[Skip to Content]
Banner
Menu
  • Connects Home
  • Explore Sessions
    • All Sessions
    • Special Lectures
    • Pardee Keynote Symposia
    • Oral Sessions
    • Poster Sessions
    • Short Courses
    • Field Trips
    • Non-Technical Events
  • Meeting Program
  • My Account
  • Home
  • GSA Connects 2025: Abstract Collection Gallery
  • Arthur L. Day Medal: Coupled Redox Cycling of Iron in Clay Minerals and Organic Matter Transformation Across Redox Interfaces

277-2 Arthur L. Day Medal: Coupled Redox Cycling of Iron in Clay Minerals and Organic Matter Transformation Across Redox Interfaces

Session: Critical Zone Science: Intersection of Processes Linked to Geomorphology, Ecology, Fire and Climate



Presenting Author:

Hailiang Dong


Author:

Dong, Hailiang1

(1) School of Earth Sciences and Resources, China University of Geosciences, Beijing, China,

Abstract:

A large fraction of organic matter (OM) in soils and sediments is associated with minerals to form mineral-OM associations, which are known to decelerate OM decomposition because of protection against microbial use. However, redox cycling of Fe at redox interfaces can transform OM, yet specific pathways of coupled Fe redox cycling and OM transformation are not well understood. In this talk, I will focus on processes and mechanisms of coupled iron-carbon (Fe-C) cycles across redox interfaces [1]. Specifically, oxygenation of structural Fe(II) in minerals generates reactive oxygen species (ROS), which directly transform OM including decomposition and polymerization [2-4]. ROS also affect extracellular enzyme activity and microbial activity, thus indirectly transforming OM [5-6]. Fe(III) reduction contributes to OM oxidation through anaerobic respiration. OM plays an important role in Fe redox cycling by serving as electron donor, acceptor, shuttle, buffer, and conductor, as well as via adsorption to and coprecipitation with Fe minerals and complexation with Fe, all of which significantly alter Fe mineralogy and their reactivity [1]. Coupled Fe-C redox cycles occur in critical zone and have major implications for greenhouse gas emission, biogeochemical cycles of elements, soil fertility and food security, biodiversity and ecosystem functions, and environmental behaviour of contaminants.

References:

[1] Dong H. et al. (2023) Nat Rev Earth Environ 4:659-673.

[2] Zeng Q et al. (2019) GCA 251:136-156.

[3] Zeng Q et al (2020) Environ Sci Technol 54:15013-15023.

[4] Hu D et al (2023) Environ Sci Technol, 57:19760-19771.

[5] Dong H et al (2023) GCA 345: 102-116

[6] Sheng Y et al (2023) Environ Sci Technol 57: 3425-3433




Geological Society of America Abstracts with Program. Vol. 57, No. 6, 2025


doi: 10.1130/abs/2025AM-5508


© Copyright 2025 The Geological Society of America (GSA), all rights reserved.

Arthur L. Day Medal: Coupled Redox Cycling of Iron in Clay Minerals and Organic Matter Transformation Across Redox Interfaces

Category

Topical Sessions

Description


Session Format: Oral

Presentation Date: 10/22/2025

Presentation Start Time: 01:50 PM

Presentation Room: HBGCC, 212AB



Back to Session
  • Powered by OpenWater: Application and Review Software | If you have any questions or need any support, please contact: meetings@geosociety.org