Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef: The Role of Reefal Carbonate Chemistry and Environmental Variability

Oceanic pH is projected to decrease by up to 0.5 units by 2100 (a process known as ocean acidification, OA), reducing the calcium carbonate saturation state of the oceans. The coastal ocean is expected to experience periods of even lower carbonate saturation state because of the inherent natural var...

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Detalles Bibliográficos
Autores principales: Burdett, Heidi L., Donohue, Penelope J. C., Hatton, Angela D., Alwany, Magdy A., Kamenos, Nicholas A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2013
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3665749/
https://www.ncbi.nlm.nih.gov/pubmed/23724073
http://dx.doi.org/10.1371/journal.pone.0064651

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3665749/
https://www.ncbi.nlm.nih.gov/pubmed/23724073
http://dx.doi.org/10.1371/journal.pone.0064651

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