Daughter taxa (time control age-window is: 0-800Ma)![]() | Granddaughter taxa | ||||
Species without central structure | |||||
![]() | ![]() | Watznaueria barnesiae Central-area closed or very narrow, with no central area structures. | |||
Watznaueria coronata | |||||
![]() | ![]() | Watznaueria fossacincta Watznaueria with a narrow central-area opening with no central area structures. | |||
![]() | Watznaueria leesiae Like W. barnesiae but >8 µm long, Late Cretaceous | ||||
Watznaueria moshkovitzii Very large Watznaueria with central-area that is closed or with only very narrow opening, with no central area structures. | |||||
![]() | Watznaueria ovata Watznaueria with a wide, vacant central area; c. area width >= rim width. | ||||
![]() | ![]() | Watznaueria supracretacea Watznaueria-like in appearance but appear flat and have relatively large, visible rim elements. | |||
Species with disjunct bar | |||||
![]() | ![]() | ![]() | ![]() | Watznaueria britannica Watznaueria with narrow central-area spanned by a transverse bar. | Watznaueria britannica subsp. britannica Watznaueria britannica subsp. minor Watznaueria gaetani ![]() Ellipsagelosphaera clausa Ellipsagelosphaera supergesta |
Watznaueria reinhardtii Watznaueria with wide central-area spanned by a slightly oblique, narrow transverse bar that broadens at both ends. | |||||
Species with conjunct bar | |||||
![]() | ![]() | Watznaueria biporta Large (8-12 µm) Watznaueria with two well-defined pores separated by a conjunct transverse bar. | |||
![]() | ![]() | ![]() | ![]() | Watznaueria cynthae Large, broadly elliptical with two variably developed central pores that pierce the inner cycle. | |
Species with axial cross | |||||
![]() | Watznaueria contracta Medium to large, broadly elliptical Watznaueria with narrow central area almost filled with axial cross bars. | ||||
Watznaueria okadai Watznaueria species with sub-axial cross in the central area, long axis crossbar sigmoidal. | |||||
![]() | Watznaueria quadriradiata Small-medium sized Watznaueria with narrow central area spanned by axial cross bars. | ||||
Species with grill | |||||
![]() | Watznaueria fasciata Small (3-5 µm) Watznaueria with relatively wide central-area spanned by around 5 parallel transverse bars. | ||||
![]() | ![]() | ![]() | Watznaueria rawsonii Small-medium sized (4-6µm) Watznaueria with relatively wide central area (approximately the same width as the rim) spanned by an irregular grill of blocky laths. In LM the grill is imperceptible or weakly birefringent. | ||
Cyclagelosphaera baticlypeata Watznaueria with broad central-area spanned by radial bars | |||||
![]() | Watznaueria sp. Specimens not identified to species level |
Taxonomy:
Distinguishing features:
Parent taxon (Watznaueriaceae): Placoliths or modified placoliths with R-unit well developed, forming proximal and distal shield elements with opposite senses of imbrication; the V-unit typically forms a narrow distal cycle near the inner edge of the shield. Central-area structures are typically disjunct. Birefringent LM image, in which the V-unit cycle appears only as a thin, dark line.
This taxon: Elliptical watznaueriacean coccoliths with central-areas that are typically closed or narrow but may be spanned by transverse bar, bars or grill. Extinction figure with clearly inflected arms.
Farinacci & Howe catalog pages: Watznaueria * , Ellipsagelosphaera * , Actinosphaera * , Caterella * , Calolithus * , Coptolithus * , Colvillea * , Maslovella * , Margolatus *
Morphology:
Lith size: 4->12µm; Data source notes: size range of included species |
Geological Range:
Last occurrence (top): at top of Danian Stage (100% up, 61.6Ma, in Selandian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within NJ8b subzone (172.30-175.79Ma, base in Toarcian stage). Data source: Total of ranges of species in this database
Plot of occurrence data:
Black, M. (1971a). Coccoliths of the Speeton Clay and Sutterby Marl. Proceedings of the Yorkshire Geological Society. 38: 381-424. gs Black, M. (1973). British Lower Cretaceous Coccoliths. I-Gault Clay (Part 2). Palaeontographical Society Monograph. 127: 49-112. gs Bown, P. R. & Cooper, M. K. E. (1998). Jurassic. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 34-85. gs O Bown, P. R. & Young, J. R. (1997). Mesozoic calcareous nannoplankton classification. Journal of Nannoplankton Research. 19(1): 21-36. gs Burnett, J. A. (1998). Upper Cretaceous. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 132-199. gs O Noël, D. (1965). Sur les Coccolithes du Jurassique Européen et d'Afrique du Nord. Essai de classification des coccolithes fossiles. Éditions du Centre National de la Recherche Scientifique, Paris. 1-209. gs Reinhardt, P. (1964). Einige Kalkflagellaten-Gattungen (Coccolithophoriden, Coccolithineen) aus dem Mesozoikum Deutschlands. Monatsberichte der Deutschen Akademie der Wissenschaften zu Berlin. 6: 749-759. gs References:
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Watznaueria compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 16-7-2025
Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=11298 Go to Archive.is to create a permanent copy of this page - citation notes |
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