Zur Entstehung „pseudolabyrinthischer” Strukturen bei sandschaligen Foraminiferen

Hagn, Herbert; Ziegler, Joseph

doi:10.1007/bf02988964

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“…In agreement with Hagn and Ziegler (1957) and Barnard and others (1981), we regard this structure to be of secondary, diagenetic origin due to the attack of the calcareous cement of the test by pyrite infilling. Scattered specimens with iron-oxide filled chambers show in thin section a partially developed ''pseudolabyrinthic-like'' wall structure.…”

Section: Systematic Taxonomysupporting

confidence: 91%

Posadia Feroniensis N. Gen., N. Sp. (Lituolida, Hormosinidae) From the Bathonian of Sardinia, Italy

Giusberti

Coccioni

2003

The Journal of Foraminiferal Research

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Detailed stratigraphical and paleobiological studies on the Mesozoic carbonate platform of eastern Sardinia (Italy) revealed the occurrence of an unknown foraminifer in the Bathonian (Middle Jurassic) Dorgali Dolostone cropping out in the Posada hill. Posadia feroniensis n. gen., n. sp., a new distinctive agglutinated foraminifer referable to the family Hormosinidae Haeckel, 1894, is formally described and figured. Posadia is morphologically characterized by an uniserial, roughly finished test with inverted ''V''-like chambers in longitudinal section.

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Section: Systematic Taxonomysupporting

confidence: 91%