From: Stable isotope evidence for the Bottom Convective Layer homogeneity in the Black Sea
Depth, m | Salinity | δ18O, ‰ | δD, ‰ |
---|---|---|---|
1.2 | 18.398 | −2.4 | −21.2 |
7.9 | 18.408 | −2.3 | −21.9 |
15.6 | 18.274 | −2.4 | −22.0 |
20.2 | 18.298 | −2.5 | −21.8 |
25.1 | 18.395 | −2.5 | −22.1 |
30.3 | 18.411 | −2.5 | −22.0 |
34.9 | 18.464 | −2.5 | −21.2 |
39.8 | 18.544 | −2.4 | −21.5 |
45.4 | 19.000 | −2.5 | −20.9 |
49.9 | 19.167 | −2.3 | −20.1 |
55.0 | 19.518 | −2.2 | −19.8 |
60.1 | 19.794 | −2.3 | −20.0 |
66.0 | 19.992 | −2.3 | −19.3 |
71.0 | 20.117 | −2.3 | −18.9 |
76.1 | 20.243 | −2.1 | −18.7 |
80.6 | 20.382 | −2.2 | −18.6 |
87.0 | 20.529 | −2.1 | −18.6 |
90.2 | 20.627 | −2.0 | −18.6 |
97.4 | 20.766 | −2.2 | −17.3 |
98.7 | 20.782 | −1.9 | −17.2 |
103 | 20.848 | −1.9 | −17.0 |
109 | 20.917 | −2.0 | −16.8 |
115 | 20.986 | −1.9 | −16.5 |
125 | 21.108 | −1.9 | −16.8 |
150 | 21.300 | −2.0 | −16.2 |
175 | 21.421 | −1.9 | −15.9 |
200 | 21.532 | −1.7 | −15.7 |
250 | 21.698 | −1.7 | −16.6 |
300 | 21.818 | −1.8 | −15.1 |
350 | 21.897 | −1.7 | −15.2 |
400 | 21.962 | −1.7 | −15.2 |
450 | 22.016 | −1.7 | −15.1 |
500 | 22.061 | −1.7 | −15.8 |
550 | 22.103 | −1.7 | −15.4 |
600 | 22.133 | −1.8 | −15.6 |
650 | 22.166 | −1.8 | −15.3 |
700 | 22.193 | −1.9 | −15.5 |
750 | 22.213 | −1.7 | −15.6 |
801 | 22.234 | −1.8 | −15.0 |
900 | 22.264 | −1.7 | −15.0 |
1000 | 22.283 | −1.7 | −15.3 |
1125 | 22.302 | −1.8 | −15.1 |
1250 | 22.313 | −1.7 | −15.1 |
1375 | 22.321 | −1.6 | −15.2 |
1500 | 22.325 | −1.6 | −15.6 |
1700 | 22.331 | −1.7 | −15.3 |
1715 | 22.331 | −1.7 | −15.1 |
1725 | 22.331 | −1.7 | −15.6 |
1751 | 22.332 | −1.6 | −15.4 |
1775* | 22.333 | −1.6 | −15.6 |
1801* | 22.333 | −1.7 | −15.3 |
1900* | 22.333 | −1.6 | −15.6 |
2000* | 22.333 | −1.6 | −15.7 |
2090* | 22.333 | −1.5 | −15.5 |
2120* | 22.333 | −1.7 | −14.6 |
2131* | 22.333 | −1.7 | −14.8 |
2134* | 22.333 | −1.5 | −14.8 |
2137* | 22.333 | −1.6 | −14.6 |
2138.7* | 22.333 | −1.6 | −14.5 |
2139.4* | 22.333 | −1.7 | −14.4 |