National Laboratory of Energy and Geology, Portugal
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Affiliated Works
sorted by decreasing year, and then by display-name
- Deglacial Diatom Assemblages And Surface Ocean Properties Overlying The Bermuda Rise
- Diatom Transfer Functions for Sea Surface Temperature and Primary Productivity in Upwelling Areas: the Cupex Project
- Late Slowdown of Atlantic Meridional Overturning Circulation During the Last Glacial Inception: New Constraints From Sedimentary (231Pa/230Th)
- Mg/Ca Paleothermometry in the Central Gulf of Cadiz During Heinrich Events
- Tracing the Influence of Mediterranean Outflow Waters on the Mid-depth Portuguese Margin Between Marine Isotope Stages 9 and 13
- CLIMATE OFF PORTUGAL DURING MARINE ISOTOPE STAGES 15-9 (570 TO 300 KA): SUBORBITAL GLACIAL VARIABILITY AND INTERGLACIAL STABILITY
- Cenozoic evolution of the Africa-Eurasia plate boundary west of Strait of Gibraltar: mechanical models based on kinematic constraints
- Precise chronology of Heinrich-1 meltwater pulses in the Nordic Seas (Invited)
- Temperature calibration along the Iberian-NW Africa margin, using modern planktonic foraminifera trace element and stable isotope ratios
- Assessing Paleoceanographic Reconstruction Uncertainties caused by No-Analogs: a NE Pacific example
- European warming linked to Greenland melting during the Last Interglacial North Atlantic climate optimum
- Iberian Margin Sea Surface Temperature during MIS 15 to 9 (580-300 ka): Glacial suborbital variability vs interglacial stability
- Interglacial Climatic Variability in Southern Europe During the Last 425,000 Years From NW Iberian Marine Pollen Records
- Overturning Circulation in the North Atlantic Ocean During Marine Isotope Stage 11c
- Pliocene-Pleistocene paleo-productivity changes in the Bering Sea: results from IODP Expedition 323 (Invited)
- Results from IODP Exp. 323 to the Bering Sea: sea ice history and seasonal productivity for the last 5 Ma
- A 5 Ma ocean history of the Bering Sea, observed through diatoms
- Gas Geochemical Results from IODP Expedition 334: Influence of Subsurface Structure and Fluid Flow on Gas Composition
- The Deglaciation and the Holocene over the Laurentian fan: a diatom report
- Constraints on the factors controlling <SUP>13</SUP>C-<SUP>18</SUP>O bond abundances in biologically precipitated carbonates from measurements of marine calcifiers cultured at variable temperature, pH, and salinity
- 3D Shallow crustal structure of Madeira island revealed from ambient noise tomography
- Mesozoic Granitic Magmatism in Macao, Southeast China