Carnets Geol. 24 (7)  

Click here to close the window!

Outline:

[1. Introduction] [2. Material and methods] [3. The original description ...]
[4. Comparison with other assemblages of microspheres] [5. Systematics]
[6. Conclusion] [Bibliographic references] and ... [Plate]


Octahedronoides tethysianus n.gen., n.sp.,
enigmatic clusters of microspheres
at the Jurassic-Cretaceous transition

Bruno R.C. Granier

2 impasse Charles Martel, F-29217 Plougonvelin (France)

Dépt. STU, Fac. Sci. Tech., UBO, 6 avenue Le Gorgeu, CS 93837, F-29238 Brest (France)

Published online in final form (pdf) on May 8, 2024
DOI 10.2110/carnets.2024.2407

[Editors: Mikhail Rogov, Michel Moullade; language editor: Phil Salvador; technical editor: Bruno Granier]

Click here to download the PDF version!

Abstract

In the literature, numerous accounts exist of microspheres scattered in the pelagic environments of the Tethys realm at the Jurassic-Cretaceous transition. These microspheres are commonly associated with genera such as Cadosina, Colomisphaera, or Stomiosphaera, and attributed to calcareous dinocysts. On the other hand, there are few records of the microsphere, initially described as Cadosina minuta Borza, 1980, which are arranged in small clusters, likely comprising six cells. This distinctive grouping and its architecture preclude attribution to the calcareous dinocysts. A new genus and a new species (as Octahedronoides tethysianus n.gen., n.sp.) are introduced to define these clusters of leiospheres, which are here reascribed to the acritarchs.

Key-words

• calcispheres;
• leiospheres;
• dinocysts;
• acritarchs;
• Berriasian

Citation

Granier B.R.C. (2024).- Octahedronoides tethysianus n.gen., n.sp., enigmatic clusters of microspheres at the Jurassic-Cretaceous transition.- Carnets Geol., Madrid, vol. 24, no. 7, p. 127-133.

Résumé

Octahedronoides tethysianus n.gen., n.sp., des amas énigmatiques de microsphčres ŕ la transition Jurassique-Crétacé.- Dans la littérature, on trouve de nombreuses références ŕ des microsphčres dispersées dans les environnements pélagiques du domaine téthysien ŕ la transition Jurassique-Crétacé. Ces microsphčres sont communément associées ŕ des genres tels que Cadosina, Colomisphaera ou Stomiosphaera, et attribuées aux dinocystes calcaires. Toutefois, il est peu fait mention de microsphčres, initialement décrites comme Cadosina minuta Borza, 1980, qui sont disposées en petits amas, probablement constitués de six cellules. Ce type distinctif de regroupement et son architecture singuličre excluent leur attribution aux dinocystes calcaires. Un nouveau genre (Octahedronoides n.gen.) et une nouvelle espčce (Octahedronoides tethysianus n.gen., n.sp.) sont introduits pour définir ces agrégats de léiosphčres, qui sont ici réattribués aux acritarches.

Mots-clefs

• calcisphčres ;
• léiosphčres ;
• dinokystes ;
• acritarches ;
• Berriasien


1. Introduction

During the revision of the geology of Busot (Alicante, Spain: Granier et al., 1995, nearing completion; Ferré & Granier, 2000), numerous calcispheres were found in thin sections alongside late Berriasian calpionellids. Amongst the smallest microspheres, some identified as Cadosina minuta Borza, 1980, are commonly found in clusters (Pl. 1 , figs. A-BI). Borza (1980) described this species as having an "unilocular spherical shell" 28 to 32 µm in diameter "with a thin micritic wall" (translated from the original German diagnosis: "Gehäuse einkammerig, kugelförmig, Gehausewand dünn, von Mikrit-Kalzit gebildet"). He also noted "that the specimens mostly occur in clusters and only rarely occur individually" (translated from the original German description: "Es ist auffällig dass die Exemplare zumeist in Gruppen auftreten und nur selten einzeln vorkommen"), which is not the case in our thin sections, where one counts more solitary occurrences than combined duos, triplets, and quartets. According to Pszczółkowski and Myczyński (2004), the "Status of Cadosina minuta Borza is not clear, as these microfossils differ from the typical representatives of the genus Cadosina (Wanner, 1940), by their thin and indistinct test wall in many specimens and common occurrence in groups composed of 2-6 specimens". The author fully supports this last opinion because most of these grouped arrangements cannot be accidental. In any case, there are compelling reasons to investigate these so-called cadosinas, supposedly representing calcareous dinoflagellate cysts. 

