Standard

Shifting Mountain Tree Line Increases Soil Organic Carbon Stability Regardless of Land Use. / Sushko, Sofia; Ivashchenko, Kristina; Komarova, Alexandra; Yudina, Anna; Makhantseva, Victoria; Elsukova, Ekaterina; Blagodatsky, Sergey.

In: Plants, Vol. 13, No. 9, 1193, 25.04.2024.

Research output: Contribution to journalArticlepeer-review

Harvard

Sushko, S, Ivashchenko, K, Komarova, A, Yudina, A, Makhantseva, V, Elsukova, E & Blagodatsky, S 2024, 'Shifting Mountain Tree Line Increases Soil Organic Carbon Stability Regardless of Land Use', Plants, vol. 13, no. 9, 1193. https://doi.org/10.3390/plants13091193, https://doi.org/10.3390/plants13091193

APA

Sushko, S., Ivashchenko, K., Komarova, A., Yudina, A., Makhantseva, V., Elsukova, E., & Blagodatsky, S. (2024). Shifting Mountain Tree Line Increases Soil Organic Carbon Stability Regardless of Land Use. Plants, 13(9), [1193]. https://doi.org/10.3390/plants13091193, https://doi.org/10.3390/plants13091193

Vancouver

Author

Sushko, Sofia ; Ivashchenko, Kristina ; Komarova, Alexandra ; Yudina, Anna ; Makhantseva, Victoria ; Elsukova, Ekaterina ; Blagodatsky, Sergey. / Shifting Mountain Tree Line Increases Soil Organic Carbon Stability Regardless of Land Use. In: Plants. 2024 ; Vol. 13, No. 9.

BibTeX

@article{aea8e283f3e0431aa1a844d11ad0a9cf,
title = "Shifting Mountain Tree Line Increases Soil Organic Carbon Stability Regardless of Land Use",
abstract = "AbstractClimate and land use changes are causing trees line to shift up into mountain meadows. The effect of this vegetation change on the partitioning of soil carbon (C) between the labile particulate organic matter (POM–C) and stable mineral-associated organic matter (MAOM–C) pools is poorly understood. Therefore, we assessed these C pools in a 10 cm topsoil layer along forest–meadow ecotones with different land uses (reserve and pasture) in the Northwest Caucasus of Russia using the size fractionation technique (POM 0.053–2.00 mm, MAOM < 0.053 mm). Potential drivers included the amount of C input from aboveground grass biomass (AGB) and forest litter (litter quantity) and their C/N ratios, aromatic compound content (litter quality), and soil texture. For both land uses, the POM–C pool showed no clear patterns of change along forest–meadow ecotones, while the MAOM–C pool increased steadily from meadow to forest. Regardless of land use, the POM–C/MAOM–C ratio decreased threefold from meadow to forest in line with decreasing grass AGB (R2 = 0.75 and 0.29 for reserve and pasture) and increasing clay content (R2 = 0.63 and 0.36 for reserve and pasture). In pastures, an additional negative relationship was found with respect to plant litter aromaticity (R2 = 0.48). Therefore, shifting the mountain tree line in temperate climates could have a positive effect on conserving soil C stocks by increasing the proportion of stable C pools.Keywords:particulate organic matter; mineral-associated organic matter; aboveground grass biomass; forest litter; 13C-NMR spectroscopy; aromaticity index; C/N ratio",
keywords = "particulate organic matter; mineral-associated organic matter; aboveground grass biomass; forest litter; 13C-NMR spectroscopy; aromaticity index; C/N ratio, 13C-NMR spectroscopy, C/N ratio, aboveground grass biomass, aromaticity index, forest litter, mineral-associated organic matter, particulate organic matter",
author = "Sofia Sushko and Kristina Ivashchenko and Alexandra Komarova and Anna Yudina and Victoria Makhantseva and Ekaterina Elsukova and Sergey Blagodatsky",
year = "2024",
month = apr,
day = "25",
doi = "10.3390/plants13091193",
language = "English",
volume = " 13",
journal = "Plants",
issn = "2223-7747",
publisher = "MDPI AG",
number = "9",

