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 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. (Godos K., Tyszka J., Radmacher W., Goleń J. (2021). Source: eForams.org under Licence '''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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