2. Material and methods

All photomicrographs were taken using a digital MU900 AmScope camera mounted on a Leitz Diaplan microscope. The material analyzed below comes from the author's collection, which is now fully registered in the collections of the 'Muséum d'Histoire naturelle de Genčve' (Switzerland). There his thin sections are ascribed the following registration numbers: MHNG-GEPI-2024-10032: Busot (East) 1994 no. 2, MHNG-GEPI-2024-10060: Busot (Calvario) 1993 no. D (BR2660), MHNG-GEPI-2024-10065: Busot (Calvario) 2010 no. 4H (BR2759)[*], MHNG-GEPI-2024-10069: Busot (Calvario) 2010 no. 8 (BR2763), and MHNG-GEPI-2024-1007069: Busot (Calvario) 2010 no. 9 (BR2764).

3. The original description of Cadosina minuta Borza, 1980: Areas of ambiguity and new geometrical interpretation

Wanner (1940) regarded Cadosina, his new genus, with Cadosina fusca his new species, as an unilocular foraminifer. He describes them as "single-chambered foraminifera with spherical or ovoid shell of porcelain-like structure. Shell provided with a true aperture. Calcareous substance of the shell appears opaque, milky white under ordinary transmitted light, and in cross-polarized light without axial cross" (translated from the original German "Diagnose": "Einkammerige Foraminiferen mit kugeligem oder ovoidem Gehäuse von porzellanartiger Struktur. Gehäuse mit einer echten Mündung versehen. Die Kalksubstanz des Gehäuses im gewöhnlichen auffallenden Lichte opak, milchweiß, im durchfallenden polarisierten Lichte bei gekreuzten Nicols ohne Achsenkreuz"). Later most authors will regard all cadosinas as calcareous dinocysts (e.g., Reháková & Michalik, 1996; Lakova et al., 1999; Ivanova & Keupp, 1999; Reháková, 2000a, 2000b).

Borza (1980) gave the following description of Cadosina minuta, his new species: "Unilocular shell, spherical or sometimes slightly oval, formed by microcrystalline calcite. In transmitted light, it is dark, rarely faintly brownish, sometimes difficult to distinguish from the micritic matrix. In reflected light, it is milky white. No opening has been observed. The shell is filled with sparite. It is noticeable that the specimens mostly occur in groups and only rarely occur individually" (translated from the original German "Beschreibung: Gehäuse einkammerig, kugelförmig, manchmal schwach oval, von Mikrit-Kalzit gebildet. In Durchlicht ist sie dunkel, selten schwachbräunlich, manchmal schwer von der mikritischen Grundmasse unterscheidbar. In Auflicht ist sie milchig-weiss. Eine Mündung ist nicht beobachtet worden. Die Kammer ist von kristallischen Kalzit ausgefüllt. Es ist auffällig dass die Exemplare zumeist in Gruppen auftreten und nur selten cinzeln vorkommen.").

From the above description, a few points deserve a clarification:

1) According to Borza (1980), "In transmitted light", the shell "is dark, rarely faintly brownish, sometimes difficult to distinguish from the micritic matrix" (translated from the original German description) with a "2-3 µm thickness of the wall" (translated from the original German "Abmessungen": "Dicke der Wand 2-3 mµ"). Considering the thickness of the petrographic slide on the thin section, which averages around 20 µm, and considering the larger dimension of the spheres, which never exceeds 30 µm, the microsphere outlines are blurred. Consequently, it is not possible to provide a reasonable estimate of the wall thickness.
Therefore, it is suggested here that the wall mostly consists of a thin organic lining and that the microcrystals on both sides of it do not necessarily represent a shell. Subsequently, individual spheres should not be considered as cadosinas, i.e., calcispheres, but as leiospheres.

