Please use this identifier to cite or link to this item:
logo share SHARE BASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE

Shifting stoichiometry: Long-term trends in stream-dissolved organic matter reveal altered C:N ratios due to history of atmospheric acid deposition

AuthorsRodríguez-Cardona, Bianca M.; Wymore, Adam S.; Argerich, Alba; Barnes, Rebecca T.; Bernal, Susana CSIC ORCID ; Brookshire, E. N. Jack; Coble, A. A.; Dodds, W. K.; Fazekas, Hannah M.; Helton, A. M.; Johnes, Penny J.; Johnson, S. L.; Jones, J. B.; Kaushal, S. S.; Kortelainen, Pirkko; López-Lloreda, Carla; Spencer, Robert G. M.; McDowell, W. H.
Keywordsatmospheric acid deposition
C:N stoichiometry
dissolved organic carbon
dissolved organic matter
dissolved organic nitrogen
long-term trends
Issue Date2021
PublisherJohn Wiley & Sons
CitationGlobal Change Biology : doi:10.1111/gcb.15965 (2021)
AbstractDissolved organic carbon (DOC) and nitrogen (DON) are important energy and nutrient sources for aquatic ecosystems. In many northern temperate, freshwater systems DOC has increased in the past 50 years. Less is known about how changes in DOC may vary across latitudes, and whether changes in DON track those of DOC. Here, we present long-term DOC and DON data from 74 streams distributed across seven sites in biomes ranging from the tropics to northern boreal forests with varying histories of atmospheric acid deposition. For each stream, we examined the temporal trends of DOC and DON concentrations and DOC:DON molar ratios. While some sites displayed consistent positive or negative trends in stream DOC and DON concentrations, changes in direction or magnitude were inconsistent at regional or local scales. DON trends did not always track those of DOC, though DOC:DON ratios increased over time for ~30% of streams. Our results indicate that the dissolved organic matter (DOM) pool is experiencing fundamental changes due to the recovery from atmospheric acid deposition. Changes in DOC:DON stoichiometry point to a shifting energynutrient balance in many aquatic ecosystems. Sustained changes in the character of DOM can have major implications for stream metabolism, biogeochemical processes, food webs, and drinking water quality (including disinfection by-products). Understanding regional and global variation in DOC and DON concentrations is important for developing realistic models and watershed management protocols to effectively target mitigation efforts aimed at bringing DOM flux and nutrient enrichment under control.
DescriptionEste artículo contiene 17 páginas, 6 figuras, 2 tablas.
Publisher version (URL)
Appears in Collections:(CEAB) Artículos

Files in This Item:
File Description SizeFormat
Rodríguez-Cardona 2021.pdf1,09 MBAdobe PDFThumbnail
Show full item record
Review this work

Page view(s)

checked on Jan 22, 2022


checked on Jan 22, 2022

Google ScholarTM


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.