FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2757639954> ?p ?o ?g. }

• W2757639954 endingPage "88" @default.
• W2757639954 startingPage "81" @default.
• W2757639954 abstract "The Qinghai-Tibetan plateau (QTP) is the largest middle-low latitude permafrost region on earth, while little is known about the microbial community in this area. Here, we investigated the bacterial community in the upper 30 cm soils in the permafrost regions on the central QTP using Illumina sequencing technology. In these soils, the most abundant phyla were Acidobacteria, Proteobacteria, and Bacteroidetes. The depth was significantly correlated with Acidobacteria, Proteobacteria, Nitrospirae, and Gemmatimonadetes. The soil pH and the gravel content were significantly positively correlated with Bacteroidetes. The active layer thickness was significantly correlated with Bacteroidetes and Arabinonates. Although these factors were closely correlated with the relative abundances of specific bacterial phyla, the overall bacterial community structure was mainly affected by pH, soil organic carbon content, and the mean annual precipitation, while the community structure had no significant relationship with the active layer thickness. Our results suggested that the permafrost region on the QTP had greatly heterogeneous environmental conditions, and the responses of microbial communities to permafrost degradation would also be affected by other factors such as precipitation, soil texture and vegetation." @default.
• W2757639954 created "2017-10-06" @default.
• W2757639954 creator A5002632116 @default.
• W2757639954 creator A5015649184 @default.
• W2757639954 creator A5025740512 @default.
• W2757639954 creator A5062189086 @default.
• W2757639954 creator A5065463000 @default.
• W2757639954 creator A5067501579 @default.
• W2757639954 date "2017-11-01" @default.
• W2757639954 modified "2023-09-29" @default.
• W2757639954 title "Bacterial communities in the upper soil layers in the permafrost regions on the Qinghai-Tibetan plateau" @default.
• W2757639954 cites W1429438452 @default.
• W2757639954 cites W1496360119 @default.
• W2757639954 cites W1562095166 @default.
• W2757639954 cites W1775995716 @default.
• W2757639954 cites W1776255253 @default.
• W2757639954 cites W1782851837 @default.
• W2757639954 cites W1908125853 @default.
• W2757639954 cites W1965426652 @default.
• W2757639954 cites W1968875816 @default.
• W2757639954 cites W1973916751 @default.
• W2757639954 cites W1975952122 @default.
• W2757639954 cites W1980680725 @default.
• W2757639954 cites W1987455229 @default.
• W2757639954 cites W1988598260 @default.
• W2757639954 cites W1991751172 @default.
• W2757639954 cites W1994663675 @default.
• W2757639954 cites W2006905434 @default.
• W2757639954 cites W2009225674 @default.
• W2757639954 cites W2020541862 @default.
• W2757639954 cites W2022866472 @default.
• W2757639954 cites W2023289133 @default.
• W2757639954 cites W2023553066 @default.
• W2757639954 cites W2027496182 @default.
• W2757639954 cites W2031036811 @default.
• W2757639954 cites W2033378871 @default.
• W2757639954 cites W2035648478 @default.
• W2757639954 cites W2035764881 @default.
• W2757639954 cites W2041383474 @default.
• W2757639954 cites W2043207844 @default.
• W2757639954 cites W2045193375 @default.
• W2757639954 cites W2061014683 @default.
• W2757639954 cites W2063805278 @default.
• W2757639954 cites W2077043162 @default.
• W2757639954 cites W2077621345 @default.
• W2757639954 cites W2092705479 @default.
• W2757639954 cites W2093922401 @default.
• W2757639954 cites W2093972211 @default.
• W2757639954 cites W2094200273 @default.
• W2757639954 cites W2094621429 @default.
• W2757639954 cites W2098627306 @default.
• W2757639954 cites W2114907359 @default.
• W2757639954 cites W2122219741 @default.
• W2757639954 cites W2131873925 @default.
• W2757639954 cites W2139710790 @default.
• W2757639954 cites W2147199223 @default.
• W2757639954 cites W2150739290 @default.
• W2757639954 cites W2153544489 @default.
• W2757639954 cites W2153608295 @default.
• W2757639954 cites W2154736508 @default.
• W2757639954 cites W2158585514 @default.
• W2757639954 cites W2167160775 @default.
• W2757639954 cites W2169510843 @default.
• W2757639954 cites W2173484664 @default.
• W2757639954 cites W2252559806 @default.
• W2757639954 cites W2275657981 @default.
• W2757639954 cites W2286444721 @default.
• W2757639954 cites W2296041506 @default.
• W2757639954 cites W2474361916 @default.
• W2757639954 cites W3147128100 @default.
• W2757639954 cites W4241890243 @default.
• W2757639954 doi "https://doi.org/10.1016/j.apsoil.2017.08.001" @default.
• W2757639954 hasPublicationYear "2017" @default.
• W2757639954 type Work @default.
• W2757639954 sameAs 2757639954 @default.
• W2757639954 citedByCount "31" @default.
• W2757639954 countsByYear W27576399542018 @default.
• W2757639954 countsByYear W27576399542019 @default.
• W2757639954 countsByYear W27576399542020 @default.
• W2757639954 countsByYear W27576399542021 @default.
• W2757639954 countsByYear W27576399542022 @default.
• W2757639954 countsByYear W27576399542023 @default.
• W2757639954 crossrefType "journal-article" @default.
• W2757639954 hasAuthorship W2757639954A5002632116 @default.
• W2757639954 hasAuthorship W2757639954A5015649184 @default.
• W2757639954 hasAuthorship W2757639954A5025740512 @default.
• W2757639954 hasAuthorship W2757639954A5062189086 @default.
• W2757639954 hasAuthorship W2757639954A5065463000 @default.
• W2757639954 hasAuthorship W2757639954A5067501579 @default.
• W2757639954 hasConcept C127313418 @default.
• W2757639954 hasConcept C134306372 @default.
• W2757639954 hasConcept C142724271 @default.
• W2757639954 hasConcept C15098985 @default.
• W2757639954 hasConcept C151730666 @default.
• W2757639954 hasConcept C159390177 @default.
• W2757639954 hasConcept C159750122 @default.
• W2757639954 hasConcept C18903297 @default.
• W2757639954 hasConcept C2775896646 @default.

• next