2) Contrary to Borza (1980), who never observed any opening, a single section out of many studied from Busot material (Pl. 1 , fig. A) shows what appears to be an unusual appendix open at its tip in a two-dimensional view. This structure or break in the wall could be related to an excystment phase.

3) As already mentioned by Borza (1980), "the specimens mostly occur in groups and only rarely occur individually" (translated from the original German description). However, scattered specimens are quite common. Pszczółkowski and Myczyński (2004) also reported the peculiar nature of these "groups composed of 2-6 specimens" of representatives of Cadosina (Wanner, 1940).
Actually, groups of microspheres appear in decreasing order of abundance as pairs (abundant), triplets (common), and quartets (rare). In contrast, groups with higher number of microspheres appear somewhat disorganized, as if they were composed of distinct clusters. Accordingly, it is suggested here that the most likely geometrical assemblage is 6 microspheres set in an octahedron (Fig. 1 ). As a matter of fact, this structure, with 12 edges, 8 faces, 2 axial planes and one equatorial plane best corresponds to the counting results of pairs (edges), triplets (faces), and quartets (planes).

Fig. 1
Click on thumbnail to enlarge the image.

Figure 1: Possible arrangement of the microspheres as an octahedron.

4) Just as 'a bicycle wheel or a pair of them is not a bicycle' and vice versa, a structured assemblage made up of several microspheres should not be identified by the name of a single microsphere, i.e., as a Cadosina sp. For this reason, a new genus is introduced here to name these peculiar assemblages.

5) The holotype of Cadosina minuta Borza, 1980, does not fit in the definition of the new genus. Therefore, a discrete holotype is selected from the Spanish material, and a new species is introduced here as well.

4. Comparison with other assemblages of microspheres

Clusters of microspheres found in Busot can be compared with:

a) Groups of cysts, i.e., pluricysts, of the Dasycladales, e.g., Terquemella, Frederica, etc. (see the review in Maksoud et al., 2021), including Russoella Barattolo, 1983, with its few cystic cavities. It is worth remembering that Dasycladales are marine benthic algae;

b) Polysphaera camerounensis Lambert & Villain, 1996, an incertae sedis tentatively ascribed to the Calcisphaerulidae sensu Villain or Thoracosphaeraceae, a family of the Class Dinophyceae. This phytoplanktonic option is more consistent with a pelagic setting at Busot. However, there are very few colonial Dinoflagellates, among which Gymnodinium catenatum H.W. Graham, 1943, which forms long-chained colonies rather than small packed clusters. Unlike the aforementioned taxa, the Busot microspheres are not embedded in a common 'shell';

c) Modern green algae of the family Scenedesmaceae Oltmanns, 1904, consist of colonies, also known as coenobia, where each one acts as a single organism. They exhibit various architectures with a variable number of cells embedded in the same mucilage. For instance, the number of cells is 4 in Tetrastrum R. Chodat, 1895, commonly 4 or 8 in Scenedesmus Meyen, 1829, and 4, 8, 16, 32, or 64 in Coelastrum Nägeli, 1849, and Hariotina P.-A. Dangeard, 1889. These numbers are part of geometric progressions starting from 4 and with common ratio of 2. They do not fit with the clusters of 6 cells characteristic of the Busot microfossils. Finally, very few fossil records of representatives of this family have been documented (e.g., Scenedesmus sp. by Fleming, 1989, in uppermost Cretaceous non-marine sediments).

