Found: 22
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Pinus nigra (European black pine) as the dominant species of the last glacial pinewoods in south-western to central Iberia: a morphological study of modern and fossil pollen.
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- Journal of Biogeography, 2015, v. 42, n. 10, p. 1998, doi. 10.1111/jbi.12566
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Moist and warm conditions in Eurasia during the last glacial of the Middle Pleistocene Transition.
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- Nature Communications, 2023, v. 14, n. 1, p. 1, doi. 10.1038/s41467-023-38337-4
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Beyond skepticism: uncovering cryptic refugia using multiple lines of evidence.
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- New Phytologist, 2014, v. 204, n. 3, p. 450, doi. 10.1111/nph.13089
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The ACER pollen and charcoal database: a global resource to document vegetation and fire response to abrupt climate changes during the last glacial period.
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- Earth System Science Data, 2017, v. 9, n. 2, p. 679, doi. 10.5194/essd-9-679-2017
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Impact of terrestrial biosphere on the atmospheric CO<sub>2</sub> concentration across Termination V.
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- Climate of the Past Discussions, 2021, p. 1, doi. 10.5194/cp-2021-143
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Regional impacts of climate change and its relevance to human evolution.
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- Evolutionary Human Sciences, 2020, v. 2, n. 1, p. 1, doi. 10.1017/ehs.2020.56
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The expansion of Central and Northern European Neolithic populations was associated with a multi-century warm winter and wetter climate.
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- Holocene, 2016, v. 26, n. 8, p. 1188, doi. 10.1177/0959683616638435
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Holocene land–sea climatic links on the equatorial Pacific coast (Bay of Guayaquil, Ecuador).
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- Holocene, 2016, v. 26, n. 4, p. 567, doi. 10.1177/0959683615612566
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- Article
Air-sea temperature decoupling in western Europe during the last interglacial-glacial transition.
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- Nature Geoscience, 2013, v. 6, n. 10, p. 837, doi. 10.1038/ngeo1924
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- Article
Position of the Polar Front along the western Iberian margin during key cold episodes of the last 45 ka.
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- Geochemistry, Geophysics, Geosystems: G3, 2009, v. 10, n. 7, p. n/a, doi. 10.1029/2009GC002398
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Contrasting intrainterstadial climatic evolution between high and middle North Atlantic latitudes: A close-up of Greenland Interstadials 8 and 12.
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- Geochemistry, Geophysics, Geosystems: G3, 2009, v. 10, n. 4, p. n/a, doi. 10.1029/2008GC002369
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Testing the Hypothesis of Fire Use for Ecosystem Management by Neanderthal and Upper Palaeolithic Modern Human Populations.
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- PLoS ONE, 2010, v. 5, n. 2, p. 1, doi. 10.1371/journal.pone.0009157
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Neanderthal Extinction by Competitive Exclusion.
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- PLoS ONE, 2008, v. 3, n. 12, p. 1, doi. 10.1371/journal.pone.0003972
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- Article
Orbital parameters controlling the western Iberian vegetation and climate during the Middle Pleistocene Transition: evidence from the extreme interglacial MIS 31.
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- Geophysical Research Abstracts, 2018, v. 20, p. 9353
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Western Mediterranean vegetation and climate dynamics during the best astronomical analogues of the Holocene: evidence from a model-data comparison.
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- Geophysical Research Abstracts, 2018, v. 20, p. 2979
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Environmental changes in SW France during the Middle to Upper Paleolithic transition from the pollen analysis of an eastern North Atlantic deep-sea core.
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- Quaternary Research, 2022, v. 110, p. 147, doi. 10.1017/qua.2022.21
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Vegetation and environmental changes at the Middle Stone Age site of Wonderkrater, Limpopo, South Africa.
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- Quaternary Research, 2017, v. 88, n. 2, p. 313, doi. 10.1017/qua.2017.42
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The complexity of millennial-scale variability in southwestern Europe during MIS 11.
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- Quaternary Research, 2016, v. 86, n. 3, p. 373, doi. 10.1016/j.yqres.2016.09.002
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Orbital- and sub-orbital-scale climate impacts on vegetation of the western Mediterranean basin over the last 48,000 yr
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- Quaternary Research, 2008, v. 70, n. 3, p. 451, doi. 10.1016/j.yqres.2008.07.002
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Saharan Dust Transport and High-Latitude Glacial Climatic Variability: The Alboran Sea Record
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- Quaternary Research, 2002, v. 58, n. 3, p. 318, doi. 10.1006/qres.2002.2383
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The Classic Marine Isotope Substage 5e
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- Quaternary Research, 2002, v. 58, n. 1, p. 14, doi. 10.1006/qres.2001.2312
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Unraveling the forcings controlling the vegetation and climate of the best orbital analogues for the present interglacial in SW Europe.
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- Climate Dynamics, 2018, v. 51, n. 1/2, p. 667, doi. 10.1007/s00382-017-3948-7
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- Article