Distinguishing features:
Parent taxon (Kamptneriaceae): Arkhangelskielids with shields predominantly formed of V-units, thus dark in cross-polarised light; R-units form bright band at core of shield.
This taxon: Tiered coccoliths with distinctive LM images consisting of a narrow to moderately-broad rim with a narrow, dark outer-cycle; a diagnostic, bright median-cycle; and a dark, inner-cycle. Central-area structures variable but generally dark in LM.
Daughter taxa (time control age-window is: 0-800Ma) | Granddaughter taxa | ||||
Species with plate in central area | |||||
Gartnerago obliquum Gartnerago with a narrow rim and a broad central area, filled with a plate pierced by numerous pores (~>10 in each quadrant); the plate is crossed by sutures, the transverse of which is slightly oblique. | |||||
Gartnerago segmentatum Similar to G. obliquum but rim broader, central area smaller. | |||||
Gartnerago costatum Similar to G. obliquum but pores larger and with cross-bars within them | |||||
Gartnerago diversum Gartnerago with protruding axial bars; perforations small, with a double row of perforations on each side of the cross-bars, with others randomly distributed | |||||
Species with narrow rim and solid plate | |||||
Gartnerago stenostaurion Small to large coccoliths characterized under LM XPL by a conspicuous, narrow, bright rim cycle and wide central area spanned by a plate. The plate is usually crossed by four radial extinction lines (two in the major axes of the coccolith ellipse and two diagonally orientated) and narrow, bright, bar-like structures, which are longitudinal and near transverse (rotated by ~10°), and birefringent when the coccolith is at 45° to the polarizing directions. | |||||
Gartnerago clarusora Central plate of 4 units with axial sutures, no axial cross; small (4-6 µm) | |||||
Gartnerago waszczakii Central plate of 6 units; large (8-11 µm) | |||||
Species with cross in centre | |||||
Gartnerago chiasta Gartnerago with diagonal cross bars. | |||||
Gartnerago margaritatus | |||||
Gartnerago praeobliquum Gartnerago with wide central area spanned by broad axial cross bars that have arrowhead-shaped ends and median suture lines. | |||||
Species with transverse bar | |||||
Gartnerago coxalliae Central area, wide, open and spanned by a complex transverse bar, which bifurcates where it joins the rim. | |||||
Gartnerago nanum Medium-sized Gartnerago with a loxolith-type rim and a narrow, perforate central area plate, which has differentiated axial bars, although the longitudinal bar may be subordinate or poorly defined. | |||||
Gartnerago ponticula Small- to medium-sized (usually <7.0 µm) Gartnerago species with an open central area spanned by a transverse, conjunct bar. | |||||
Gartnerago theta Gartnerago with a wide central area spanned by a narrow transverse bar which delimits two, large D-shaped openings; a finely perforate proximal net is seen in good preservation (Black, 1975, Pl. 34, figs 6-8). | |||||
Gartnerago sp. Specimens not identified to species level |
Taxonomy:
Farinacci & Howe catalog pages: Gartnerago * , Cribricatillus * , Laffittius *
Distinguishing features:
Parent taxon (Kamptneriaceae): Arkhangelskielids with shields predominantly formed of V-units, thus dark in cross-polarised light; R-units form bright band at core of shield.
This taxon: Tiered coccoliths with distinctive LM images consisting of a narrow to moderately-broad rim with a narrow, dark outer-cycle; a diagnostic, bright median-cycle; and a dark, inner-cycle. Central-area structures variable but generally dark in LM.
Morphology:
LITHS: placolith, elliptical, CA: cross-axial, grill, plate, pores, diagonal cross, bar, closed, CROSS-POLARS: rim-bicyclic, V-prominent, R-prominent, |
Lith size: 4->12µm; Data source notes: size range of included species |
Geological Range:
Last occurrence (top): at top of Maastrichtian Stage (100% up, 66Ma, in Danian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within Late Aptian Substage (113.20-118.70Ma, base in Aptian stage). Data source: Total of ranges of species in this database
Plot of occurrence data:
Black, M. (1973). British Lower Cretaceous Coccoliths. I-Gault Clay (Part 2). Palaeontographical Society Monograph. 127: 49-112. gs Bukry, D. (1969). Upper Cretaceous coccoliths from Texas and Europe. University of Kansas Paleontological Contributions, Articles. 51 (Protista 2): 1-79. gs O Burnett, J. A. (1998). Upper Cretaceous. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 132-199. gs O Gartner, S. (1968). Coccoliths and related calcareous nannofossils from Upper Cretaceous deposits of Texas and Arkansas. University of Kansas Paleontological Contributions, Articles. 48 (Protista 1): 1-56. gs O Noël, D. (1969). Arkhangelskiella (coccolithes Crétacés) et formes affines du Bassin de Paris. Revue de Micropaléontologie. 11: 191-204. gs Stover, L. E. (1966). Cretaceous coccoliths and associated nannofossils from France and the Netherlands. Micropaleontology. 12(2): 133-167. gsReferences:
Gartnerago compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 8-9-2024
Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=10457 Go to Archive.is to create a permanent copy of this page - citation notes |
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