| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8868705 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2017 | 45 Pages |
Abstract
The conodont fauna showed a significant change in provincialism from the Ordovician to the Silurian, i.e., from a latitudinal pattern to a longitudinal pattern. The Hirnantian glaciation may be one of the controlling factors which resulted in the reorganization of the conodont faunas and the change of their living habits and ecological requirement.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Zhongyang Chen, Peep Männik, Junxuan Fan,