Palaeoenvironmental reconstruction of the Upper Viséan Paprotnia Beds (Bardo Unit, Polish Sudetes) deposition on the ichnological and palaeontological investigations

Muszer, Jolanta; Uglik, Małgorzata

doi:10.7306/gq.1095

Cited by 4 publications

(5 citation statements)

References 85 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…1). To the NW and W, the intrusion is in sharp contact with the BSU, which consists largely of non-metamorphosed Devonian to Early Carboniferous sedimentary rocks (Kryza et al 2008b;Muszer and Uglik 2013;Bojanowski et al 2014), and by the greenschist-to amphibolite-facies rocks of the Kłodzko metamorphic complex , metamorphosed in the Early Palaeozoic to pre-Late Devonian (Wojciechowska 1975). The BSU overlies (with a sedimentary contact) the Kłodzko metamorphic complex (Kryza et al 2008a).…”

Section: The Kłodzko-złoty Stok Intrusionmentioning

confidence: 99%

“…The ages overlap with contemporaneous volcanism in the Sudetes and the Jawornik granitoids dated at ~ 350 and ~ 340 Ma (Białek 2014). The first marks the presence of a marine fauna (Muszer and Uglik 2013) whilst the second records a middle crustal pressure of 4-6 kbar (Białek 2001(Białek , 2014. Because of the similar ages, a plane in 3D space can be drawn, estimating where the present day surface was at ~ 334-344 Ma.…”

Section: Post-emplacement Tiltingmentioning

confidence: 99%

“…In the case of the KZSI, palaeontological evidence from the Paprotnia Beds (Muszer and Uglik 2013) shows that after ca. 334 Ma, recorded by bentonites, the eastern bank of the Intra-Sudetic Basin started to be lifted up, going from a deep to shallow sea level, and later emerging as land.…”

Section: Post-emplacement Tiltingmentioning

confidence: 99%

See 2 more Smart Citations

Multiphase magmatic activity in the Variscan Kłodzko–Złoty Stok intrusion, Polish Sudetes: evidence from SHRIMP U–Pb zircon ages

Jokubauskas¹,

Bagiński²,

Macdonald³

et al. 2017

Int J Earth Sci (Geol Rundsch)

View full text Add to dashboard Cite

The Kłodzko-Złoty Stok intrusion (KZSI), located in the NE part of the Bohemian Massif of Central Europe, has preserved records of the magmatic and tectonic activity of the Variscan orogeny in the Sudetes. KZSI is extraordinarily complex texturally, and shows a very wide range of chemical, isotopic and mineralogical compositions which indicates a complex, multiphase history of intrusion. New SHRIMP U-Pb zircon ages provide evidence of two magmatic episodes with a distinctive hiatus between them at ~ 326-308 Ma. The youngest dated zircons (303.8 ± 3.8/4.2 Ma) are from the Laski leucocratic hornblende-biotite monzogranite and mark a short interval of post-collisional reactivation of the magma system. Zircons from a biotite-hornblende diorite sheet from the northern part of KZSI yielded an age of 349 ± 3.4/3.7 Ma, interpreted as indicating the initial phase of an early Carboniferous, multi-pulse episode. The evolution of the magmatic system can be tied to a 334.4 ± 2.9/3.3 Ma zircon age for melanocratic syenites from Podzamek which represent lamprophyric melt. Based on textural and compositional data and field relationships we interpret the intrusion as having been tilted post-emplacement towards the NW. This, together with the new dating results, ties the early Carboniferous episode of KZSI activity and the Jawornik granitoids (5 km to the SE) to the same magmatic system and arguably to bentonites of the Paprotnia beds (5 km to the NW), all representing different levels of such a system. The newly estimated late Carboniferous age from Laski ties part of the KZSI to other late Carboniferous Sudetic intrusions and late Carboniferous-Permian volcanism.

show abstract

Section: The Kłodzko-złoty Stok Intrusionmentioning

confidence: 99%

Section: Post-emplacement Tiltingmentioning

confidence: 99%

See 1 more Smart Citation

Multiphase magmatic activity in the Variscan Kłodzko–Złoty Stok intrusion, Polish Sudetes: evidence from SHRIMP U–Pb zircon ages

Jokubauskas¹,

Bagiński²,

Macdonald³

et al. 2017

Int J Earth Sci (Geol Rundsch)

