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1. Quantifying ecosystem services of rewetted peatlands − the MoorFutures methodologies

2. Rewetting does not return drained fen peatlands to their old selves

3. Denial of long-term issues with agriculture on tropical peatlands will have devastating consequences

4. Greenhouse gas emission factors associated with rewetting of organic soils

5. Die neuen MoorFutures - Kohlenstoffzertifikate mit ökologischen Zusatzleistungen. The new MoorFutures - carbon credits including additional ecosystem services

6. Klimaschutz durch Wiedervernässung von kohlenstoffreichen Böden

7. Investing in nature: Developing ecosystem service markets for peatland restoration

8. Peatlands and biodiversity

10. Towards robust subsidence-based soil carbon emission factors for peat soils in south-east Asia, with special reference to oil palm plantations.

11. Towards developing IPCC methane 'emission factors' for peatlands (organic soils).

12. Greenhouse gas emissions from managed peat soils: is the IPCC reporting guidance realistic?

13. Hydrological self-regulation of domed peatlands in south-east Asia and consequences for conservation and restoration.

14. FOREWORD.

15. Plant roots but not hydrology control microbiome composition and methane flux in temperate fen mesocosms.

16. Active afforestation of drained peatlands is not a viable option under the EU Nature Restoration Law.

18. The unexpected long period of elevated CH 4 emissions from an inundated fen meadow ended only with the occurrence of cattail (Typha latifolia).

19. Long-term rewetting of degraded peatlands restores hydrological buffer function.

20. Long-Term Rewetting of Three Formerly Drained Peatlands Drives Congruent Compositional Changes in Pro- and Eukaryotic Soil Microbiomes through Environmental Filtering.

21. Prompt rewetting of drained peatlands reduces climate warming despite methane emissions.

22. A radiative forcing analysis of tropical peatlands before and after their conversion to agricultural plantations.

23. Denial of long-term issues with agriculture on tropical peatlands will have devastating consequences.

24. Carbon accumulation in a permafrost polygon peatland: steady long-term rates in spite of shifts between dry and wet conditions.

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