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dc.contributor.authorYano, Yuriko
dc.contributor.authorBrookshire, E.N. Jack
dc.contributor.authorHolsinger, J.
dc.contributor.authorWeaver, Tad
dc.date.accessioned2015-12-28T22:59:03Z
dc.date.available2015-12-28T22:59:03Z
dc.date.issued2015-05
dc.identifier.citationYano, Y., E. N. Jack Brookshire, Holsinger J., and Tad Weaver. "Long-term snowpack manipulation promotes large loss of bioavailable nitrogen and phosphorus in a subalpine grassland." Biogeochemistry 124, no. 1 (May 2015): 319-333. DOI:https://dx.doi.org/10.1007/s10533-015-0100-9.en_US
dc.identifier.issn0168-2563
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/9469
dc.description.abstractNutrient retention in ecosystems requires synchrony between the supply of bioavailable nutrients released via mineralization and nutrient uptake by plants. Though disturbance and chronic nutrient loading are known to alter nitrogen (N) and phosphorus (P) dynamics and induce nutrient export, whether long-term shifts in climate affect source-sink synchrony, and ultimately primary productivity, remains uncertain. This is particularly true for snow-dominated ecosystems, which are naturally subject to lags between nutrient inputs and uptake. To address how climate change may affect nutrient source-sink synchrony we examined the impacts of deepened snowpack on N and P losses in a subalpine grassland in the Northern Rocky Mountains, USA, where we have experimentally increased snowpack depths by two- and four-times ambient snow for 45 years. Long-term snow addition resulted in remarkably high levels of bioavailable-N leaching (up to 16 kg ha^-1 year^-1) that were 11-80 times higher than those under ambient snowpack. Estimated bioavailable-P losses also increased with snow addition, but to a lesser degree (up to 0.3 kg ha^-1 year^-1), indicating greater enhancement of N losses over P losses during snowmelt. Because these losses could not be explained by changes in nutrient inputs in snowpack or by changes in plant-soil turnover, our results suggest that high bioavailable-N leaching under deep snowpack originates not from a lack of N limitation of plant productivity, but rather from enhanced subnivean microbial processes followed by snowmelt leaching prior to the growing season. This is supported by reduced soil N pools in the snow treatments. Snow-dominated regions are projected to experience shifts in seasonal snowpack regime. These shifts may ultimately affect the stoichiometric balance between available N and P and future plant productivity.en_US
dc.titleLong-term snowpack manipulation promotes large loss of bioavailable nitrogen and phosphorus in a subalpine grasslanden_US
dc.typeArticleen_US
mus.citation.extentfirstpage319en_US
mus.citation.extentlastpage333en_US
mus.citation.issue1en_US
mus.citation.journaltitleBiogeochemistryen_US
mus.citation.volume124en_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doi10.1007/s10533-015-0100-9en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.collegeCollege of Letters & Scienceen_US
mus.relation.departmentEcology.en_US
mus.relation.departmentLand Resources & Environmental Sciences.en_US
mus.relation.universityMontana State University - Bozemanen_US


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