Ph. MourguiartThierry CorrègeDenis WirrmannJaime ArgolloMaria Eugenia MontenegroM. PourchetPierre Carbonel2026-03-222026-03-22199810.1016/s0031-0182(98)00068-6https://doi.org/10.1016/s0031-0182(98)00068-6https://andeanlibrary.org/handle/123456789/44241Citaciones: 85enOstracodHoloceneGeologyStructural basinSalinityPleistoceneFlooding (psychology)Water levelPhysical geographyPaleontologyHolocene palaeohydrology of Lake Titicaca estimated from an ostracod-based transfer functionarticle