Foraminifera taxon details

Farinacciella Cherchi, Radoičić & Schroeder, 2016 †

1322876  (urn:lsid:marinespecies.org:taxname:1322876)

accepted
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marine, brackish, fresh, terrestrial
fossil only
feminine
Cherchi, A.; Radoičić, R.; Schroeder, R. (2016). Farinacciella ramalhoi, n. gen., n. sp., a larger foraminifer from the Kimmeridgian–lower Tithonian of the Neo-Tethyan realm. <em>Journal of Mediterranean Earth Sciences.</em> 8: 53-61., available online at https://rosa.uniroma1.it/rosa04/mediterranean_earth_sciences/article/download/16526/15950/32452
page(s): p. 54 [details] Available for editors  PDF available [request]
Original description  Diagnosis: test free, microgranular. Juvenile stage of the probably megalospheric, high conical specimens are made up of...  
Original description  Diagnosis: test free, microgranular. Juvenile stage of the probably megalospheric, high conical specimens are made up of trochospirally arranged chambers. Adult stage at the first flat cuneiform, later ?reniform to disc-shaped. Arcuate chambers subdivided by a median wall into two lateral parts, which are divided into lateral chamberlets by lateral partitions. Conditioned by the cross-wise oblique stolon system, these partitions alternate in position from one chamber to the next. The juvenile stage of the disc-shaped microspheric specimens is made up of small, irregularly coiled chambers, followed by a series of predominantly annular chambers. These clearly increase in volume during the ontogenesis, but exhibit the general structural features of the presumably megalospheric specimens.
(Cherchi et al. (2016)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Farinacciella Cherchi, Radoicic & Schroeder, 2016 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1322876 on 2025-11-23
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2019-01-27 11:46:47Z
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original description Cherchi, A.; Radoičić, R.; Schroeder, R. (2016). Farinacciella ramalhoi, n. gen., n. sp., a larger foraminifer from the Kimmeridgian–lower Tithonian of the Neo-Tethyan realm. <em>Journal of Mediterranean Earth Sciences.</em> 8: 53-61., available online at https://rosa.uniroma1.it/rosa04/mediterranean_earth_sciences/article/download/16526/15950/32452
page(s): p. 54 [details] Available for editors  PDF available [request]
From editor or global species database
Original description  Diagnosis: test free, microgranular. Juvenile stage of the probably megalospheric, high conical specimens are made up of trochospirally arranged chambers. Adult stage at the first flat cuneiform, later ?reniform to disc-shaped. Arcuate chambers subdivided by a median wall into two lateral parts, which are divided into lateral chamberlets by lateral partitions. Conditioned by the cross-wise oblique stolon system, these partitions alternate in position from one chamber to the next. The juvenile stage of the disc-shaped microspheric specimens is made up of small, irregularly coiled chambers, followed by a series of predominantly annular chambers. These clearly increase in volume during the ontogenesis, but exhibit the general structural features of the presumably megalospheric specimens.
(Cherchi et al. (2016)). [details]
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