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Table 4 Pentacyclic triterpenoid compounds identified in the two studied charcoal-bearing samples from 88-m- and 93-m-depth of borehole RMB#2 in the Rajmahal Basin. The peak assignment (peak number) is according to Fig. 12 below

From: Palaeobotanical and biomarker evidence for Early Permian (Artinskian) wildfire in the Rajmahal Basin, India

Peak number

Compound

Base peak

Molecular ion

1

30-Norhopane

191

398

2

17α(H)-22,29,30-Trisnorhopane (Tm)

191

370

3

17β(H)-22,29,30-Trisnorhopane

149

370

4

30-Norneohop-13(18)-ene

191

396

5

30-Norhopane

191

398

6

17β(H),21α(H)-30-Norhopane

177

398

7

αβ-Hopane

191

412

8

Neohop-13(18)-ene isomer

191

410

9

17β(H),21β(H)-30-Norhopane

177

398

10

αβ-Hopane

191

412

11

17α(H),21β(H)-Homohopane (22 S)

191

426

12

17α(H),21β(H)-Homohopane (22 R)

191

424

13

ββ-Hopane

191

412

14

17β(H),21β(H)-Homohopane

205

426

15

17β(H),21β(H)-30,31-Bishomohopane

219

440