Middle Ordovician carbonate facies development, conodont biostratigraphy and faunal diversity patterns at the Lynna River, northwestern Russia-Reference-Cited by-同舟云学术

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Middle Ordovician carbonate facies development, conodont biostratigraphy and faunal diversity patterns at the Lynna River, northwestern Russia

Published:2020 Issue:1 Volume:69 Page:37
ISSN:1736-4728
Container-title:Estonian Journal of Earth Sciences
language:en
Short-container-title:Estonian J. Earth Sci.

Author:

Lindskog A,Eriksson M E,Rasmussen J A,Dronov A,Rasmussen C M

Publisher

Estonian Academy Publishers

Subject

General Earth and Planetary Sciences,Water Science and Technology

Cited by 10 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Darriwilian conodont biostratigraphy from the Rio Francia section, Central Precordillera, Argentina: A new insight into the Darriwilian conodont biozones;Journal of South American Earth Sciences;2024-11

2. Global pattern of conodont similarity and faunal constraints during the highstand of the Evae eustatic event (late Floian, Lower Ordovician);Journal of Palaeogeography;2024-08

3. Oxygenation of the Baltoscandian shelf linked to Ordovician biodiversification;Nature Geoscience;2023-10-12

4. Stratigraphy, conodont biostratigraphy and correlation of the San Juan Formation (Lower-Middle Ordovician) in the Villicum Range, Eastern Precordillera, Argentina;Newsletters on Stratigraphy;2023-07-14

5. Coupled biostratigraphy and chemostratigraphy at Lanna, Sweden: A key section for the Floian–lower Darriwilian interval (Lower–Middle Ordovician);Palaeogeography, Palaeoclimatology, Palaeoecology;2023-04

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