Benthic foraminiferal biostratigraphy of the lower and middle Campanian of the Polish Lowlands and its application for interregional correlation

Dubicka, Zofia

doi:10.1016/j.cretres.2015.06.012

Cited by 14 publications

(19 citation statements)

References 11 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…An ammonite-belemnite zonation proposed by Błaszkiewicz (1980), described from the Campanian and Maastrichtian of the Middle Vistula River, has never been used for the studied sequence. Recently, the inoceramid zonation of the Santonian and Campanian of the Miechów Synclinorium was published by Walaszczyk (1992), Jagt et al (2004), Jurkowska et al (2015), ammonite zonation by Machalski et al (2004), and foraminiferal biostratigraphy by Dubicka (2015). The authors correlate the biostratigraphical zonations with the belemnites/echinoids zonation described from North Germany (Schulz et al 1984) (Text- fig.…”

Section: Sphenoceramus Uintacrinusmentioning

confidence: 95%

See 1 more Smart Citation

Inoceramid stratigraphy and depositional architecture of the Campanian and Maastrichtian of the Miechów Synclinorium (southern Poland)

Jurkowska¹

2016

Acta Geologica Polonica

View full text Add to dashboard Cite

Dynamic evolution of the Campanian and Maastrichtian (Upper Cretaceous) of the Miechow Synclinorium is presented. Through chronostratigraphic analysis, the geometry of the Campanian and Maastrichtian of the area is interpreted, while microfacies analysis allowed determination of some of the paleoenvironmental parameters (rate of sedimentation, bottom condition and terrigenous input). The chronostratigraphy is based on inoceramid biostratigraphy. Nine inoceramid zones are recognized: Sphenoceramus patootensiformis, Sphaeroceramus sarumensis-Cataceramus dariensis and ‘Inoceramus’ azerbaydjanensis-‘Inoceramus’ vorhelmensis, ‘Inoceramus’ tenuilineatus, Sphaeroceramus pertenuiformis, ‘Inoceramus’ inkermanensis and ‘Inoceramus’ costaecus- ‘Inoceramus’ redbirdensis (Campanian); Endocostea typica and Trochoceramus radiosus (Maastrichtian). Five unconformities (isochronous in the study area) represented by horizons of slower sedimentation rate, were recognized. They correlate with eustatic sea-level changes, well recorded in European successions (Jarvis et al. 2002, 2006; Niebuhr et al. 2011). Unconformity horizons allow six alloformations to be distinguished. The thickness of particular chronostratigraphic units within the Campanian and Lower Maastrichtian increases progressively toward the axis of the Danish-Polish Trough, which indicates that the inversion of the trough could not have started before the Late Maastrichtian.

show abstract

Section: Sphenoceramus Uintacrinusmentioning

confidence: 95%

“…Wierzchowisko [N 50°22ʹ 9.35ʺ; E 19°49'5.21ʺ]; abandoned quarry in the S. patootensiformis and S. sarumensis-C. dariensis Zone (see Jagt et al 2004;Jurkowska et al 2015;Dubicka 2015). The exposed succession is represented by opokas with marly intercalations; a single chert horizon occurs in the middle of the succession.…”

Section: Biała Wielkamentioning

confidence: 99%

Inoceramid stratigraphy and depositional architecture of the Campanian and Maastrichtian of the Miechów Synclinorium (southern Poland)

Jurkowska¹

2016

Acta Geologica Polonica

View full text Add to dashboard Cite

show abstract

“…In the Dorotka sec tion, we also no ticed the oc cur rence of Globorotalites emdyensis (= G. hiltermanni). Since this spe cies has not been re corded in the stratigraphically lower Inoceramus azerbaydjanensis-Inoceramus vorhelmensis inoceramid Zone of the Pol ish Low land (Dubicka, 2015), its first ap pear ance seems to be in the Cataceramus subcompressus inoceramid Zone and the Bostrychoceras polyplocum ammonite Zone. This po si tion cor re sponds to the FO of Globorotalites emdyensis (= G. hiltermanni) re corded in the Lägerdorf-Kronsmoor suc cession, i.e.…”

Section: Foraminiferal Succession Planktonic Foraminiferamentioning

confidence: 99%

Foraminiferal bioevents in the upper Campanian to lowest Maastrichtian of the Middle Vistula River section, Poland

