The Cenomanian-Turonian boundary represents a time of biotic changes affecting the diversity of larger foraminifera in shallow-water carbonate platform facies. Apart of the several taxa that suffered extinction, there is an additional cluster showing some stratigraphic occurrences before and after the CTB. Here we report a further example from the Cenomanian of the Mount Pastrik (Albanian-Kosovan boundary) that is represented by a new species within the Peneroplidae, Vandenbroeckia causae sp. nov. So far, representatives of this genus were only reported from the Campanian and Maastrichtian. The retrieval of Vandenbroeckia before CTB suggests that the genus escaped the extinction, re-appearing in the uppermost Cretaceous under a renewed specific status.

Cenomanian-Turonian 边界代表了生物变化影响浅水碳酸盐台地相中较大有孔虫多样性的时期。除了几个灭绝的分类群，还有一个集群显示了 CTB 之前和之后的一些地层事件。在这里，我们报告了一个来自帕斯特里克山（阿尔巴尼亚-科索沃边界）的森诺曼尼亚的另一个例子，它由 Peneroplidae，Vandenbroeckia causae sp. 中的一个新物种代表。十一月 迄今为止，该属的代表仅在坎帕尼亚和马斯特里赫特有报道。的检索Vandenbroeckia CTB之前表明属逃脱灭绝，重新出现在最上面的白垩纪下重新特定的状态。