From: Stable isotope evidence for the Bottom Convective Layer homogeneity in the Black Sea
Depth, m | Salinity | δ18O, ‰ | δD, ‰ |
---|---|---|---|
1.6 | 18.290 | −2.4 | −21.8 |
10.0 | 18.294 | −2.3 | −21.7 |
20.1 | 18.291 | −2.5 | −21.5 |
30.0 | 18.291 | −2.3 | −21.3 |
40.1 | 18.292 | −2.3 | −21.4 |
59.9 | 18.942 | −2.2 | −20.5 |
65.0 | 19.362 | −2.2 | −20.0 |
71.0 | 19.673 | −2.2 | −19.5 |
77.0 | 19.992 | −2.1 | −19.0 |
81.9 | 20.135 | −2.2 | −19.4 |
87.1 | 20.322 | −2.2 | −19.3 |
91.1 | 20.460 | −2.0 | −19.0 |
94.0 | 20.474 | −2.1 | −18.4 |
94.0 | 20.474 | −2.0 | −18.5 |
96.9 | 20.565 | −2.0 | −18.4 |
100 | 20.616 | −2.1 | −17.9 |
103 | 20.673 | −2.1 | −18.1 |
106 | 20.736 | −2.0 | −17.7 |
108 | 20.786 | −1.9 | −17.9 |
110 | 20.834 | −1.9 | −17.6 |
113 | 20.885 | −2.1 | −17.2 |
116 | 20.936 | −1.9 | −17.6 |
119 | 20.971 | −1.9 | −17.3 |
122 | 21.009 | −1.9 | −17.9 |
125 | 21.050 | −2.0 | −17.1 |
135 | 21.143 | −1.9 | −17.1 |
150 | 21.273 | −1.9 | −16.7 |
175 | 21.424 | −1.7 | −16.8 |
200 | 21.516 | −1.9 | −17.0 |
300 | 21.794 | −1.7 | −16.3 |
400 | 21.943 | −1.6 | −16.2 |
700 | 22.187 | −1.6 | −14.9 |
1000 | 22.285 | −1.6 | −14.9 |
1300 | 22.316 | −1.7 | −15.1 |
1500 | 22.324 | −1.6 | −15.4 |
1700 | 22.330 | −1.6 | −15.2 |
1732 | 22.332 | −1.5 | −15.8 |
1749* | 22.333 | −1.7 | −16.2 |
1800* | 22.333 | −1.4 | −15.4 |
1900* | 22.333 | −1.4 | −15.1 |
2001* | 22.333 | −1.6 | −15.1 |
2090* | 22.333 | −1.7 | −15.2 |
2120* | 22.333 | −1.6 | −15.4 |
2131* | 22.333 | −1.5 | −14.9 |
2134* | 22.333 | −1.5 | −15.2 |
2136.5* | 22.333 | −1.5 | −15.5 |
2138.5* | 22.333 | −1.6 | −15.3 |
2140.6* | 22.333 | −1.4 | −15.6 |