Table 1 Data summary of FT-ICR analyses.

From: Exploring the link between molecular cloud ices and chondritic organic matter in laboratory

Samples

Ice

Pre-accretion

Post-aqueous

Murchison

Duration

0

5

1

10

30

100

-

Attributions

3

3964

3808

2301

2746

3424

5661a

H/C

11

1.67 ± 0.05

1.42 ± 0.04

1.37 ± 0.04

1.40 ± 0.04

1.32 ± 0.04

1.66b

O/C

3

0.39 ± 0.05

0.34 ± 0.04

0.28 ± 0.03

0.32 ± 0.04

0.32 ± 0.04

0.20b

N/C

1

0.22 ± 0.01

0.14 ± 0.01

0.13 ± 0.01

0.12 ± 0.01

0.10 ± 0.01

0.03b

DBE

0

6

7

7

7

8

8b

CHNO

-

3512

2739

1836

2268

2591

3796

H/C

-

1.72 ± 0.05

1.45 ± 0.04

1.38 ± 0.04

1.40 ± 0.04

1.34 ± 0.04

1.45

O/C

-

0.40 ± 0.05

0.35 ± 0.04

0.27 ± 0.03

0.31 ± 0.04

0.32 ± 0.04

0.32

N/C

-

0.16 ± 0.01

0.12 ± 0.01

0.11 ± 0.01

0.11 ± 0.01

0.10 ± 0.01

0.06

CHO

-

351

1021

407

472

771

1684

H/C

-

1.39 ± 0.04

1.32 ± 0.04

1.29 ± 0.04

1.41 ± 0.04

1.26 ± 0.04

1.81

O/C

-

0.25 ± 0.03

0.33 ± 0.04

0.36 ± 0.04

0.42 ± 0.05

0.33 ± 0.04

0.14

CHN

-

63

22

28

6

15

165

H/C

-

0.94 ± 0.03

0.72 ± 0.04

1.20 ± 0.07

1.36 ± 0.08

1.10 ± 0.03

1.61

N/C

-

0.089 ± 0.005

0.055 ± 0.003

0.15 ± 0.01

0.26 ± 0.02

0.13 ± 0.01

0.11

  1. Numbers of molecular attributions, average elemental ratios, average double bond equivalent (DBE), and number of molecular attributions per families for the different samples, initial ice, pre-accretional organic residue, and post-aqueous organic products after 1, 10, 30, and 100 days of aqueous alteration at 150 °C compared to Murchison SOM. Elemental ratios are weighted by ion intensities. Errors for elemental ratio of residues are extrapolated from the data in Fresneau et al. 201728 assuming no difference between FT-Orbitrap-MS and FT-ICR-MS analyses since for same residues similar elemental ratio are obtained.
  2. aonly taking into account molecular attributions containing C, H, N, and/ O atoms.
  3. bonly considering molecular attributions containing C, H, N, and/or O atoms in Murchison SOM data.