40 citations as recorded by crossref.

1. Tropically-driven climate shifts in southwestern Europe during MIS 19, a low eccentricity interglacial M. Sánchez Goñi et al. https://doi.org/10.1016/j.epsl.2016.05.018
2. Sea-Air CO2 Exchange in the SW Iberian Upwelling System during Two Contrasting Climate Cycles: 860–780 ka and 630–520 ka G. Martin-Garcia https://doi.org/10.3390/geosciences8120454
3. The Carbon-Sulfur Link in the Remineralization of Organic Carbon in Surface Sediments H. Bradbury et al. https://doi.org/10.3389/feart.2021.652960
4. Assessing Sedimentary Boundary Layer Calcium Carbonate Precipitation and Dissolution Using the Calcium Isotopic Composition of Pore Fluids D. James et al. https://doi.org/10.3389/feart.2021.601194
5. Digital Twin in the Maritime Domain: A Review and Emerging Trends N. Madusanka et al. https://doi.org/10.3390/jmse11051021
6. A reference time scale for Site U1385 (Shackleton Site) on the SW Iberian Margin D. Hodell et al. https://doi.org/10.1016/j.gloplacha.2015.07.002
7. Pleistocene calcareous nannofossil biochronology at IODP Site U1385 (Expedition 339) B. Balestra et al. https://doi.org/10.1016/j.gloplacha.2015.10.004
8. Ichnological analysis of Pleistocene sediments from the IODP Site U1385 “Shackleton Site” on the Iberian margin: Approaching paleoenvironmental conditions F. Rodríguez-Tovar & J. Dorador https://doi.org/10.1016/j.palaeo.2014.04.027
9. Contourites and bottom current reworked sands: Bed facies model and implications S. de Castro et al. https://doi.org/10.1016/j.margeo.2020.106267
10. Deep-sea trace fossil and benthic foraminiferal assemblages across glacial Terminations 1, 2 and 4 at the “Shackleton Site” (IODP Expedition 339, Site U1385) F. Rodríguez-Tovar et al. https://doi.org/10.1016/j.gloplacha.2015.05.003
11. Response of macrobenthic and foraminifer communities to changes in deep-sea environmental conditions from Marine Isotope Stage (MIS) 12 to 11 at the “Shackleton Site” F. Rodríguez-Tovar et al. https://doi.org/10.1016/j.gloplacha.2015.08.012
12. Virtual special issue on IODP Expedition 339: The Mediterranean outflow F. Hernández-Molina et al. https://doi.org/10.1016/j.margeo.2016.05.009
13. Sedimentary processes and depositional environments of a continuous marine succession across the Lower–Middle Pleistocene boundary: Kokumoto Formation, Kazusa Group, central Japan N. Nishida et al. https://doi.org/10.1016/j.quaint.2015.06.045
14. Paleoclimatic and paleoceanographic records through Marine Isotope Stage 19 at the Chiba composite section, central Japan: A key reference for the Early–Middle Pleistocene Subseries boundary Y. Suganuma et al. https://doi.org/10.1016/j.quascirev.2018.04.022
15. Dinoflagellate cyst population evolution throughout past interglacials: Key features along the Iberian margin and insights from the new IODP Site U1385 (Exp 339) F. Eynaud et al. https://doi.org/10.1016/j.gloplacha.2015.12.004
16. Quantitative estimation of bioturbation based on digital image analysis J. Dorador & F. Rodríguez-Tovar https://doi.org/10.1016/j.margeo.2014.01.003
17. Similar millennial climate variability on the Iberian margin during two early Pleistocene glacials and MIS 3 B. Birner et al. https://doi.org/10.1002/2015PA002868
18. Oceanic heat pulses fueling moisture transport towards continental Europe across the mid-Pleistocene transition A. Bahr et al. https://doi.org/10.1016/j.quascirev.2017.11.009
19. Severe cooling episodes at the onset of deglaciations on the Southwestern Iberian margin from MIS 21 to 13 (IODP site U1385) G. Martin-Garcia et al. https://doi.org/10.1016/j.gloplacha.2015.11.001
20. Unraveling the forcings controlling the vegetation and climate of the best orbital analogues for the present interglacial in SW Europe D. Oliveira et al. https://doi.org/10.1007/s00382-017-3948-7