c) Acritarchs are predominantly known from the Precambrian; there are fewer records from the Paleozoic (e.g., Cambrian in Kovář et al., 2023, or Harvey, 2023), the Mesozoic (e.g., Jurassic in Sarjeant, 1976; Cretaceous in Habib & Knapp, 1982, or Schrank, 2003), or the Cenozoic (e.g., Oligocene in Fechner, 1996). Palynological preparations from the Middle Cambrian of the Czech Republic (Kovář et al., 2023) yield five acritarch genera, namely Adara (Fombella, 1977), Cymatiosphaera Wetzel, 1933, Eliasum Fombella, 1977, Synsphaeridium Eisenack, 1965, and Timofeevia Vanguestaine, 1978, which have been found to form monogeneric clusters. Because these clusters consist of a highly variable number of specimens, ranging from two to more than 100 hystrichospheres, they differ markedly in size and organization. They may appear as "massive, densely packed accumulations", "specimens arranged in 'filament-like' rows", or "clusters of loosely aggregated specimens"; no common pattern of organization was observed. Similarly, palynological preparations from the Lower Cambrian of the Canada have been found to yield "strut-form" (...), "ring-form (Kahfia-like)" (...), and "plate-form (including Tapetisphaerites-like) colonies" (Harvey, 2023). However, even though it is the best option in terms of structural convergence, none of these arrangements match with those of the clusters of microspheres observed in Busot thin sections. Today, additional rock samples are required to implement palynological investigative techniques. The Busot microspheres are not concatenated. They are not in direct contact with each other either, but commonly leave a space of approximately half a microsphere diameter. However, there likely existed strong, albeit invisible, links between them. It is presumed that these leiospheres were originally encased in a non-fossilized substance, likely a mucilage, which kept them together during the early stages of fossilization.

5. Systematics

Group: Acritarcha Evitt, 1963

Genus: Octahedronoides n.gen.

Etymology: From the supposed architecture of a cluster of six new microspheres.

Type species: Octahedronoides tethysianus n.gen., n.sp.

Diagnosis: Loose but orderly arranged (in rhombohedral- or tetragonal-sphenoidal manner) colonies of a few leiospheres, never arranged in filaments, nor in struts, rings, or plates.

Species: Octahedronoides tethysianus n.gen., n.sp.

(Pl. 1 , figs. C-BI)

Synonymy:

? 1980 Cadosina minuta n.sp., Borza, p. 263-264, Pl. (Taf.) I, figs. 1-4 [holotype: Pl. (Taf.) 1, fig. 1]

1980 Cadosina minuta n.sp., Borza, p. 263-264, Pl. (Taf.) I, figs. 5-12

1992 Cadosina minuta, Bucur, Fig. 2.h

1994 Cadosina minuta, Vašicek et al., Pl. 8, fig. 4

1999 Cadosina minuta, Lakova et al., Pl. III, fig. 16

2000a Cadosina minuta, Reháková, Pl. II, fig. 15

2000b Cadosina minuta, Reháková, Pl. IV, fig. 8

2003 Cadosina minuta, Pszczółkowski, Fig. 13.9-10

2004 "Cadosina" minuta, Pszczółkowski & Myczyński, p. 152, Fig. 8.8

2007 Cadosina minuta, Lukeneder & Reháková, Fig. 6.F

2011 Cadosina minuta, Reháková, Pl. 9, fig. 18

2017 Cadosina minuta, Ivanova & Kietzmann, Fig. 7.21-24

2020 Cadosina minuta, Petrova, Fig. 5.w-y

Etymology: The new specific epiteth refers to the Tethys Ocean (with the superfluous qualifier tethysianus), not to the goddess Tethys (with the qualifier tethyanus, see discussion in Granier, 2022).

Locality: Busot, Alicante, Spain (Granier et al., 1995, nearing completion; Ferré & Granier, 2000).

Paleoenvironmental setting: The microfacies of the thin sections correspond to bioclastic wackestones, slightly silty (quartz), with a mixture of hemipelagic and reworked shallow-water material. They indicate sedimentation occurring on a paleoslope, i.e., on the transitional zone between the Prebetic platform and the Subbetic basin.

