Effects of Biological Soil Crusts on Enzyme Activities and Microbial Community in Soils of an Arid Ecosystem.
Bacteria
/ enzymology
Biodiversity
Carbon
/ metabolism
Carbon Cycle
Cyanobacteria
/ growth & development
Desert Climate
Ecosystem
Environmental Monitoring
Enzyme Activation
Fungi
/ enzymology
Hydrogen-Ion Concentration
Hydrolases
/ metabolism
Lichens
/ growth & development
Microbiota
Monophenol Monooxygenase
Nitrogen
/ metabolism
Soil
/ chemistry
Soil Microbiology
Tunisia
Water
Biological soil crusts
Desert
Enzyme activities
Microbial community
Soil depth
Soil properties
Journal
Microbial ecology
ISSN: 1432-184X
Titre abrégé: Microb Ecol
Pays: United States
ID NLM: 7500663
Informations de publication
Date de publication:
Jan 2019
Jan 2019
Historique:
received:
17
11
2017
accepted:
04
06
2018
pubmed:
21
6
2018
medline:
23
1
2019
entrez:
21
6
2018
Statut:
ppublish
Résumé
Arid ecosystems constitute 41% of land's surface and play an important role in global carbon cycle. In particular, biological soil crusts (BSC) are known to be a hotspot of carbon fixation as well as mineralization in arid ecosystems. However, little information is available on carbon decomposition and microbes in BSC and key controlling variables for microbial activities in arid ecosystems. The current study, carried out in South Mediterranean arid ecosystem, aimed to evaluate the effects of intact and removed cyanobacteria/lichen crusts on soil properties, soil enzyme activities, and microbial abundances (bacteria and fungi). We compared five different treatments (bare soil, soil with intact cyanobacteria, soil with cyanobacteria removed, soil with intact lichens, and soil with lichens removed) in four different soil layers (0-5, 5-10, 10-15, and 15-20 cm). Regardless of soil treatments, activities of hydrolases and water content increased with increasing soil depth. The presence of lichens increased significantly hydrolase activities, which appeared to be associated with greater organic matter, nitrogen, and water contents. However, phenol oxidase was mainly controlled by pH and oxygen availability. Neither fungal nor bacterial abundance exhibited a significant correlation with enzyme activities suggesting that soil enzyme activities are mainly controlled by edaphic and environmental conditions rather than source microbes. Interestingly, the presence of lichens reduced the abundance of bacteria of which mechanism is still to be investigated.
Identifiants
pubmed: 29922904
doi: 10.1007/s00248-018-1219-8
pii: 10.1007/s00248-018-1219-8
doi:
Substances chimiques
Soil
0
Water
059QF0KO0R
Carbon
7440-44-0
Monophenol Monooxygenase
EC 1.14.18.1
Hydrolases
EC 3.-
Nitrogen
N762921K75
Types de publication
Journal Article
Langues
eng
Sous-ensembles de citation
IM
Pagination
201-216Subventions
Organisme : National Research Foundation of Korea
ID : 2016R1D1A1A02937049
Organisme : National Research Foundation of Korea
ID : 20110030040
Organisme : National Research Foundation of Korea
ID : 2016R1D1A1A02937049
Organisme : Korea Forest Service
ID : 2017096A001719BB01
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