The impact of climate change on the flux and fate of metals in freshwater systems: implications for metal exposures across different scales
The impact of climate change on the flux and fate of metals in freshwater systems: implications for metal exposures across different scales
Climate change and chemical pollution are two of the gravest environmental concerns, and it is becoming increasingly recognised that climate change and climate variability will alter the environmental distribution and toxicity of chemical pollutants. Trace metals are an established pollutant group where decades of research have been able to determine causal links between environmental concentrations and water chemistry, and accumulation and toxic effects. In the present paper, we assert that to fully comprehend the impact of climate change on metal bioavailability and exposures in freshwaters, three distinct scales need to be understood: (i) the global scale of metal biogeochemical cycling which will alter metal inputs from soil into freshwater; (ii) the environmental scale of fluctuating water chemistry parameters that will change metal complexation dynamics; and (iii) the organismal scale at which climate-induced physiological modifications at the site of uptake may alter the bioaccumulation of metals and climate-induced impairments of cellular function that will change toxicity. At each scale much is already known about the processes and pathways that govern metal input, bioavailability and impacts on biota, but the key impact of climate variability is to alter the frequency, intensity, and rates at which these processes occur with the underlying commonality throughout scales being a shift to a more dynamic system. In an increasingly dynamic environment, it is the kinetics of both chemical and biological reactions that become more important compared to predictions of metal bioavailability from currently utilised thermodynamic equilibrium-based models. Extending such models to include climate variability is not easy, but to begin such a process would ultimately lead to more accurate and realistic applications to policy guidance.
CLIMATE CHANGE, Biogeochemical cycle, metal cycling, Physiology, adaptation, acclimation
Khan, Farhan K.
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Bury, Nicolas R.
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Cooper, Christopher A.
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Boyle, David
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Middleton, Elizabeth
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Herzog, Simon D.
74446e81-47b6-4d64-a890-2cc4f860f5ab
16 October 2025
Khan, Farhan K.
9d562827-9703-43a0-90b2-f49e11829d7c
Bury, Nicolas R.
696daba0-5cc9-444c-be9a-c678808712c6
Cooper, Christopher A.
f2970360-9caa-4c48-87b8-5c41534b39c8
Boyle, David
1787d846-af60-4482-aa98-b3b661749662
Middleton, Elizabeth
376cd732-3181-4b8f-a856-8e82a899b5ac
Herzog, Simon D.
74446e81-47b6-4d64-a890-2cc4f860f5ab
Khan, Farhan K., Bury, Nicolas R., Cooper, Christopher A., Boyle, David, Middleton, Elizabeth and Herzog, Simon D.
(2025)
The impact of climate change on the flux and fate of metals in freshwater systems: implications for metal exposures across different scales.
Environmental Research, 287, [123057].
Abstract
Climate change and chemical pollution are two of the gravest environmental concerns, and it is becoming increasingly recognised that climate change and climate variability will alter the environmental distribution and toxicity of chemical pollutants. Trace metals are an established pollutant group where decades of research have been able to determine causal links between environmental concentrations and water chemistry, and accumulation and toxic effects. In the present paper, we assert that to fully comprehend the impact of climate change on metal bioavailability and exposures in freshwaters, three distinct scales need to be understood: (i) the global scale of metal biogeochemical cycling which will alter metal inputs from soil into freshwater; (ii) the environmental scale of fluctuating water chemistry parameters that will change metal complexation dynamics; and (iii) the organismal scale at which climate-induced physiological modifications at the site of uptake may alter the bioaccumulation of metals and climate-induced impairments of cellular function that will change toxicity. At each scale much is already known about the processes and pathways that govern metal input, bioavailability and impacts on biota, but the key impact of climate variability is to alter the frequency, intensity, and rates at which these processes occur with the underlying commonality throughout scales being a shift to a more dynamic system. In an increasingly dynamic environment, it is the kinetics of both chemical and biological reactions that become more important compared to predictions of metal bioavailability from currently utilised thermodynamic equilibrium-based models. Extending such models to include climate variability is not easy, but to begin such a process would ultimately lead to more accurate and realistic applications to policy guidance.
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2025 Khan et al 2025 Env Res 287 123057
- Version of Record
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1-s2.0-S0013935125023102-main
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More information
Accepted/In Press date: 9 October 2025
e-pub ahead of print date: 10 October 2025
Published date: 16 October 2025
Keywords:
CLIMATE CHANGE, Biogeochemical cycle, metal cycling, Physiology, adaptation, acclimation
Identifiers
Local EPrints ID: 507211
URI: http://eprints.soton.ac.uk/id/eprint/507211
ISSN: 0013-9351
PURE UUID: 32c6d559-1bfd-4259-8da6-1550f1cce50e
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Date deposited: 01 Dec 2025 17:47
Last modified: 02 Dec 2025 03:05
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Contributors
Author:
Farhan K. Khan
Author:
Nicolas R. Bury
Author:
Christopher A. Cooper
Author:
David Boyle
Author:
Elizabeth Middleton
Author:
Simon D. Herzog
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