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MB Sample ID: SA125768

Local Sample ID:107
Subject ID:SU001565
Subject Type:Human
Subject Species:Homo sapiens
Taxonomy ID:9606
Gender:Female

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Subject:

Subject ID:SU001565
Subject Type:Human
Subject Species:Homo sapiens
Taxonomy ID:9606
Gender:Female

Factors:

Local Sample IDMB Sample IDFactor Level IDLevel ValueFactor Name
107SA125768FL015404PakistanSite
107SA125768FL01540439GA_delivery
107SA125768FL01540410GA_sampling

Collection:

Collection ID:CO001560
Collection Summary:The study comprises a single urine sample for each participant (n = 99) that was collected at a prenatal visit after ultrasound confirmed a gestation < 20 weeks. Ultrasound imaging was performed by trained sonologists in compliance with standard-of-care. All study sites employed a uniform method of GA assessment, urine collection and handling. Urine samples were aliquoted and frozen at -80°C within 2 hours. Deidentified urine aliquots were shipped on dry ice from each biorepository to Stanford University as a single batch and under continuous temperature monitoring. Urine samples from 20 healthy pregnancies collected between 8 and 19 weeks of gestation at the Lucile Packard Children’s Hospital at Stanford University, served as the validation cohort.
Sample Type:Urine
Storage Conditions:-80℃

Treatment:

Treatment ID:TR001580
Treatment Summary:There was no treatment.

Sample Preparation:

Sampleprep ID:SP001573
Sampleprep Summary:Urine aliquots were prepared and analyzed in a random order as previously described (Contrepois et al., 2015). Briefly, frozen urine samples were thawed on ice and centrifuged at 17,000g for 10 min at 4°C. Supernatants (25 µl) were then diluted 1:4 with 75% acetonitrile and 100% water for HILIC- and RPLC-MS experiments, respectively. Each sample was spiked-in with 15 analytical-grade internal standards (IS). Samples for HILIC-MS experiments were further centrifuged at 21,000g for 10 min at 4°C to precipitate proteins.

Combined analysis:

Analysis ID AN002470 AN002471 AN002472 AN002473
Analysis type MS MS MS MS
Chromatography type HILIC HILIC Reversed phase Reversed phase
Chromatography system Thermo Dionex Ultimate 3000 RS Thermo Dionex Ultimate 3000 RS Thermo Dionex Ultimate 3000 RS Thermo Dionex Ultimate 3000 RS
Column SeQuant ZIC-HILIC (100 x 2.1mm,3.5um) SeQuant ZIC-HILIC (100 x 2.1mm,3.5um) Hypersil GOLD (150 x 2.1mm,1.9um) Hypersil GOLD (150 x 2.1mm,1.9um)
MS Type ESI ESI ESI ESI
MS instrument type Orbitrap Orbitrap Orbitrap Orbitrap
MS instrument name Thermo Q Exactive HF hybrid Orbitrap Thermo Q Exactive HF hybrid Orbitrap Thermo Q Exactive HF hybrid Orbitrap Thermo Q Exactive HF hybrid Orbitrap
Ion Mode POSITIVE NEGATIVE POSITIVE NEGATIVE
Units MS count MS Counts MS Counts MS Counts

Chromatography:

Chromatography ID:CH001810
Chromatography Summary:HILIC experiments were performed using a ZIC-HILIC column 2.1x100 mm, 3.5μm, 200Å (Merck Millipore) and mobile phase solvents consisting of 10mM ammonium acetate in 50/50 acetonitrile/water (A) and 10 mM ammonium acetate in 95/5 acetonitrile/water (B).(Contrepois et al., 2015)
Instrument Name:Thermo Dionex Ultimate 3000 RS
Column Name:SeQuant ZIC-HILIC (100 x 2.1mm,3.5um)
Column Temperature:40
Flow Rate:0.5 ml/min
Solvent A:95% acetonitrile/5% water; 10 mM ammonium acetate
Solvent B:95% acetonitrile/5% water; 10 mM ammonium acetate
Chromatography Type:HILIC
  
Chromatography ID:CH001811
Chromatography Summary:RPLC experiments were performed using a Hypersil GOLD column 2.1 x 150 mm, 1.9 µm, 175Å (Thermo Scientific) and mobile phase solvents consisting of 0.06% acetic acid in water (A) and 0.06% acetic acid in methanol (B). (Contrepois et al., 2015)
Chromatography Comments:Hypersil GOLD column 2.1 x 150 mm, 1.9 µm, 175Å (Thermo Scientific)
Instrument Name:Thermo Dionex Ultimate 3000 RS
Column Name:Hypersil GOLD (150 x 2.1mm,1.9um)
Column Temperature:60
Flow Rate:0.6 ml/min
Solvent A:100% water; 0.06% acetic acid
Solvent B:100% methanol; 0.06% acetic acid
Chromatography Type:Reversed phase

