Fluvial biofilm phosphorus entrapment shifts from intracellular to extracellular dominance along a multifactorial longitudinal river gradient

Abstract. Phosphorus (P) entrapment by biofilms can be distinguished into the intracellular P entrapment (the P uptake by microbial cells) and the extracellular P entrapment via the extracellular polymeric substances. It is unknown how these two P entrapment pathways behave in natural ecosystems in which gradients of environmental drivers such as P, labile dissolved organic matter (DOM) and light occur. Another key aspect in P dynamics at the sediment-water interface is microbial activity. Microbially mediated mineralization of DOM and microbial activity in general is suspected to be a driver of internal P mobilization from the sediments. Here we brought such expectations into a real-world context by analysing the P entrapment patterns of benthic biofilms and the P release potential from the sediments along a longitudinal gradient in a third order river in front of the background of key microbial metabolic variables. The gradient consists of increasing P availability, DOM lability and light availability. We found a gradual shift in the dominance of P entrapment from higher intracellular P entrapment in the upstream biofilms to higher extracellular P entrapment in the downstream biofilms. This shift towards dominance of extracellular P entrapment was accompanied by an increase in the P release potential from the sediment. The increasing P release potential was also connected to high extracellular enzyme activity of alkaline phosphatase, an enzyme involved in the mineralization of P from organic compounds. We further found that a balanced ratio between intracellular and extracellular P was connected to a higher C metabolic diversity. All this evidence suggests an influence of the benthic biofilms on P dynamics at the sediment-water interface. This research advocates for a more integrated perspective that accounts for both intracellular and extracellular biofilm-mediated processes.

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Published
2025-10-10
DOI
https://doi.org/10.5194/egusphere-2025-4844
Primary Topic
Aquatic Invertebrate Ecology and Behavior
Type
article
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article

Fluvial biofilm phosphorus entrapment shifts from intracellular to extracellular dominance along a multifactorial longitudinal river gradient

Markus Weitere, Karla Münzner, David Kneis, Núria Perujo et al.
Aquatic Invertebrate Ecology and Behavior
article

Fluvial biofilm phosphorus entrapment shifts from intracellular to extracellular dominance along a multifactorial longitudinal river gradient

Markus Weitere, Karla Münzner, David Kneis, Núria Perujo, Simon Wentritt
article en

Abstract

Abstract. Phosphorus (P) entrapment by biofilms can be distinguished into the intracellular P entrapment (the P uptake by microbial cells) and the extracellular P entrapment via the extracellular polymeric substances. It is unknown how these two P entrapment pathways behave in natural ecosystems in which gradients of environmental drivers such as P, labile dissolved organic matter (DOM) and light occur. Another key aspect in P dynamics at the sediment-water interface is microbial activity. Microbially mediated mineralization of DOM and microbial activity in general is suspected to be a driver of internal P mobilization from the sediments. Here we brought such expectations into a real-world context by analysing the P entrapment patterns of benthic biofilms and the P release potential from the sediments along a longitudinal gradient in a third order river in front of the background of key microbial metabolic variables. The gradient consists of increasing P availability, DOM lability and light availability. We found a gradual shift in the dominance of P entrapment from higher intracellular P entrapment in the upstream biofilms to higher extracellular P entrapment in the downstream biofilms. This shift towards dominance of extracellular P entrapment was accompanied by an increase in the P release potential from the sediment. The increasing P release potential was also connected to high extracellular enzyme activity of alkaline phosphatase, an enzyme involved in the mineralization of P from organic compounds. We further found that a balanced ratio between intracellular and extracellular P was connected to a higher C metabolic diversity. All this evidence suggests an influence of the benthic biofilms on P dynamics at the sediment-water interface. This research advocates for a more integrated perspective that accounts for both intracellular and extracellular biofilm-mediated processes.

Helmholtz Centre for Environmental Research (DE), Lund University (SE), Technische Universität Dresden (DE)
Deutsche Forschungsgemeinschaft
Openalex Percentile: Top 73%
Aquatic Invertebrate Ecology and Behavior
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