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Letná Formation

The Letná Formation is a Late Ordovician geologic formation of the Prague Basin, Bohemian Massif in the Czech Republic. The formation crops out in the Czech capital, more specifically at Letná Hill, after which the formation is named. The type locality is located at Malá Strana, Holešovice district.

Description
The Letná Formation was first formally defined in 1966 by Havlíček and Vaněk and crops out in the Prague Basin, a northeast–southwest trending minibasin stretching over between Rokycany in the southwest and Úvaly in the northeast. The Prague Basin contains an Ordovician to Devonian succession in the larger Bohemian Massif. The formation conformably overlies the Libeň Formation and is overlain by the Vinice Formation. The Letná Formation is the thickest unit in the sedimentary sequence with a thickness of more than between Beroun and Prague. The formation consists of a rhythmic alternation of sandstones (greywackes and subgreywackes), A rather diverse fauna composed of brachiopods, trilobites, echinoderms, conularids, and non-trilobite arthropods has been found in outcrops located between Zdice and Chrustenice. This area probably represented a rather shallow environment in the northwestern part of the basin. The fossils are usually fragmentary and preserved as internal or external moulds associated with angular claystone fragments within quartzose sandstones to siltstones. Accumulations of these fossil remains are commonly found in thick-bedded quartzose sandstones of light-grey and yellow or grey-brown color, which might have been deposited in areas sheltered from wave activity by sand bars. Fossilized gut remains have been observed in four of the about twenty trilobite species present in the Letná Formation: Birmanites ingens, Dalmanitina socialis, Deanaspis goldfussi and Selenopeltis buchi. These four trilobites belong to the Dalmanitina-Deanaspis Association, characterizing rather proximal and shallow environments of the Letná Formation. Most of the non-trilobite arthropods discovered in this formation, including forms with non-mineralized exoskeletons, are also found associated with D. goldfussi and/or D. socialis. This suggests that the development of conditions conducive to soft-tissue fossilization was not uncommon in the environment represented by the Dalmanitina-Deanaspis Association. == Fossil content ==
Fossil content
The following fossils were reported from the formation: • Trilobites • Actinopeltis completaBirmanites ingensCalymenella parvulaCaryon bohemicusCekovia transfugaColpocoryphe grandisDalmanitina socialisZeliszkella (Zeliszkella) hawleiGirvanopyge sp.Heterocyclopyge sp.Prionocheilus sp. • Non-trilobite arthropods • Duslia insignisBohemiacarisCrinoids • Caleidocrinus multiramusLingulataLingula deletaOrbiculoidea grandisSchizocrania incolaSchizotreta sp.Gastropods • Asinomphalus antiquaBucania draboviensisBucanopsina calypsoBucanopsis comataCyrtodiscus procerHolopea antiquataTritonophon bohemicaT. peeliParagastropodaAntispira praecoxBivalves • Astarte convergensConcavodonta ponderataGrammysia catilloidesLeptodesma patriciaModiolopsis veteranaMyoplusia bilunataPraenucula bohemicaP. disparDeceptrix sp.Palaeoneilo sp.Alena pustulosaCrustaceans • Nothozoe pollensOstracods • Cerninella bohemicaCrescentilla pugnaxCytheropsis testisHastatellina sp.Trubinella latensRostroconchiaRibeiria apusoidesBlastoideaMespilocystites bohemicusAnatifopsis sp.RhynchonellataSvobodaina ellipsoidesJezercia chrustenicensisDrabovinella draboviensisHirnantia ulrichiDrabovia asperulaD. fascicostataD. reduxChrustenopora sp.Onniella sp.Saukrodictya sp.CraniataPetrocrania obsoletaStrophomenataAegiromena aquilaBicuspina cavaB. multicostellataRafinesquina occulataTergomyaBarrandicellopsis extenuataCytherina graegariaDactylogonia blyskavensisSinuitopsis neglectaTentaculitaConchicolites confertusEdrioasteroideaHemicystites bohemicusH. velatusEocrinoideaAscocystites drabowiensisA. cf. micrasterEchinosphaerites infaustusMacrocystella bohemicaCystidea obsconditaRhombifera bohemicaStylophoraMitrocystites mitraSolutaDendrocystites sedgwickiScyphozoaAnaconularia anomalaArchaeoconularia fecundaA. insignisConularia rugulosaExoconularia exquisitaMetaconularia pyramidataPseudoconularia grandissimaP. nobilisMerostomataTriopus draboviensisPolychaetaSerpulites sp.MachaeridiaPlumulites folliculumAlgaeDendrocystis barrandei • Other • Chasmatoporella havlicekiVersispira contraria == Gallery ==
Gallery
Bicuspina multicostellata CRF.jpg|Bicuspina multicostellata Caleidocrinus multiramus CRF.jpg|Caleidocrinus multiramus Duslia insignis 34234.JPG|Duslia insignis Holopeidae - Holopea praestans.JPG|Holopea praestans == See also ==
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