Works by Finzi, Adrien C.
Results: 63
Microbial Community Responses to Atmospheric Carbon Dioxide Enrichment in a Warm-Temperate Forest.
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- Ecosystems, 2006, v. 9, n. 2, p. 215, doi. 10.1007/s10021-005-0078-6
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Soil–Nitrogen Cycling in a Pine Forest Exposed to 5 Years of Elevated Carbon Dioxide.
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- Ecosystems, 2003, v. 6, n. 5, p. 444, doi. 10.1007/s10021-003-0205-1
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- Article
Roots Mediate the Effects of Snowpack Decline on Soil Bacteria, Fungi, and Nitrogen Cycling in a Northern Hardwood Forest.
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- Frontiers in Microbiology, 2019, p. N.PAG, doi. 10.3389/fmicb.2019.00926
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Identifying Data Needed to Reduce Parameter Uncertainty in a Coupled Microbial Soil C and N Decomposition Model.
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- Journal of Geophysical Research. Biogeosciences, 2021, v. 126, n. 12, p. 1, doi. 10.1029/2021JG006593
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A parsimonious modular approach to building a mechanistic belowground carbon and nitrogen model.
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- Journal of Geophysical Research. Biogeosciences, 2017, v. 122, n. 9, p. 2418, doi. 10.1002/2017JG003796
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Seasonal variation in the temperature sensitivity of proteolytic enzyme activity in temperate forest soils.
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- Journal of Geophysical Research. Biogeosciences, 2012, v. 117, n. G1, p. n/a, doi. 10.1029/2011JG001688
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Ecosystem responses to elevated CO<sub>2</sub> governed by plant-soil interactions and the cost of nitrogen acquisition.
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- New Phytologist, 2018, v. 217, n. 2, p. 507, doi. 10.1111/nph.14872
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Terrestrial nitrogen cycling in Earth system models revisited.
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- New Phytologist, 2016, v. 210, n. 4, p. 1165, doi. 10.1111/nph.13997
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Are above- and below-ground phenology in sync?
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- New Phytologist, 2015, v. 205, n. 3, p. 1054, doi. 10.1111/nph.13111
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Fungal functioning in a pine forest: evidence from a <sup>15</sup> N-labeled global change experiment.
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- New Phytologist, 2014, v. 201, n. 4, p. 1431, doi. 10.1111/nph.12578
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Carbon and nitrogen dynamics during forest stand development: a global synthesis.
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- New Phytologist, 2011, v. 190, n. 4, p. 977, doi. 10.1111/j.1469-8137.2011.03645.x
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Re-assessment of plant carbon dynamics at the Duke free-air CO<sub>2</sub> enrichment site: interactions of atmospheric [CO<sub>2</sub>] with nitrogen and water availability over stand development.
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- New Phytologist, 2010, v. 185, n. 2, p. 514, doi. 10.1111/j.1469-8137.2009.03078.x
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Deep peat warming increases surface methane and carbon dioxide emissions in a black spruce-dominated ombrotrophic bog.
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- Global Change Biology, 2017, v. 23, n. 12, p. 5398, doi. 10.1111/gcb.13806
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- Article
Does elevated CO<sub>2</sub> alter silica uptake in trees?
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- Frontiers in Plant Science, 2015, v. 5, p. 1, doi. 10.3389/fpls.2014.00793
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Inconsistent definitions of "urban" result in different conclusions about the size of urban carbon and nitrogen stocks.
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- Ecological Applications, 2012, v. 22, n. 3, p. 1015, doi. 10.1890/11-1250.1
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ATMOSPHERIC DEPOSITION MAY AFFECT NORTHERN HARDWOOD FOREST COMPOSITION BY ALTERING SOIL NUTRIENT SUPPLY.
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- Ecological Applications, 2007, v. 17, n. 7, p. 1929, doi. 10.1890/06-2067.1
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SOIL NITROGEN CYCLING UNDER ELEVATED CO<sub>2</sub>: A SYNTHESIS OF FOREST FACE EXPERIMENTS.
