Taxon description
Nõlvak & Bauert, G., 2015
Belonechitina intonsa has sometimes a subcylindrical chamber, whereas the maximum chamber diameter is observed near the basal margin. The vesicle wall and the base are covered with short simple spines of similar length. In cases of poor preservation (when the spines are removed) it may be difficult to distinguish B. intonsa from C. viruana
Type specimen data
holotype : Department of Geology, TalTech GIT 544-41 , Kerguta 565 borehole , Kukruse Stage , 157.1 m
Synonymy list
2006 Belonechitina wesenbergensis s.l. — Nõlvak & Bauert , pp. pl. IV, fig. 9
Selection of related publications
Stouge, S., Bauert, G., Bauert, H., Nõlvak, J., Rasmussen, J. A. 2016. Upper Middle to lower Upper Ordovician chitinozoans and conodonts from the Bliudziai-150 core, southern Lithuania. Canadian Journal of Earth Sciences 53, 8, 781-787. DOI:10.1139/cjes-2015-0205
Nõlvak, J., Bauert, G. 2015. New biostratigraphically important chitinozoans from the Kukruse Regional Stage, Upper Ordovician of Baltoscandia. Estonian Journal of Earth Sciences 64, 3, 218-224. DOI:10.3176/earth.2015.28
Occurrence in samples (CONOP)
Mehikoorma 421 borehole : 4 sample(s)
Ruhnu 500 borehole : 2 sample(s)
Kerguta 565 borehole : 2 sample(s)
Tartu 453 borehole : 4 sample(s)
Bliudžiai 150 borehole : 4 sample(s)
Vasknarva 639 borehole : 1 sample(s)
Kovel-1 borehole : 6 sample(s)
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Classification
References based on distribution
- Nõlvak & Bauert, G., 2015 Kerguta 565 borehole 157.1 - 159.1 Kukruse Stage