Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8868300 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2018 | 71 Pages |
Abstract
We present new chronological constraints for a reference European palaeoflora based on integrated stratigraphic, palaeobotanical, palaeomagnetic and micropalaeontological analysis carried out on the Pliocene section of Caâ² Viettone, northwestern Italy. This site is characterized by rich fossil plant records of high taxonomic diversity, good preservation, and varied taphonomic mode. Palaeofloral analysis shows that the Caâ² Viettone assemblage reflects a chronologically delimited and distinguishable stage of vegetation development in northern Italy (called Caâ² Viettone Florenkomplex). Palaeomagnetic analyses show a dominant normal polarity that, however, seems to be the result of a remagnetization process due to secondary oxidation. Layers with no evidence of oxidation have registered a reverse polarity, which likely represents the original magnetization of the sediments. These results, in combination with biochronological indications, suggest that deposition of the succession preceded the Gilbert-Gauss reversal and took place during the final part of the Gilbert chron. This confirms a late Zanclean age for the rich Caâ² Viettone palaeoflora and allows us to propose this locality both as reference for a regional Florenkomplex and as a representative example of terrestrial vegetation in Europe during the early Pliocene warm interval.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Edoardo Martinetto, Evdokia Tema, Andrea Irace, Donata Violanti, Marco Ciuto, Elena Zanella,