This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.1111/gcb.71033. This is version 3 of this Preprint.
Temperate forest floors: Ecosystem hub in transition?
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Abstract
The forest floor (FF) plays a key role in carbon, nutrient, and water cycling. It is the biologically most active compartment of forest
soils, highly responsive to environmental conditions. Yet, its response to current changes in environmental conditions and forest
management is understudied. Temperate forests are among the best studied ecosystems globally, providing the necessary ecological
and biogeochemical background information to assess FF changes. Here, we focus on identifying existing knowledge and gaps in our
understanding of the functioning of the FF. Interactions between FF biota and abiotic FF components show multifactorial depend-
encies with environmental conditions and drive FF turnover. Vice versa, the turnover of FF regulates carbon, nutrient, and water cy-
cling. With slow litter decomposition and limited bioturbation, organic matter accumulates, nutrients cycle tightly within the FF, and
water passes through this layer partly along preferential pathways. With rapid litter decomposition and intense bioturbation, FF accu-
mulation is little, the mineral soil is the main nexus for plant nutrient uptake and organic matter transformation, and water infiltrates
the mineral soil more homogeneously. The interconnectedness with the adjacent ecosystem compartments is a crucial feature of the
FF, feeding back to its functioning and making it a central hub of forest processes. The FF morphology reflects these processes and
therefore has untapped potential as an indicator of soil and ecosystem health. Under forest change, the FF might lose its functionality, with negative impacts on nutrient provision, water storage, and carbon sequestration. Consequences for forest growth could be strong
and even detrimental. Hence, improved knowledge of FF characteristics and their linkages to mineral soils and aboveground ecosys-
tem compartments is crucial for assessing forest resilience to progressing environmental changes.
DOI
https://doi.org/10.31223/X5BB4G
Subjects
Forest Sciences, Life Sciences
Keywords
Forest Floor, Interconnectedness, climate change, Ecosystem Services
Dates
Published: 2025-12-04 12:00
Last Updated: 2026-08-26 17:04
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Conflict of interest statement:
Non
Data Availability:
Review, no data created
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Comment #261 Jörg Niederberger @ 2025-12-08 11:02
Please see manuscript for complete list of authors and affiliations.