Holotype: The quartet in Plate 1 , fig. AG, MHNG-GEPI-2024-10065: Busot (Calvario) 2010 no. 4H (BR2759).

Additional studied material (paratypes): Plate 1 , figs. C, H-X, Z-AD, AF, AH-BI, MHNG-GEPI-2024-10065: Busot (Calvario) 2010 no. 4H (BR2759).

Stratigraphic horizon: Calpionellopsis Zone (zone D), upper Berriasian; lower part of the "Minuta zone", upper Berriasian-lower Valanginian.

Diagnosis: Aggregates of at least two spherical to ovoid unilocular microspheres with a diameter rarely exceeding 30 µm, commonly 25 µm. In thin sections, microspheres appear in decreasing order of abundance as pairs (abundant), triplets (common), and quartets (rare). Accordingly, it is suggested here that the most likely geometrical assemblage is 6 microspheres set in an octahedron (Fig. 1 ), i.e., a structure exhibiting 12 edges, 8 faces, 2 axial planes, and one equatorial plane. The largest dimension of a colony may reach 80 µm.

Stratigraphic range: The species is known from the lower Berriasian Elliptica Subzone of the Calpionella Zone (Borza, 1980; Michalík et al., 1990; Řehánek, 1992) to the lower Valanginian Calpionellites Zone (Borza, 1980; Reháková, 2000a, 2000b). Řehánek (1992) created a 'Minuta zone' based on its total range whereas Reháková (2000a) introduced a 'Minuta acme zone' that should be restricted to the upper part of the lower Valanginian. Considering the observed abundance of this microfossil in sample MHNG-GEPI-2024-10065: Busot (Calvario) 2010 no. 4H (BR2759), dated as late Berriasian by calpionellid biostratigraphy, it is suggested to abandon the acme zone and only refer to the newly renamed 'Tethysianus zone', a total range zone (instead of the former 'Minuta zone').

6. Conclusion

Octahedronoides tethysianus n.gen., n.sp., are planktonic organisms forming small colonies, a feature which excludes their ascription to the calcareous dinocysts, but justifies their transfer to the acritarchs. More rock samples should be collected because palynological techniques of investigation need to be implemented to definitively validate the reascription of these assemblages of organic-walled microspheres.

Acknowledgements

The two last field campaigns in SE Spain (in September 2010 and April 2024) were made possible thanks to a grant from the Association 'Carnets de Géologie'. The author would like to acknowledge the various contributions from several colleagues, namely the late Roque Aguado Merlo (1961-2023), José Miguel Andreu Rodes, Mohamed Benzaggagh, Joachim Blau, Eric Böker, the late Robert Busnardo (1926–2018), the late Bernard Clavel (1938-2018), Antonio Estévez Rubio, Bruno Ferré, Bernard C. Lambert, Eric Monteil, Stéphane Reboulet, Emmanuel Robert, and Aurélien Virgone for their contribution to a better understanding the stratigraphy in the Busot village, Alicante (Spain). The author is grateful to Daria K. Ivanova (Sofia), Joachim Blau (Frankfurt am Main), Malcolm Hart (Plymouth), and Tom Harvey (Leicester) for their comments, which helped improve the manuscript. Thanks are also due to Phil Salvador who kindly checked the final version of the English text.

Bibliographic references

Barattolo F. (1983).- Su alcuni organi riproduttori isolati di Dasicladacee nel Cretacico dell'Appennino.- Bollettino della Societŕ dei Naturalisti in Napoli, vol. 92, p. 17-49.

Borza K. (1980).- Cadosina minuta n.sp. aus der unteren Kreide der Westkarpaten.- Geologický Zborník - Geologica Carpathica, Bratislava, vol. 31, no. 3, p. 263-299.

Bucur I.I. (1992).- Calpionellids and calcispheres from the Upper Jurassic-Lower Cretaceous deposits in the Resita-Moldova Noua zone, Southern Carpathians, Romania.- Cretaceous Research, vol. 13, p. 565-576.

