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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Bibliographic Details

Main Authors:	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.
Format:	Artículo
Language:	Inglés
Published:	2017
Subjects:	Suelo Soil Climatic Factors Nitrogen Isotopes Carbon Factores Climáticos Nitrógeno Isótopos Carbono
Online Access:	http://hdl.handle.net/20.500.12123/1132 https://www.nature.com/articles/srep08280 https://doi.org/10.1038/srep08280