| Cariaco Basin, core-top sediment PL07-105Bx Venezuela | −5.4 ± 0.4 ε | | 2 | authigenic fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-105Bx Venezuela | −2.4 ± 0.3 ε | | 2 | silicate fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-111Bx Venezuela | −5.3 ± 0.2 ε | | 2 | authigenic fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-111Bx Venezuela | −3.2 ± 0.1 ε | | 2 | silicate fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-22Bx Venezuela | −5.9 ± 0.1 ε | | 2 | authigenic fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-22Bx Venezuela | −3 ± 0.1 ε | | 2 | silicate fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-69Bx Venezuela | −5.1 ε | | 2 | authigenic fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-69Bx Venezuela | −2.1 ± 2.1 ε | | 2 | silicate fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-82Bx Venezuela | −5.2 ± 0.1 ε | | 2 | authigenic fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-82Bx Venezuela | −3 ± 0.7 ε | | 2 | silicate fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-89Bx Venezuela | −3.9 ± 0.3 ε | | 2 | authigenic fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Cariaco Basin, core-top sediment PL07-89Bx Venezuela | −3.1 ± 0.2 ε | | 2 | silicate fraction | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Black Sea, deep euxinic sediments (KNR 134 39 BC 21 box core) | −2 ± 0.5 ε | | 4 | authigenic fraction of the 1-2 cm level | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Black Sea, deep euxinic sediments (KNR 134 39 BC 21 box core) | −1.9 ± 0.2 ε | | 4 | silicate fraction of the 1-2 cm level | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Black Sea, deep euxinic sediments (KNR 134 39 BC 21 box core) | −2.2 ± 0.1 ε | | 2 | authigenic fraction of the 2-3 cm level | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Black Sea, deep euxinic sediments (KNR 134 39 BC 21 box core) | −2.3 ± 0.2 ε | | 4 | silicate fraction of the 2-3 cm level | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Black Sea, deep euxinic sediments (KNR 134 39 BC 21 box core) | −2.2 ± 0.1 ε | | 4 | authigenic fraction of the 3-4 cm level | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Black Sea, deep euxinic sediments (KNR 134 39 BC 21 box core) | −1.8 ± 0.5 ε | | 4 | silicate fraction of the 3-4 cm level | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Black Sea, deep euxinic sediments (KNR 134 39 BC 21 box core) | −2.4 ± 0.1 ε | | 4 | authigenic fraction of the 30-31 cm level | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Black Sea, deep euxinic sediments (KNR 134 39 BC 21 box core) | −1.9 ± 0.1 ε | | 4 | silicate fraction of the 30-31 cm level | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Black Sea, deep euxinic sediments (KNR 134 39 BC 21 box core) | −2.8 ± 0.1 ε | | 3 | authigenic fraction of the 48-49 cm level | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Black Sea, deep euxinic sediments (KNR 134 39 BC 21 box core) | −2 ± 0.2 ε | | 2 | silicate fraction of the 48-49 cm level | Owens et al. (2017), Thallium-isotopic compositions of euxinic sediments as a proxy for g… |
| Lanmuchang stream sediment (SD05) China | 0.44 ± 0.35 ε | | | | Kersten et al. (2014), Tracing anthropogenic thallium in soil using stable isotope compos… |
| Gaofeng River sediments downstream of the Yunfu pyrite mine China | −4.87 ± 0.3 ε | | 1 | zone A1 sediment, at the mining effluent outlet | Ouyang et al. (2023), Stable thallium (Tl) isotopic signature as a reliable source tracer… |
| Gaofeng River sediments downstream of the Yunfu pyrite mine China | 3.95 ± 0.3 ε | | 1 | pyrite tailings lake sediment (zone A2) | Ouyang et al. (2023), Stable thallium (Tl) isotopic signature as a reliable source tracer… |
| Gaofeng River sediments downstream of the Yunfu pyrite mine China | −3.16 ± 0.11 ε | −3.24 / −3.08 ε | 2 | sediments between the tailings lake and the treatment station (zones A3 and A4) | Ouyang et al. (2023), Stable thallium (Tl) isotopic signature as a reliable source tracer… |
| Gaofeng River sediments downstream of the Yunfu pyrite mine China | −6.7 ± 0.3 ε | | 1 | sediments below the treatment station outfall (zones B1 and B2) | Ouyang et al. (2023), Stable thallium (Tl) isotopic signature as a reliable source tracer… |
| Gaofeng River sediments downstream of the Yunfu pyrite mine China | 0.24 ± 0.67 ε | −0.23 / 0.72 ε | 2 | sediments before and after the confluence (zones C2 and D1) | Ouyang et al. (2023), Stable thallium (Tl) isotopic signature as a reliable source tracer… |
| Gaofeng River sediments downstream of the Yunfu pyrite mine China | −2.55 ± 0.3 ε | | 1 | sediment downstream of the confluence (zone D2) | Ouyang et al. (2023), Stable thallium (Tl) isotopic signature as a reliable source tracer… |
| Gaofeng River sediments downstream of the Yunfu pyrite mine China | −2.07 ± 0.3 ε | | 1 | Nanshan River background sediments (zones E3 and E4) | Ouyang et al. (2023), Stable thallium (Tl) isotopic signature as a reliable source tracer… |
