Increased fluvial runoff terminated inorganic aragonite precipitation on the Northwest Shelf of Australia during the early Holocene

Inorganic precipitation of aragonite is a common process within tropical carbonate environments. Across the Northwest Shelf of Australia (NWS) such precipitates were abundant in the late Pleistocene, whereas present-day sedimentation is dominated by calcitic bioclasts. This study presents sedimentol...

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Detalles Bibliográficos
Autores principales: Hallenberger, Maximilian, Reuning, Lars, Gallagher, Stephen J., Back, Stefan, Ishiwa, Takeshige, Christensen, Beth A., Bogus, Kara
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6892919/
https://www.ncbi.nlm.nih.gov/pubmed/31797994
http://dx.doi.org/10.1038/s41598-019-54981-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6892919/
https://www.ncbi.nlm.nih.gov/pubmed/31797994
http://dx.doi.org/10.1038/s41598-019-54981-7

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