Ammonoid-calibrated sporomorph assemblages reflect a shift from hygrophytic to xerophytic elements in the late Anisian (Middle Triassic) of the Southern Alps (Italy)

Author:

Dal Corso Jacopo,Roghi Guido,Kustatscher Evelyn,Preto Nereo,Gianolla Piero,Manfrin Stefano,Mietto Paolo

Funder

Promotion of Educational Policies, University and Research Department of the Autonomous Province of Bolzano–South Tyrol

Publisher

Elsevier BV

Subject

Paleontology,Ecology, Evolution, Behavior and Systematics

Reference66 articles.

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2. Avanzini, M., Bargossi, G.M., Borsato, A., Selli, L., Balboni, M., Bazzoli, G., Campedel, P., Demozzi, M., Groaz, O., Ferretti, P., Moretti, A., Passamani, S., Piccin, G., Piffer, G., Piubelli, D., Santacattarina, M., Spanò, M., Tomasoni R., Vallone, R., Varrone, D., Viganò, A., Zampedri, G.,Zandonai, F., 2010. Note Illustrative della Carta Geologica d'Italia alla scala 1:50.000, foglio 060 “Trento”. Servizio Geologico d'Italia, APAT.

3. Triassic ammonoid biostratigraphy: an overview;Balini,2010

4. High-resolution magnetostratigraphic and lithostratigraphic correlations in the Middle Triassic pelagic carbonates from the Dolomites (northern Italy);Brack;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2000

5. Towards a better definition of the Anisian/Ladinian boundary: new biostratigraphic data and correlation of boundary section from the Southern Alps;Brack;Eclogae Geol. Helv.,1993

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