Every reference with a DOI in the deposited reference list resolved to a known
work in Crossref or DataCite at the dated check, and none carried a retraction,
withdrawal, or removal notice.
The 68 checked references that resolve
resolves10.5194/bg-17-3859-2020Reviews and syntheses: Soil responses to manipulated precipitation changes – an assessment of meta-analyses
resolves10.1002/2013JG002400Carbon isotopes for estimating soil decomposition and physical mixing in well‐drained forest soils
resolves10.1111/gcb.14548Soil organic carbon stability in forests: Distinct effects of tree species identity and traits
resolves10.1029/2001GB001822Turnover and storage of C and N in five density fractions from California annual grassland surface soils
resolves10.1051/forest:2006042Temperate forest trees and stands under severe drought: a review of ecophysiological responses, adaptation processes and long-term consequences
resolves10.1002/jpln.201700015Three decades following afforestation are sufficient to yield δ<sup>13</sup>C depth profiles
resolves10.1111/nph.18157Carbon allocation to root exudates is maintained in mature temperate tree species under drought
resolves10.1016/j.soilbio.2020.107969Physical mechanisms for soil moisture effects on microbial carbon-use efficiency in a sandy loam soil in the western United States
resolves10.5194/gmd-11-937-2018ORCHIDEE-SOM: modeling soil organic carbon (SOC) and dissolved organic carbon (DOC) dynamics along vertical soil profiles in Europe
resolves10.1111/gcb.12982Integrating plant litter quality, soil organic matter stabilization, and the carbon saturation concept
resolves10.1002/rcm.5129Guidelines and recommended terms for expression of stable‐isotope‐ratio and gas‐ratio measurement results
resolves10.1111/gcb.12113The
<scp>M</scp>
icrobial
<scp>E</scp>
fficiency‐
<scp>M</scp>
atrix
<scp>S</scp>
tabilization (
<scp>MEMS</scp>
) framework integrates plant litter decomposition with soil organic matter stabilization: do labile plant inputs form stable soil organic matter?
resolves10.1007/s10533-007-9100-8Density fractionation of forest soils: methodological questions and interpretation of incubation results and turnover time in an ecosystem context
resolves10.1016/j.catena.2019.104091Small altitudinal change and rhizosphere affect the SOM light fractions but not the heavy fraction in European beech forest soil
resolves10.1111/gcb.12816Rhizosphere processes are quantitatively important components of terrestrial carbon and nutrient cycles
resolves10.1071/SR9940285Study of free and occluded particulate organic matter in soils by solid state 13C Cp/MAS NMR spectroscopy and scanning electron microscopy
resolves10.1002/ecs2.3399The Kroof experiment: realization and efficacy of a recurrent drought experiment plus recovery in a beech/spruce forest
resolves10.1016/j.foreco.2013.03.014Organic layer and clay content control soil organic carbon stocks in density fractions of differently managed German beech forests
resolves10.1111/gcb.12558Organic carbon stocks and sequestration rates of forest soils in <scp>G</scp>ermany
resolves10.1016/j.orggeochem.2006.05.002Organic matter stabilization in young calcareous soils as revealed by density fractionation and analysis of lignin-derived constituents
resolves10.1111/plb.12461Impact of interspecific competition and drought on the allocation of new assimilates in trees
resolves10.1073/pnas.2014084117Rhizosphere activity in an old-growth forest reacts rapidly to changes in soil moisture and shapes whole-tree carbon allocation
resolves10.1111/ele.13651Root‐derived inputs are major contributors to soil carbon in temperate forests, but vary by mycorrhizal type
resolves10.1007/s10705-007-9147-xSoil carbon stocks under present and future climate with specific reference to European ecoregions
resolves10.1111/gcb.14859Conceptualizing soil organic matter into particulate and mineral‐associated forms to address global change in the 21st century
resolves10.1016/j.soilbio.2017.12.006Multiple exchange processes on mineral surfaces control the transport of dissolved organic matter through soil profiles
