Pelargonidin
Formula: [C15H11O5]+ (271.0606)
Chinese Name: 天竺葵素
BioDeep ID: BioDeep_00000004158
( View LC/MS Profile)
SMILES: Oc(c3)ccc(c3)c([o+1]1)c(O)cc(c(O)2)c(cc(O)c2)1
Found 7 Sample Hits
m/z | Adducts | Species | Organ | Scanning | Sample | |
---|---|---|---|---|---|---|
236.0438 | [M+H-2H2O]+PPM:12.7 |
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. |
|
272.0663 | [M+H]+PPM:6 |
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. |
|
294.0491 | [M+Na]+PPM:2.6 |
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. |
|
272.0665 | [M+H]+PPM:5.2 |
Posidonia oceanica | root | MALDI (CHCA) |
20190613_MS1_A19r-18 - MTBLS1746Resolution: 17μm, 246x264
|
|
236.0444 | [M+H-2H2O]+PPM:10.1 |
Posidonia oceanica | root | MALDI (CHCA) |
MS1_20180404_PO_1200 - MTBLS1746Resolution: 17μm, 193x208
|
|
272.0667 | [M+H]+PPM:4.5 |
Posidonia oceanica | root | MALDI (CHCA) |
MS1_20180404_PO_1200 - MTBLS1746Resolution: 17μm, 193x208
|
|
294.0484 | [M+Na]+PPM:5 |
Posidonia oceanica | root | MALDI (CHCA) |
MS1_20180404_PO_1200 - MTBLS1746Resolution: 17μm, 193x208
|
|
Pelargonidin, also known as pelargonidin chloride (CAS: 134-04-3) is an anthocyanin. Anthocyanins are water-soluble glycosides and acylglycosides of anthocyanidins, which are polyhydroxy and polymethoxyl derivatives of a 2-phenylbenzopyrylium (flavylium) cation. They are widely distributed in foods of plant origin, especially in fruits and vegetables with dark red and blue colours. Numerous epidemiologic and clinical trials show that fruits and vegetables, many of which are rich in anthocyanins, may be related to the decreased incidence of many chronic and degenerative diseases, including heart disease, cancer, and aging. Antioxidant mechanisms were suggested as potential means of disease prevention. Anthocyanins are strong antioxidants in vitro. In most cases, fruits and vegetables with high anthocyanin content were shown to have higher antioxidant capacity than other fruits and vegetables. Whether anthocyanins are effective antioxidants in vivo remains an open question primarily because of the relatively low apparent absorption of anthocyanins compared with other phenolic compounds (PMID: 15465754). BioTransformer predicts that pelargonidin is a product of 5-[(6-{[(2-carboxyacetyl)oxy]methyl}-3,4,5-trihydroxyoxan-2-yl)oxy]-3,7-dihydroxy-2-(4-hydroxyphenyl)-1λ⁴-chromen-1-ylium metabolism via a glycoside-hydrolysis reaction occurring in human gut microbiota and catalyzed by an EC.3.2.1.X enzyme (PMID: 30612223). Anthocyanin pigment present in many plants, flowers and fruits, e.g. cherries, raspberries, radishes, orchids, brassicas, Petunia subspecies Glycosides also widely distributed. Pelargonidin is found in many foods, some of which are almond, radish (variety), garden tomato, and tarragon.