MS:

MS ID:MS002290
Analysis ID:AN002470
Instrument Name:Thermo Q Exactive HF hybrid Orbitrap
Instrument Type:Orbitrap
MS Type:ESI
MS Comments:Data processing. Data from each mode were independently analyzed using Progenesis QI software (v2.3) (Nonlinear Dynamics). Metabolic features from blanks and that did not show sufficient linearity upon dilution in QC samples (r < 0.6) were discarded. Only metabolic features present in > 2/3 of the samples were kept for further analysis. Inter- and intra-batch variations were corrected by applying locally estimated scatterplot smoothing local regression (LOESS) on pooled samples injected repetitively along the batches (span = 0.75). Data were acquired in four batches for HILIC and RPLC modes. Dilution effects were corrected using probabilistic quotient normalization (PQN) (Rosen Vollmar et al., 2019). Missing values were imputed by drawing from a random distribution of low values in the corresponding sample. Data from each mode were then merged, producing a dataset containing 6,630 metabolic features. Metabolite abundances were reported as spectral counts. Metabolic feature annotation. Peak annotation was first performed by matching experimental m/z, retention time and MS/MS spectra to an in-house library of analytical-grade standards. Remaining peaks were identified by matching experimental m/z and fragmentation spectra to publicly available databases including HMDB (http://www.hmdb.ca/), MoNA (http://mona.fiehnlab.ucdavis.edu/) and MassBank (http://www.massbank.jp/) using the R package ‘MetID’ (v0.2.0) (Shen et al., 2019). Briefly, metabolic feature tables from Progenesis QI were matched to fragmentation spectra with a m/z and a retention time window of ± 15 ppm and ± 30 s (HILIC) and ± 20 s (RPLC), respectively. When multiple MS/MS spectra match a single metabolic feature, all matched MS/MS spectra were used for the identification. Next, MS1 and MS2 pairs were searched against public databases and a similarity score was calculated using the forward dot–product algorithm which considers both fragments and intensities (Stein and Scott, 1994). Metabolites were reported if the similarity score was above 0.4. Spectra from metabolic features of interest important in random forest models (see below) were further investigated manually to confirm identification.
Ion Mode:POSITIVE
Capillary Temperature:375C
Capillary Voltage:3.4kV
Collision Energy:25 & 35 NCE
Collision Gas:N2
Dry Gas Temp:310C
  
MS ID:MS002291
Analysis ID:AN002471
Instrument Name:Thermo Q Exactive HF hybrid Orbitrap
Instrument Type:Orbitrap
MS Type:ESI
MS Comments:Data processing. Data from each mode were independently analyzed using Progenesis QI software (v2.3) (Nonlinear Dynamics). Metabolic features from blanks and that did not show sufficient linearity upon dilution in QC samples (r < 0.6) were discarded. Only metabolic features present in > 2/3 of the samples were kept for further analysis. Inter- and intra-batch variations were corrected by applying locally estimated scatterplot smoothing local regression (LOESS) on pooled samples injected repetitively along the batches (span = 0.75). Data were acquired in four batches for HILIC and RPLC modes. Dilution effects were corrected using probabilistic quotient normalization (PQN) (Rosen Vollmar et al., 2019). Missing values were imputed by drawing from a random distribution of low values in the corresponding sample. Data from each mode were then merged, producing a dataset containing 6,630 metabolic features. Metabolite abundances were reported as spectral counts. Metabolic feature annotation. Peak annotation was first performed by matching experimental m/z, retention time and MS/MS spectra to an in-house library of analytical-grade standards. Remaining peaks were identified by matching experimental m/z and fragmentation spectra to publicly available databases including HMDB (http://www.hmdb.ca/), MoNA (http://mona.fiehnlab.ucdavis.edu/) and MassBank (http://www.massbank.jp/) using the R package ‘MetID’ (v0.2.0) (Shen et al., 2019). Briefly, metabolic feature tables from Progenesis QI were matched to fragmentation spectra with a m/z and a retention time window of ± 15 ppm and ± 30 s (HILIC) and ± 20 s (RPLC), respectively. When multiple MS/MS spectra match a single metabolic feature, all matched MS/MS spectra were used for the identification. Next, MS1 and MS2 pairs were searched against public databases and a similarity score was calculated using the forward dot–product algorithm which considers both fragments and intensities (Stein and Scott, 1994). Metabolites were reported if the similarity score was above 0.4. Spectra from metabolic features of interest important in random forest models (see below) were further investigated manually to confirm identification.
Ion Mode:NEGATIVE
Capillary Temperature:375C
Capillary Voltage:3.4kV
Collision Energy:25 & 35 NCE
Collision Gas:N2
Dry Gas Temp:310C
  