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- Ecological Applications, 2003, v. 13, n. 6, p. 1508, doi. 10.1890/03-5055
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Canopy tree-soil interactions within temperate forests: species effects on pH and cations.
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- Ecological Applications, 1998, v. 8, n. 2, p. 447, doi. 10.2307/2641084
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Canopy tree-soil interactions within temperate forests: Species effects on soil...
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- Ecological Applications, 1998, v. 8, n. 2, p. 440, doi. 10.2307/2641083
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PROGRESSIVE NITROGEN LIMITATION OF ECOSYSTEM PROCESSES UNDER ELEVATED CO2 IN A WARM-TEMPERATE FOREST.
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- Ecology, 2006, v. 87, n. 1, p. 15, doi. 10.1890/04-1748
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THE UPTAKE OF AMINO ACIDS BY MICROBES AND TREES IN THREE COLD-TEMPERATE FORESTS.
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- Ecology, 2005, v. 86, n. 12, p. 3345, doi. 10.1890/04-1460
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SOIL CARBON SEQUESTRATION AND TURNOVER IN A PINE FOREST AFTER SEX YEARS OF ATMOSPHERIC CO<sub>2</sub> ENRICHMENT.
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- Ecology, 2005, v. 86, n. 7, p. 1835, doi. 10.1890/04-1205
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FOREST LITTER PRODUCTION, CHEMISTRY, AND DECOMPOSITION FOLLOWING TWO YEARS OF FREE-AIR CO[sub 2]....
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- Ecology, 2001, v. 82, n. 2, p. 470, doi. 10.2307/2679873
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Assessing why two introduced conzya differ in their...
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- Ecology, 1996, v. 77, n. 3, p. 791, doi. 10.2307/2265502
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The Harvard Forest Carbon Budget: Patterns, Processes and Responses to Global Change.
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- Geophysical Research Abstracts, 2018, v. 20, p. 1437
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Mycorrhiza-mediated competition between plants and decomposers drives soil carbon storage.
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- Nature, 2014, v. 505, n. 7484, p. 543, doi. 10.1038/nature12901
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Carbon budget of the Harvard Forest Long‐Term Ecological Research site: pattern, process, and response to global change.
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- Ecological Monographs, 2020, v. 90, n. 4, p. 1, doi. 10.1002/ecm.1423
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Rhizosphere processes are quantitatively important components of terrestrial carbon and nutrient cycles.
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- Global Change Biology, 2015, v. 21, n. 5, p. 2082, doi. 10.1111/gcb.12816
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A big-microsite framework for soil carbon modeling.
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- Global Change Biology, 2014, v. 20, n. 12, p. 3610, doi. 10.1111/gcb.12718
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The effect of experimental warming and precipitation change on proteolytic enzyme activity: positive feedbacks to nitrogen availability are not universal.
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- Global Change Biology, 2012, v. 18, n. 8, p. 2617, doi. 10.1111/j.1365-2486.2012.02685.x
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Greater seed production in elevated CO<sub>2</sub> is not accompanied by reduced seed quality in Pinus taeda L.
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- Global Change Biology, 2010, v. 16, n. 3, p. 1046, doi. 10.1111/j.1365-2486.2009.02007.x
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Forest fine-root production and nitrogen use under elevated CO<sub>2</sub>: contrasting responses in evergreen and deciduous trees explained by a common principle.
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- Global Change Biology, 2009, v. 15, n. 1, p. 132, doi. 10.1111/j.1365-2486.2008.01710.x
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Soil carbon sequestration in a pine forest after 9 years of atmospheric CO<sub>2</sub> enrichment.
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- Global Change Biology, 2008, v. 14, n. 12, p. 2910, doi. 10.1111/j.1365-2486.2008.01701.x
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Fine root dynamics in a loblolly pine forest are influenced by free-air-CO<sub>2</sub>-enrichment: a six-year-minirhizotron study.
