How vegetation patches drive soil development and organic matter formation on polar islands
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How vegetation patches drive soil development and organic matter formation on polar islands. / Prater, Isabel; Hrbáček, Filip; Braun, Christina; Vidal, Alix; Meier, Lars Arne; Nývlt, Daniel; Mueller, Carsten W.
In: Geoderma Regional, Vol. 27, e00429, 12.2021.Research output: Contribution to journal › Journal article › Research › peer-review
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TY - JOUR
T1 - How vegetation patches drive soil development and organic matter formation on polar islands
AU - Prater, Isabel
AU - Hrbáček, Filip
AU - Braun, Christina
AU - Vidal, Alix
AU - Meier, Lars Arne
AU - Nývlt, Daniel
AU - Mueller, Carsten W.
N1 - Funding Information: We are grateful for the funding within the DFG Priority Programme 1158 “Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas” ( MU 3021/8-1 ). The work of FH and DN has been supported by the Ministry of Education, Youth and Sports of the Czech Republic projects no. LM2015078 (Czech Polar Research Infrastructure), and CZ.02.1.01/0.0/0.0/16_013/0001708 (Ecopolaris). The work of CB in the field season 2016/2017 has been supported by the German Federal Environment Agency (UBA) under the grant agreement UFOPLAN 3715 19 213 0 , logistics support was provided by Russian Antarctic Expedition, Aerovías DAP and Antarctica XXI. We thank Maria Greiner for her assistance with physical soil fractionation and elemental analyses. Publisher Copyright: © 2021 Elsevier B.V.
PY - 2021/12
Y1 - 2021/12
N2 - As Antarctica is strongly affected by climate change and global warming, the factors that mainly determine soil development might also shift from the dominance of physical to biochemical processes. Vegetation is restricted to the margins of the Antarctic continent with the Antarctic Peninsula being a region of patchily distributed vegetation. While on James Ross Island in the Weddell Sea only cryptogams can be found, on King George Island in the Southern Ocean also vascular plants are present. As rates of soil development and the build-up of soil organic matter are very low in these polar conditions, it can be hypothesized that vegetation patches comprise hot spots for biogeochemical soil processes. To analyze the effect of vegetation on soils in maritime Antarctica, we investigated vegetated and vegetation-free soils from both islands. On both islands, we found clearly higher carbon and nitrogen contents in vegetated soils. Using physical fractionation, we could demonstrate that the amount of free and occluded particulate organic matter is also higher in soils under vegetation, but at the same time, that clay-sized mineral-associated organic matter contributes most to carbon storage in all soils. The dominance of aromatic compounds in vegetation-free soils was disclosed by 13C NMR spectroscopy as well as a larger proportion of compounds with a lower molecular weight in vegetated soils. Thus, vegetation patches lead to soil organic matter containing higher amounts of bioavailable substrates that can be assumed to foster microbial activity and thus drive further soil development in a warmer future. However, in the cold arid environments a propagation of aridity might result in vegetation dieback and thus in a ceasing of biological soil activity driving a slowing of soil development.
AB - As Antarctica is strongly affected by climate change and global warming, the factors that mainly determine soil development might also shift from the dominance of physical to biochemical processes. Vegetation is restricted to the margins of the Antarctic continent with the Antarctic Peninsula being a region of patchily distributed vegetation. While on James Ross Island in the Weddell Sea only cryptogams can be found, on King George Island in the Southern Ocean also vascular plants are present. As rates of soil development and the build-up of soil organic matter are very low in these polar conditions, it can be hypothesized that vegetation patches comprise hot spots for biogeochemical soil processes. To analyze the effect of vegetation on soils in maritime Antarctica, we investigated vegetated and vegetation-free soils from both islands. On both islands, we found clearly higher carbon and nitrogen contents in vegetated soils. Using physical fractionation, we could demonstrate that the amount of free and occluded particulate organic matter is also higher in soils under vegetation, but at the same time, that clay-sized mineral-associated organic matter contributes most to carbon storage in all soils. The dominance of aromatic compounds in vegetation-free soils was disclosed by 13C NMR spectroscopy as well as a larger proportion of compounds with a lower molecular weight in vegetated soils. Thus, vegetation patches lead to soil organic matter containing higher amounts of bioavailable substrates that can be assumed to foster microbial activity and thus drive further soil development in a warmer future. However, in the cold arid environments a propagation of aridity might result in vegetation dieback and thus in a ceasing of biological soil activity driving a slowing of soil development.
KW - C NMR spectroscopy
KW - Antarctic Peninsula
KW - James Ross Island
KW - King George Island
KW - Mineral-associated organic matter
KW - Particulate organic matter
KW - Vegetation-soil interaction
U2 - 10.1016/j.geodrs.2021.e00429
DO - 10.1016/j.geodrs.2021.e00429
M3 - Journal article
AN - SCOPUS:85113758573
VL - 27
JO - Geoderma Regional
JF - Geoderma Regional
SN - 2352-0094
M1 - e00429
ER -
ID: 281410295