Diatomeen aus dem Eozän Norddeutschlands

Cenozoic Diatom Biostratigraphy of the Equatorial and Southern Atlantic Ocean

“…Diablo Area, California (Kanaya, 1957). In this study it was commonly found in the middle Eocene sediments of Site 356, and Jousé (1968) (Benda, 1972;Grunow, 1884) and of Barbados, Cambridge Estate (Grunow, 1884). In this study this species was found in the middle Eocene of Site 356.…”

“…of Barbados (Schmidt et al, 1874-); early Eocene of Mors, Jutland (Grunow, 1884;Benda, 1972), and middle Eocene of Site 356 (this study).…”

“…Paleogene diatoms have been described from wellknown land sections: as Mors, Denmark (early Eocene) by Heiberg (1863), Grunow (1866Grunow ( , 1884, Kitton (1870/71), Prinz (1881), Prinz and Van Ermengem (1883), Van Ermengem (1885), Van Heurck (1880-1885, Stolley (1899), Tsumura (1963), and Benda (1972); from localities in north Germany, early Eocene sediments (Schulz, 1927) and Hustedt in Wetzel (1935) described diatoms from a section near Heiligenhafen (late Eocene) and Benda (1965) from the Tarras of Fehmarn (upper early Eocene); from middle Eocene localities in the Soviet Union, in west Siberia and west Kazakstan and late Eocene localities in west Siberia and the Ukraine Proschkina-Lavrenko (1949, Jousé (1951aJousé ( , 1955, Rudkevic et al (1957), Krotov andShibkova (1959, 1961), Rubina and Drosnes (1961), Sheshukova-Poretzkaya and Gleser (1964), Paramonova (1965), Gleser (1966Gleser ( , 1968Gleser ( , 1969Gleser ( , 1970, and Jousé and Gleser (1974). The late Eocene diatoms of the Kreyenhagen shale were described by Hanna (1931).…”

“…Emphasis was put on stratigraphical work only later on, as in Benda (1972) and in the study of Kanaya (1957), who gave the observed ranges of diatoms found in the early late Eocene sedimentary sequence of the Kellogg and "Sidney" shales, near Mt. Diablo, California, and who also made a semi-quantitative diatom analysis.…”

“…and Simbirsk (Paleocene) and the early Eocene of Mors Jutland (Benda, 1972;Grunow, 1884). In this study it was found in the middle Eocene of Site 356.…”