Daughter taxa (time control age-window is: 0-800Ma) | ||||
Blackites inversus Large, narrow, spine-like nannofossil that tapers towards both ends and has a narrow central canal. | ||||
Blackites minusculus | ||||
Blackites perlongus Rhabdolith with a tall, narrow, club-like (claviform) spine that is not as broad as the coccolith rim. The rim is usually relatively narrow and the outer cycle is significantly smaller the inner. Some specimens have a collar at the base of the spine. | ||||
Blackites rectus Small rhabdolith with thin base and narrow spine. | ||||
Blackites singulus Long, slender spine that tapers gradually and has a characteristic thickening at the broader end. The spine is birefringent when parallel with the polarising directions, has a narrow, axial canal and is typically seen with no basal coccolith. | ||||
Blackites spinosus Rhabdolith with a tall, narrow, styliform spine that tapers gradually to a point; the outer surface is smooth. The width of the spine is around half that of the coccolith but considerable taller (x 4-6). The rim is relatively broad and distinctly convex. | ||||
Blackites stilus A rhabdolith-like nannofossil comprising a tapering spine-like structure with a narrow to broad central canal. No basal coccolith has yet been observed at the wider end although a distinct widening occurs there. | ||||
Blackites subtilis | ||||
Blackites tenuis Rhabdolith with a tall, narrow, styliform spine that is narrow at its base, broadens slightly and then tapers to a point but is never as broad as the coccolith rim. The rim is relatively narrow with a bright inner cycle. | ||||
Blackites tortilis Long spine that tapers at both ends and displays a characteristic spiralling pattern in XPL. The spine has a narrow axial canal and is typically seen with no basal coccolith. | ||||
Blackites trochos | ||||
Blackites truncatus |
Taxonomy:
Distinguishing features:
Parent taxon (Blackites): Coccoliths process-bearing with complex base including outer rim, radial lath and lamellar cycles
This taxon: Spine tall with narrow central opening
Farinacci & Howe catalog pages:
Size:
Lith size: 8->30µm; |
Geological Range:
Last occurrence (top): at top of Oligocene Epoch (100% up, 23Ma, in Aquitanian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within NP9 zone (55.86-57.21Ma, base in Thanetian stage). Data source: Total of ranges of species in this database
Plot of occurrence data:
B. spinosus group compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 20-9-2024
Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=61 Go to Archive.is to create a permanent copy of this page - citation notes |
This policy contains information about your privacy. By posting, you are declaring that you understand this policy:
This policy is subject to change at any time and without notice.
These terms and conditions contain rules about posting comments. By submitting a comment, you are declaring that you agree with these rules:
Failure to comply with these rules may result in being banned from submitting further comments.
These terms and conditions are subject to change at any time and without notice.
Comments