Science report
| 
05 Nov 2013
Science report |
| 05 Nov 2013
The "Shackleton Site" (IODP Site U1385) on the Iberian Margin
D. A. Hodell
Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge, UK
L. Lourens
Institute of Earth Sciences, Utrecht University, Utrecht, the Netherlands
D. A. V. Stow
Institute of Petroleum Engineering, Heriot-Watt University Edinburgh, UK
J. Hernández-Molina
Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey, UK
C. A. Alvarez Zarikian
Integrated Ocean Drilling Program, Texas A&M University, College Station TX, USA
the Shackleton Site Project Members
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Cited
43 citations as recorded by crossref.
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- Benthic paleoenvironmental response to late Pleistocene climate variability at the SW Iberian Margin: an ichnofabric approach J. Dorador et al. https://doi.org/10.1080/10420940.2026.2726225
- 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
- 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
- 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
- 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
- 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
- Quantitative estimation of bioturbation based on digital image analysis J. Dorador & F. Rodríguez-Tovar https://doi.org/10.1016/j.margeo.2014.01.003
- 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
- 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
- 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
- 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
- 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
- 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
- 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
- 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
- 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
- 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
- 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
- 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
- Digital Twin in the Maritime Domain: A Review and Emerging Trends N. Madusanka et al. https://doi.org/10.3390/jmse11051021
- 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
- Pleistocene calcareous nannofossil biochronology at IODP Site U1385 (Expedition 339) B. Balestra et al. https://doi.org/10.1016/j.gloplacha.2015.10.004
- 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
- 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
- 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
- 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
- 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
- Metagenomics of the Iberian Margin: IODP Site U1385 J. Russell et al. https://doi.org/10.1180/gbi.2026.10007
- 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
- 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
- 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
- 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
- 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
- Protracted ocean circulation slowdown drove exceptional ice-sheet melting during ice age termination IV H. Hu et al. https://doi.org/10.1038/s41467-026-73733-6
- 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
- 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
- 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
- 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
- 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
- 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
- Virtual special issue on IODP Expedition 339: The Mediterranean outflow D. Hodell et al. https://doi.org/10.1016/j.gloplacha.2016.06.016
- A salty start to modern ocean circulation G. Filippelli https://doi.org/10.1126/science.1255553
Latest update: 02 Nov 2026
