26 citations as recorded by crossref.

1. Factors controlling labile soil organic matter vulnerability to loss following disturbance as assessed by measurement of soil‐respired δ13CO2 A. Zakharova et al. 10.1111/ejss.12209
2. Temperature-mediated changes in microbial carbon use efficiency and 13C discrimination C. Lehmeier et al. 10.5194/bg-13-3319-2016
3. Gross primary production responses to warming, elevated CO2, and irrigation: quantifying the drivers of ecosystem physiology in a semiarid grassland E. Ryan et al. 10.1111/gcb.13602
4. Bulk and isotopic characterization of biogenic CO2 sources and variability in the Weyburn injection area D. Risk et al. 10.1016/j.ijggc.2013.02.024
5. Progress and challenges in using stable isotopes to trace plant carbon and water relations across scales C. Werner et al. 10.5194/bg-9-3083-2012
6. An inorganic CO2 diffusion and dissolution process explains negative CO2 fluxes in saline/alkaline soils J. Ma et al. 10.1038/srep02025
7. Carbon allocation and carbon isotope fluxes in the plant-soil-atmosphere continuum: a review N. Brüggemann et al. 10.5194/bg-8-3457-2011
8. Persistent wind-induced enhancement of diffusive CO2transport in a mountain forest snowpack D. Bowling & W. Massman 10.1029/2011JG001722
9. Isotope characterisation of deep aquifers in the Gwda catchment, northern Poland T. Kotowski & S. Satora 10.1515/logos-2016-0014
10. Modeling soil CO2 production and transport to investigate the intra-day variability of surface efflux and soil CO2 concentration measurements in a Scots Pine Forest (Pinus Sylvestris, L.) S. Goffin et al. 10.1007/s11104-015-2381-0
11. Environmental forcing does not induce diel or synoptic variation in the carbon isotope content of forest soil respiration D. Bowling et al. 10.5194/bg-12-5143-2015
12. Characterization of the soil CO2 production and its carbon isotope composition in forest soil layers using the flux-gradient approach S. Goffin et al. 10.1016/j.agrformet.2013.11.005
13. A downward CO2 flux seems to have nowhere to go J. Ma et al. 10.5194/bg-11-6251-2014
14. Loss of labile carbon following soil disturbance determined by measurement of respired ∂13CO2 A. Zakharova et al. 10.1016/j.soilbio.2013.10.001
15. Partitioning NEE for absolute C input into various ecosystem pools by combining results from eddy-covariance, atmospheric flux partitioning and 13CO2 pulse labeling M. Riederer et al. 10.1007/s11104-014-2371-7
16. Drought alters respired δ13CO2 from autotrophic, but not heterotrophic soil respiration D. Risk et al. 10.1016/j.soilbio.2012.01.025
17. Isotope partitioning of soil respiration: A Bayesian solution to accommodate multiple sources of variability K. Ogle & E. Pendall 10.1002/2014JG002794
18. Inter-comparison of three models for δ 13 C of respiration with four regression approaches C. Chen et al. 10.1016/j.agrformet.2017.08.002
19. The effect of physical back-diffusion of13CO2tracer on the coupling between photosynthesis and soil CO2efflux in grassland S. Burri et al. 10.1080/10256016.2014.893237
20. Carbon dynamics in aboveground biomass of co‐dominant plant species in a temperate grassland ecosystem: same or different? U. Ostler et al. 10.1111/nph.13800
21. Autotrophic component of soil respiration is repressed by drought more than the heterotrophic one in dry grasslands J. Balogh et al. 10.5194/bg-13-5171-2016
22. Interannual variation in seasonal drivers of soil respiration in a semi-arid Rocky Mountain meadow A. Moyes & D. Bowling 10.1007/s10533-012-9797-x
23. Iso-FD: A novel method for measuring the isotopic signature of surface flux N. Nickerson et al. 10.1016/j.soilbio.2013.03.010
24. Subsurface approaches for measuring soil CO2isotopologue flux: Theory and application N. Nickerson et al. 10.1002/2013JG002508
25. Effects of Warming and Precipitation on Soil CO2 Flux and Its Stable Carbon Isotope Composition in the Temperate Desert Steppe N. Guo et al. 10.3390/su14063351
26. Dual-chamber measurements of δ13C of soil-respired CO2 partitioned using a field-based three end-member model F. Albanito et al. 10.1016/j.soilbio.2011.12.011