M/Z: 391.0208
Hit 6 annotations: L-Galacturonic acid calcium salt_[M+H-2H2O]+
; Orotidylic acid_[M+Na]+
; (11e)-16-bromo-17,19-dihydroxy-4-methyl-3,7-dioxatricyclo[13.4.0.0⁶,⁸]nonadeca-1(19),9,11,15,17-pentaene-2,13-dione_[M+H-H2O]+
; 2-(2,6-dichloro-3,5-dimethoxyphenyl)furo[2,3-h]chromen-4-one_[M+H]+
; 19,20-dichloro-16-oxapentacyclo[12.10.0.0²,¹¹.0⁴,⁹.0¹⁵,²²]tetracosa-1(14),2(11),3,5,7,9,12,15(22),17,19,23-undecaen-21-one_[M+H]+
; 6-Hydroxy-5-[(4-sulfophenyl)azo]-2-naphthalenesulfonic acid_[M+H-H2O]+
- Confirmed: 这个参考离子已经通过手动审计得到确认和验证。
- Reliable: 这个参考离子可能在特定的解剖组织环境中高度保守。
- Unreliable: 这个参考离子具有较高的排名价值,但缺乏可重复性。
- Unavailable: 由于排名价值低且缺乏可重复性,这个参考离子不应用于注释。
Found 9 Reference Ions Near m/z 391.0208
NovoCell ID | m/z | Mass Window | Metabolite | Ranking | Anatomy Context |
---|---|---|---|---|---|
MSI_000053992 Reliable | 391.0214 | 391.0212 ~ 391.0215 MzDiff: 1.6 ppm |
(11e)-16-bromo-17,19-dihydroxy-4-methyl-3,7-dioxatricyclo[13.4.0.0⁶,⁸]nonadeca-1(19),9,11,15,17-pentaene-2,13-dione (BioDeep_00002090478) Formula: C18H17BrO6 (408.0208) |
3.65 (50%) | MALDI - CHCA [NOVOCELL:BACKGROUND] blank |
MSI_000013246 Unavailable | 391.0213 | 391.0213 ~ 391.0213 MzDiff: none |
L-Galacturonic acid calcium salt (BioDeep_00000011682) Formula: C12H18CaO14 (426.0322) |
-0.88 (100%) | Plant [PO:0005020] vascular bundle |
MSI_000013547 Unreliable | 391.0213 | 391.0213 ~ 391.0213 MzDiff: none |
L-Galacturonic acid calcium salt (BioDeep_00000011682) Formula: C12H18CaO14 (426.0322) |
0.8 (100%) | Plant [PO:0005417] phloem |
MSI_000018807 Unreliable | 391.0213 | 391.0213 ~ 391.0213 MzDiff: none |
L-Galacturonic acid calcium salt (BioDeep_00000011682) Formula: C12H18CaO14 (426.0322) |
1.31 (100%) | Plant [PO:0020124] root stele |
MSI_000019794 Unavailable | 391.0213 | 391.0213 ~ 391.0213 MzDiff: none |
L-Galacturonic acid calcium salt (BioDeep_00000011682) Formula: C12H18CaO14 (426.0322) |
-0.41 (100%) | Plant [PO:0025197] stele |
MSI_000032390 Unreliable | 391.0208 | 391.0208 ~ 391.0208 MzDiff: none |
(11e)-16-bromo-17,19-dihydroxy-4-methyl-3,7-dioxatricyclo[13.4.0.0⁶,⁸]nonadeca-1(19),9,11,15,17-pentaene-2,13-dione (BioDeep_00002090478) Formula: C18H17BrO6 (408.0208) |
1.59 (100%) | Posidonia oceanica [PO:0005020] vascular bundle |
MSI_000033746 Unreliable | 391.0208 | 391.0208 ~ 391.0208 MzDiff: none |
(11e)-16-bromo-17,19-dihydroxy-4-methyl-3,7-dioxatricyclo[13.4.0.0⁶,⁸]nonadeca-1(19),9,11,15,17-pentaene-2,13-dione (BioDeep_00002090478) Formula: C18H17BrO6 (408.0208) |
0.72 (100%) | Posidonia oceanica [PO:0005352] xylem |
MSI_000037955 Unavailable | 391.0213 | 391.0213 ~ 391.0213 MzDiff: none |
(11e)-16-bromo-17,19-dihydroxy-4-methyl-3,7-dioxatricyclo[13.4.0.0⁶,⁸]nonadeca-1(19),9,11,15,17-pentaene-2,13-dione (BioDeep_00002090478) Formula: C18H17BrO6 (408.0208) |
-0.14 (100%) | Posidonia oceanica [UBERON:0000329] hair root |
MSI_000040416 Unavailable | 391.0215 | 391.0215 ~ 391.0215 MzDiff: none |
19,20-dichloro-16-oxapentacyclo[12.10.0.0²,¹¹.0⁴,⁹.0¹⁵,²²]tetracosa-1(14),2(11),3,5,7,9,12,15(22),17,19,23-undecaen-21-one (BioDeep_00002194205) Formula: C23H12Cl2O2 (390.0214) |
-0.2 (100%) | Posidonia oceanica [PO:0005417] phloem |
Found 9 Sample Hits
Metabolite | Species | Sample | |
---|---|---|---|
L-Galacturonic acid calcium salt Formula: C12H18CaO14 (426.0322) Adducts: [M+H-2H2O]+ (Ppm: 7.4) |
Plant (Root) |
MPIMM_035_QE_P_PO_6pmResolution: 30μm, 165x170
|
|
