Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6446796 | Quaternary Science Reviews | 2013 | 20 Pages |
Abstract
The Neocaspian period should be considered a biozone rather than a chronozone, as the environmental conditions reconstructed from dinocyst assemblages are different in shallow shelf waters and in the deep basins.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Suzanne A.G. Leroy, Ata A. Kakroodi, Salomon Kroonenberg, Hamid K. Lahijani, Habib Alimohammadian, Aman Nigarov,