Long - term legacy of land - use change in soils from a subtropical rainforest relating microbiological and physicochemical parameters

Tropical and subtropical ecosystems are widely affected by the expansion of agriculture over pristine lands. Despite research efforts, knowledge of the impact of land-use change on soil is still limited by intrinsic variability, inconsistent results and inadequate replication. This study aimed to better understand the consequences of land-use change by focusing on long-term effects on both soil biotic and abiotic parameters. For this purpose, we selected three productive farms under similar management, each of them with pristine forest sites and agricultural sites that had been deforested for 15 and 30 years. In each site, we analysed soil microbiological (phospholipid fatty acids [PLFAs], biomass and activity) and physicochemical parameters. Long-term land-use change caused a detriment in soil microbial biomass, activity and fungal abundance, but only small changes in PLFA composition. In fact, PLFA composition was more affected by soil physicochemical properties such as carbon-to-nutrient ratios and labile carbon than by land use. Some physicochemical parameters (e.g., organic carbon and nutrients) were also negatively affected by land-use change and were more sensitive to time under agricultural use than microbiological parameters. The lower sensitivity of microbiological parameters could be the result of severe drought conditions at sampling, which may have affected soil microbial communities in both land uses. We were also able to detect associations between specific microbiological and physicochemical parameters. Among these, we identified some that seemed to result from their co-variation in response to land-use change and others that seemed to be independent of land use. Overall, our results show that soils can suffer further deterioration several years after deforestation. In order to restore soil health in these degraded lands, we need to keep on investigating the physical, chemical and biological mechanisms responsible for this deterioration.

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Main Authors: Tosi, Micaela, Chludil, Hugo Daniel, Correa, Olga Susana, Vogrig, Jimena Andrea, Montecchia, Marcela Susana
Format: Texto biblioteca
Language:eng
Subjects:DEFORESTATION, MICROBIAL, ACTIVITY, MICROBIAL BIOMASS, PLFA, SOIL ORGANIC CARBON, YUNGAS, ,
Online Access:http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=54567
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id KOHA-OAI-AGRO:54567
record_format koha
institution UBA FA
collection Koha
country Argentina
countrycode AR
component Bibliográfico
access En linea
En linea
databasecode cat-ceiba
tag biblioteca
region America del Sur
libraryname Biblioteca Central FAUBA
language eng
topic DEFORESTATION
MICROBIAL
ACTIVITY
MICROBIAL BIOMASS
PLFA
SOIL ORGANIC CARBON
YUNGAS

DEFORESTATION
MICROBIAL
ACTIVITY
MICROBIAL BIOMASS
PLFA
SOIL ORGANIC CARBON
YUNGAS
spellingShingle DEFORESTATION
MICROBIAL
ACTIVITY
MICROBIAL BIOMASS
PLFA
SOIL ORGANIC CARBON
YUNGAS

