Convergence of soil nitrogen isotopes across global climate gradients

Quantifying global patterns of terrestrial nitrogen (N) cycling is central to predicting future patterns of primary productivity, carbon sequestration, nutrient fluxes to aquatic systems, and climate forcing. With limited direct measures of soil N cycling at the global scale, syntheses of the 15N:14...

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Detalles Bibliográficos

Autores principales:	Craine, Joseph M., Elmore, Andrew J., Wang, Lixing, Augusto, Laurent, Baisden, Troy, Brookshire, E.N.J., Cramer, Michael D., Hasselquist, Niles, Hobbie, Erik A., Kahmen, Ansgar, Kaba, Keisuke, Kranabetter, M., Mack, M., Marin-Spiotta, E., Mayor, J.R., McLauchlan, K.K., Michelsen, A., Nardoto, G.B., Oliveira, R.S., Perakis, S.S., Peri, Pablo Luis, Quesada, C., Richter, A., Schipper, L.A., Stevenson, B.A., Turner, B.L., Viani, R.A.G., Wanek, W., Zeller, B.
Formato:	Artículo
Lenguaje:	Inglés
Publicado:	2017
Materias:	Suelo Soil Climatic Factors Nitrogen Isotopes Carbon Factores Climáticos Nitrógeno Isótopos Carbono
Acceso en línea:	http://hdl.handle.net/20.500.12123/1132 https://www.nature.com/articles/srep08280 https://doi.org/10.1038/srep08280