Long-Term Effects of Climate and Litter Chemistry on Rates and Stable Fractions of Decomposing Scots Pine and Norway Spruce Needle Litter—A Synthesis

We have reviewed information on early-, late- and limit-value decomposition stages for litter of Norway spruce (<i>Picea abies</i>) and Scots pine (<i>Pinus silvestris</i>). This synthesis covers c 16 studies/papers made along a climatic gradient; range in mean annual tempera...

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Main Authors: Björn Berg, Mikael Lönn
Format: Article
Language:English
Published: MDPI AG 2022-01-01
Series:Forests
Subjects:
Online Access:https://www.mdpi.com/1999-4907/13/1/125
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author Björn Berg
Mikael Lönn
author_facet Björn Berg
Mikael Lönn
author_sort Björn Berg
collection DOAJ
description We have reviewed information on early-, late- and limit-value decomposition stages for litter of Norway spruce (<i>Picea abies</i>) and Scots pine (<i>Pinus silvestris</i>). This synthesis covers c 16 studies/papers made along a climatic gradient; range in mean annual temperature (MAT) from −1 to +7 °C and mean annual precipitation (MAP) from 425 to 1070 mm. Scots pine has an early stage dominated by carbohydrate decomposition and a late stage dominated by decomposition of lignin; Norway spruce has just one stage dominated by lignin decomposition. We used data for annual mass loss to identify rate-regulating factors in both stages; climate data, namely, MAT and MAP, as well as substrate properties, namely, nitrogen (N), acid unhydrolyzable residue (AUR), manganese (Mn). Early-stage decomposition for Scots pine litter was dominated positively by MAT; the late stage was dominated negatively by MAT, N, and AUR, changing with decomposition stage; there was no effect of Mn. Norway spruce litter had no early stage; decomposition in the lignin-dominated stage was mainly negative to MAP, a negative relationship to AUR and non-significant relationships to N and MAT. Mn had a positive relationship. Limit values for decomposition, namely, the accumulated mass loss at which decomposition is calculated to be zero, were related positively to Mn and AUR for Scots pine litter and negatively to AUR for Norway spruce litter. With different sets of rate-regulating factors as well as different compounds/elements related to the limit values, the decomposition patterns or pathways are different.
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spelling doaj.art-ec4c24faaf7442ad94ae610594d8e3b82023-11-23T13:48:15ZengMDPI AGForests1999-49072022-01-0113112510.3390/f13010125Long-Term Effects of Climate and Litter Chemistry on Rates and Stable Fractions of Decomposing Scots Pine and Norway Spruce Needle Litter—A SynthesisBjörn Berg0Mikael Lönn1Department of Forest Sciences, University of Helsinki, FIN-00014 Helsinki, FinlandFaculty of Engineering, Sustainable Development Department of Electrical Engineering, Mathematics, and Science, University of Gävle, SE-801 76 Gävle, SwedenWe have reviewed information on early-, late- and limit-value decomposition stages for litter of Norway spruce (<i>Picea abies</i>) and Scots pine (<i>Pinus silvestris</i>). This synthesis covers c 16 studies/papers made along a climatic gradient; range in mean annual temperature (MAT) from −1 to +7 °C and mean annual precipitation (MAP) from 425 to 1070 mm. Scots pine has an early stage dominated by carbohydrate decomposition and a late stage dominated by decomposition of lignin; Norway spruce has just one stage dominated by lignin decomposition. We used data for annual mass loss to identify rate-regulating factors in both stages; climate data, namely, MAT and MAP, as well as substrate properties, namely, nitrogen (N), acid unhydrolyzable residue (AUR), manganese (Mn). Early-stage decomposition for Scots pine litter was dominated positively by MAT; the late stage was dominated negatively by MAT, N, and AUR, changing with decomposition stage; there was no effect of Mn. Norway spruce litter had no early stage; decomposition in the lignin-dominated stage was mainly negative to MAP, a negative relationship to AUR and non-significant relationships to N and MAT. Mn had a positive relationship. Limit values for decomposition, namely, the accumulated mass loss at which decomposition is calculated to be zero, were related positively to Mn and AUR for Scots pine litter and negatively to AUR for Norway spruce litter. With different sets of rate-regulating factors as well as different compounds/elements related to the limit values, the decomposition patterns or pathways are different.https://www.mdpi.com/1999-4907/13/1/125decompositionacid unhydrolyzable residuemanganesenitrogenplant litterlimit values
spellingShingle Björn Berg
Mikael Lönn
Long-Term Effects of Climate and Litter Chemistry on Rates and Stable Fractions of Decomposing Scots Pine and Norway Spruce Needle Litter—A Synthesis
Forests
decomposition
acid unhydrolyzable residue
manganese
nitrogen
plant litter
limit values
title Long-Term Effects of Climate and Litter Chemistry on Rates and Stable Fractions of Decomposing Scots Pine and Norway Spruce Needle Litter—A Synthesis
title_full Long-Term Effects of Climate and Litter Chemistry on Rates and Stable Fractions of Decomposing Scots Pine and Norway Spruce Needle Litter—A Synthesis
title_fullStr Long-Term Effects of Climate and Litter Chemistry on Rates and Stable Fractions of Decomposing Scots Pine and Norway Spruce Needle Litter—A Synthesis
title_full_unstemmed Long-Term Effects of Climate and Litter Chemistry on Rates and Stable Fractions of Decomposing Scots Pine and Norway Spruce Needle Litter—A Synthesis
title_short Long-Term Effects of Climate and Litter Chemistry on Rates and Stable Fractions of Decomposing Scots Pine and Norway Spruce Needle Litter—A Synthesis
title_sort long term effects of climate and litter chemistry on rates and stable fractions of decomposing scots pine and norway spruce needle litter a synthesis
topic decomposition
acid unhydrolyzable residue
manganese
nitrogen
plant litter
limit values
url https://www.mdpi.com/1999-4907/13/1/125
work_keys_str_mv AT bjornberg longtermeffectsofclimateandlitterchemistryonratesandstablefractionsofdecomposingscotspineandnorwayspruceneedlelitterasynthesis
AT mikaellonn longtermeffectsofclimateandlitterchemistryonratesandstablefractionsofdecomposingscotspineandnorwayspruceneedlelitterasynthesis