Peryt¹,

Dubicka²

2015

Self Cite

View full text Add to dashboard Cite

These events are re corded in very sim i lar strati graphic po si tions in the Lägerdorf-Kronsmoor succes sion (north ern Ger many) and in the suc ces sion of east ern Eng land and, at least some of them, in east ern Eu rope. Accord ingly they can serve as im por tant mark ers for strati graphic cor re la tion across Eu rope. The FOs of the plank tonic spe cies, Rugoglobigerina milamensis, R. hexacamerata and R. pennyi, in the up per most part of the "Inoceramus" redbirdensis Zone, are very close to the Campanian/Maastrichtian bound ary as de fined by inoceramid bi valves (Walaszczyk, 2004) and we pro pose these plank tonic foraminiferal bioevents as a good proxy for this bound ary in tem per ate re gions.

show abstract

“…The available data suggest, moreover, that the majority of first appearances recognized in most of the taxa reflect actual evolutionary events. Several evolutionary lineages of arenobuliminids, bolivinoidids, gavelinellids, globorotalitids or stensioeinids have been recognized in these sediments (Vasilenko 1961;Carter and Hart 1977;Edwards 1981;Hart and Swiecicki 1988;Bailey et al 2009;Peryt 2014, 2016;Dubicka 2015).…”

Section: Review Of the Biostratigraphically Critical Groups Used In Tmentioning

confidence: 99%

“…Twenty-eight benthic foraminiferal zones, corresponding to an interval from the middle Coniacian (Volviceramus involutus Zone) up to the end of the Maastrichtian (Hoploscaphites constrictus johnjagti Zone sensu Machalski 2005a), are distinguished based on the material from more than 50 sections, published in Dubicka and Peryt 2011, 2016Dubicka 2015;Jurkowska et al 2015;Machalski et al 2016;Peryt and Dubicka 2016 (see Text-figs 3, 4). The foraminiferal zones are correlated against the macrofossil zonations of Błaszkiewicz (1980), Walaszczyk (1997Walaszczyk ( , 2004, Jagt et al (2004), Remin, (2012Remin, ( , 2015, and Jurkowska (2016), recognized in the same outcrops (Text- fig.…”

Section: Benthic Foraminiferal Biozonation (Z Dubicka)mentioning

confidence: 99%

Integrated biostratigraphy of the Santonian through Maastrichtian (Upper Cretaceous) of extra-Carpathian Poland

Walaszczyk¹,

Dubicka²,

Olszewska-Nejbert³

et al. 2016

Acta Geologica Polonica

Self Cite

View full text Add to dashboard Cite

The biostratigraphic importance, current zonations, and potential for the recognition of the standard chronostratigraphic boundaries of five palaeontological groups (benthic foraminifers, ammonites, belemnites, inoceramid bivalves and echinoids), critical for the stratigraphy of the Santonian through Maastrichtian (Upper Cretaceous) of extra-Carpathian Poland, are presented and discussed. The summary is based on recent studies in selected sections of southern Poland (Nida Synclinorium; Puławy Trough including the Middle Vistula River composite section; and Mielnik and Kornica sections of south-eastern Mazury-Podlasie Homocline) and of western Ukraine (Dubivtsi). The new zonation based on benthic forams is presented for the entire interval studied. Zonations for ammonites, belemnites and inoceramid bivalves are compiled. All stage boundaries, as currently defined or understood, may easily be constrained or precisely located with the groups discussed: the base of the Santonian with the First Occurrence (FO) of the inoceramid Cladoceramus undulatoplicatus; the base of the Campanian with the Last Occurrence (LO) of the crinoid Marsupites testudinarius and approximated by the range of the foraminifer Stensioeina pommerana; and the base of the Maastrichtian approximated by the FO of the inoceramid bivalve Endocostea typica and the FO of the belemnite Belemnella vistulensis. The positions of substage boundaries, as currently understood, are constrained in terms of the groups discussed.

show abstract

Benthic foraminiferal biostratigraphy of the lower and middle Campanian of the Polish Lowlands and its application for interregional correlation

Cited by 14 publications

References 11 publications

Inoceramid stratigraphy and depositional architecture of the Campanian and Maastrichtian of the Miechów Synclinorium (southern Poland)

Inoceramid stratigraphy and depositional architecture of the Campanian and Maastrichtian of the Miechów Synclinorium (southern Poland)

Foraminiferal bioevents in the upper Campanian to lowest Maastrichtian of the Middle Vistula River section, Poland

Integrated biostratigraphy of the Santonian through Maastrichtian (Upper Cretaceous) of extra-Carpathian Poland

Contact Info

Product

Resources

About