Overview: Global change effects on terrestrial biogeochemistry at the plant–soil interface

Abstract. “Global change” significantly alters organic matter and element cycling, but many of the underlying processes and consequences remain poorly understood. The interface of plants and soil plays a central role, coupling the atmosphere, hydrosphere, biosphere and lithosphere and integrating biological and geochemical processes. The contributions to this special issue address questions on both biotic and abiotic interactions underlying responses of terrestrial biogeochemical cycling to a range of global changes, including increases in atmospheric CO2 concentrations, warming, drought and altered water regimes. In this overview, we synthesize key findings of the contributing empirical, conceptual and modelling-based studies covering responses of plants to elevated CO2; the role of soil organisms in modulating responses to warming; impacts of global change on soil organic carbon, nitrogen, and mineral nutrient availability; and the influence of altered water-table depth caused by global change on greenhouse gas emissions. The showcased studies were conducted in regions from the Arctic to the tropics and highlight the manifold impacts of global change on various ecosystem components controlling biogeochemical processes occurring at the plant–soil interface. This multi-ecosystem interdisciplinary understanding is crucial for deciphering feedbacks of terrestrial ecosystems to the climate system.

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Institutions

Publication Details

Journal
Biogeosciences
Published
2024-09-06
DOI
https://doi.org/10.5194/bg-21-3959-2024
Citations
7
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
2.34

Funders

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article

Overview: Global change effects on terrestrial biogeochemistry at the plant–soil interface

Emily F. Solly, Alberto Canarini, Lucia Fuchslueger, Albert C. Brangarí
7 citations
Biogeosciences
Soil Carbon and Nitrogen Dynamics
2.34
article

Overview: Global change effects on terrestrial biogeochemistry at the plant–soil interface

Emily F. Solly, Alberto Canarini, Lucia Fuchslueger, Albert C. Brangarí
article en
7 citations

Abstract

Abstract. “Global change” significantly alters organic matter and element cycling, but many of the underlying processes and consequences remain poorly understood. The interface of plants and soil plays a central role, coupling the atmosphere, hydrosphere, biosphere and lithosphere and integrating biological and geochemical processes. The contributions to this special issue address questions on both biotic and abiotic interactions underlying responses of terrestrial biogeochemical cycling to a range of global changes, including increases in atmospheric CO2 concentrations, warming, drought and altered water regimes. In this overview, we synthesize key findings of the contributing empirical, conceptual and modelling-based studies covering responses of plants to elevated CO2; the role of soil organisms in modulating responses to warming; impacts of global change on soil organic carbon, nitrogen, and mineral nutrient availability; and the influence of altered water-table depth caused by global change on greenhouse gas emissions. The showcased studies were conducted in regions from the Arctic to the tropics and highlight the manifold impacts of global change on various ecosystem components controlling biogeochemical processes occurring at the plant–soil interface. This multi-ecosystem interdisciplinary understanding is crucial for deciphering feedbacks of terrestrial ecosystems to the climate system.

BiogeosciencesVol. 21(17)
University of Vienna (AT), Helmholtz Centre for Environmental Research (DE), Lund University (SE), Kyoto University (JP), German Centre for Integrative Biodiversity Research (DE), Institute for Biodiversity (DE), Environment Agency Austria (AT)
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, Svenska Forskningsrådet Formas, Norges Forskningsråd, Japan Society for the Promotion of Science, Horizon 2020
Openalex Percentile: Top 12%
Soil Carbon and Nitrogen Dynamics
2.34
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