Difference between revisions of "Foraminiferal Organic Lining"

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[[Image:FOLs-Fig1.jpg|thumb|right|900px| <font size="2">'''Fig. 1.''' Foraminiferal organic linings from (A-L) Middle Jurassic and (M-Y) Upper Cretaceous. All linings belong the same Globothalamea class.
 
[[Image:FOLs-Fig1.jpg|thumb|right|900px| <font size="2">'''Fig. 1.''' Foraminiferal organic linings from (A-L) Middle Jurassic and (M-Y) Upper Cretaceous. All linings belong the same Globothalamea class.
  
The aperture and the [[apertural face]] (coloured pink) in a biserial form - ''Textularia'' aff. ''goesi'' Cushman. SEM graphs of specimens from the Gulf of Aqaba, Red Sea. Recent. '''A-B''': apertural (A) and peripheral (B) views of an intact specimen. Note the smooth surfaces characteristic of the faces of many [[agglutinated]] forms. '''a''': aperture; '''af''': [[apertural face]]; '''sut''': (chamber) [[suture]] (Hottinger, 2006; fig. 48 [http://paleopolis.rediris.es/cg/CG2006_M02/index.html] '''CC'''/BY-NC-SA)]]
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(Godos K., Tyszka J., Radmacher W., Goleń J. (2021). '''CC'''/BY-NC-SA)]]
 
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Revision as of 18:35, 11 June 2021

Fig. 1. Foraminiferal organic linings from (A-L) Middle Jurassic and (M-Y) Upper Cretaceous. All linings belong the same Globothalamea class. (Godos K., Tyszka J., Radmacher W., Goleń J. (2021). CC/BY-NC-SA)


Definition

  • according to Tyszka et al. (2021):

FORAMINIFERAL ORGANIC LINING (FOL) - a residual organic remnant of foraminifera left after dissolution of its mineral test, usually following palynological extraction procedures.

See also

References

Godos K., Tyszka J., Radmacher W., Goleń J. (2021). Global Database of Foraminiferal Organic Linings: ForamL Version 1.0: Media:ForamL ver.1.0.pdf

Tyszka J., Godos K., Goleń J., Radmacher W. (2021). Submitted to Earth-Science Reviews

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