View source for Foraminiferal Organic Lining

[[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. This figure presents FOLs from (A-L) Pieniny Klippen Belt and (M-Y) Basque–Cantabrian Basin coming from time intervals separated by ca. 100 Ma apart. All organic linings show similar globular growth patterns, however, Jurassic FOLs are larger than Cretaceous ones. Source: eForams.org under Licence CC-BY-NC-SA. 

 (Godos K., Tyszka J., Radmacher W., Goleń J. (2021). '''CC'''/BY-NC-SA)]]
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==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==
*[[organic lining]]

==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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