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Universiteit Gent; Faculteit Wetenschappen; Vakgroep Geologie; Renard Centre of Marine Geology (RCMG), more
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| Publications (6) |
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| A1 Publications (6) [show] |
- Huang, Q.; Hou, R.; Lin, L.; Li, H.; Liu, S.; Cheng, Y.; Xu, X. (2023). Bioaccumulation and trophic transfer of organophosphate flame retardants and their metabolites in the estuarine food web of the Pearl River, China. Environ. Sci. Technol. 57(9): 3549-3561. https://dx.doi.org/10.1021/acs.est.2c05619, more
- Liu, S.; Hernandez-Molina, F.J.; Rodrigues, S.; Van Rooij, D. (2023). Deep-water circulation in the northeast Atlantic during the mid- and Late Cretaceous. Geology (Boulder Colo.) 51(6): 515-520. https://dx.doi.org/10.1130/G50886.1, more
 Liu, S.; Liang, Z.J.; Zhang, B.D.; Su, H.X.; Lei, Z.Y.; Su, M. (2022). Carbonate contourite drifts in the southwest South China Sea: Sedimentary, paleoceanographic and economic implications. Front. Mar. Sci. 9: 946231. https://dx.doi.org/10.3389/fmars.2022.946231, more- Liu, S.; Hernández-Molina, F.J.; Yang, C.; Zhang, C.; Huang, X.; Yin, S.; Garcia, M.; Van Rooij, D.; Wang, C.; Zhuo, H.; Chen, H.; Lei, Y.; Lin, Z.; Luo, K.; Su, M. (2022). Oceanographic consequences of the Bransfield Strait (Antarctica) opening. Geology (Boulder Colo.) 50(12): 1403-1408. https://dx.doi.org/10.1130/G50389.1, more
- Liu, S.; Hernández-Molina, F.J.; Ercilla, G.; Van Rooij, D. (2020). Sedimentary evolution of the Le Danois contourite drift systems (southern Bay of Biscay, NE Atlantic): a reconstruction of the Atlantic Mediterranean Water circulation since the Pliocene. Mar. Geol. 427: 106217. https://hdl.handle.net/10.1016/j.margeo.2020.106217, more
- Liu, S.; Van Rooij, D.; Vandorpe, T.; González-Pola, C.; Ercilla, G.; Hernández-Molina, F.J. (2019). Morphological features and associated bottom-current dynamics in the Le Danois Bank region (southern Bay of Biscay, NE Atlantic): A model in a topographically constrained small basin. Deep-Sea Res., Part 1, Oceanogr. Res. Pap. 149: 103054. https://dx.doi.org/10.1016/j.dsr.2019.05.014, more
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