Liriodenine

3,5-dioxa-11-azapentacyclo[10.7.1.0^{2,6.0^{8,20.0^{14,19]icosa-1(20),2(6),7,9,11,14,16,18-octaen-13-one

Formula: C17H9NO3 (275.0582)
Chinese Name: 鹅掌楸碱
BioDeep ID: BioDeep_00000000915 ( View LC/MS Profile)
SMILES: C1OC2=C(O1)C3=C4C(=C2)C=CN=C4C(=O)C5=CC=CC=C53



Found 20 Sample Hits

m/z Adducts Species Organ Scanning Sample
258.0507 [M+H-H2O]+
PPM:16.5
Vitis vinifera Fruit MALDI (DHB)
grape_dhb_91_1 - Grape Database
Resolution: 50μm, 120x114

Description

Grape berries fruit, condition: Ripe

276.0611 [M+H]+
PPM:16
Vitis vinifera Fruit MALDI (DHB)
grape_dhb_91_1 - Grape Database
Resolution: 50μm, 120x114

Description

Grape berries fruit, condition: Ripe

298.0418 [M+Na]+
PPM:19
Vitis vinifera Fruit MALDI (DHB)
grape_dhb_91_1 - Grape Database
Resolution: 50μm, 120x114

Description

Grape berries fruit, condition: Ripe

258.0505 [M+H-H2O]+
PPM:17.3
Vitis vinifera Fruit MALDI (DHB)
grape_dhb_164_1 - Grape Database
Resolution: 17μm, 136x122

Description

Grape berries fruit, condition: Late

276.061 [M+H]+
PPM:16.4
Vitis vinifera Fruit MALDI (DHB)
grape_dhb_164_1 - Grape Database
Resolution: 17μm, 136x122

Description

Grape berries fruit, condition: Late

298.0419 [M+Na]+
PPM:18.7
Vitis vinifera Fruit MALDI (DHB)
grape_dhb_164_1 - Grape Database
Resolution: 17μm, 136x122

Description

Grape berries fruit, condition: Late

258.0508 [M+H-H2O]+
PPM:16.1
Vitis vinifera Fruit MALDI (DHB)
grape_dhb_163_1 - Grape Database
Resolution: 17μm, 132x115

Description

Grape berries fruit, condition: Late

276.0611 [M+H]+
PPM:16
Vitis vinifera Fruit MALDI (DHB)
grape_dhb_163_1 - Grape Database
Resolution: 17μm, 132x115

Description

Grape berries fruit, condition: Late

298.0418 [M+Na]+
PPM:19
Vitis vinifera Fruit MALDI (DHB)
grape_dhb_163_1 - Grape Database
Resolution: 17μm, 132x115

Description

Grape berries fruit, condition: Late

258.0516 [M+H-H2O]+
PPM:13
Posidonia oceanica root MALDI (CHCA)
20190614_MS1_A19r-20 - MTBLS1746
Resolution: 17μm, 262x276

Description

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.

276.0622 [M+H]+
PPM:12
Posidonia oceanica root MALDI (CHCA)
20190614_MS1_A19r-20 - MTBLS1746
Resolution: 17μm, 262x276

Description

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.

298.042 [M+Na]+
PPM:18.3
Posidonia oceanica root MALDI (CHCA)
20190614_MS1_A19r-20 - MTBLS1746
Resolution: 17μm, 262x276

Description

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.

276.0625 [M+H]+
PPM:10.9
Posidonia oceanica root MALDI (CHCA)
20190822_MS1_A19r-19 - MTBLS1746
Resolution: 17μm, 303x309

Description

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.

298.044 [M+Na]+
PPM:11.6
Posidonia oceanica root MALDI (CHCA)
20190822_MS1_A19r-19 - MTBLS1746
Resolution: 17μm, 303x309

Description

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.

258.0508 [M+H-H2O]+
PPM:16.1
Posidonia oceanica root MALDI (CHCA)
20190613_MS1_A19r-18 - MTBLS1746
Resolution: 17μm, 246x264

Description

276.0624 [M+H]+
PPM:11.3
Posidonia oceanica root MALDI (CHCA)
20190613_MS1_A19r-18 - MTBLS1746
Resolution: 17μm, 246x264

Description

240.0404 [M+H-2H2O]+
PPM:16.6
Posidonia oceanica root MALDI (CHCA)
20190828_MS1_A19r-22 - MTBLS1746
Resolution: 17μm, 292x279

Description

258.0513 [M+H-H2O]+
PPM:14.2
Posidonia oceanica root MALDI (CHCA)
MS1_20180404_PO_1200 - MTBLS1746
Resolution: 17μm, 193x208

Description

276.0626 [M+H]+
PPM:10.6
Posidonia oceanica root MALDI (CHCA)
MS1_20180404_PO_1200 - MTBLS1746
Resolution: 17μm, 193x208

Description

298.0427 [M+Na]+
PPM:16
Posidonia oceanica root MALDI (CHCA)
MS1_20180404_PO_1200 - MTBLS1746
Resolution: 17μm, 193x208

Description


Liriodenine is an oxoaporphine alkaloid that is 4,5,6,6a-tetradehydronoraporphin-7-one substituted by a methylenedioxy group across positions 1 and 2. It is isolated from Annona glabra and has been shown to exhibit antimicrobial and cytotoxic activities. It has a role as a metabolite, an antineoplastic agent, an antimicrobial agent, an EC 3.1.1.7 (acetylcholinesterase) inhibitor, an EC 3.2.1.20 (alpha-glucosidase) inhibitor and an antifungal agent. It is a cyclic ketone, an oxacycle, an organic heteropentacyclic compound, an alkaloid antibiotic and an oxoaporphine alkaloid. It is functionally related to an aporphine. Liriodenine is a natural product found in Magnolia mexicana, Annona purpurea, and other organisms with data available. Liriodenine, also known as oxoushinsunine or micheline b, is a member of the class of compounds known as aporphines. Aporphines are quinoline alkaloids containing the dibenzo[de,g]quinoline ring system or a dehydrogenated derivative thereof. Liriodenine is practically insoluble (in water) and a strong basic compound (based on its pKa). Liriodenine can be found in cherimoya and custard apple, which makes liriodenine a potential biomarker for the consumption of these food products. Liriodenine is a bio-active isolate of the Chinese medicinal herb Zanthoxylum nitidum .