Soil organic matter molecular composition and state of decomposition in three locations of the European Arctic
Increased mineralization of the organic matter (OM) stored in permafrost is expected to constitute the largest additional global warming potential from terrestrial ecosystems exposed to a warmer climate. Chemical composition of permafrost OM is thought to be a key factor controlling the sensitivity...
Published in: | Biogeochemistry |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Online Access: | https://hal.science/hal-01594926 https://doi.org/10.1007/s10533-017-0373-2 |
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ftagroparistech:oai:HAL:hal-01594926v1 2024-05-12T07:52:12+00:00 Soil organic matter molecular composition and state of decomposition in three locations of the European Arctic Pengerud, Annelene Dignac, Marie-France Certini, Giacomo Strand, Line Tau Forte, Claudia Rasse, Daniel P. Department of Plant and Environmental Norwegian University of Life Sciences (NMBU) Ecologie fonctionnelle et écotoxicologie des agroécosystèmes (ECOSYS) Institut National de la Recherche Agronomique (INRA)-AgroParisTech Université Paris-Saclay Dipartimento di Scienze delle Produzioni Vegetali, del Suolo e dell’Ambiente Agroforestale (DiPSA) Università degli Studi di Firenze = University of Florence = Université de Florence (UniFI) Division for Environment and Natural Resources Norsk institutt for bioøkonomi=Norwegian Institute of Bioeconomy Research (NIBIO) 2017 https://hal.science/hal-01594926 https://doi.org/10.1007/s10533-017-0373-2 en eng HAL CCSD Springer Verlag info:eu-repo/semantics/altIdentifier/doi/10.1007/s10533-017-0373-2 hal-01594926 https://hal.science/hal-01594926 doi:10.1007/s10533-017-0373-2 PRODINRA: 406132 WOS: 000411147100006 ISSN: 0168-2563 EISSN: 1573-515X Biogeochemistry https://hal.science/hal-01594926 Biogeochemistry, 2017, 135 (3), pp.277-292. ⟨10.1007/s10533-017-0373-2⟩ Cryogenic processes Lignin Non-cellulosic sugars 13C NMR Palsa Permafrost Climate change [SDV]Life Sciences [q-bio] info:eu-repo/semantics/article Journal articles 2017 ftagroparistech https://doi.org/10.1007/s10533-017-0373-2 2024-04-18T00:00:00Z Increased mineralization of the organic matter (OM) stored in permafrost is expected to constitute the largest additional global warming potential from terrestrial ecosystems exposed to a warmer climate. Chemical composition of permafrost OM is thought to be a key factor controlling the sensitivity of decomposition to warming. Our objective was to characterise OM from permafrost soils of the European Arctic: two mineral soils—Adventdalen, Svalbard, Norway and Vorkuta, northwest Russia—and a “palsa” (ice-cored peat mound patterning in heterogeneous permafrost landscapes) soil in Neiden, northern Norway, in terms of molecular composition and state of decomposition. At all sites, the OM stored in the permafrost was at an advanced stage of decomposition, although somewhat less so in the palsa peat. By comparing permafrost and active layers, we found no consistent effect of depth or permafrost on soil organic matter (SOM) chemistry across sites. The permafrost-affected palsa peat displayed better preservation of plant material in the deeper layer, as indicated by increasing contribution of lignin carbon to total carbon with depth, associated to decreasing acid (Ac) to aldehyde (Al) ratio of the syringyl (S) and vanillyl (V) units, and increasing S/V and contribution of plant-derived sugars. By contrast, in Adventdalen, the Ac/Al ratio of lignin and the Alkyl C to O-alkyl C ratio in the NMR spectra increased with depth, which suggests less oxidized SOM in the active layer compared to the permafrost layer. In Vorkuta, SOM characteristics in the permafrost profile did not change substantially with depth, probably due to mixing of soil layers by cryoturbation. The composition and state of decomposition of SOM appeared to be site-specific, in particular bound to the prevailing organic or mineral nature of soil when attempting to predict the SOM proneness to degradation. The occurrence of processes such as palsa formation in organic soils and cryoturbation should be considered when up-scaling and predicting the responses ... Article in Journal/Newspaper Adventdalen Arctic Climate change Global warming Ice Northern Norway Northwest Russia palsa permafrost Svalbard Vorkuta AgroParisTech: HAL (Institut des sciences et industries du vivant et de l'environnement) Arctic Svalbard Norway Adventdalen ENVELOPE(16.264,16.264,78.181,78.181) Neiden ENVELOPE(29.377,29.377,69.696,69.696) Biogeochemistry 135 3 277 292 |
institution |
Open Polar |
collection |
AgroParisTech: HAL (Institut des sciences et industries du vivant et de l'environnement) |
op_collection_id |
ftagroparistech |
language |
English |
topic |
Cryogenic processes Lignin Non-cellulosic sugars 13C NMR Palsa Permafrost Climate change [SDV]Life Sciences [q-bio] |
spellingShingle |
Cryogenic processes Lignin Non-cellulosic sugars 13C NMR Palsa Permafrost Climate change [SDV]Life Sciences [q-bio] Pengerud, Annelene Dignac, Marie-France Certini, Giacomo Strand, Line Tau Forte, Claudia Rasse, Daniel P. Soil organic matter molecular composition and state of decomposition in three locations of the European Arctic |
