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Statements

Subject Item
n2:RIV%2F60077344%3A_____%2F13%3A00398219%21RIV14-AV0-60077344
rdf:type
n5:Vysledek skos:Concept
dcterms:description
Soil biota were studied at four post-mining areas along a climatic gradient in the USA. The natural climax vegetation was hardwood forest (TN, IN), tallgrass prairie (IL), or shortgrass prairie (WY). Two chronosequences were used in each state, each contained young (2-5y) and old (15-20y) post-mining and a site with the area's climax vegetation. All sites were sampled in spring 2008 and 2011. Microbial biomass, microbial respiration, ergosterol, composition of microbial community (using phospholipid fatty acids), community composition of soil nematodes and macrofauna, soil chemistry, and soil microstructure (using thin soil sections) were studied. Total carbon and nitrogen content increased with successional age, while total phosphorus was often greater in young post-mining sites than in climax sites. Microbial biomass in forest chronosequences increased with age, actinobacteria were associated with prairie sites, and fungi were associated with forest sites. Root-feeding nematodes and macroflora were dominant in the shortgrass prairie sites. Earthworms were absent in such shortgrass sites but were present in the wetter, eastern sites. In forest chronosequences, other saprophages, litter transformers, and microphagous groups were also abundant. Absence of saprophagous groups, and especially earthworms, resulted in the absence of bioturbation in shortgrass prairie sites while worm casts and other biogenic structures formed an important part of the soil profile in other chronosequences. Both young and old restoration sites were much closer to the climax condition in shortgrass prairie than in the other sites. The shortgrass prairie soil community contained abundant root-feeding organisms, which may establish quicker than the more saprophagous soil biota that were abundant at the other sites. Soil biota were studied at four post-mining areas along a climatic gradient in the USA. The natural climax vegetation was hardwood forest (TN, IN), tallgrass prairie (IL), or shortgrass prairie (WY). Two chronosequences were used in each state, each contained young (2-5y) and old (15-20y) post-mining and a site with the area's climax vegetation. All sites were sampled in spring 2008 and 2011. Microbial biomass, microbial respiration, ergosterol, composition of microbial community (using phospholipid fatty acids), community composition of soil nematodes and macrofauna, soil chemistry, and soil microstructure (using thin soil sections) were studied. Total carbon and nitrogen content increased with successional age, while total phosphorus was often greater in young post-mining sites than in climax sites. Microbial biomass in forest chronosequences increased with age, actinobacteria were associated with prairie sites, and fungi were associated with forest sites. Root-feeding nematodes and macroflora were dominant in the shortgrass prairie sites. Earthworms were absent in such shortgrass sites but were present in the wetter, eastern sites. In forest chronosequences, other saprophages, litter transformers, and microphagous groups were also abundant. Absence of saprophagous groups, and especially earthworms, resulted in the absence of bioturbation in shortgrass prairie sites while worm casts and other biogenic structures formed an important part of the soil profile in other chronosequences. Both young and old restoration sites were much closer to the climax condition in shortgrass prairie than in the other sites. The shortgrass prairie soil community contained abundant root-feeding organisms, which may establish quicker than the more saprophagous soil biota that were abundant at the other sites.
dcterms:title
Soil biota in post-mining sites along a climatic gradient in the USA: Simple communities in shortgrass prairie recover faster than complex communities in tallgrass prairie and forest Soil biota in post-mining sites along a climatic gradient in the USA: Simple communities in shortgrass prairie recover faster than complex communities in tallgrass prairie and forest
skos:prefLabel
Soil biota in post-mining sites along a climatic gradient in the USA: Simple communities in shortgrass prairie recover faster than complex communities in tallgrass prairie and forest Soil biota in post-mining sites along a climatic gradient in the USA: Simple communities in shortgrass prairie recover faster than complex communities in tallgrass prairie and forest
skos:notation
RIV/60077344:_____/13:00398219!RIV14-AV0-60077344
n5:predkladatel
n19:ico%3A60077344
n3:aktivita
n16:I n16:S n16:P
n3:aktivity
I, P(ME08019), S
n3:cisloPeriodika
December
n3:dodaniDat
n10:2014
n3:domaciTvurceVysledku
n8:2347156 n8:4914066 n8:1277839 n8:1271954
n3:druhVysledku
n18:J
n3:duvernostUdaju
n4:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
106186
n3:idVysledku
RIV/60077344:_____/13:00398219
n3:jazykVysledku
n15:eng
n3:klicovaSlova
restoration; succession; ergosterol; macrofauna; microbial biomass; PLFA
n3:klicoveSlovo
n6:restoration n6:macrofauna n6:ergosterol n6:microbial%20biomass n6:PLFA n6:succession
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[78C1479715C3]
n3:nazevZdroje
Soil Biology and Biochemistry
n3:obor
n11:EH
n3:pocetDomacichTvurcuVysledku
4
n3:pocetTvurcuVysledku
13
n3:projekt
n17:ME08019
n3:rokUplatneniVysledku
n10:2013
n3:svazekPeriodika
67
n3:tvurceVysledku
Cajthaml, T. Tajovský, Karel Kolaříková, K. Jílková, V. Pižl, Václav Nawrot, J. Frouz, Jan Šimáčková, H. Háněl, Ladislav Stahl, P. D. Groninger, J. W. Burešová, A. Franklin, J.
n3:wos
000327107700025
s:issn
0038-0717
s:numberOfPages
14
n12:doi
10.1016/j.soilbio.2013.08.025