Articles | Volume 34, issue 1
https://doi.org/10.1144/jmpaleo2013-013
https://doi.org/10.1144/jmpaleo2013-013
01 Jan 2015
 | 01 Jan 2015

Small-sized Trochammina assemblages in deep-water Eocene flysch deposits (Outer Carpathians, Poland) and their palaeoecological implications

Anna Waśkowska

Cited articles

L., Alegret, S., Ortiz, I., Arenillas and E., Molina: What happens when the ocean is overheated? The foraminiferal response across the Paleocene-Eocene Thermal Maximum at the Alamedilla section (Spain), Geological Society of America Bulletin, 122, 1616-1624, 2010.
E., Alve: Colonization of new habitats by benthic foraminifera: A review, Earth-Science Reviews, 46, 167-185, 1999.
G. J., Arreguin-Rodriguez, L., Alegret and S., Ortiz: Glomospira Acme during the Paleocene–Eocene Thermal Maximum: Response to CaCo3 dissolution or to ecological forces?, Journal of Foraminiferal Research, 43, 40-54, 2013.
K., Bąk: Deep-water agglutinated foraminiferal changes across the Cretaceous/Tertiary and Paleocene/Eocene transitions in the deep flysch environment; eastern Outer Carpathians (Bieszczady Mts, Poland)In (Eds), Proceedings of the Sixth International Workshop on Agglutinated ForaminiferaGrzybowski Foundation, Special Publication, 8: 1–56., 2004.
M., Bąk and W., Barwicz-Piskorz: Stratigraphical and ecological significance of Early Eocene radiolarians from the Subsilesian Series, Polish Flysch Carpathians, Annales Societatis Geologorum Poloniae, 75, 139-115, 2005.