Fechner G.G. (1996).- Septarienton und Stettiner Sand als Fazieseinheiten im Rupelium der östlichen Mark Brandenburg: Palynologisch-fazielle Untersuchungen bei Bad Freienwalde.- Berliner geowissenschaftliche Abhandlungen, Reihe E 18, 77-119.

Ferré B. & Granier B. (2000).- Roveacrinus berthoui nov. sp., Early Hauterivian representative of Roveacrinidae (Roveacrinida, Crinoidea) of Busot (Alicante, Spain).- Geologica carpathica, Bratislava, vol. 51, no. 2, p. 101-107.

Fleming R.F. (1989).- Fossil Scenedesmus (Chlorococcales) from the Raton Formation, Colorado and New Mexico, U.S.A.- Review of Palaeobotany and Palynology, vol. 59, p. 1-6.

Granier B. (2022).- Tethysian, Tethyan or ... Tethys Ocean and Tethys.- Carnets Geol., Madrid, vol. 22, Editorial Note 1, p. 681-683. DOI: 10.2110/carnets.2022.22EN1

Granier B., Virgone A., Busnardo R. & Bulot L.G. (1995).- Des calpionelles dans l'Hauterivien supérieur. Découverte exceptionnelle ŕ Busot (Alicante, Espagne).- Comptes-Rendus de l'Académie des Sciences (Série II a), Paris, t. 321, p. 1179-1186.

Habib D. & Knapp S.D. (1982).- Stratigraphic utility of Cretaceous small acritarchs.- Micropaleontology, vol. 28, no. 4, p. 335-371. 

Harvey T.H.P. (2023).- Colonial green algae in the Cambrian plankton.- Proceedings of the Royal Society B, vol. 290, no. 2009, article 20231882, 12 p. DOI: 10.1098/rspb.2023.1882

Ivanova D.K. & Kietzmann D.A. (2017).- Calcareous dinoflagellate cysts from the Tithonian - Valanginian Vaca Muerta Formation in the southern Mendoza area of the Neuquen Basin, Argentina.- Journal of South American Earth Sciences, Vol. 77, p. 150-169.

Kovář V., Fatka O. & Vodička J. (2023).- Acritarch clusters from the Cambrian (Miaolingian) of the Příbram-Jince Basin, Czech Republic.- Palynology, vol. 47, no. 1, article 2115574, 18 p.

Lakova I., Stoykova K. & Ivanova D. (1999).- Calpionellid, nannofossil and calcareous dinocyst bioevents and integrated biochronology of the Tithonian to Valanginian in the Western Balkanides, Bulgaria.- Geologica Carpathica, Bratislava, vol. 50, no. 2, p. 151-168.

Lambert B. & Villain J.-M. (1996).- Polysphaera camerounensis, nouveau genre et nouvelle espčce de "Micropithonelle" de l'Albien supérieur du Cameroun méridional.- Géologie de l'Afrique et de l'Atlantique Sud : Actes Colloques Angers 1994, p. 123-143.

Lukeneder A. & Reháková D. (2007).- Chronostratigraphic significance of an early Valanginian (Cretaceous) calpionellid association (Hochkogel section, Upper Austria, Northern Calcareous Alps).- Geological Quarterly, Warszawa, vol. 51, no. 1, p. 27-38.

Maksoud S., Granier B., Huang D. & Azar D. (2021).- Edgellia libanica n. organo-gen., n. organo-sp., a new Dasycladalean organ from the Lower Cretaceous of Lebanon.- Arabian Journal of Geosciences, vol. 14, article 1337, 11 p.

Michalík J., Reháková D. & Peterčáková M. (1990).- Stratigraphy of the Jurassic-Cretaceous boundary beds in the Kýsuca sequence of the Klippen Belt, Western Carpathians, Brodno section near Žilina.- Knihovnička Zemního plynu a nafty, vol. 9b, p. 57-71.

