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Climatic, physical, and biogeochemical changes drive rapid oxygen loss and recovery in a marine ecosystem
Dissolved oxygen (DO) concentrations shape the biogeochemistry and ecological structure of aquatic ecosystems; as a result, understanding how and why DO varies in space and time is of fundamental importance. Using high-resolution, in situ DO time-series collected over the course of a year in a novel...
Autores principales: | , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6834605/ https://www.ncbi.nlm.nih.gov/pubmed/31695057 http://dx.doi.org/10.1038/s41598-019-52430-z |