Effects of warming and litter positions on litter decomposition in a boreal peatland

Litter decomposition is an important source of carbon accumulation in the permafrost peatlands. Climate warming has led to shrub expansions and accelerated litter mixing with soils and fluctuations in the water table. However, little is known about how changes in the position of the litter will affe...

Full description

Bibliographic Details
Main Authors: Guobao Ma, Xianwei Wang, Xiaoxin Sun, Shujie Wang, Yu Du, Jingyi Jiang
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-12-01
Series:Frontiers in Ecology and Evolution
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fevo.2022.1078104/full
_version_ 1811200222815059968
author Guobao Ma
Guobao Ma
Xianwei Wang
Xiaoxin Sun
Xiaoxin Sun
Shujie Wang
Shujie Wang
Yu Du
Jingyi Jiang
Jingyi Jiang
author_facet Guobao Ma
Guobao Ma
Xianwei Wang
Xiaoxin Sun
Xiaoxin Sun
Shujie Wang
Shujie Wang
Yu Du
Jingyi Jiang
Jingyi Jiang
author_sort Guobao Ma
collection DOAJ
description Litter decomposition is an important source of carbon accumulation in the permafrost peatlands. Climate warming has led to shrub expansions and accelerated litter mixing with soils and fluctuations in the water table. However, little is known about how changes in the position of the litter will affect litter decomposition under climate warming. To reveal the mechanisms of response of the location of litter in the soil and climate warming to litter decomposition in permafrost peatlands. Here, we selected the evergreen shrub, Chamaedaphne calyculata, and the deciduous shrub, Vaccinium uliginosum, from the permafrost peatlands of the Greater Hing’an Mountains, China. The leaf litter was placed on the soil surface (no-mixing) and mixed with the soil (soil-litter mixing), and then it was incubated for 124 days at 15°C (control) and 20°C (warming). Our results showed that warming significantly increased the CO2 emission rates of C. calyculata and V. uliginosum by 19.9 and 17.4%, respectively. When compared to no-mixing, the CO2 emission rates were reduced (not significantly) by 1.5 (C. calyculata) and increased 13.6% (V. uliginosum) with soil-litter mixing. Interestingly, soil-litter mixing suppressed the positive effect of warming on the CO2 emission rates relative to no-mixing, and the suppressing effects in the V. uliginosum subplot were stronger than those in the C. calyculata subplot. Specifically, warming significantly increased the CO2 emissions of C. calyculata by 27.4% under no-mixing but the increase decreased to 13.1% under soil-litter mixing. Similarly, warming induced significant increases in the CO2 emissions of V. uliginosum, with an increase of 38.8% under no-mixing but non-significant increases (1.9%) were observed under soil-litter mixing. The combination of the enzyme activities of β-1,4-glucosidase, β-1,4-xylosidase and β-D-1,4-cellobiosidase and laccase and phenolics explained more than 60.0% of the variability in the CO2 emissions of C. calyculata and V. uliginosum, respectively. Our study highlights the importance of litter positions in mediating the responses of litter decomposition to climate warming and shrub expansions in the northern peatlands.
first_indexed 2024-04-12T02:01:02Z
format Article
id doaj.art-1e321c8d37484cea9bfc38763e885c2e
institution Directory Open Access Journal
issn 2296-701X
language English
last_indexed 2024-04-12T02:01:02Z
publishDate 2022-12-01
publisher Frontiers Media S.A.
record_format Article
series Frontiers in Ecology and Evolution
spelling doaj.art-1e321c8d37484cea9bfc38763e885c2e2022-12-22T03:52:40ZengFrontiers Media S.A.Frontiers in Ecology and Evolution2296-701X2022-12-011010.3389/fevo.2022.10781041078104Effects of warming and litter positions on litter decomposition in a boreal peatlandGuobao Ma0Guobao Ma1Xianwei Wang2Xiaoxin Sun3Xiaoxin Sun4Shujie Wang5Shujie Wang6Yu Du7Jingyi Jiang8Jingyi Jiang9Key Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaKey Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, Northeast Forestry University, Harbin, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaKey Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, Northeast Forestry University, Harbin, ChinaHeilongjiang Sanjiang Plain Wetland Ecosystem Research Station, Fuyuan, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaKey Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, Northeast Forestry