21. Stratigraphic variation in ichnofabrics at the “Shackleton Site” (IODP Site U1385) on the Iberian Margin: Paleoenvironmental implications J. Dorador & F. Rodríguez-Tovar https://doi.org/10.1016/j.margeo.2015.09.008
22. Coccolithophore productivity at the western Iberian Margin during the Middle Pleistocene (310–455 ka) – evidence from coccolith Sr∕Ca data C. Cavaleiro et al. https://doi.org/10.5194/cp-16-2017-2020
23. Comparison of qualitative and quantitative dinoflagellate cyst approaches in reconstructing glacial-interglacial climate variability at West Iberian Margin IODP ‘Shackleton’ Site U1385 M. Datema et al. https://doi.org/10.1016/j.marmicro.2017.08.003
24. A NOVEL APPLICATION OF DIGITAL IMAGE TREATMENT BY QUANTITATIVE PIXEL ANALYSIS TO TRACE FOSSIL RESEARCH IN MARINE CORES J. DORADOR & F. RODRÍGUEZ-TOVAR https://doi.org/10.2110/palo.2014.044
25. Early Pleistocene calcareous nannofossil assemblages from the Gulf of Cadiz reveal glacial-interglacial and millennial-scale variability S. Trotta et al. https://doi.org/10.1016/j.palaeo.2022.111304
26. Surface-to-deep-ocean ecosystem responses to orbital-to-millennial-scale paleoceanographic variability across the mid-Brunhes at the Iberian margin A. González-Lanchas et al. https://doi.org/10.1016/j.gloplacha.2025.105205
27. Climate changes in south western Iberia and Mediterranean Outflow variations during two contrasting cycles of the last 1Myrs: MIS 31–MIS 30 and MIS 12–MIS 11 M. Sánchez Goñi et al. https://doi.org/10.1016/j.gloplacha.2015.11.006
28. Coupled ocean–land millennial-scale changes 1.26millionyears ago, recorded at Site U1385 off Portugal P. Tzedakis et al. https://doi.org/10.1016/j.gloplacha.2015.10.008
29. Coccolithophore variability from the Shackleton Site (IODP Site U1385) through MIS 16-10 P. Maiorano et al. https://doi.org/10.1016/j.gloplacha.2015.07.009
30. Automated Image Analysis of Mud and Mudrock Microstructure and Characteristics of Hemipelagic Sediments: IODP Expedition 339 S. Bankole et al. https://doi.org/10.1007/s12583-019-1210-4
31. Techniques for the non-destructive and continuous analysis of sediment cores. Application in the Iberian continental margin J. Frigola et al. https://doi.org/10.21701/bolgeomin.126.2-3.014
32. A micropalaeontological perspective on export productivity, oxygenation and temperature in NE Atlantic deep-waters across Terminations I and II P. Grunert et al. https://doi.org/10.1016/j.gloplacha.2015.06.002
33. Coccolithophore and benthic foraminifera distribution patterns in the Gulf of Cadiz and Western Iberian Margin during Integrated Ocean Drilling Program (IODP) Expedition 339 B. Balestra et al. https://doi.org/10.1016/j.jmarsys.2017.01.005
34. An exceptional record of millennial-scale climate variability in the southern Iberian Margin during MIS 6: Impact on the formation of sapropel S6 F. Sierro & N. Andersen https://doi.org/10.1016/j.quascirev.2022.107527
35. High resolution digital image treatment to color analysis on cores from IODP Expedition 339: Approaching lithologic features and bioturbational influence J. Dorador & F. Rodríguez-Tovar https://doi.org/10.1016/j.margeo.2016.02.005
36. Zoophycos in deep‐sea sediments indicates high and seasonal primary productivity: Ichnology as a proxy in palaeoceanography during glacial–interglacial variations J. Dorador et al. https://doi.org/10.1111/ter.12224
37. Virtual special issue on IODP Expedition 339: The Mediterranean outflow D. Hodell et al. https://doi.org/10.1016/j.gloplacha.2016.06.016
38. Millennial‐Scale Climate Variability and Dinoflagellate‐Cyst‐Based Seasonality Changes Over the Last ~150 kyrs at “Shackleton Site” U1385 M. Datema et al. https://doi.org/10.1029/2018PA003497
39. Abrupt intrinsic and extrinsic responses of southwestern Iberian vegetation to millennial‐scale variability over the past 28 ka A. Cutmore et al. https://doi.org/10.1002/jqs.3392
40. A salty start to modern ocean circulation G. Filippelli https://doi.org/10.1126/science.1255553