Gallic acid
Formula: C7H6O5 (170.0215)
Chinese Name: 没食子酸, 五倍子酸, 鞣酸
BioDeep ID: BioDeep_00000000108
( View LC/MS Profile)
SMILES: OC(=O)C1=CC(O)=C(O)C(O)=C1
Found 13 Sample Hits
m/z | Adducts | Species | Organ | Scanning | Sample | |
---|---|---|---|---|---|---|
193.0108 | [M+Na]+PPM:0.3 |
Vitis vinifera | Fruit | MALDI (DHB) |
grape_dhb_91_1 - Grape DatabaseResolution: 50μm, 120x114
Grape berries fruit, condition: Ripe |
|
193.0108 | [M+Na]+PPM:0.3 |
Vitis vinifera | Fruit | MALDI (DHB) |
grape_dhb_164_1 - Grape DatabaseResolution: 17μm, 136x122
Grape berries fruit, condition: Late |
|
193.0108 | [M+Na]+PPM:0.3 |
Vitis vinifera | Fruit | MALDI (DHB) |
grape_dhb_163_1 - Grape DatabaseResolution: 17μm, 132x115
Grape berries fruit, condition: Late |
|
153.018 | [M+H-H2O]+PPM:1.5 |
Posidonia oceanica | root | MALDI (CHCA) |
20190614_MS1_A19r-20 - MTBLS1746Resolution: 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. |
|
193.0097 | [M+Na]+PPM:5.4 |
Posidonia oceanica | root | MALDI (CHCA) |
20190614_MS1_A19r-20 - MTBLS1746Resolution: 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. |
|
153.0183 | [M+H-H2O]+PPM:0.4 |
Posidonia oceanica | root | MALDI (CHCA) |
20190613_MS1_A19r-18 - MTBLS1746Resolution: 17μm, 246x264
|
|
193.0108 | [M+Na]+PPM:0.3 |
Posidonia oceanica | root | MALDI (CHCA) |
20190613_MS1_A19r-18 - MTBLS1746Resolution: 17μm, 246x264
|
|
153.0181 | [M+H-H2O]+PPM:0.9 |
Posidonia oceanica | root | MALDI (CHCA) |
MS1_20180404_PO_1200 - MTBLS1746Resolution: 17μm, 193x208
|
|
170.0455 | [M-H2O+NH4]+PPM:4.2 |
Posidonia oceanica | root | MALDI (CHCA) |
MS1_20180404_PO_1200 - MTBLS1746Resolution: 17μm, 193x208
|
|
193.0099 | [M+Na]+PPM:4.4 |
Posidonia oceanica | root | MALDI (CHCA) |
MS1_20180404_PO_1200 - MTBLS1746Resolution: 17μm, 193x208
|
|
193.0069 | [M+Na]+PPM:19.9 |
Homo sapiens | esophagus | DESI () |
LNTO22_1_9 - MTBLS385Resolution: 75μm, 89x74
|
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153.0196 | [M+H-H2O]+PPM:8.9 |
Homo sapiens | esophagus | DESI () |
LNTO22_1_5 - MTBLS385Resolution: 75μm, 135x94
|
|
153.0192 | [M+H-H2O]+PPM:6.3 |
Homo sapiens | esophagus | DESI () |
LNTO22_1_8 - MTBLS385Resolution: 75μm, 69x61
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Gallic acid is an odorless white solid. Sinks in water. (USCG, 1999) Gallic acid is a trihydroxybenzoic acid in which the hydroxy groups are at positions 3, 4, and 5. It has a role as an astringent, a cyclooxygenase 2 inhibitor, a plant metabolite, an antioxidant, an antineoplastic agent, a human xenobiotic metabolite, an EC 1.13.11.33 (arachidonate 15-lipoxygenase) inhibitor, an apoptosis inducer and a geroprotector. It is a conjugate acid of a gallate. Gallic acid is a metabolite found in or produced by Escherichia coli (strain K12, MG1655). Gallic Acid is a natural product found in Visnea mocanera, Ardisia paniculata, and other organisms with data available. Gallic acid is a metabolite found in or produced by Saccharomyces cerevisiae. A colorless or slightly yellow crystalline compound obtained from nutgalls. It is used in photography, pharmaceuticals, and as an analytical reagent. See also: Gallic acid monohydrate (active moiety of); Paeonia lactiflora root (part of); Galium aparine whole (part of) ... View More ... Gallic acid is an organic acid, also known as 3,4,5-trihydroxybenzoic acid, found in gallnuts, sumac, witch hazel, tea leaves, oak bark, and other plants. The chemical formula is C6H2(OH)3CO2H. Gallic acid is widely distributed in plants and is found both free and as part of tannins. It is commonly used in the pharmaceutical industry. Gallic acid can also be used to synthesize the hallucinogenic alkaloid mescaline, also known as 3,4,5-trimethoxyphenethylamine. Salts and esters of gallic acid are termed gallates. Gallic acid has been found to be s metabolite of Aspergillus (PMID:24031294). A trihydroxybenzoic acid in which the hydroxy groups are at positions 3, 4, and 5. Present in red wine. Japan approved food antioxidant additive Gallic acid. CAS Common Chemistry. CAS, a division of the American Chemical Society, n.d. https://commonchemistry.cas.org/detail?cas_rn=149-91-7 (retrieved 2024-07-01) (CAS RN: 149-91-7). Licensed under the Attribution-Noncommercial 4.0 International License (CC BY-NC 4.0). Gallic acid (3,4,5-Trihydroxybenzoic acid) is a natural polyhydroxyphenolic compound and an free radical scavenger to inhibit cyclooxygenase-2 (COX-2)[1]. Gallic acid has various activities, such as antimicrobial, antioxidant, antimicrobial, anti-inflammatory, and anticance activities[2]. Gallic acid (3,4,5-Trihydroxybenzoic acid) is a natural polyhydroxyphenolic compound and an free radical scavenger to inhibit cyclooxygenase-2 (COX-2)[1]. Gallic acid has various activities, such as antimicrobial, antioxidant, antimicrobial, anti-inflammatory, and anticance activities[2].