[HTML][HTML] Evidence for preservation of organic carbon interacting with iron in material displaced from retrogressive thaw slumps: Case study in Peel Plateau, western …

M Thomas, A Monhonval, C Hirst, L Bröder, S Zolkos… - Geoderma, 2023 - Elsevier
In northern high latitudes, rapid warming is set to amplify carbon-climate feedbacks by
enhancing permafrost thaw and biogeochemical transformation of large amounts of soil …

[HTML][HTML] Mineral organic carbon interactions in dry versus wet tundra soils

A Monhonval, E Mauclet, C Hirst, N Bemelmans… - Geoderma, 2023 - Elsevier
Mineral organic carbon interactions (aggregation, organo-mineral associations and organo-
metallic complexes) enhance the protection of organic carbon (OC) from microbial …

[HTML][HTML] Pan-Arctic soil element bioavailability estimations

P Stimmler, M Goeckede, B Elberling… - Earth System …, 2023 - essd.copernicus.org
Arctic soils store large amounts of organic carbon and other elements, such as amorphous
silicon, silicon, calcium, iron, aluminum, and phosphorous. Global warming is projected to …

[HTML][HTML] Strontium isotopes trace the dissolution and precipitation of mineral organic carbon interactions in thawing permafrost

A Monhonval, C Hirst, J Strauss, EAG Schuur… - Geoderma, 2023 - Elsevier
Interactions between minerals and organic carbon (OC) in soils are key to stabilize OC and
mitigate greenhouse gas emissions upon permafrost thaw. However, changes in soil water …

[HTML][HTML] Tracing changes in base cation sources for Arctic tundra vegetation upon permafrost thaw

E Mauclet, C Hirst, A Monhonval, EI Stevenson… - Geoderma, 2023 - Elsevier
Upon permafrost thaw, the volume of soil accessible to plant roots increases which modifies
the acquisition of plant-available resources. Tundra vegetation is actively responding to the …

Evidence for late winter biogeochemical connectivity in permafrost soils

C Hirst, A Monhonval, E Mauclet, M Thomas… - … Earth & Environment, 2023 - nature.com
The permafrost active layer is a key supplier of soil organic carbon and mineral nutrients to
Arctic rivers. In the active layer, sites of soil-water exchange are locations for organic carbon …

Thermokarst processes increase the supply of stabilizing surfaces and elements (Fe, Mn, Al, and Ca) for mineral–organic carbon interactions

A Monhonval, J Strauss, M Thomas… - Permafrost and …, 2022 - Wiley Online Library
The stabilizing properties of mineral–organic carbon (OC) interactions have been studied in
many soil environments (temperate soils, podzol lateritic soils, and paddy soils). Recently …

Processes controlling geogenic arsenic distribution in soils formed from iron-rich sedimentary rocks

A Vandeuren, B Pereira, C Van de Casteele… - Journal of Hazardous …, 2025 - Elsevier
Soils formed from Fe-rich sedimentary rocks can contain elevated As contents. Although the
geogenic origin of As in these soils is recognized, the processes controlling its distribution …

The role of coastal Yedoma deposits and continental shelf sediments in the Arctic Ocean silicon cycle

NE Ray, J Martens, M Ajmar, T Tesi… - Global …, 2024 - Wiley Online Library
The availability of silicon (Si) in the ocean plays an important role in regulating
biogeochemical and ecological processes. The Si budget of the Arctic Ocean appears …

A Third of Organic Carbon Is Mineral Bound in Permafrost Sediments Exposed by the World's Largest Thaw Slump, Batagay, Siberia

M Thomas, LL Jongejans, J Strauss… - Permafrost and …, 2024 - Wiley Online Library
Organic carbon (OC) in permafrost interacts with the mineral fraction of soil and sediments,
representing< 1% to~ 80% of the total OC pool. Quantifying the nature and controls of …