ArticleNature communications2022
Ordovician-Silurian true polar wander as a mechanism for severe glaciation and mass extinction.
Article in Nature communications, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 papers.
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
4 citing papers in PubMed.
- Devonian northward drift of the Qaidam-Kunlun continent constrains the early evolution of the Paleo-Tethys Ocean.National science review · 2026Article
- Tempo of the Late Ordovician mass extinction controlled by the rate of climate change.Science advances · 2025Article
- Maintenance of the great late Ediacaran ice age.Nature communications · 2025Article
- In-situ δScientific reports · 2023Article
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Authors and funding
6 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The Ordovician-Silurian transition experienced severe, but enigmatic, glaciation, as well as a paradoxical combination of mass extinction and species origination. Here we report a large and fast true polar wander (TPW) event that occurred 450-440 million years ago based on palaeomagnetic data from South China and compiled reliable palaeopoles from all major continents. Collectively, a ~50˚ wholesale rotation with maximum continental speeds of ~55 cm yr
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