Calymene blumenbachii (fossil trilobite) (Much Wenlock Limestone, Middle Silurian; Wrens Nest, Dudley, England) 7 : 無料・フリー素材/写真
Calymene blumenbachii (fossil trilobite) (Much Wenlock Limestone, Middle Silurian; Wrens Nest, Dudley, England) 7 / James St. John
| ライセンス | クリエイティブ・コモンズ 表示 2.1 |
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| 説明 | Calymene blumenbachii Brongniart, 1822 - fossil trilobite from the Silurian of England.Trilobites are extinct marine arthropods. They first appear in Lower Cambrian rocks and the entire group went extinct at the end of the Permian. Trilobites had a calcitic exoskeleton and nonmineralizing parts underneath (legs, gills, gut, etc.). The calcite skeleton is most commonly preserved in the fossil record, although soft-part preservation is known in some trilobites (Ex: Burgess Shale and Hunsruck Slate). Trilobites had a head (cephalon), a body of many segments (thorax), and a tail (pygidium). Molts and carcasses usually fell apart quickly - most trilobite fossils are isolated parts of the head (cranidium and free cheeks), individual thoracic segments, or isolated pygidia. The name "trilobite" was introduced in 1771 by Johann Ernst Immanuel Walch and refers to the tripartite division of the trilobite body - it has a central axial lobe that runs longitudinally from the head to the tail, plus two side lobes (pleural lobes).One of the most famous trilobites is Calymene blumenbachii from Dudley, England. These were first discovered in the 1700s during quarrying of Silurian limestones near the town of Dudley, England. They are nicknamed "Dudley bugs" (pronounced "Doodly Boogs" by locals).Classification: Arthropoda, Trilobita, Polymerida, CalymenidaeStratigraphy: Much Wenlock Limestone, Homerian Stage, Wenlockkian Series, mid-SilurianLocality: quarry at Wrens Nest, town of Dudley, England |
| 撮影日 | 2025-04-26 14:06:38 |
| 撮影者 | James St. John |
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