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Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera.
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- Paleoceanography & Paleoclimatology, 2021, v. 36, n. 4, p. 1, doi. 10.1029/2020PA004153
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Hydrological variations of the intermediate water masses of the western Mediterranean Sea during the past 20 ka inferred from neodymium isotopic composition in foraminifera and cold-water corals.
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- Climate of the Past, 2017, v. 13, n. 1, p. 17, doi. 10.5194/cp-13-17-2017
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- Article
Hydrological variations of the intermediate water masses of the western Mediterranean Sea during the past 20&ka inferred from neodymium isotopic composition in foraminifera and cold-water corals.
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- Climate of the Past Discussions, 2016, v. 12, n. 13, p. 1, doi. 10.5194/cp-2016-64
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- Article
Past hydrological and cold water coral growth variations at the SW Rockall Trough margin (NE Atlantic) during the Holocene.
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- Geophysical Research Abstracts, 2018, v. 20, p. 5018
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RECONSTRUCTION OF OCEAN CIRCULATION BASED ON NEODYMIUM ISOTOPIC COMPOSITION: Potential Limitations and Application to the Mid-Pleistocene Transition.
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- Oceanography, 2020, v. 33, n. 2, p. 80, doi. 10.5670/oceanog.2020.205
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South Atlantic intermediate water advances into the North-east Atlantic with reduced Atlantic meridional overturning circulation during the last glacial period.
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- Geochemistry, Geophysics, Geosystems: G3, 2016, v. 17, n. 6, p. 2336, doi. 10.1002/2016GC006281
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- Article
Neodymium isotopic composition in foraminifera and authigenic phases of the South China Sea sediments: Implications for the hydrology of the North Pacific Ocean over the past 25 kyr.
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- Geochemistry, Geophysics, Geosystems: G3, 2015, v. 16, n. 11, p. 3883, doi. 10.1002/2015GC005871
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- Article