}

RIS

TY - JOUR

T1 - Shifting Mountain Tree Line Increases Soil Organic Carbon Stability Regardless of Land Use

AU - Sushko, Sofia

AU - Ivashchenko, Kristina

AU - Komarova, Alexandra

AU - Yudina, Anna

AU - Makhantseva, Victoria

AU - Elsukova, Ekaterina

AU - Blagodatsky, Sergey

PY - 2024/4/25

Y1 - 2024/4/25

N2 - AbstractClimate and land use changes are causing trees line to shift up into mountain meadows. The effect of this vegetation change on the partitioning of soil carbon (C) between the labile particulate organic matter (POM–C) and stable mineral-associated organic matter (MAOM–C) pools is poorly understood. Therefore, we assessed these C pools in a 10 cm topsoil layer along forest–meadow ecotones with different land uses (reserve and pasture) in the Northwest Caucasus of Russia using the size fractionation technique (POM 0.053–2.00 mm, MAOM < 0.053 mm). Potential drivers included the amount of C input from aboveground grass biomass (AGB) and forest litter (litter quantity) and their C/N ratios, aromatic compound content (litter quality), and soil texture. For both land uses, the POM–C pool showed no clear patterns of change along forest–meadow ecotones, while the MAOM–C pool increased steadily from meadow to forest. Regardless of land use, the POM–C/MAOM–C ratio decreased threefold from meadow to forest in line with decreasing grass AGB (R2 = 0.75 and 0.29 for reserve and pasture) and increasing clay content (R2 = 0.63 and 0.36 for reserve and pasture). In pastures, an additional negative relationship was found with respect to plant litter aromaticity (R2 = 0.48). Therefore, shifting the mountain tree line in temperate climates could have a positive effect on conserving soil C stocks by increasing the proportion of stable C pools.Keywords:particulate organic matter; mineral-associated organic matter; aboveground grass biomass; forest litter; 13C-NMR spectroscopy; aromaticity index; C/N ratio

AB - AbstractClimate and land use changes are causing trees line to shift up into mountain meadows. The effect of this vegetation change on the partitioning of soil carbon (C) between the labile particulate organic matter (POM–C) and stable mineral-associated organic matter (MAOM–C) pools is poorly understood. Therefore, we assessed these C pools in a 10 cm topsoil layer along forest–meadow ecotones with different land uses (reserve and pasture) in the Northwest Caucasus of Russia using the size fractionation technique (POM 0.053–2.00 mm, MAOM < 0.053 mm). Potential drivers included the amount of C input from aboveground grass biomass (AGB) and forest litter (litter quantity) and their C/N ratios, aromatic compound content (litter quality), and soil texture. For both land uses, the POM–C pool showed no clear patterns of change along forest–meadow ecotones, while the MAOM–C pool increased steadily from meadow to forest. Regardless of land use, the POM–C/MAOM–C ratio decreased threefold from meadow to forest in line with decreasing grass AGB (R2 = 0.75 and 0.29 for reserve and pasture) and increasing clay content (R2 = 0.63 and 0.36 for reserve and pasture). In pastures, an additional negative relationship was found with respect to plant litter aromaticity (R2 = 0.48). Therefore, shifting the mountain tree line in temperate climates could have a positive effect on conserving soil C stocks by increasing the proportion of stable C pools.Keywords:particulate organic matter; mineral-associated organic matter; aboveground grass biomass; forest litter; 13C-NMR spectroscopy; aromaticity index; C/N ratio

KW - particulate organic matter; mineral-associated organic matter; aboveground grass biomass; forest litter; 13C-NMR spectroscopy; aromaticity index; C/N ratio

KW - 13C-NMR spectroscopy

KW - C/N ratio

KW - aboveground grass biomass

KW - aromaticity index

KW - forest litter

KW - mineral-associated organic matter

KW - particulate organic matter

UR - https://www.mendeley.com/catalogue/359aadd7-b782-3cb5-b3a6-92f4c0db4ddc/

U2 - 10.3390/plants13091193

DO - 10.3390/plants13091193

M3 - Article

VL - 13

JO - Plants

JF - Plants

SN - 2223-7747

IS - 9

M1 - 1193

ER -

ID: 119222906