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

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

ABSTRACT Organic carbon (OC) in permafrost interacts with the mineral fraction of soil and sediments, representing

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Permafrost and periglacial processes 2024-07, Vol.35 (3), p.278-293
Hauptverfasser: Thomas, Maxime, Jongejans, Loeka L., Strauss, Jens, Vermylen, Chloé, Calcus, Sacha, Opel, Thomas, Kizyakov, Alexander, Wetterich, Sebastian, Grosse, Guido, Opfergelt, Sophie
Format: Artikel
Sprache:eng
Schlagworte:
Batagay
Carbon
Climate feedback
Degradability
headwall
Headwalls
Heavy metals
Interglacial periods
iron
Iron oxides
Landforms
Microorganisms
Mineralization
Mineralogy
Minerals
mineral–organic carbon interactions
Organic carbon
Organic soils
Permafrost
Physicochemical processes
Residence time
retrogressive thaw slumps
Sediment
Sediment samplers
Sediment samples
Sediments
Stratigraphy
thermo‐erosion
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:ABSTRACT Organic carbon (OC) in permafrost interacts with the mineral fraction of soil and sediments, representing
ISSN:1045-6740
1099-1530
DOI:10.1002/ppp.2230