Orotidylic acid Formula: C10H13N2O11P (368.0257) Adducts: [M+Na]+ (Ppm: 14.3) |
Mus musculus (Lung) |
image2Resolution: 40μm, 550x256
Supplementary Figure S6. Ion distribution images for (a) [PC36:4+Na]+ (m/z 804.5514) and (b)
[PC38:6+Na]+ (m/z 828.5515) obtained from mouse lung tissue collected 6 h after administration of D9-
choline and U13C-DPPC–containing CHF5633. Parts-per-million (ppm) mass errors are indicated in
parentheses. (c) Magnification of the boxed region in (a) with selected bronchiolar regions outlined in
white boxes. (d) The corresponding H&E-stained tissue section with the same selected bronchiolar
regions outlined in black boxes. These data demonstrate the co-localisation of the polyunsaturated lipids
PC36:4 and PC38:6 with the bronchiolar regions of the lung. All MSI images were visualised using
total ion current normalisation and hotspot removal (high quantile = 99%). |
|
(11e)-16-bromo-17,19-dihydroxy-4-methyl-3,7-dioxatricyclo[13.4.0.0⁶,⁸]nonadeca-1(19),9,11,15,17-pentaene-2,13-dione Formula: C18H17BrO6 (408.0208) Adducts: [M+H-H2O]+ (Ppm: 8.3) |
Posidonia oceanica (root) |
20190614_MS1_A19r-20Resolution: 17μm, 262x276
Seagrasses are one of the most efficient natural sinks of carbon dioxide (CO2) on Earth. Despite covering less than 0.1% of coastal regions, they have the capacity to bury up to 10% of marine organic matter and can bury the same amount of carbon 35 times faster than tropical rainforests. On land, the soil’s ability to sequestrate carbon is intimately linked to microbial metabolism. Despite the growing attention to the link between plant production, microbial communities, and the carbon cycle in terrestrial ecosystems, these processes remain enigmatic in the sea. Here, we show that seagrasses excrete organic sugars, namely in the form of sucrose, into their rhizospheres. Surprisingly, the microbial communities living underneath meadows do not fully use this sugar stock in their metabolism. Instead, sucrose piles up in the sediments to mM concentrations underneath multiple types of seagrass meadows. Sediment incubation experiments show that microbial communities living underneath a meadow use sucrose at low metabolic rates. Our metagenomic analyses revealed that the distinct community of microorganisms occurring underneath meadows is limited in their ability to degrade simple sugars, which allows these compounds to persist in the environment over relatively long periods of time. Our findings reveal how seagrasses form blue carbon stocks despite the relatively small area they occupy. Unfortunately, anthropogenic disturbances are threatening the long-term persistence of seagrass meadows. Given that these sediments contain a large stock of sugars that heterotopic bacteria can degrade, it is even more important to protect these ecosystems from degradation. |
|
2-(2,6-dichloro-3,5-dimethoxyphenyl)furo[2,3-h]chromen-4-one Formula: C19H12Cl2O5 (390.0062) Adducts: [M+H]+ (Ppm: 19.8) |
Posidonia oceanica (root) |
20190822_MS1_A19r-19Resolution: 17μm, 303x309
