The human footprint in the carbon cycle of temperate and boreal forests

By Federico Magnani, Maurizio Mencuccini, M. Borghetti, P. Berbigier, Frank Berninger, Sylvain Delzon, A. Grelle, Pertti Hari, P. Jarvis, P. Kolari and 11 more. Nature, 2007

984 citations recorded by the source corpus.

Subfields: Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/48379f44c1fd00f340d196f14de4e4be368c814d

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Citations in the corpus

Contrasting effects of low and high nitrogen additions on soil CO2 flux components and ectomycorrhizal fungal sporocarp production in a boreal forest (2012, background): “In that study, a negative effect of N fertilizer on the respi- ration of EM hyphae was found using high N addition, as was also seen in a N-addition experiment in temper- ate forest (Nilsson & Wallander, 2003).”
Evaluation of terrestrial carbon cycle models for their response to climate variability and to CO2 trends (2013, neutral): “However, it should be noted that since other factors such as ecosystem management and nitrogen deposition could also explain the trend of RLS over the last three decades (Zaehle et al., 2006; Magnani et al., 2007; Ciais et al., 2008; Bellassen et al., 2010; Zaehle & Dalmonech, 2011), the sensitivity”
Microbial contributions to climate change through carbon cycle feedbacks (2008, background): “Many interacting factors affect the sink activity of terrestrial ecosystems, including natural and anthropo- genic disturbances (Magnani et al., 2007), agricultural land use (Smith et al., 2008), nitrogen (N) enrichment (Beedlow et al., 2004), sulphur deposition (Monteith et al., 2007) and changes…”
Nitrogen addition stimulates forest litter decomposition and disrupts species interactions in Patagonia, Argentina (2011, background): “Increases in N availably due to N deposition have stimulated forest growth (Magnani et al., 2007; Thomas et al., 2010) and decreased organic matter decomposition in temperate forests of industrialized areas of the Northern Hemisphere (Janssens et al., 2010).”
Climate control of terrestrial carbon exchange across biomes and continents (2010, background): “…M, Aurela, M, Barcza, Z, Barr, A, Berbigier, P, Beringer, J, Bernhofer, C, Black, AT, Bolstad, PV, Bosveld, FC, Broadmeadow, MSJ, Buchmann, N, Burns, SP, Cellier, P, Chen, J, Chen, J, Ciais, P, Clement, R, Cook, BD, Curtis, PS, Dail, DB, Dellwik, E, Delpierre, N, Desai, AR, Dore, S, Dragoni,”
Geostatistical estimation of forest biomass in interior Alaska combining Landsat-derived tree cover, sampled airborne lidar and field observations (2017, background): “Understanding that the taiga-tundra ecotone is one of the most vulnerable environmental systems to climate change and that its boreal forests can contribute substantially to the global carbon cycle, methods are needed to begin monitoring forest carbon stocks and fluxes for these systems (Gauthier et”
Fluxes of dissolved organic and inorganic nitrogen in relation to stand characteristics and latitude in Scots pine and Norway spruce stands in Finland (2008, background): “This can, to some extent, mitigate the rise in atmospheric CO2 concentrations by stimulating the sequestration of carbon in biomass (Townsend et al. 1996, Magnani et al. 2007).”
Carbon cost of plant nitrogen acquisition: A mechanistic, globally applicable model of plant nitrogen uptake, retranslocation, and fixation (2010, background): “[2] Nitrogen (N) controls plant growth and net primary productivity (NPP) in most terrestrial ecosystems and is tightly coupled with the global carbon (C) cycle [Lloyd, 1999; Magnani et al., 2007; Vitousek and Howarth, 1991].”