Holmia is a genus of a well known group of extinct arthropods, the trilobites, that lived during the Lower Cambrian (Atdabanian) in what are now Scandinavia, Poland and Morocco.
Holmia Temporal range:
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Holmia kjerulfi, as depicted by Kiaer, 1916 | |
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Genus: | Holmia Matthew, 1890[1]
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Etymology
editHolmia is the Latin name for Stockholm, in the neighborhood of which early finds of this trilobite were collected. H. kjerulfi was named in honor of the Norwegian geologist and paleontologist Theodor Kjerulf.
Taxonomy
editSpecies previously assigned to Holmia
edit- H. hyperborea = Mesolenellus hyperborea
- H. ljungneri = Fallotaspis ljungneri
- H. lundgreni = Elliptocephala lundgreni
- H. macer = Mummaspis macer
- H. mickwitzi = Schmidtiellus mickwitzi
- H. mirabilis = Elliptocephala mirabilis
- H. rowei = Esmeraldina rowei
Distribution
edit- H. kjerulfi occurs in the Lower Cambrian of Norway (near Tomten, Sparagmite Formation, Mjøsen, Atdabanian, 60.9° N, 10.7° E),[1] and Poland (Ocieseki Sandstone Formation, Holy Cross Mountains, Atdabanian, 51.0° N, 20.0° E).[3]
- H. grandis occurs in the Lower Cambrian of Norway (near Tomten, Sparagmite Formation, Mjøsen, Atdabanian, 60.9° N, 10.7° E).[1]
- H. glabra and H. orienta are found in the Lower Cambrian of Poland (Ocieseki Sandstone Formation, Holy Cross Mountains, Atdabanian).[3]
- H. lapponica was found in the Lower Cambrian of Sweden (Grammajukku Formation, Holmia kjerulfi-zone, on the NE shore of Lake Långvattnet near Långsjöby, 10 km W of the village of Storuman, county of Västerbotten, southern Swedish Lapland).[2]
- H. palpebra was collected from the Lower Cambrian of Sweden (Upper part of the Grammajukku Formation, in the Holmia kjerulfi-zone, E bank of the Torbacken rivulet, about 600 m South-Southwest of Delliknäs , the Laisvall area, central Swedish Lapland).[2]
- Unidentified specimen probably belonging to Holmia are also known from the Lower Cambrian of Morocco (Issafen Formation, Antatlasia gutta-pluviae/Sectigena-zone, Atdabanian),[4] and Sweden (shore 600 m North of Gislövshammar , Gislöv Formation, Atdabanian (55.5° N, 14.3° E).[5]
References
edit- ^ a b c d Kiaer, J. (1916). "The Lower Cambrian Holmia fauna at Tomten in Norway". Videnskapsselskapets Skrifter. I. Matematisk - Naturvitenskapelig Klasse (10): 140.
- ^ a b c Lieberman, B. S. (1999). "Systematic Revision of the Olenelloidea (Trilobita, Cambrian)" (PDF). Bulletin of the Peabody Museum of Natural History. 45. Archived from the original (PDF) on 2016-06-24. Retrieved 2012-10-30.
- ^ a b Orlowski, S (1975). "Jednostki litostratygraficzne kambru i gornego prekambru Gor Swietokrzyskich" [Cambrian and Upper Precambrian lithostratigraphic units in the Holy Cross Mountains]. Acta Geologica Polonica. 25 (3): 431–448. Archived from the original on 2014-03-22.
- ^ Geyer, G.; Palmer, A. R. (1995). "Neltneriidae and Holmiidae (Trilobita) from Morocco and the problem of Early Cambrian intercontinental correlation". Journal of Paleontology. 69 (3): 459–474. Bibcode:1995JPal...69..459G. doi:10.1017/S0022336000034867. S2CID 129135494.
- ^ Bergström, J.; Ahlberg, P. (1984). "Uppermost lower Cambrian biostratigraphy in Scania, Sweden". Geologiska Föreningen i Stockholm Förhandlingar. 103 (2): 193–214. doi:10.1080/11035898109454518.