From: Stable isotope evidence for the Bottom Convective Layer homogeneity in the Black Sea
Depth, m | H2S, μM | δ34S (H2S), ‰ | δ34S (SO4), ‰ |
---|---|---|---|
1.2 | − | − | 21.0 |
1250 | 342 | −41.1 | 22.9 |
1500 | 353 | −41.0 | 23.1 |
1700 | 368 | −41.2 | 23.0 |
1715 | 363 | −40.0 | 22.9 |
1725 | 375 | −40.4 | 22.9 |
1751 | 378 | −40.6 | 23.1 |
1775 | 379 | −40.7 | 23.1 |
1801 | 382 | −40.2 | 22.9 |
1900 | 382 | −40.6 | 23.3 |
2000 | 382 | −40.0 | 23.4 |
2090 | 383 | −41.9 | 23.2 |
2120 | 381 | −40.9 | 23.0 |
2131 | 381 | −40.7 | 23.1 |
2134 | 381 | −40.8 | 23.2 |
2137 | 379 | −41.0 | 23.2 |
2138.7 | 381 | −40.7 | 22.9 |
2139.4 | 383 | −41.0 | 22.9 |