MS ID:MS002292
Analysis ID:AN002472
Instrument Name:Thermo Q Exactive HF hybrid Orbitrap
Instrument Type:Orbitrap
MS Type:ESI
MS Comments:Data processing. Data from each mode were independently analyzed using Progenesis QI software (v2.3) (Nonlinear Dynamics). Metabolic features from blanks and that did not show sufficient linearity upon dilution in QC samples (r < 0.6) were discarded. Only metabolic features present in > 2/3 of the samples were kept for further analysis. Inter- and intra-batch variations were corrected by applying locally estimated scatterplot smoothing local regression (LOESS) on pooled samples injected repetitively along the batches (span = 0.75). Data were acquired in four batches for HILIC and RPLC modes. Dilution effects were corrected using probabilistic quotient normalization (PQN) (Rosen Vollmar et al., 2019). Missing values were imputed by drawing from a random distribution of low values in the corresponding sample. Data from each mode were then merged, producing a dataset containing 6,630 metabolic features. Metabolite abundances were reported as spectral counts. Metabolic feature annotation. Peak annotation was first performed by matching experimental m/z, retention time and MS/MS spectra to an in-house library of analytical-grade standards. Remaining peaks were identified by matching experimental m/z and fragmentation spectra to publicly available databases including HMDB (http://www.hmdb.ca/), MoNA (http://mona.fiehnlab.ucdavis.edu/) and MassBank (http://www.massbank.jp/) using the R package ‘MetID’ (v0.2.0) (Shen et al., 2019). Briefly, metabolic feature tables from Progenesis QI were matched to fragmentation spectra with a m/z and a retention time window of ± 15 ppm and ± 30 s (HILIC) and ± 20 s (RPLC), respectively. When multiple MS/MS spectra match a single metabolic feature, all matched MS/MS spectra were used for the identification. Next, MS1 and MS2 pairs were searched against public databases and a similarity score was calculated using the forward dot–product algorithm which considers both fragments and intensities (Stein and Scott, 1994). Metabolites were reported if the similarity score was above 0.4. Spectra from metabolic features of interest important in random forest models (see below) were further investigated manually to confirm identification.
Ion Mode:POSITIVE
Capillary Temperature:375C
Capillary Voltage:3.4kV
Collision Energy:25 & 50 NCE
Collision Gas:N2
Dry Gas Temp:310C
  
MS ID:MS002293
Analysis ID:AN002473
Instrument Name:Thermo Q Exactive HF hybrid Orbitrap
Instrument Type:Orbitrap
MS Type:ESI
MS Comments:Data processing. Data from each mode were independently analyzed using Progenesis QI software (v2.3) (Nonlinear Dynamics). Metabolic features from blanks and that did not show sufficient linearity upon dilution in QC samples (r < 0.6) were discarded. Only metabolic features present in > 2/3 of the samples were kept for further analysis. Inter- and intra-batch variations were corrected by applying locally estimated scatterplot smoothing local regression (LOESS) on pooled samples injected repetitively along the batches (span = 0.75). Data were acquired in four batches for HILIC and RPLC modes. Dilution effects were corrected using probabilistic quotient normalization (PQN) (Rosen Vollmar et al., 2019). Missing values were imputed by drawing from a random distribution of low values in the corresponding sample. Data from each mode were then merged, producing a dataset containing 6,630 metabolic features. Metabolite abundances were reported as spectral counts. Metabolic feature annotation. Peak annotation was first performed by matching experimental m/z, retention time and MS/MS spectra to an in-house library of analytical-grade standards. Remaining peaks were identified by matching experimental m/z and fragmentation spectra to publicly available databases including HMDB (http://www.hmdb.ca/), MoNA (http://mona.fiehnlab.ucdavis.edu/) and MassBank (http://www.massbank.jp/) using the R package ‘MetID’ (v0.2.0) (Shen et al., 2019). Briefly, metabolic feature tables from Progenesis QI were matched to fragmentation spectra with a m/z and a retention time window of ± 15 ppm and ± 30 s (HILIC) and ± 20 s (RPLC), respectively. When multiple MS/MS spectra match a single metabolic feature, all matched MS/MS spectra were used for the identification. Next, MS1 and MS2 pairs were searched against public databases and a similarity score was calculated using the forward dot–product algorithm which considers both fragments and intensities (Stein and Scott, 1994). Metabolites were reported if the similarity score was above 0.4. Spectra from metabolic features of interest important in random forest models (see below) were further investigated manually to confirm identification.
Ion Mode:NEGATIVE
Capillary Temperature:375C
Capillary Voltage:3.4kV
Collision Energy:25 & 50 NCE
Collision Gas:N2
Dry Gas Temp:310C
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