resolves10.1007/s10533-020-00721-3The linkage of 13C and 15N soil depth gradients with C:N and O:C stoichiometry reveals tree species effects on organic matter turnover in soil
resolves10.5194/bg-15-5929-2018Reviews and syntheses: Carbon use efficiency from organisms to ecosystems – definitions, theories, and empirical evidence
resolves10.1111/nph.16389Root exudation of mature beech forests across a nutrient availability gradient: the role of root morphology and fungal activity
resolves10.1016/j.soilbio.2013.01.002Responses of soil heterotrophic respiration to moisture availability: An exploration of processes and models
resolves10.3389/fpls.2021.715127Leaf Shedding and Non-Stomatal Limitations of Photosynthesis Mitigate Hydraulic Conductance Losses in Scots Pine Saplings During Severe Drought Stress
resolves10.1111/j.1365-2389.2012.01465.xCarbon isotopes of water‐extractable organic carbon in a depth profile of forest soil imply a dynamic relationship with soil carbon
resolves10.1111/gcb.13957Quantitative losses vs. qualitative stability of ectomycorrhizal community responses to 3 years of experimental summer drought in a beech–spruce forest
resolves10.1007/s11104-006-9120-5Recent carbon and nitrogen accumulation and acidification in soils of two Scots pine ecosystems in Southern Germany
resolves10.1073/pnas.1216053111Temperature drives global patterns in forest biomass distribution in leaves, stems, and roots
resolves10.4155/cmt.13.77Global soil carbon: understanding and managing the largest terrestrial carbon pool
resolves10.5194/bg-10-1675-2013Storage and stability of organic carbon in soils as related to depth, occlusion within aggregates, and attachment to minerals
resolves10.1111/nph.15361Evidence for the primacy of living root inputs, not root or shoot litter, in forming soil organic carbon
resolves10.1007/s10533-009-9359-zSequential density fractionation across soils of contrasting mineralogy: evidence for both microbial- and mineral-controlled soil organic matter stabilization
resolves10.1111/1365-2435.13236Mycelia‐derived C contributes more to nitrogen cycling than root‐derived C in ectomycorrhizal alpine forests
The 20 references without a DOI — listed, not checked
no DOI — not checkedref7
no DOI — not checkedLessons learned from a long-term irrigation experiment in a dry Scots pine forest: Impacts on traits and functioning
no DOI — not checkedHow tree roots respond to drought
no DOI — not checkedWater for Carbon
no DOI — not checkedConversion of cropland into grassland: Implications for soil organic-carbon stocks in two soils with different texture
no DOI — not checkedEffects of mixing tree species and water availability on soil organic carbon stocks are depth dependent in a temperate podzol
no DOI — not checkedCase Study "Kranzberger Forst
no DOI — not checkedref39
no DOI — not checkedBeyond bulk: Density fractions explain heterogeneity in global soil carbon abundance and persistence
no DOI — not checkedClimate Change and Land: an IPCC special report on climate change, desertification, land degradation, sustainable land management, food security, and greenhouse gas fluxes in terrestrial ecosystems
no DOI — not checkedref45
no DOI — not checkedStable isotopes reveal that fungal residues contribute more to mineral-associated organic matter pools than plant residues
no DOI — not checkedref49
no DOI — not checkedTowards improved modeling of SOC decomposition: soil water potential beyond the wilting point
no DOI — not checkedTo transform or not to transform: using generalized linear mixed models to analyse reaction time data
no DOI — not checkedPredicting Soil Organic Carbon Mineralization Rates Using ?13C, Assessed by Near-Infrared Spectroscopy, in Depth Profiles Under Permanent Grassland Along a Latitudinal Transect in Chile
no DOI — not checkedImpact of European Beech Forest Diversification on Soil Organic Carbon and Total Nitrogen Stocks-A Meta
no DOI — not checkedGlobal distribution, formation and fate of mineral-associated soil organic matter under a changing climate: A trait-based perspective
no DOI — not checkedref82
no DOI — not checkedTopsoil organic carbon increases but its stability declines after five years of reduced throughfall
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