High trochospiral architecture is relatively uncommon in rotaliid foraminifera as it is observed in a few species throughout the stratigraphic record of their 100 My history. Such a feature is recorded within the lockhartiniid group, for example in the Paleogene genus Sakesaria, whereas it is not reported from the Cretaceous. We describe two new Late Cretaceous species, Extentaspira pichezziae gen. nov., sp. nov. and Extentaspira pampaloniae sp. nov., displaying high trochospiral test, from the shallow-water facies of the Apennine and Adriatic carbonates platforms of Central and Northeastern Italy. Besides the absence of dimorphism, high trochospiral test architecture suggests an adaptation to an infaunal lifestyle. These occurrences may provide further evidence on the paleo-biogeographic gradient with the nearby Late Cretaceous Pyrenean gulf.

Late Cretaceous high trochospiral rotaliid foraminifera from Italy

Consorti L.
;
2024

Abstract

High trochospiral architecture is relatively uncommon in rotaliid foraminifera as it is observed in a few species throughout the stratigraphic record of their 100 My history. Such a feature is recorded within the lockhartiniid group, for example in the Paleogene genus Sakesaria, whereas it is not reported from the Cretaceous. We describe two new Late Cretaceous species, Extentaspira pichezziae gen. nov., sp. nov. and Extentaspira pampaloniae sp. nov., displaying high trochospiral test, from the shallow-water facies of the Apennine and Adriatic carbonates platforms of Central and Northeastern Italy. Besides the absence of dimorphism, high trochospiral test architecture suggests an adaptation to an infaunal lifestyle. These occurrences may provide further evidence on the paleo-biogeographic gradient with the nearby Late Cretaceous Pyrenean gulf.
2024
Istituto di Scienze Marine - ISMAR - Sede Secondaria Trieste
Biostratigraphy
Cretaceous
Evolution
Rotaliid foraminifera
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/519373
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