Matches in SemOpenAlex for { <https://semopenalex.org/work/W4386826209> ?p ?o ?g. }
- W4386826209 abstract "Abstract Background To investigate microbial communities and their contributions to carbon and nutrient cycling along water gradients can enhance our comprehension of climate change impacts on ecosystem services. Results We conducted an assessment of microbial communities, metagenomic functions, and metabolomic profiles within four ecosystems, i.e., desert grassland (DG), shrub-steppe (SS), forest (FO) and marsh (MA) in the Altai region of Xinjiang, China. Soil total carbon (TC), total nitrogen, NH 4 + , and NO 3 - increased linearly, but pH decreased with soil water gradients. Microbial abundances and richness also increased with soil moisture except the abundances of fungi and protists being lowest in MA. Within prokaryotes, the relative abundances of Proteobacteria and Acidobacteria increased, whereas those of Actinobacteria and Thaumarchaeota decreased along water gradients. In fungi and protists, Basidiomycota and Mortierellomycota, Evosea and Endomyxa became dominant in FO and MA, respectively, but the relative abundance of Cercozoa decreased along soil moisture gradients. The β-diversity of microbiomes, metagenomic and metabolomic functioning were linearly distributed along soil moisture gradients, significantly associated with soil factors of TC, NH 4 + , and pH. For soil metagenomic functions, the metabolic genes related to Carbohydrate (CO 2 fixation, Di- and oligosaccharides, Fermentation, and One-carbon metabolism), Iron (Iron acquisition in Vibrio and Campylobacter iron metabolism) decreased with soil moisture, while genes related to the metabolisms of Nitrogen (Ammonia assimilation, Denitrification, Nitrogen fixation, and Nitrosative stress) and Potassium (Potassium homeostasis) increased linearly along water gradients. Additionally, MA harbored the most abundant metabolomics dominated by lipids and lipid-like molecules (Erucic acid, Hypogeic acid, and Kojibiose, etc.), and organic oxygen compounds (Maltotetraose, Quinone, Sucrose, and Trehalose, etc.), except certain metabolites showing decline trends along water gradients, such as N'-Hydroxymethylnorcotinine and 5-Hydroxyenterolactone. Conclusions Our study suggests that future ecosystem succession facilitated by changes in rainfall patterns will significantly alter soil microbial taxa, functional potential and metabolite fractions." @default.
- W4386826209 created "2023-09-19" @default.
- W4386826209 creator A5016274986 @default.
- W4386826209 creator A5017061461 @default.
- W4386826209 creator A5029696014 @default.
- W4386826209 creator A5029979568 @default.
- W4386826209 creator A5037748165 @default.
- W4386826209 creator A5038681658 @default.
- W4386826209 creator A5043137013 @default.
- W4386826209 creator A5046405098 @default.
- W4386826209 creator A5062352579 @default.
- W4386826209 creator A5062396427 @default.
- W4386826209 creator A5074566205 @default.
- W4386826209 creator A5075067853 @default.
- W4386826209 creator A5087233793 @default.
- W4386826209 date "2023-09-18" @default.
- W4386826209 modified "2023-09-26" @default.
- W4386826209 title "Linear responses of soil microbiomes, metagenomic and metabolomic functioning across ecosystems along water gradients in the Altai region, northwestern China" @default.
- W4386826209 cites W1179364747 @default.
- W4386826209 cites W1543344293 @default.
- W4386826209 cites W1593988446 @default.
- W4386826209 cites W1798831561 @default.
- W4386826209 cites W1824181430 @default.
- W4386826209 cites W1966221859 @default.
- W4386826209 cites W1968020619 @default.
- W4386826209 cites W1972486375 @default.
- W4386826209 cites W1975301557 @default.
- W4386826209 cites W1980680725 @default.
- W4386826209 cites W1981851600 @default.
- W4386826209 cites W1993562651 @default.
- W4386826209 cites W1994572639 @default.
- W4386826209 cites W1995875735 @default.
- W4386826209 cites W1996296626 @default.
- W4386826209 cites W2000235815 @default.
- W4386826209 cites W2006116244 @default.
- W4386826209 cites W2007929767 @default.
- W4386826209 cites W2009906332 @default.
- W4386826209 cites W2010414371 @default.
- W4386826209 cites W2016884406 @default.
- W4386826209 cites W2023535481 @default.
- W4386826209 cites W2024319543 @default.
- W4386826209 cites W2024495058 @default.
- W4386826209 cites W2028721845 @default.
- W4386826209 cites W2029291201 @default.
- W4386826209 cites W2030178771 @default.
- W4386826209 cites W2031672959 @default.
- W4386826209 cites W2035416463 @default.
- W4386826209 cites W2036897871 @default.
- W4386826209 cites W2049018318 @default.
- W4386826209 cites W2049469558 @default.
- W4386826209 cites W2062291736 @default.
- W4386826209 cites W2066363284 @default.
- W4386826209 cites W2068517568 @default.
- W4386826209 cites W2068975114 @default.
- W4386826209 cites W2074294833 @default.
- W4386826209 cites W2075536793 @default.
- W4386826209 cites W2081183202 @default.
- W4386826209 cites W2082534739 @default.
- W4386826209 cites W2086970467 @default.
- W4386826209 cites W2087777284 @default.
- W4386826209 cites W2088833470 @default.
- W4386826209 cites W2093519717 @default.
- W4386826209 cites W2098432852 @default.
- W4386826209 cites W2099656668 @default.
- W4386826209 cites W2106320450 @default.
- W4386826209 cites W2107597310 @default.
- W4386826209 cites W2108562483 @default.
- W4386826209 cites W2109628725 @default.
- W4386826209 cites W2110300022 @default.
- W4386826209 cites W2110741069 @default.
- W4386826209 cites W2115565814 @default.
- W4386826209 cites W2115837704 @default.
- W4386826209 cites W2118269781 @default.
- W4386826209 cites W2122814689 @default.
- W4386826209 cites W2123388186 @default.
- W4386826209 cites W2123890146 @default.
- W4386826209 cites W2124637227 @default.
- W4386826209 cites W2127602818 @default.
- W4386826209 cites W2128528017 @default.
- W4386826209 cites W2129083787 @default.
- W4386826209 cites W2131271579 @default.
- W4386826209 cites W2133740866 @default.
- W4386826209 cites W2136724468 @default.
- W4386826209 cites W2137164960 @default.
- W4386826209 cites W2139710790 @default.
- W4386826209 cites W2140341891 @default.
- W4386826209 cites W2146939523 @default.
- W4386826209 cites W2148663653 @default.
- W4386826209 cites W2149308626 @default.
- W4386826209 cites W2149669193 @default.
- W4386826209 cites W2149941565 @default.
- W4386826209 cites W2151936673 @default.
- W4386826209 cites W2152739587 @default.
- W4386826209 cites W2154401636 @default.
- W4386826209 cites W2154736508 @default.
- W4386826209 cites W2159593578 @default.
- W4386826209 cites W2159675211 @default.
- W4386826209 cites W2161550924 @default.
- W4386826209 cites W2164488392 @default.
- W4386826209 cites W2165108567 @default.