DEFORESTATION
MICROBIAL
ACTIVITY
MICROBIAL BIOMASS
PLFA
SOIL ORGANIC CARBON
YUNGAS
Tosi, Micaela
Chludil, Hugo Daniel
Correa, Olga Susana
Vogrig, Jimena Andrea
Montecchia, Marcela Susana
Long - term legacy of land - use change in soils from a subtropical rainforest relating microbiological and physicochemical parameters
description Tropical and subtropical ecosystems are widely affected by the expansion of agriculture over pristine lands. Despite research efforts, knowledge of the impact of land-use change on soil is still limited by intrinsic variability, inconsistent results and inadequate replication. This study aimed to better understand the consequences of land-use change by focusing on long-term effects on both soil biotic and abiotic parameters. For this purpose, we selected three productive farms under similar management, each of them with pristine forest sites and agricultural sites that had been deforested for 15 and 30 years. In each site, we analysed soil microbiological (phospholipid fatty acids [PLFAs], biomass and activity) and physicochemical parameters. Long-term land-use change caused a detriment in soil microbial biomass, activity and fungal abundance, but only small changes in PLFA composition. In fact, PLFA composition was more affected by soil physicochemical properties such as carbon-to-nutrient ratios and labile carbon than by land use. Some physicochemical parameters (e.g., organic carbon and nutrients) were also negatively affected by land-use change and were more sensitive to time under agricultural use than microbiological parameters. The lower sensitivity of microbiological parameters could be the result of severe drought conditions at sampling, which may have affected soil microbial communities in both land uses. We were also able to detect associations between specific microbiological and physicochemical parameters. Among these, we identified some that seemed to result from their co-variation in response to land-use change and others that seemed to be independent of land use. Overall, our results show that soils can suffer further deterioration several years after deforestation. In order to restore soil health in these degraded lands, we need to keep on investigating the physical, chemical and biological mechanisms responsible for this deterioration.
format Texto
topic_facet
DEFORESTATION
MICROBIAL
ACTIVITY
MICROBIAL BIOMASS
PLFA
SOIL ORGANIC CARBON
YUNGAS
author Tosi, Micaela
Chludil, Hugo Daniel
Correa, Olga Susana
Vogrig, Jimena Andrea
Montecchia, Marcela Susana
author_facet Tosi, Micaela
Chludil, Hugo Daniel
Correa, Olga Susana
Vogrig, Jimena Andrea
Montecchia, Marcela Susana
author_sort Tosi, Micaela
title Long - term legacy of land - use change in soils from a subtropical rainforest relating microbiological and physicochemical parameters
title_short Long - term legacy of land - use change in soils from a subtropical rainforest relating microbiological and physicochemical parameters
title_full Long - term legacy of land - use change in soils from a subtropical rainforest relating microbiological and physicochemical parameters
title_fullStr Long - term legacy of land - use change in soils from a subtropical rainforest relating microbiological and physicochemical parameters
title_full_unstemmed Long - term legacy of land - use change in soils from a subtropical rainforest relating microbiological and physicochemical parameters
title_sort long - term legacy of land - use change in soils from a subtropical rainforest relating microbiological and physicochemical parameters
url http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=54567
http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=
http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=
http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=
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spelling KOHA-OAI-AGRO:545672022-08-16T13:28:32Zhttp://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=54567http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=http://ceiba.agro.uba.ar/cgi-bin/koha/opac-detail.pl?biblionumber=AAGLong - term legacy of land - use change in soils from a subtropical rainforest relating microbiological and physicochemical parametersTosi, MicaelaChludil, Hugo DanielCorrea, Olga SusanaVogrig, Jimena AndreaMontecchia, Marcela Susanatextengapplication/pdfTropical and subtropical ecosystems are widely affected by the expansion of agriculture over pristine lands. Despite research efforts, knowledge of the impact of land-use change on soil is still limited by intrinsic variability, inconsistent results and inadequate replication. This study aimed to better understand the consequences of land-use change by focusing on long-term effects on both soil biotic and abiotic parameters. For this purpose, we selected three productive farms under similar management, each of them with pristine forest sites and agricultural sites that had been deforested for 15 and 30 years. In each site, we analysed soil microbiological (phospholipid fatty acids [PLFAs], biomass and activity) and physicochemical parameters. Long-term land-use change caused a detriment in soil microbial biomass, activity and fungal abundance, but only small changes in PLFA composition. In fact, PLFA composition was more affected by soil physicochemical properties such as carbon-to-nutrient ratios and labile carbon than by land use. Some physicochemical parameters (e.g., organic carbon and nutrients) were also negatively affected by land-use change and were more sensitive to time under agricultural use than microbiological parameters. The lower sensitivity of microbiological parameters could be the result of severe drought conditions at sampling, which may have affected soil microbial communities in both land uses. We were also able to detect associations between specific microbiological and physicochemical parameters. Among these, we identified some that seemed to result from their co-variation in response to land-use change and others that seemed to be independent of land use. Overall, our results show that soils can suffer further deterioration several years after deforestation. In order to restore soil health in these degraded lands, we need to keep on investigating the physical, chemical and biological mechanisms responsible for this deterioration.Tropical and subtropical ecosystems are widely affected by the expansion of agriculture over pristine lands. Despite research efforts, knowledge of the impact of land-use change on soil is still limited by intrinsic variability, inconsistent results and inadequate replication. This study aimed to better understand the consequences of land-use change by focusing on long-term effects on both soil biotic and abiotic parameters. For this purpose, we selected three productive farms under similar management, each of them with pristine forest sites and agricultural sites that had been deforested for 15 and 30 years. In each site, we analysed soil microbiological (phospholipid fatty acids [PLFAs], biomass and activity) and physicochemical parameters. Long-term land-use change caused a detriment in soil microbial biomass, activity and fungal abundance, but only small changes in PLFA composition. In fact, PLFA composition was more affected by soil physicochemical properties such as carbon-to-nutrient ratios and labile carbon than by land use. Some physicochemical parameters (e.g., organic carbon and nutrients) were also negatively affected by land-use change and were more sensitive to time under agricultural use than microbiological parameters. The lower sensitivity of microbiological parameters could be the result of severe drought conditions at sampling, which may have affected soil microbial communities in both land uses. We were also able to detect associations between specific microbiological and physicochemical parameters. Among these, we identified some that seemed to result from their co-variation in response to land-use change and others that seemed to be independent of land use. Overall, our results show that soils can suffer further deterioration several years after deforestation. In order to restore soil health in these degraded lands, we need to keep on investigating the physical, chemical and biological mechanisms responsible for this deterioration.DEFORESTATIONMICROBIALACTIVITYMICROBIAL BIOMASSPLFASOIL ORGANIC CARBONYUNGASEuropean journal of soil science