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A REAPPRAISAL OF THE ITALIAN RECORD OF THE CRETACEOUS PACHYCORMID FISH PROTOSPHYRAENA LEIDY, 1857

JACOPO AMALFITANO, LUCA GIUSBERTI, ELIANA FORNACIARI & GIORGIO CARNEVALE

SUPPLEMENTARY DATA

Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy)

vol. 123(3): 475-485. November 2017

C

alCareousnannofossilanalysisofsample

CDl 782

The sample was prepared from unprocessed material as smear slides and examined using a light microscope at 1250x magnification. A count of the calcareous nannofossil assemblage was carried out in a predetermined area of about 7-9 mm2 (four vertical transects; modified after Gardin & Monechi, 1998).

The results of the analysis are reported below.

The sample contains a few common calcareous nannofossils in a poor state of preservation, show-ing marked dissolution. The genus Watznaueria (a dissolution resistant taxon) is dominant in the calcareous

nannofossil assemblage. In particular, the genus Watznaueria is represented by 91 specimens. The rest of the

assemblage includes: Braarudosphaera bigelowii (1), Cribrosphaerella ehrenbergii (1), Diloma galei (1), Discorhabdus

sp. (2), Eiffellithus eximius (2), Eiffellithus turriseiffelii (1), Eiffellithus sp. (1), Lithastrinus septenarius (1), Lithraphi-dites carniolensis (1), Lucianorhabdus quadrifidus (1+3cf.), Quadrum gartneri (3), Prediscosphaera sp. (4), Retecapsa angustiforata (8), Tranolithus orionatus (1+ 2cf.), Zeugrhabdotus embergeri (1), Zeugrhabdotus sp.(1).

Biozone and Age of Sample

The presence of Lithastrinus septenarius indicates the calcareous nannofossil Zones UC9-UC11 of

Burnett (1999). The absence of Micula staurophora would permit us to further constrain the specimen to

the UC9 Zone, however paleoenvironmental controls could have excluded Micula staurophora. Therefore,

we prefer to assign the sample to Zones UC9-UC11 of Burnett (1999). On this basis, the age of CDL 782 corresponds to the late Turonian-Coniacian, and ranges from 76.82 Ma to 85.56 Ma according to Gradstein et al. (2012).

referenCes

Burnett J.A. (1999) - Upper Cretaceous. In: Bown P.R. (Ed.) - Calcareous Nannofossil Biostratigraphy. Springer Science+Business media, LLC:132-199 (reprint with corrections).

Gardin S. & Monechi S. (1998) - Palaeoecological change in the middle to low latitude calcareous nannoplankton at the Cretaceous/ Tertiary boundary. Bull. Soc. Geol. Fr. 5: 709-723.

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