topic_facet |
Cryogenic processes Lignin Non-cellulosic sugars 13C NMR Palsa Permafrost Climate change [SDV]Life Sciences [q-bio] |
description |
Increased mineralization of the organic matter (OM) stored in permafrost is expected to constitute the largest additional global warming potential from terrestrial ecosystems exposed to a warmer climate. Chemical composition of permafrost OM is thought to be a key factor controlling the sensitivity of decomposition to warming. Our objective was to characterise OM from permafrost soils of the European Arctic: two mineral soils—Adventdalen, Svalbard, Norway and Vorkuta, northwest Russia—and a “palsa” (ice-cored peat mound patterning in heterogeneous permafrost landscapes) soil in Neiden, northern Norway, in terms of molecular composition and state of decomposition. At all sites, the OM stored in the permafrost was at an advanced stage of decomposition, although somewhat less so in the palsa peat. By comparing permafrost and active layers, we found no consistent effect of depth or permafrost on soil organic matter (SOM) chemistry across sites. The permafrost-affected palsa peat displayed better preservation of plant material in the deeper layer, as indicated by increasing contribution of lignin carbon to total carbon with depth, associated to decreasing acid (Ac) to aldehyde (Al) ratio of the syringyl (S) and vanillyl (V) units, and increasing S/V and contribution of plant-derived sugars. By contrast, in Adventdalen, the Ac/Al ratio of lignin and the Alkyl C to O-alkyl C ratio in the NMR spectra increased with depth, which suggests less oxidized SOM in the active layer compared to the permafrost layer. In Vorkuta, SOM characteristics in the permafrost profile did not change substantially with depth, probably due to mixing of soil layers by cryoturbation. The composition and state of decomposition of SOM appeared to be site-specific, in particular bound to the prevailing organic or mineral nature of soil when attempting to predict the SOM proneness to degradation. The occurrence of processes such as palsa formation in organic soils and cryoturbation should be considered when up-scaling and predicting the responses ... |
author2 |
Department of Plant and Environmental Norwegian University of Life Sciences (NMBU) Ecologie fonctionnelle et écotoxicologie des agroécosystèmes (ECOSYS) Institut National de la Recherche Agronomique (INRA)-AgroParisTech Université Paris-Saclay Dipartimento di Scienze delle Produzioni Vegetali, del Suolo e dell’Ambiente Agroforestale (DiPSA) Università degli Studi di Firenze = University of Florence = Université de Florence (UniFI) Division for Environment and Natural Resources Norsk institutt for bioøkonomi=Norwegian Institute of Bioeconomy Research (NIBIO) |
format |
Article in Journal/Newspaper |
author |
Pengerud, Annelene Dignac, Marie-France Certini, Giacomo Strand, Line Tau Forte, Claudia Rasse, Daniel P. |
author_facet |
Pengerud, Annelene Dignac, Marie-France Certini, Giacomo Strand, Line Tau Forte, Claudia Rasse, Daniel P. |
author_sort |
Pengerud, Annelene |
title |
Soil organic matter molecular composition and state of decomposition in three locations of the European Arctic |
title_short |
Soil organic matter molecular composition and state of decomposition in three locations of the European Arctic |
title_full |
Soil organic matter molecular composition and state of decomposition in three locations of the European Arctic |
title_fullStr |
Soil organic matter molecular composition and state of decomposition in three locations of the European Arctic |
title_full_unstemmed |
Soil organic matter molecular composition and state of decomposition in three locations of the European Arctic |
title_sort |
soil organic matter molecular composition and state of decomposition in three locations of the european arctic |
publisher |
HAL CCSD |
publishDate |
2017 |
url |
https://hal.science/hal-01594926 https://doi.org/10.1007/s10533-017-0373-2 |
long_lat |
ENVELOPE(16.264,16.264,78.181,78.181) ENVELOPE(29.377,29.377,69.696,69.696) |
geographic |
Arctic Svalbard Norway Adventdalen Neiden |
geographic_facet |
Arctic Svalbard Norway Adventdalen Neiden |
genre |
Adventdalen Arctic Climate change Global warming Ice Northern Norway Northwest Russia palsa permafrost Svalbard Vorkuta |
genre_facet |
Adventdalen Arctic Climate change Global warming Ice Northern Norway Northwest Russia palsa permafrost Svalbard Vorkuta |
op_source |
ISSN: 0168-2563 EISSN: 1573-515X Biogeochemistry https://hal.science/hal-01594926 Biogeochemistry, 2017, 135 (3), pp.277-292. ⟨10.1007/s10533-017-0373-2⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1007/s10533-017-0373-2 hal-01594926 https://hal.science/hal-01594926 doi:10.1007/s10533-017-0373-2 PRODINRA: 406132 WOS: 000411147100006 |
op_doi |
https://doi.org/10.1007/s10533-017-0373-2 |
container_title |
Biogeochemistry |
container_volume |
135 |
container_issue |
3 |
container_start_page |
277 |
op_container_end_page |
292 |
_version_ |
1798843630600847360 |