2019
DOI: 10.5061/dryad.v2k2607
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Data from: Isotopic evidence for oligotrophication of terrestrial ecosystems

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(2 citation statements)
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“…We extracted foliar d 15 N and [N] data from Craine et al (2018) (Craine et al, 2019), in which each d 15 N and [N] value represents an average for a given species at a given site (defined by 0.1°l atitude/longitude or c. 11 km) in 1 yr. We subsampled this data to only include EM and AM plants in the United States (n = 2138: n EM = 845, n AM = 1293, n species = 299). While we were initially only interested in trees, data from AM trees were far less abundant than EM trees, resulting in an imbalanced dataset.…”
Section: Spatial Foliar D 15 N Analysis: Data Compilationmentioning
confidence: 99%
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“…We extracted foliar d 15 N and [N] data from Craine et al (2018) (Craine et al, 2019), in which each d 15 N and [N] value represents an average for a given species at a given site (defined by 0.1°l atitude/longitude or c. 11 km) in 1 yr. We subsampled this data to only include EM and AM plants in the United States (n = 2138: n EM = 845, n AM = 1293, n species = 299). While we were initially only interested in trees, data from AM trees were far less abundant than EM trees, resulting in an imbalanced dataset.…”
Section: Spatial Foliar D 15 N Analysis: Data Compilationmentioning
confidence: 99%
“…Specifically, we tested whether (1) plant and fungal N concentrations and d 15 N declined in an area experiencing CO 2 rise and increasing N deposition and (2) trajectories of plant d 15 N and N concentrations diverged by mycorrhizal type. We also analyzed a subset of previously published foliar d 15 N values (Craine et al, 2019) to parse the effects of CO 2 rise, N deposition, and mycorrhizal controls of d 15 N. In this second dataset, we tested the extent to which (1) CO 2 rise or N deposition explains declines in foliar d 15 N and (2) d 15 N trajectories diverged by mycorrhizal type with CO 2 rise or N deposition.…”
Section: Introductionmentioning
confidence: 99%