens and Tilsley, 1995

Liobole is a lower Carboniferous proetid trilobite.

Contents

Etymology

Liobole was described from material found in the Moravian Karst. [1] The species shown is from the lower carboniferous of SW England. [2]

Distribution

Liobole is found in the European Culm facies and has been collected from the lower Carboniferous across Europe for example from (Visian) deposits of SW England and (Tournaisian) of Poland and as far east as China. [3]

Taxonomy

Identified as proetid trilobite from the lower Visean Brezina formation by Chlupáč 1966.

Related Research Articles

The Carboniferous is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period 358.9 million years ago (Mya), to the beginning of the Permian Period, 298.9 million years ago. The name Carboniferous means "coal-bearing", from the Latin carbō ("coal") and ferō, and refers to the many coal beds formed globally during that time.

<span class="mw-page-title-main">Devonian</span> Fourth period of the Paleozoic Era 419-359 million years ago

The Devonian is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, 419.2 million years ago (Mya), to the beginning of the Carboniferous, 358.9 Mya. It is named after Devon, England, where rocks from this period were first studied.

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<span class="mw-page-title-main">Trilobite</span> Class of extinct, Paleozoic arthropods

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<span class="mw-page-title-main">Tournaisian</span> First stage of the Carboniferous

The Tournaisian is in the ICS geologic timescale the lowest stage or oldest age of the Mississippian, the oldest subsystem of the Carboniferous. The Tournaisian age lasted from 358.9 Ma to 346.7 Ma. It is preceded by the Famennian and is followed by the Viséan.

<span class="mw-page-title-main">Viséan</span> Second stage of the Carboniferous

The Visean, Viséan or Visian is an age in the ICS geologic timescale or a stage in the stratigraphic column. It is the second stage of the Mississippian, the lower subsystem of the Carboniferous. The Visean lasted from 346.7 to 330.9 Ma. It follows the Tournaisian age/stage and is followed by the Serpukhovian age/stage.

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Trinodus is a very small to small blind trilobite, a well known group of extinct marine arthropods, which lived during the Ordovician, in what are now the Yukon Territories, Virginia, Italy, Czech Republic, Poland, Denmark, Sweden, Svalbard, Ireland, Scotland, Wales, Iran, Kazakhstan and China. It is one of the last of the Agnostida order to survive.

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References

  1. Chlupáč, I. (1966). "The Upper Devonian and Lower Carboniferous trilobites of The Moravian Karst". Sbor. Geol. Věd, Ř.P. 7: 1–143.
  2. Owens, R.M. (1995). "An atheloptic trilobite assemblage from the Carboniferous of North Devon". Geological Magazine. 132 (6): 713–728. doi:10.1017/S0016756800018938. S2CID   129158199.
  3. Hahn, G. (2005). "Kulm trilobites (Lower Carboniferous) from S-China" (PDF). Paläontologische Zeitschrift. 79 (3): 371–375. doi:10.1007/BF02991929. S2CID   128582636.