12 citations as recorded by crossref.

1. Characterization of phreatic overgrowths on speleothems precipitated in the northern Adriatic during a sea-level stillstand at ca. 2.8 ka N. Lončar et al. 10.1017/qua.2023.65
2. The World Atlas of Last Interglacial Shorelines (version 1.0) A. Rovere et al. 10.5194/essd-15-1-2023
3. Phreatic overgrowths on speleothems (POS) from the Mallorca caves: Morphology, mineralogy, and crystal fabric classification A. Entrena et al. 10.1002/esp.5967
4. Last Interglacial sea-level proxies in the western Mediterranean C. Cerrone et al. 10.5194/essd-13-4485-2021
5. Teasing Apart Impacts of Human Activity and Regional Drought on Madagascar’s Large Vertebrate Fauna: Insights From New Excavations at Tsimanampesotse and Antsirafaly L. Godfrey et al. 10.3389/fevo.2021.742203
6. Reoccupation of late Quaternary relative sea level indicators in a tectonically quasi-stable coastal area in Southern Italy (Cilento headland): Insights into the Last Interglacial stillstands V. De Santis et al. 10.1016/j.geomorph.2025.109692
7. Unveiling the potential of karst vadose deposits in constraining Quaternary tectonic subsidence D. Ballesteros et al. 10.1002/esp.5915
8. Last interglacial and MIS 9e relative sea-level highstands in the Central Mediterranean: a reappraisal from coastal cave deposits in the Cilento area, Southern Italy I. Isola et al. 10.1016/j.qsa.2024.100212
9. Constraining the end of the Last Interglacial (MIS 5e) relative sea-level highstand in central Mediterranean: New data from Grotta delle Capre, central Italy B. Giaccio et al. 10.1016/j.gloplacha.2023.104321
10. Deep submerged speleothems in the Sansha Yongle Blue Hole (South China Sea) as determination of low sea levels during the Last Glacial Maximum X. Yu et al. 10.3389/fmars.2022.1079301
11. Chronology of Pleistocene sedimentary cycles in the western Mediterranean L. del Valle et al. 10.1016/j.quascirev.2023.108451
12. Submerged Speleothems and Sea Level Reconstructions: A Global Overview and New Results from the Mediterranean Sea F. Antonioli et al. 10.3390/w13121663