Palynological investigation in the lower jurassic of the vicentinian alps (Northeastern Italy)

The present paper emphasizes the applicability of palynological data as an aid to the solution of the problems related to the correlation of non-ammonitiferous Liassic strata in the Southern Alps with the ammonoid-based standard stages as recognized in the outer-Alpine part of Europe.In the Noriglio Grey Limestone Formation of the Vicentinian Alps, northeastern Italy, rich and well-preserved Liassic palynological assemblages can be abundantly found in the marly intercalations of its upper part; in the lower part palynological assemblages have appeared to be very rare. A qualitative and quantitative analysis of the assemblages has indicated the presence of a single palynological assemblage zone. Minor compositional differences do not warrant a zonal subdivision.The overall composition of the assemblages is characterized by the general dominance of Circulina and smooth trilete spores in combination with a large amount of relatively rarely occurring forms of spores, pollen grains and other acid-resistant microfossils.Because of the presence of rich and well-preserved material, it has been possible to detect a relatively wide range of variability within species of Tigrisporites, Foveosporites, Porcellispora and Crassosphaera.Among the forms which could not be matched with previously described taxa the new formgenus Skarbysporites is formally erected together with the new species Skarbysporites elsendoornii, Skarbysporites puntii, Foveosporites visscheri and Tigrisporites jonkeri. Moreover, an emended diagnosis of Circulina is proposed, implicating the assignment to this formgenus of most forms generally included in Classo pollis. Also the generic diagnosis of Tigrisporites is emended.An evaluation of the Liassic palynological assemblages from the outer-Alpine part of Europe with special reference to their potential in characterizing the ammonoid-based chronostratigraphical subdivisions may indicate that two temporal subdivisions of the Liassic Series on the basis of palynological characteristics are now slowly becoming discernable: an assemblage zone characterizing the Hettangian, Sinemurian and Lower Pliensbachian, and an assemblage zone characterizing the Upper Pliensbachian and Toarcian.Because of the possibility of a correlation with the latter zone, the assemblages from the Noriglio Grey Limestone Formation can be reasonably regarded to be indicative of a Late Pliensbachian—Toarchian age of the source-strata.When considering the ammonoid evidence from the overlying “Cape San Vigilio Oolite” it may be concluded that the upper part of the lower subdivision of the Noriglio Grey Limestone Formation and the Rotzo Member represent the Upper Pliensbachian—Lower Toarcian.Because of its potential in correlating non-ammonitiferous strata from the Southern Alps with the successions in northwestern Europe, it is believed that palynology may earn a prominent place in regional Liassic chronostratigraphy.