Relationships between humus profiles and C cycling, first results from a Mediterranean pine forest

Pine species used for land restoration in the Mediterranean basin since the late 19th century are nowadays showing symptoms of degradation. Forest degradation may reduce the forest potential to act as a C sink, or even increase the C losses through greenhouse gas (GHG) emissions. Microbial processes...

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Main Author: ROMINA LORENZETTI
Format: Article
Language:English
Published: University of Bologna 2019-01-01
Series:EQA
Subjects:
Online Access:https://eqa.unibo.it/article/view/8435
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author ROMINA LORENZETTI
author_facet ROMINA LORENZETTI
author_sort ROMINA LORENZETTI
collection DOAJ
description Pine species used for land restoration in the Mediterranean basin since the late 19th century are nowadays showing symptoms of degradation. Forest degradation may reduce the forest potential to act as a C sink, or even increase the C losses through greenhouse gas (GHG) emissions. Microbial processes strongly affect SOM decomposition and therefore C fluxes. Since the first and most important modifications of microbial processes occur within humus profiles, humus characteristics and structure might affect microbial processes and GHG emissions. The study was carried out to relate C cycling in a degraded pine forest with the morphology and characteristics of the humus profiles.The study area was located near Florence (Central Italy) in a reforest area planted with Black pine, Brutia pine, and Cypress. In spring 2016, 9 humus profiles were described, sampled and classified, and CO2 and CH4 fluxeswere measured. Humus profiles were analyzed for bulk density, particle size, N, C, lime content and pH. Bio macroaggregates of the first mineral horizon were separated by moist sieving in three size classes ( <1 mm, 1-4 mm, >4 mm) for the humus classification. Statistical relationships were checked by a Spearman test.Eumacroamphi was the main humus form, while Dysmull and Pachiamphi were less frequent. There were significant correlations between CH4 fluxes and both the thickness of the transition from organic to inorganic horizons, and the percentage of aggregates in different size classes. CO2 emission did not provide significant correlations with humus features. These first results suggest that the activity of methanotrophic bacteria responsible for CH4 uptake might be lower where the thickness of the transition between the organic and mineral horizons is larger.
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spelling doaj.art-67db6c2bb4734ec1980611e1f3a901d52022-12-22T03:56:06ZengUniversity of BolognaEQA2039-98982281-44852019-01-01330375310.6092/issn.2281-4485/84357728Relationships between humus profiles and C cycling, first results from a Mediterranean pine forestROMINA LORENZETTI0Research Center Agriculture and Environment (AA) Via di Lanciola, 12/A 50125 Firenze,Pine species used for land restoration in the Mediterranean basin since the late 19th century are nowadays showing symptoms of degradation. Forest degradation may reduce the forest potential to act as a C sink, or even increase the C losses through greenhouse gas (GHG) emissions. Microbial processes strongly affect SOM decomposition and therefore C fluxes. Since the first and most important modifications of microbial processes occur within humus profiles, humus characteristics and structure might affect microbial processes and GHG emissions. The study was carried out to relate C cycling in a degraded pine forest with the morphology and characteristics of the humus profiles.The study area was located near Florence (Central Italy) in a reforest area planted with Black pine, Brutia pine, and Cypress. In spring 2016, 9 humus profiles were described, sampled and classified, and CO2 and CH4 fluxeswere measured. Humus profiles were analyzed for bulk density, particle size, N, C, lime content and pH. Bio macroaggregates of the first mineral horizon were separated by moist sieving in three size classes ( <1 mm, 1-4 mm, >4 mm) for the humus classification. Statistical relationships were checked by a Spearman test.Eumacroamphi was the main humus form, while Dysmull and Pachiamphi were less frequent. There were significant correlations between CH4 fluxes and both the thickness of the transition from organic to inorganic horizons, and the percentage of aggregates in different size classes. CO2 emission did not provide significant correlations with humus features. These first results suggest that the activity of methanotrophic bacteria responsible for CH4 uptake might be lower where the thickness of the transition between the organic and mineral horizons is larger.https://eqa.unibo.it/article/view/8435humus profilesoilGHGorganic Carbonmethane
spellingShingle ROMINA LORENZETTI
Relationships between humus profiles and C cycling, first results from a Mediterranean pine forest
EQA
humus profile
soil
GHG
organic Carbon
methane
title Relationships between humus profiles and C cycling, first results from a Mediterranean pine forest
title_full Relationships between humus profiles and C cycling, first results from a Mediterranean pine forest
title_fullStr Relationships between humus profiles and C cycling, first results from a Mediterranean pine forest
title_full_unstemmed Relationships between humus profiles and C cycling, first results from a Mediterranean pine forest
title_short Relationships between humus profiles and C cycling, first results from a Mediterranean pine forest
title_sort relationships between humus profiles and c cycling first results from a mediterranean pine forest
topic humus profile
soil
GHG
organic Carbon
methane
url https://eqa.unibo.it/article/view/8435
work_keys_str_mv AT rominalorenzetti relationshipsbetweenhumusprofilesandccyclingfirstresultsfromamediterraneanpineforest