N6-Carboxymethyllysine

(2S)-2-amino-6-[(carboxymethyl)amino]hexanoic acid

Formula: C8H16N2O4 (204.111)
Chinese Name: N-ε-羧甲基-L-赖氨酸, N6-(羧甲基)-L-赖氨酸
BioDeep ID: BioDeep_00000169756 ( View LC/MS Profile)
SMILES: N[C@@H](CCCCNCC(O)=O)C(O)=O



Found 15 Sample Hits

m/z Adducts Species Organ Scanning Sample
243.2051 [M+K]+
PPM:15
Rattus norvegicus Epididymis MALDI (DHB)
epik_dhb_head_ito03_17 - MTBLS58
Resolution: 17μm, 208x108

Description

1 male adult wild-type rat was obtained from Inserm U1085 - Irset Research Institute (University of Rennes1, France). Animals were age 60 days and were reared under ad-lib conditions. Care and handling of all animals complied with EU directive 2010/63/EU on the protection of animals used for scientific purposes. The whole epididymis was excised from each animal immediately post-mortem, loosely wrapped rapidly in an aluminum foil and a 2.5% (w/v) carboxymethylcellulose (CMC) solution was poured to embed the epididymis to preserve their morphology. To remove air bubbles, the filled aluminum molds was gently freezed by depositing it on isopentane or dry ice, then on the nitrogen vapors and finally by progressively dipping the CMC/sample coated with aluminum foil into liquid nitrogen (or only flush with liquid nitrogen). Frozen tissues were stored at -80 °C until use to avoid degradation.

243.2047 [M+K]+
PPM:16.7
Rattus norvegicus Epididymis MALDI (DHB)
epik_dhb_head_ito03_18 - MTBLS58
Resolution: 17μm, 208x104

Description

243.2051 [M+K]+
PPM:15
Rattus norvegicus Epididymis MALDI (DHB)
epik_dhb_head_ito08_43 - MTBLS58
Resolution: 17μm, 298x106

Description

243.2052 [M+K]+
PPM:14.6
Rattus norvegicus Epididymis MALDI (DHB)
epik_dhb_head_ito08_44 - MTBLS58
Resolution: 17μm, 299x111

Description

243.2051 [M+K]+
PPM:15
Rattus norvegicus Epididymis MALDI (DHB)
epik_dhb_head_ito08_46 - MTBLS58
Resolution: 17μm, 298x106

Description

243.2053 [M+K]+
PPM:14.2
Rattus norvegicus Epididymis MALDI (DHB)
epik_dhb_head_ito08_47 - MTBLS58
Resolution: 17μm, 301x111

Description

243.2054 [M+K]+
PPM:13.8
Rattus norvegicus Epididymis MALDI (DHB)
epik_dhb_head_ito08_48 - MTBLS58
Resolution: 17μm, 294x107

Description

243.2051 [M+K]+
PPM:15
Rattus norvegicus Epididymis MALDI (DHB)
epik_dhb_head_ito01_04 - MTBLS58
Resolution: 17μm, 178x91

Description

243.2051 [M+K]+
PPM:15
Rattus norvegicus normal MALDI (DHB)
epik_dhb_head_ito01_05 - MTBLS58
Resolution: 17μm, 183x105

Description

243.2048 [M+K]+
PPM:16.3
Rattus norvegicus Epididymis MALDI (DHB)
epik_dhb_head_ito01_06 - MTBLS58
Resolution: 17μm, 183x103

Description

243.2054 [M+K]+
PPM:13.8
Rattus norvegicus Epididymis MALDI (DHB)
epik_dhb_head_ito03_14 - MTBLS58
Resolution: 17μm, 205x103

Description

204.134 [M-H2O+NH4]+
PPM:1.3
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.

204.1341 [M-H2O+NH4]+
PPM:0.8
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.

204.1344 [M-H2O+NH4]+
PPM:0.7
Posidonia oceanica root MALDI (CHCA)
20190613_MS1_A19r-18 - MTBLS1746
Resolution: 17μm, 246x264

Description

204.1342 [M-H2O+NH4]+
PPM:0.3
Posidonia oceanica root MALDI (CHCA)
MS1_20180404_PO_1200 - MTBLS1746
Resolution: 17μm, 193x208

Description


N6-Carboxymethyllysine (CML), also known as epsilon-(carboxymethyl)lysine, belongs to the class of organic compounds known as L-alpha-amino acids. These are alpha-amino acids which have the L-configuration of the alpha-carbon atom. CML is a Maillard reaction product, or dietary advanced glycation end-products (d-AGE), formed as a result of the thermal treatment of foods. Due to its chemical stability and its ubiquity in foods and in vivo, CML is used as a biomarker for the ingestion of thermally treated foods. CML is metabolized by intestinal bacteria under anaerobic conditions (PMID: 31091091).