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	1	Soil drying with experimental warming depends on ecosystem type and warming method: First results of the Soil Warming to Depth Data Integration Effort (SWEDDIE) Enthalten in Earth system science data discussions 20.02.2026: 1-28. 28 S.
	2	Subsoil particulate organic matter is more responsive to 10 years of whole–soil warming than mineral–associated organic matter in a temperate forest Enthalten in EGUsphere 14.11.2025: 1-32. 32 S.
	3	Warming accelerates the decomposition of root-derived hydrolysable lipids in a temperate forest and is depth- and compound class-dependent Enthalten in Soil Bd. 11, 2025, Nr. 2: 1077-1093. 17 S.
	4	Nine years of warming and nitrogen addition in the Tibetan grassland promoted loss of soil organic carbon but did not alter the bulk change in chemical structure Enthalten in Biogeosciences Bd. 21, 2024, Nr. 2: 575-589. 15 S.
	5	Calcium is associated with specific soil organic carbon decomposition products Enthalten in EGUsphere 27.11.2024: 1-12. 12 S.
	6	Nine years of warming and nitrogen addition in the Tibetan grassland promoted loss of soil organic carbon but did not alter the bulk change of chemical structure Enthalten in Biogeosciences discussions 01.09.2023: 1-43. 43 S.
	7	Whole-soil warming decreases abundance and modifies the community structure of microorganisms in the subsoil but not in surface soil Enthalten in Soil Bd. 7, 2021, Nr. 2: 477-494. 18 S.
	8	Whole soil warming decreases abundance and modifies community structure of microorganisms in subsoil but not in surface soil Enthalten in Soil discussions 2021: 1-30
	9	Publisher Correction: Global-scale evidence for the refractory nature of riverine black carbon Enthalten in Nature geoscience 9.10.2018: 1
	10	How relevant is recalcitrance for the stabilization of organic matter in soils? † Enthalten in Journal of plant nutrition and soil science Bd. 171, 2008, Nr. 1: 91-110. 20 S.

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