11 citations as recorded by crossref.

1. Cushion bogs are stronger carbon dioxide net sinks than moss-dominated bogs as revealed by eddy covariance measurements on Tierra del Fuego, Argentina D. Holl et al. 10.5194/bg-16-3397-2019
2. Methane fluxes but not respiratory carbon dioxide fluxes altered under Si amendment during drying – rewetting cycles in fen peat mesocosms A. Hömberg et al. 10.1016/j.geoderma.2021.115338
3. Element mobility related to rock weathering and soil formation at the westward side of the southernmost Patagonian Andes B. Klaes et al. 10.1016/j.scitotenv.2022.152977
4. Divergent effect of silicon on greenhouse gas production from reduced and oxidized peat organic matter A. Hömberg et al. 10.1016/j.geoderma.2020.114916
5. A Microbial Functional Group‐Based CH 4 Model Integrated Into a Terrestrial Ecosystem Model: Model Structure, Site‐Level Evaluation, and Sensitivity Analysis C. Song et al. 10.1029/2019MS001867
6. Influence of land-use change and season on soil greenhouse gas emissions from a tropical wetland: A stepwise explorative assessment R. Ondiek et al. 10.1016/j.scitotenv.2021.147701
7. Control of carbon and nitrogen accumulation by vegetation in pristine bogs of southern Patagonia W. Schuster et al. 10.1016/j.scitotenv.2021.151293
8. Plant mediated methane efflux from a boreal peatland complex A. Korrensalo et al. 10.1007/s11104-021-05180-9
9. A 14,000 year peatland record of environmental change in the southern Gutland region, Luxembourg K. Schittek et al. 10.1177/0959683621994645
10. Cushion bog plant community responses to passive warming in southern Patagonia V. Pancotto et al. 10.5194/bg-18-4817-2021
11. Plant communities control long term carbon accumulation and biogeochemical gradients in a Patagonian bog P. Mathijssen et al. 10.1016/j.scitotenv.2019.05.310