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Proglacial freshwaters are significant and previously unrecognized sinks of atmospheric CO(2)
Carbon dioxide (CO(2)) emissions from freshwater ecosystems are almost universally predicted to increase with climate warming. Glacier-fed rivers and lakes, however, differ critically from those in nonglacierized catchments in that they receive little terrestrial input of organic matter for decompos...
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| Publicado no: | Proc Natl Acad Sci U S A |
|---|---|
| Main Authors: | , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2019
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6731667/ https://ncbi.nlm.nih.gov/pubmed/31427515 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1904241116 |
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