View full text Add to dashboard Cite

show abstract

“…In the Sudetes, Thalassinoides has been de scribed from the Car bon if er ous by Muszer and Uglik (2013), from the Mid dle Trias sic, Lower Muschelkalk (Chrz¹stek, 2013a) and from the Upper Cre ta ceous (Rotnicka, 2005;Leszczyñski, 2010;Chrz¹stek, 2013b, c;Chrz¹stek and So³czerski, 2016). Rotnicka (2005) cited this ichnogenus from the Cenomanian and Turonian of the Sto³owe Moun tains (Intra-Sudetic Synclinorium) from offshore/shelf set tings.…”

Section: Palaeoenvironmentmentioning

confidence: 99%

Rosarichnoides sudeticus igen. et isp. nov. and associated fossils from the Coniacian of the North Sudetic Synclinorium (SW Poland)

Chrząstek

Muszer

Solecki

et al. 2018

Self Cite

View full text Add to dashboard Cite

“…Mis sis sip pian trace fos sils from the cen tral part of the Pol ish Sudetes are best known from the Up per Visean of the Bardo Unit Haydukiewicz, 2009, 2010;Muszer and Uglik, 2013). For many years they were men tioned, with out de scription, from the Intra-Sudetic Synclinorium (¯akowa, 1958, 1960Teisseyre, 1968a;Nemec et al, 1982;Mastalerz, 1987Mastalerz, , 1995.…”

Section: Introductionmentioning

confidence: 99%

First discovery of Mississippian trace fossils in the Świebodzice Unit from the Witoszów region (SW Poland)

Muszer

2020

Self Cite

View full text Add to dashboard Cite

As so ci ate Ed i tor: Micha³ Zatoñ Abun dant and mod er ately di verse trace fos sil as sem blage have been dis cov ered for the first time in mudstones of the Pogorza³a For ma tion from the Witoszów re gion, SW Po land. Fif teen ichnospecies in clud ing four teen ichnogenera are described. The ichnofauna is dom i nated by Dictyodora liebeana and con tains nu mer ous Palaeophycus tubularis, rarer Archaeonassa fossulata, Archaeonassa isp., Chondrites cf. intricatus, Curvolithus sim plex, Diplopodichnus biformis, Lockeia isp., ?Lophoctenium isp., Nereites isp., Phycosiphon isp., Protovirgularia isp., ?Psammichnites isp., Taenidium isp. and one ichnospecies of fish swim ming trails, Undichna cf. bri tan nica. Some other struc tures (wave rip ples in flu enced by micro bial mats and zig zag struc tures) also oc cur. The trace fos sil as sem blages dif fer in var i ous ex po sures, but three of them are sim i lar and dis play the Dictyodora liebeana ichnoassemblage. It is rep re sented mostly by the etho log i cal cat e go ries fodinichnia and repichnia, with fewer pascichnia, domichnia and cubichnia. This new data from the OEwiebodzice Unit sheds light on the palae on tol ogy, age and palaeoenvironment of the Pogorza³a For ma tion. The oc cur rence of D. liebeana and U. cf. bri tan nica in di cates the Mis sis sip pian age of most mudstones stud ied, for merly con sid ered Up per De vo nian. The trace fos sil as sem blage be longs to the non-stan dard Nereites ichnofacies, with out graphoglyptids. The lithological fea tures of mudstones, trace fos sil as sem blage and pov erty of macrofauna, tes tify to their de po si tion in a deeper sed i men ta tion zone be low storm wave base, most likely in dysaerobic, pro-delta con di tions. This study sug gests that rocks con tain ing D. liebeana may form a cor re la tive ho ri zon in the OEwiebodzice Unit.

show abstract

Palaeoenvironmental reconstruction of the Upper Viséan Paprotnia Beds (Bardo Unit, Polish Sudetes) deposition on the ichnological and palaeontological investigations

Cited by 4 publications

References 85 publications

Multiphase magmatic activity in the Variscan Kłodzko–Złoty Stok intrusion, Polish Sudetes: evidence from SHRIMP U–Pb zircon ages

Multiphase magmatic activity in the Variscan Kłodzko–Złoty Stok intrusion, Polish Sudetes: evidence from SHRIMP U–Pb zircon ages

Rosarichnoides sudeticus igen. et isp. nov. and associated fossils from the Coniacian of the North Sudetic Synclinorium (SW Poland)

First discovery of Mississippian trace fossils in the Świebodzice Unit from the Witoszów region (SW Poland)

Contact Info

Product

Resources

About