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Soil organic matter and biogenic-abiogenic interactions in soils of Larsemann Hills and Bunger Hills, East Antarctica
Although Antarctic soils are usually described as weakly developed, recent studies indicated the significant variability in soil forming conditions across the sixth continent as well as considerable diversity of soils. The identification of pedogenetic processes in Antarctica is crucial for understanding not only the current state of its environment, but also for better understanding of soil development on Earth through time. Our study provides a detailed investigation of micromorphological features and molecular composition of organic matter of soil and soil-like bodies of remote areas of East Antarctica - Larsemann Hills and Bunger Hills, which are characterized by harsh environmental conditions. Studied soils showed predominantly coarse structure and low organic carbon content, alkaline to almost neutral pH range. Thin sections of studied soils were characterized by predominance of grains of quartz, feldspars, and other primary minerals with angular shapes indicating relatively weak degree of their alteration. All studied humic substances are characterized by the predominance of aliphatic structures. Moreover, it was observed that studied humic acids contains significant amounts of carbohydrates, polysaccharides, esters and amino acids and hydrophilic fragments predominate. Organo-mineral interactions were mostly connected with development of biofilms in the topsoil horizons with the maximal biological activity among studied soils.journal articl
Petrology and Mineralogy of Beardsley (H5) Chondrite
The 15th Symposium on Polar Science/Ordinary sessions [OA] Antarctic Meteorite, Thu. 5 Dec. / 3F Conference room, The Institute of Statistical Mathematicsconference outpu
A comparison of manual and automatic methods for the detection of geological features within large 3D seismic data
The 15th Symposium on Polar Science/Interdisciplinary sessions [ID] Polar data science, Thu. 5 Dec. / 3F Conference room, National Institute of Polar Researchconference outpu
Detection of surface environmental variations using infrasound waves and their migrated sources in the Lützow-Holm Bay, East Antarctica
The 15th Symposium on Polar Science/Interdisciplinary sessions [ID] Polar data science, Thu. 5 Dec. / 3F Conference room, National Institute of Polar Researchconference outpu
Development and publication of an online database of Antarctic microbial strain catalogs and genome information
The 15th Symposium on Polar Science/Interdisciplinary sessions [ID] Polar data science, Thu. 5 Dec. / Entrance Hall (1st floor), National Institute of Polar Researchconference outpu
Effect of delayed sea ice retreat on zooplankton communities in the Pacific Arctic Ocean: A generalized dissimilarity modeling approach
The 15th Symposium on Polar Science/Ordinary sessions [OB] Polar biology, Wed. 4 Dec. / Entrance Hall (1st floor), National Institute of Polar Researchconference outpu
Characteristics and Provenance of Basalts from the Continental Slope off Cape Darnley, East Antarctica: Evidence for Links to the West Antarctic Rift System
The 15th Symposium on Polar Science/Ordinary sessions [OG] Polar geosciences, Wed. 4 Dec. / 3F Conference room, National Institute of Polar Researchconference outpu
Fast-ice observations via an array of wave-ice buoys and the EM-induction sensor during JARE65
The 15th Symposium on Polar Science/Ordinary sessions [OG] Polar geosciences, Wed. 4 Dec. / 3F Conference room, National Institute of Polar Researchconference outpu
Seismic imaging of the crust and lithospheric mantle of the Pan-African mobile belt, the Lützow-Holm Complex, East Antarctica
The 15th Symposium on Polar Science/Ordinary sessions [OG] Polar geosciences, Wed. 4 Dec. / 3F Conference room, National Institute of Polar Researchconference outpu
Growth history of garnet in pelitic gneisses from the highest-grade Ryoke metamorphic complex in Yanai area, SW Japan
The 15th Symposium on Polar Science/Ordinary sessions [OG] Polar geosciences, Wed. 4 Dec. / Entrance Hall (1st floor), National Institute of Polar Researchconference outpu