The turnover of continental planktonic diatoms near the middle/late Miocene boundary and their Cenozoic evolution.

Fossil evidence indicates that modern assemblages of temperate nonmarine planktonic diatoms began near the middle/late Miocene boundary when the genus Actinocyclus, an important constituent of lacustrine planktonic diatom assemblages during the early to middle Miocene, was replaced by genera of the...

Full description

Bibliographic Details
Main Authors: Tatsuya Hayashi, William N Krebs, Megumi Saito-Kato, Yoshihiro Tanimura
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2018-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC5988279?pdf=render

Similar Items