Seagrasses are among the most efficient sinks of carbon dioxide on Earth. While carbon sequestration in terrestrial plants is linked to the microorganisms living in their soils, the interactions of seagrasses with their rhizospheres are poorly understood. Here, we show that the seagrass, Posidonia oceanica excretes sugars, mainly sucrose, into its rhizosphere. These sugars accumulate to µM concentrations—nearly 80 times higher than previously observed in marine environments. This finding is unexpected as sugars are readily consumed by microorganisms. Our experiments indicated that under low oxygen conditions, phenolic compounds from P. oceanica inhibited microbial consumption of sucrose. Analyses of the rhizosphere community revealed that many microbes had the genes for degrading sucrose but these were only expressed by a few taxa that also expressed genes for degrading phenolics. Given that we observed high sucrose concentrations underneath three other species of marine plants, we predict that the presence of plant-produced phenolics under low oxygen conditions allows the accumulation of labile molecules across aquatic rhizospheres. |
|
(11e)-16-bromo-17,19-dihydroxy-4-methyl-3,7-dioxatricyclo[13.4.0.0⁶,⁸]nonadeca-1(19),9,11,15,17-pentaene-2,13-dione Formula: C18H17BrO6 (408.0208) Adducts: [M+H-H2O]+ (Ppm: 10.1) |
Posidonia oceanica (root) |
20190613_MS1_A19r-18Resolution: 17μm, 246x264
|
|
(11e)-16-bromo-17,19-dihydroxy-4-methyl-3,7-dioxatricyclo[13.4.0.0⁶,⁸]nonadeca-1(19),9,11,15,17-pentaene-2,13-dione Formula: C18H17BrO6 (408.0208) Adducts: [M+H-H2O]+ (Ppm: 9.6) |
Posidonia oceanica (root) |
20190828_MS1_A19r-22Resolution: 17μm, 292x279
|
|
19,20-dichloro-16-oxapentacyclo[12.10.0.0²,¹¹.0⁴,⁹.0¹⁵,²²]tetracosa-1(14),2(11),3,5,7,9,12,15(22),17,19,23-undecaen-21-one Formula: C23H12Cl2O2 (390.0214) Adducts: [M+H]+ (Ppm: 18.4) |
Posidonia oceanica (root) |
MS1_20180404_PO_1200Resolution: 17μm, 193x208
|
|
6-Hydroxy-5-[(4-sulfophenyl)azo]-2-naphthalenesulfonic acid Formula: C16H12N2O7S2 (408.0086) Adducts: [M+H-H2O]+ (Ppm: 15.8) |
Mus musculus (Liver) |
Salmonella_final_pos_recalResolution: 17μm, 691x430
A more complete and holistic view on host–microbe interactions is needed to understand the physiological and cellular barriers that affect the efficacy of drug treatments and allow the discovery and development of new therapeutics. Here, we developed a multimodal imaging approach combining histopathology with mass spectrometry imaging (MSI) and same section imaging mass cytometry (IMC) to study the effects of Salmonella Typhimurium infection in the liver of a mouse model using the S. Typhimurium strains SL3261 and SL1344. This approach enables correlation of tissue morphology and specific cell phenotypes with molecular images of tissue metabolism. IMC revealed a marked increase in immune cell markers and localization in immune aggregates in infected tissues. A correlative computational method (network analysis) was deployed to find metabolic features associated with infection and revealed metabolic clusters of acetyl carnitines, as well as phosphatidylcholine and phosphatidylethanolamine plasmalogen species, which could be associated with pro-inflammatory immune cell types. By developing an IMC marker for the detection of Salmonella LPS, we were further able to identify and characterize those cell types which contained S. Typhimurium.
[dataset] Nicole Strittmatter. Holistic Characterization of a Salmonella Typhimurium Infection Model Using Integrated Molecular Imaging, metabolights_dataset, V1; 2022. https://www.ebi.ac.uk/metabolights/MTBLS2671. |
|
m/z_391.0216 Formula: - (n/a) Adducts: (Ppm: 0) |
Mus musculus (brain) |
Brain02_Bregma-3-88Resolution: 17μm, 288x282
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