Identification of Biotic Constituents

Author:

Horowitz Alan Stanley,Potter Paul Edwin

Publisher

Springer Berlin Heidelberg

Reference265 articles.

1. Agip Mineraria, 1959, Microfacies Italiana: S. Donato Milanese, AGIP Mineraria, 35 p., 145 pIs. Beautifully illustrated, generally two or three photomicrographs per plate; little text. Plates arranged by age (Carboniferous to Miocene). Biotic constituents, principally foraminifers and algae, commonly are identified to generic and specific levels and names are indexed. Pertinent bibliography.

2. Bonet, Frederico, 1952, La facies Urgoniana del Cretácico Medio en la región de Tampico: Asoc. Mexicana Geólogos Petroleros Bol., v. 4, p. 153-262, 50 figs. Fifty photomicrographs (1 to 3 per page) illustrate the major facies and biotic constituents of this middle Cretaceous sequence.

3. Bonet, Frederico, 1956, Zonificación microfaunistica de las calizas Cretacicas del este de Mexico: Asoc. Mexicana Geologos Petroleros Bol., v. 8, p. 389–488, 31 pIs., 4 figs., 3 tables (reprinted XXCongreso Geol. Internatl., 102 p.).Principally taxonomic discussion and description of foraminifers, tintinnines, and problematic fossils that were used to zone the late Jurassic and Cretaceous rocks of eastern Mexico. Mostly two figures per plate; excellent photomicrographs for such high magnification (commonly 100 to 500 power). Identifications largely to specific level. English abstract.

4. Borza, Karol, 1969, Die Mikrofazies und Mikrofossilien des Oberjuras und der Unterkreide der Klippenzone der Westkarpaten: Bratislava, Slovenskej Akademie Vied, 124p., 88pls., 12 figs.Not seen.

5. Bozorgnia, Fathollah, and Banafti, SALEH, 1964, Microfacies and microorganisms of the Paleozoic through Tertiary sediments of some parts of Iran: Teheran, National Iranian Oil Company, 22 p., 158 pIs.Brief stratigraphic text and appropriate references introduce excellent photomicrographs arranged by age (Precambrian to Oligocene); biotic debris of Cambrian to Oligocene age illustrated. Identifications, largely of foraminifers, are to generic and specific level.

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