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dc.contributor.authorButler, Sarah M.  Concept link
dc.contributor.authorMelillo, Jerry M.  Concept link
dc.contributor.authorJohnson, J. E.  Concept link
dc.contributor.authorMohan, Jacqueline E.  Concept link
dc.contributor.authorSteudler, Paul A.  Concept link
dc.contributor.authorLux, H.  Concept link
dc.contributor.authorBurrows, E.  Concept link
dc.contributor.authorSmith, R. M.  Concept link
dc.contributor.authorVario, C. L.  Concept link
dc.contributor.authorScott, Lindsay  Concept link
dc.contributor.authorHill, T. D.  Concept link
dc.contributor.authorAponte, N.  Concept link
dc.contributor.authorBowl, F.  Concept link
dc.date.accessioned2012-04-19T14:52:59Z
dc.date.available2012-04-19T14:52:59Z
dc.date.issued2011-10-05
dc.identifier.citationOecologia 168 (2012): 819-828en_US
dc.identifier.urihttps://hdl.handle.net/1912/5137
dc.description© The Author(s), 2011. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Oecologia 168 (2012): 819-828, doi:10.1007/s00442-011-2133-7.en_US
dc.description.abstractGlobal climate change is expected to affect terrestrial ecosystems in a variety of ways. Some of the more well-studied effects include the biogeochemical feedbacks to the climate system that can either increase or decrease the atmospheric load of greenhouse gases such as carbon dioxide and nitrous oxide. Less well-studied are the effects of climate change on the linkages between soil and plant processes. Here, we report the effects of soil warming on these linkages observed in a large field manipulation of a deciduous forest in southern New England, USA, where soil was continuously warmed 5°C above ambient for 7 years. Over this period, we have observed significant changes to the nitrogen cycle that have the potential to affect tree species composition in the long term. Since the start of the experiment, we have documented a 45% average annual increase in net nitrogen mineralization and a three-fold increase in nitrification such that in years 5 through 7, 25% of the nitrogen mineralized is then nitrified. The warming-induced increase of available nitrogen resulted in increases in the foliar nitrogen content and the relative growth rate of trees in the warmed area. Acer rubrum (red maple) trees have responded the most after 7 years of warming, with the greatest increases in both foliar nitrogen content and relative growth rates. Our study suggests that considering species-specific responses to increases in nitrogen availability and changes in nitrogen form is important in predicting future forest composition and feedbacks to the climate system.en_US
dc.description.sponsorshipThis work was supported by the National Institute for Climate Change Research (DOE-DE-FCO2-06-ER64157), DOE BER (DE-SC0005421) and the Harvard Forest Long-Term Ecological Research program (NSF-DEB-0620443).en_US
dc.format.mimetypeapplication/msword
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherSpringeren_US
dc.relation.urihttps://doi.org/10.1007/s00442-011-2133-7
dc.rightsAttribution-NonCommercial 3.0 Unported*
dc.rights.urihttp://creativecommons.org/licenses/by-nc/3.0/*
dc.titleSoil warming alters nitrogen cycling in a New England forest : implications for ecosystem function and structureen_US
dc.typeArticleen_US
dc.identifier.doi10.1007/s00442-011-2133-7


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Except where otherwise noted, this item's license is described as Attribution-NonCommercial 3.0 Unported