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Cited by 38 publications
(22 citation statements)
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“…Jelcza Wielka [N 50° 30ʹ 47ʺ; E 20° 24ʹ 52.24ʺ]; abandoned quarry in the village of Jelcza Wielka (in previous publications referred to as Wrocieryż). Foraminiferal stratigraphy of the exposed highly sandy opokas was provided by Dubicka and Peryt (2012), and it correlates with the T. radiosus Zone. Specimens of the scaphitid ammonite Hoploscaphites constrictus were also described from the section (Machalski, personal communication 2014).…”
Section: Lower Maastrichtianmentioning
confidence: 99%
“…Jelcza Wielka [N 50° 30ʹ 47ʺ; E 20° 24ʹ 52.24ʺ]; abandoned quarry in the village of Jelcza Wielka (in previous publications referred to as Wrocieryż). Foraminiferal stratigraphy of the exposed highly sandy opokas was provided by Dubicka and Peryt (2012), and it correlates with the T. radiosus Zone. Specimens of the scaphitid ammonite Hoploscaphites constrictus were also described from the section (Machalski, personal communication 2014).…”
Section: Lower Maastrichtianmentioning
confidence: 99%
“…The morphologic changes that affect the Bolivinoides lineage are expressed by the following: (1) a progressive increase in test size, (2) the evolution from "cudgelshaped" (Dubicka and Peryt, 2016) to rhomboidal outline, (3) the development of two parallel rows of tubercles in the median part of the test, and (4) an increase in the number of lobes. These evolutionary trends observed in Bolivinoides taxa seem to be similar worldwide, as reported in NW Australia (Edgell, 1954), Palestine (Reiss, 1954), SW Russia (Vasilenko, 1961;Benyamovsky et al, 2012), NW Germany (Hiltermann and Koch, 1950;Hiltermann, 1963), Trinidad (Beckmann and Koch, 1964;Bolli et al, 1994), England (Barr, 1966), Libya (Barr, 1970), the SE of the USA (Petters, 1977), the western Atlantic (Olsson, 1977), Egypt (El-Nady, 2006;Anan, 2011aAnan, , 2011bAnan, , 2017, Iraq (Jaff et al, 2014;Jaff, 2015), and Poland and western Ukraine (Dubicka and Peryt, 2012aDubicka et al, 2015;Peryt and Dubicka, 2015). These distinct evolutionary trends are specifically constrained between the Santonian and Maastrichtian, and this consistency has allowed use of the group in refined biozonation (Salaj, 1980;Odin, 2001Odin, , 2002Tronchetti, 2001;Robaszynski, 2006).…”
Section: Biostratigraphic Importance Of Bolivinoides Speciesmentioning
confidence: 99%
“…Benthic foraminifera are commonly used as a powerful proxy to reconstruct the degree of oxygenation and availability of organic matter influx on the seafloor and beyond the water/sediment interface Gooday, 1988;Murray, 1991;Loubere, 1994;Jorissen et al, 1995Jorissen et al, , 2007Widmark and Speijer, 1997a;Van der Zwaan et al, 1999). Furthermore, benthic foraminiferal morphology and assemblage composition, as well as the geochemical records of their tests (δ 18 O and δ 13 C), are used to highlight different deep water masses and to infer environmental parameters such as salinity, temperature, oxygenation, trophic flux and climate changes (Berggren and Aubert, 1975;Tjalsma, 1977;Tjalsma and Lohmann, 1983;Nyong and Olsson, 1984;Olsson and Nyong, 1984;Corliss, 1985Corliss, , 1991Van Morkhoven et al, 1986;Corliss and Chen, 1988;Barrera and Huber, 1990;Barrera, 1994;Damak-Derbel, 1994;Loubere, 1994;Speijer, 1994;Speijer, 1997a, 1997b;Leckie et al, 1998;Alegret et al, 2003;Kaminski and Gradstein, 2005;MacLeod et al, 2005;Friedrich et al, 2006;Voigt et al, 2009;Zili et al, 2009;Zili, 2010;Gallala, 2010;Dubicka and Peryt, 2012a;Alegeret and Thomas, 2013;Jorissen et al, 2017;Elamri et al, 2018). Using morphological parameters and relative abu...…”
Section: Palaeoecologymentioning
confidence: 99%
“…On the basis of belemnites, the lower part of the Mielnik succession represents the upper part of the 'boreal' lower Campanian (undivided belemnite zones Gonioteuthis gracilis and Belemnellocamax mammillatus) and the upper Campanian Belemnella mucronata Zone (Olszewska, 1990;Olszewska-Nejbert & Świerczewska-Gładysz, 2011). The upper part of the Mielnik succession belongs to the lower Maastrichtian foraminiferal Rugoglobigerina pennyi Zone (Peryt, 1981), the IV or V Assemblage Zone (Dubicka & Peryt, 2012a) and the Belemnella inflata Zone (Olszewska, 1990). The Campanian and Maastrichtian strata are divided by discontinuities, expressed as hardgrounds, which represent large parts of the upper Campanian and lower Maastrichtian.…”
Section: Eastern Polandmentioning
confidence: 99%