All abstracts by Isabel Cacho in conference series: Goldschmidt
(2025) Implication of Transport Processes on the Grain-Size Specific Distribution of Radiogenic Isotopes Nd, Sr and Pb in Marine SedimentsHewage PL, Pena LD, Català A, Cacho I, Haghipour N, Hodell D, Eglinton TI & Ausín B
(2025) Sediment Provenance and Transport Pathways along the Atlantic Iberian Margin
Campderrós S, Pena LD, Garcia-Solsona E, Paredes-Paredes E, Català A, Haghipour N & Cacho I
(2023) Surface Ocean Cooling led Freshening on the Iberian Margin during the Abrupt Cooling Event in Marine Isotope Stage 6
Zhang H, Huang Y, Wijker R, Cacho I, Torner J, Santos MC, Kost O, Wei B & Stoll H
(2021) Tracking Last Deglacial Changes in Western Mediterranean Deep-Intermediate Ventilation
Inglavaga R, Cacho I, Català A, Frigola J, Perez-Asensio JN & Pena LD
(2020) Deep Oceanographic Changes in the South Tyrrhenian Sea during the Time of Last Mediterranean Sapropel Formation
Trias-Navarro S, Cacho I, Pena L, De La Fuente M, Català A, Paredes E, Garcia-Solsona E, Frigola J, Lirer F & Caruso A
(2019) Resolving the Rapid Rate of Deglaciation over Termination II in Speleothem Records
Stoll H, Cacho I, Gasson E, Moreno A, Perez C, Cheng H, Edwards RL & Iglesias M
(2019) Isotope Ratio Measurements of Small Nd, Sr and Pb Amounts with a Plasma 3 MC-ICPMS
Paredes E, Pena LD & Cacho I
(2014) Interpreting Climatic Signals from Stalagmite Trace Element and Isotopic Records Using Simple Geochemical Models and Growth Rate Constraints
Stoll H, Moreno A, Cacho I, Mendez-Vicente A, Cheng H & Edwards RL
(2011) Productivity and Circulation Changes during the Last Deglaciation from Biomarkers and Nd Isotopes
Calvo E, Pena L, Pelejero C & Cacho I
(2010) Meridional Advection of Southern Ocean Intermediate Waters during the Last Deglaciation from Nd Isotopes in Foraminifera
Pena LD, Jones KM, Goldstein SL, Hemming SR & Cacho I
(2009) Southern Ocean Intermediate Waters in Tropical Pacific Thermocline
Pena LD, Jones KM, Goldstein SL, Hemming SR & Cacho I
(2009) Speleothem Evidence for Coupling between Iberian Peninsula Hydrology and North Atlantic Oceanic and Atmospheric Modes
Stoll H, Moreno A, Banasiak A, Jimenez-Sanchez M, Cacho I, Vadillo I, Burns S, Dominguez-Cuesta MJ, Edwards RL & Cheng H
(2008) Resolving the Opal Paradox in the Glacial Eastern Equatorial Pacific: Implications for the Biological Pump of Carbon
Pichevin L, Reynolds B, Ganeshram R & Cacho I
(2002) Reconstructing Alboran Sea Hydrography during the Last Organic Rich Layer Formation
Cacho I, Sierro F, Shackleton N, Elderfield H & Grimalt J
(2002) Saharan Dust Transport and High Latitude Glacial Climatic Variability at Millennial Time-Scale
Moreno A, Cacho I, Canals M, Prins MA, Sánchez-Goñi MF & Grimalt JO
(2002) Apparent Long-Term Cooling of the Sea Surface in the Northeast Atlantic and Mediterranean during the Holocene
Marchal O, Cacho I, Stocker T, Grimalt J, Calvo E & Martrat B
(2000) Were the Iberian Peninsula Environmental Changes Triggered by the Marine Changes of the Last Glacial Period?
Sanchez Goñi MF, Turon J, Cacho I, Grimalt J, Sierro FJ, Flores JA & Shackleton N