Taxonomy and Phylogeny of the Trocholinidae (Involutinina)

Biostratigraphy and tectonic significance of lowermost Cretaceous carbonate rocks of the Circum-Rhodope Belt (Chalkidhiki Peninsula and Thrace region, NE Greece)

“…The taxonomic determination of foraminifera follows their systematics as elaborated by Tappan (1987, 1992), the reclassification scheme of agglutinated foraminifera proposed by Kaminski (2004), and some taxonomical revision papers of Neagu (1994Neagu ( , 1995, Bucur (1997) and Rigaud et al (2013) for calcareous foraminifera.…”

“…The most important species in terms of stratigraphic value and abundance in the samples are given with their stratigraphic and geographic distribution based on the following papers: Charollais et al (1966), Hottinger (1967, Neagu (1968Neagu ( , 1970aNeagu ( ,b, 1979Neagu ( , 1984Neagu ( , 1985Neagu ( , 1986Neagu ( , 1999, Septfontaine (1974Septfontaine ( , 1980Septfontaine ( , 1988, Darsac (1983), Loeblich and Tappan (1985), Bucur (1988Bucur ( , 1993Bucur ( , 1997, Chiocchini et al (1994Chiocchini et al ( , 2012, Bucur et al (1995Bucur et al ( , 2004aBucur et al ( , 2004bBucur et al ( , 2010Bucur et al ( , 2013, Ivanova (1999), Schlagintweit and Ebli (1999) Rigaud et al (2013). The ordering of species is consistent with the classification scheme of Loeblich and Tappan (1987) and the reclassification of agglutinated foraminifera proposed by Kaminski (2004).…”

The uppermost Albian–lower Cenomanian Bielba Formation of the type-area (Cantabria, northern Spain): facies, biostratigraphy, and benthic Foraminifera

“…The high-rank classification follows Pawlowski et al (2013) and the low-rank suprageneric classification refers to Loeblich and Tappan (1987), Kaminski (2004) with some modifications of Rigaud et al (2013), Hottinger (2014, and concerning some rotaliids and trocholinids.…”

“…Note in a the attaching to a coscinoconid test of (below) by marginal test extensions (arrows); axial sections (a, b), oblique section (d). c, e Paracoscinoconus burlini (Gorbatchik) Rigaud et al 2013). Thin-sections: CR- Bi-45 (a, b, d, f, g), CR-Bi-23 (c), CR-Bi-38 (e, j), i) Siphovalvulina may display a rare visible keriothekal wall structure, and the aperture may become cribrate in the last chambers in advanced forms.…”

“…The tests are recrystallized and preserved as sparry calcite without detectable microstructural features. The spiral side is thickened as typical for the genus Frentzenella (see Rigaud et al 2013).…”