Petrova S. (2020).- Uppermost Berriasian macro- and microfossil assemblages from the Ticha Formation of the Eastern Fore-Balkan Mts (Bulgaria).- Geologica Balcanica, Sofia, vol. 49, no. 3, p. 19-37.

Pszczółkowski A. (2003).- Kościeliska Marl Formation (Lower Cretaceous) in the Polish Western Tatra Mountains: Lithostratigraphy and microfossil zones.- Studia Geologica Polonica, Kraków, vol. 121, p. 7-50.

Pszczółkowski A. & Myczyński R. (2004).- Ammonite-supported microfossil and nannoconid stratigraphy of the Tithonian-Hauterivian limestones in selected sections of the Branisko Succession, Pieniny Klippen Belt (Poland).- Studia Geologica Polonica, Kraków, vol. 123, p. 133-197.

Reháková D. (2000a).- Evolution and distribution of the Late Jurassic and Early Cretaceous calcareous dinoflagellates recorded in the Western Carpathian pelagic carbonate facies.- Mineralia Slovaca, Bratislava, vol. 32, no. 2, p. 79-88.

Reháková D. (2000b).- Calcareous dinoflagellate and calpionellid bioevents versus sea-level fluctuations recorded in the West-Carpathian (Late Jurassic/Early Cretaceous) pelagic environments.- Geologica Carpathica, Bratislava, vol. 51, no. 4, p. 229-243.

Reháková D., Matyja B.A., Wierzbowski A., Schlögl J., Krobicki M. & Barski M. (2011).- Stratigraphy and microfacies of the Jurassic and lowermost Cretaceous of the Veliky Kamenets section (Pieniny klippen Belt, Carpathians, western Ukraine).- Volumina Jurassica, Varsaw, vol. IX, p. 61-104.

Reháková D. & Michalik J. (1996).- Stomiosphaera or Orthopithonella? Cadosina or Obliquipithonella? Notes on ultrastructure and systematic position of some Jurassic-Cretaceous calcareous dinoflagellates from Western Carpathians.- Mineralia Slovaca, Bratislava, vol. 28, p. 92-98.

Řehánek J. (1992).- Valuable species of cadosinids and stomiosphaerids for determination of the Jurassic-Cretaceous boundary (vertical distribution, biozonation).- Scripta (Geology), Leiden, vol. 22, p. 117-122.

Sarjeant W.A.S. (1976). English Jurassic dinoflagellate cysts and acritarchs: A reexamination of some type and figured specimens.- Geoscience and Man, vol. 15, no. 1, p. 1-24.

Schrank E. (2003).- Small acritarchs from the Upper Cretaceous: Taxonomy, biological affinities and palaeoecology.- Review of Palaeobotany and Palynology, vol. 123, p. 199-235.

Vašicek Z., Michalik J. & Reháková D. (1994).- Early Cretaceous stratigraphy, palaeogeography and life in western Carpathians.- Beringeria, Würzburg, Heft 10, p. 3-169.

Wanner J. (1940).- Gesteinbildende Foraminiferen aus Malm und Unterkreide des östlichen Ostindischen Archipels nebst Bemer kungen über Orbulinaria Rhumbler und andere verwandte Foraminiferen.- Paläontologische Zeitschrift, vol. 22, no. 2, p. 75-79.


Plate

Plate 1: ? Cadosina minuta Borza, 1980 (A-B), and Octahedronoides tethysianus n.gen., n.sp. (C-BI). Most photomicrographs are from thin section MHNG-GEPI-2024-10065: Busot (Calvario) 2010 no. 4H (BR2759), except for: a) figs. D, F, Y from thin section Busot (Calvario) 2010, no. 8; b) fig. E from thin section Busot (East) 1994, no. 2; c) fig. G from thin section Busot (Calvario) 1993, no. D60; and d) fig. AE from thin section Busot (Calvario) 2010, no. 9. Scale bar (on fig. J) = 100 µm.

Pl. 1
Click on thumbnail to enlarge the image.



X

[*] Microspheres are particularly abundant in this sample.