University, Harbin, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaKey Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, Northeast Forestry University, Harbin, ChinaLitter decomposition is an important source of carbon accumulation in the permafrost peatlands. Climate warming has led to shrub expansions and accelerated litter mixing with soils and fluctuations in the water table. However, little is known about how changes in the position of the litter will affect litter decomposition under climate warming. To reveal the mechanisms of response of the location of litter in the soil and climate warming to litter decomposition in permafrost peatlands. Here, we selected the evergreen shrub, Chamaedaphne calyculata, and the deciduous shrub, Vaccinium uliginosum, from the permafrost peatlands of the Greater Hing’an Mountains, China. The leaf litter was placed on the soil surface (no-mixing) and mixed with the soil (soil-litter mixing), and then it was incubated for 124 days at 15°C (control) and 20°C (warming). Our results showed that warming significantly increased the CO2 emission rates of C. calyculata and V. uliginosum by 19.9 and 17.4%, respectively. When compared to no-mixing, the CO2 emission rates were reduced (not significantly) by 1.5 (C. calyculata) and increased 13.6% (V. uliginosum) with soil-litter mixing. Interestingly, soil-litter mixing suppressed the positive effect of warming on the CO2 emission rates relative to no-mixing, and the suppressing effects in the V. uliginosum subplot were stronger than those in the C. calyculata subplot. Specifically, warming significantly increased the CO2 emissions of C. calyculata by 27.4% under no-mixing but the increase decreased to 13.1% under soil-litter mixing. Similarly, warming induced significant increases in the CO2 emissions of V. uliginosum, with an increase of 38.8% under no-mixing but non-significant increases (1.9%) were observed under soil-litter mixing. The combination of the enzyme activities of β-1,4-glucosidase, β-1,4-xylosidase and β-D-1,4-cellobiosidase and laccase and phenolics explained more than 60.0% of the variability in the CO2 emissions of C. calyculata and V. uliginosum, respectively. Our study highlights the importance of litter positions in mediating the responses of litter decomposition to climate warming and shrub expansions in the northern peatlands.https://www.frontiersin.org/articles/10.3389/fevo.2022.1078104/fullboreal peatlandlitter decompositionsoil-litter incubationCO2 fluxesenzyme activity
spellingShingle Guobao Ma
Guobao Ma
Xianwei Wang
Xiaoxin Sun
Xiaoxin Sun
Shujie Wang
Shujie Wang
Yu Du
Jingyi Jiang
Jingyi Jiang
Effects of warming and litter positions on litter decomposition in a boreal peatland
Frontiers in Ecology and Evolution
boreal peatland
litter decomposition
soil-litter incubation
CO2 fluxes
enzyme activity
title Effects of warming and litter positions on litter decomposition in a boreal peatland
title_full Effects of warming and litter positions on litter decomposition in a boreal peatland
title_fullStr Effects of warming and litter positions on litter decomposition in a boreal peatland
title_full_unstemmed Effects of warming and litter positions on litter decomposition in a boreal peatland
title_short Effects of warming and litter positions on litter decomposition in a boreal peatland
title_sort effects of warming and litter positions on litter decomposition in a boreal peatland
topic boreal peatland
litter decomposition
soil-litter incubation
CO2 fluxes
enzyme activity
url https://www.frontiersin.org/articles/10.3389/fevo.2022.1078104/full
work_keys_str_mv AT guobaoma effectsofwarmingandlitterpositionsonlitterdecompositioninaborealpeatland
AT guobaoma effectsofwarmingandlitterpositionsonlitterdecompositioninaborealpeatland
AT xianweiwang effectsofwarmingandlitterpositionsonlitterdecompositioninaborealpeatland
AT xiaoxinsun effectsofwarmingandlitterpositionsonlitterdecompositioninaborealpeatland
AT xiaoxinsun effectsofwarmingandlitterpositionsonlitterdecompositioninaborealpeatland
AT shujiewang effectsofwarmingandlitterpositionsonlitterdecompositioninaborealpeatland
AT shujiewang effectsofwarmingandlitterpositionsonlitterdecompositioninaborealpeatland
AT yudu effectsofwarmingandlitterpositionsonlitterdecompositioninaborealpeatland
AT jingyijiang effectsofwarmingandlitterpositionsonlitterdecompositioninaborealpeatland
AT jingyijiang effectsofwarmingandlitterpositionsonlitterdecompositioninaborealpeatland