Devonian to Carboniferous continental-scale carbonate turnover in Western Laurentia (North America): upwelling or climate cooling?

The Devonian to Carboniferous (DC) transition coincided with a green-to-ice house climatic shift, anoxia, disappearance of lower latitude carbonate banks, and turnover from warm-to-cool water carbonate factories. In western Laurentia, the switch to carbonate factories dominated by cool-water biota w...

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Detalles Bibliográficos
Autores principales: Hedhli, Makram, Dewing, Keith, Beauchamp, Benoit, Grasby, Stephen E., Meyer, Rudi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2022
Materias:
Original Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9314305/
https://www.ncbi.nlm.nih.gov/pubmed/35910009
http://dx.doi.org/10.1007/s10347-022-00653-4

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9314305/
https://www.ncbi.nlm.nih.gov/pubmed/35910009
http://dx.doi.org/10.1007/s10347-022-00653-4

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