Table 1 Stable carbon isotope (δ13Corg), total organic carbon (TOC), total inorganic carbonate (TIC), pyrite sulfur isotopes (δ34Spy), and total sulfur (TS) data of the Xiahuapidianzi Formation samples from Hongmiaozi Basin.
Num | Depth(m) | δ13Corg (‰) | TOC (%) | δ34Spyr (‰) | TS (%) | TIC (%) |
|---|---|---|---|---|---|---|
1 | 395.80 | − 24.1 | 1.58 | 5.4 | 0.67 | 11.9 |
2 | 419.60 | − 24.9 | 1.77 | 4.5 | 0.4 | 11.1 |
3 | 443.55 | − 23.7 | 0.48 | 9.1 | 2.3 | 7.5 |
4 | 464.65 | − 26.5 | 1.59 | 14.1 | 0.82 | 15.4 |
5 | 489.65 | − 24.9 | 1.17 | 12.3 | 0.58 | 1.6 |
6 | 495.40 | − 23.0 | 0.69 | 8.7 | 0.31 | 7.7 |
7 | 505.15 | − 24.1 | 1.35 | 13.1 | 0.21 | 10.0 |
8 | 513.00 | − 22.7 | 0.92 | 17.0 | 0.31 | 7.9 |
9 | 522.50 | − 25.5 | 2.35 | 12.3 | 0.67 | 12.6 |
10 | 525.65 | − 25.0 | 1.1 | 12.6 | 0.38 | 9.2 |
11 | 549.90 | − 24.0 | 1.3 | 4.0 | 0.45 | 11.0 |
12 | 568.15 | − 24.5 | 1.42 | 4.8 | 0.63 | 10.8 |
13 | 573.20 | − 22.8 | 1.22 | 5.6 | 0.28 | 10.6 |
14 | 586.81 | − 22.7 | 1.01 | – | – | 10.8 |
15 | 657.65 | − 23.4 | 0.75 | 3.7 | 0.42 | 8.7 |
16 | 665.10 | − 22.9 | 0.71 | 7.9 | 0.93 | 9.7 |
17 | 670.30 | − 24.4 | 1.27 | 7.7 | 0.57 | 5.8 |
18 | 676.35 | − 23.7 | – | – | – | 11.7 |
19 | 681.35 | − 24.4 | 0.6 | 9.1 | 0.62 | 6.1 |
20 | 692.72 | − 24.2 | 0.77 | 4.4 | 0.88 | 5.3 |
21 | 703.25 | − 26.5 | 1.25 | 10.5 | 0.97 | 3.4 |
22 | 710.35 | − 25.9 | 1.75 | 8.2 | 1.15 | 32.2 |
23 | 715.28 | − 26.7 | 1.29 | 13.0 | 0.27 | 32.8 |
24 | 719.73 | − 25.9 | 0.98 | 11.1 | 0.86 | 19.0 |
25 | 724.28 | − 27.2 | 1.87 | 14.6 | 0.96 | 40.9 |
26 | 727.15 | − 25.3 | 1.21 | 16.4 | 0.66 | 28.2 |
27 | 732.95 | − 26.8 | 1.1 | 11.5 | 0.86 | 14.6 |
28 | 735.81 | − 25.4 | 0.74 | 12.1 | 0.91 | 24.4 |
29 | 742.08 | − 25.9 | 1.43 | 11.7 | 1.23 | 16.3 |
30 | 747.15 | − 26.1 | 1.31 | 9.1 | 1.35 | 5.9 |
31 | 751.83 | − 25.6 | 0.64 | 11.9 | 0.65 | 7.1 |
32 | 761.80 | − 25.1 | 0.88 | 11.9 | 0.68 | 11.9 |
33 | 767.38 | − 24.8 | 0.71 | 6.1 | 0.2 | 6.2 |
34 | 824.25 | − 25.8 | 0.41 | 13.4 | 0.16 | 6.1 |
35 | 855.65 | − 26.3 | 0.43 | 10.9 | 0.32 | 6.4 |