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Black Sea, water column (southwestern basin)

Black Sea, off Turkey

Other media

Type
Other medium

Largest modern euxinic basin, highly restricted. Oxic surface water (-2.2) carries the composition of continental inputs (rivers about -2), not that of the open ocean (-6.0), despite Mediterranean water from the Bosporus; below the chemocline, Tl drops (7.2 to 0.3 pg/g) and ε205Tl rises to +0.4: pyrite forming in the water column preferentially takes up light Tl (α of 0.99992 closed-system, 0.99971 steady-state) (Owens et al., 2017). Coordinates from Table 4.

ε205Tl in ε units (parts per 10,000) Values of the same system

Standard : NIST SRM 997

ValueRangenMineral or matrixSource
−2.2 ± 0.3 ε4seawater at 30 m
Published mean of 4 analyses; ± 0.3 ε (2 SD); 7.2 ± 1.3 pg/g Tl; above the chemocline.
Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g…
−0.8 ± 0.3 ε2seawater at 100 m
Published mean of 2 analyses; ± 0.3 ε (2 SD); 2.2 ± 0.0 pg/g Tl; within the chemocline.
Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g…
0.4 ± 0.3 ε1seawater at 150 m
Single analysis; ± 0.3 ε (2 SD, SAFe D1 reproducibility); 0.3 pg/g Tl; below the chemocline, heaviest and most Tl-poor value.
Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Black Sea, water column (southwestern basin), isotope signatures. https://www.isofind.tech/isotopes/en/sites/mer-noire-colonne-d-eau-sud-ouest-du-bassin/ (accessed 2026-10-16).

@misc{isofind2026blackseawatercolumnsouthweste,
  title = {Black Sea, water column (southwestern basin), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/mer-noire-colonne-d-eau-sud-ouest-du-bassin/},
  note = {Accessed 2026-10-16}
}

Updated : 2026-10-16