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- Global Change Biology, 2008, v. 14, n. 3, p. 588, doi. 10.1111/j.1365-2486.2007.01523.x
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Temporal dynamics and spatial variability in the enhancement of canopy leaf area under elevated atmospheric CO<sub>2</sub>.
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- Global Change Biology, 2007, v. 13, n. 12, p. 2479, doi. 10.1111/j.1365-2486.2007.01455.x
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Exposure to an enriched CO<sub>2</sub> atmosphere alters carbon assimilation and allocation in a pine forest ecosystem.
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- Global Change Biology, 2003, v. 9, n. 10, p. 1378, doi. 10.1046/j.1365-2486.2003.00662.x
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Species control variation in litter decomposition in a pine forest exposed to elevated CO<sub>2</sub>.
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- Global Change Biology, 2002, v. 8, n. 12, p. 1217, doi. 10.1046/j.1365-2486.2002.00551.x
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Primary productivity of planet earth: biological determinants and physical constraints in terrestrial and aquatic habitats.
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- Global Change Biology, 2001, v. 7, n. 8, p. 849, doi. 10.1046/j.1365-2486.2001.00448.x
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Belowground carbon flux links biogeochemical cycles and resource-use efficiency at the global scale.
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- Ecology Letters, 2016, v. 19, n. 12, p. 1419, doi. 10.1111/ele.12690
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Roots and fungi accelerate carbon and nitrogen cycling in forests exposed to elevated CO<sub>2</sub>.
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- Ecology Letters, 2012, v. 15, n. 9, p. 1042, doi. 10.1111/j.1461-0248.2012.01827.x
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Increases in the flux of carbon belowground stimulate nitrogen uptake and sustain the long-term enhancement of forest productivity under elevated CO.
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- Ecology Letters, 2011, v. 14, n. 4, p. 349, doi. 10.1111/j.1461-0248.2011.01593.x
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Enhanced root exudation induces microbial feedbacks to N cycling in a pine forest under long-term CO.
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- Ecology Letters, 2011, v. 14, n. 2, p. 187, doi. 10.1111/j.1461-0248.2010.01570.x
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Reduced snow cover alters root-microbe interactions and decreases nitrification rates in a northern hardwood forest.
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- Ecology, 2016, v. 97, n. 12, p. 3359, doi. 10.1002/ecy.1599
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Substrate supply, fine roots, and temperature control proteolytic enzyme activity th temperate forest soils.
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- Ecology, 2011, v. 92, n. 4, p. 892, doi. 10.1890/10-1803.1
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Ready or Not, Garlic Mustard Is Moving In: Alliaria petiolata as a Member of Eastern North American Forests.
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- BioScience, 2008, v. 58, n. 5, p. 426, doi. 10.1641/B580510
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Inverse analysis of coupled carbon--nitrogen cycles against multiple datasets at ambient and elevated CO<sub>2</sub>.
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- Journal of Plant Ecology, 2016, v. 9, n. 3, p. 285, doi. 10.1093/jpe/rtv059
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Canopy N and P dynamics of a southeastern US pine forest under elevated CO<sub>2</sub>.
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- Biogeochemistry, 2004, v. 69, n. 3, p. 363, doi. 10.1023/B:BIOG.0000031058.90586.2a
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Plant--soil interactions: ecological aspects and evolutionary implications
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- Biogeochemistry, 1998, v. 42, n. 1-2, p. 1, doi. 10.1023/a:1005962124317
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Ectomycorrhizal fungi are associated with reduced nitrogen cycling rates in temperate forest soils without corresponding trends in bacterial functional groups.
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- Oecologia, 2021, v. 196, n. 3, p. 863, doi. 10.1007/s00442-021-04966-z
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Microbial carbon use efficiency predicted from genome-scale metabolic models.
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- Nature Communications, 2019, v. 10, n. 1, p. N.PAG, doi. 10.1038/s41467-019-11488-z
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