Yes Antonino is right. It is a fragment of Cuneolina which ranges from Valanginian to Maastrichtian.
Check my book:
BouDagher-Fadel, MK; (2008) Evolution and Geological Significance of Larger Benthic Foraminifera. Developments in Palaeontology and Stratigraphy: Vol.21. ELSEVIER
I join the opinion of my colleagues who have written before me. I would recommend you to take into consideration the book of BauDagher-Fadel, 2008 as well as articles of Neagu 2000 and Schlagintweit, Gawlick, 2005 relating to cuneoliniform foraminifera: