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Abrantes F. Increased upwelling off Portugal during the last glaciation: Diatom evidence. Marine Micropaleontology. 1991;17(3-4):285 - 310. doi:10.1016/0377-8398(91)90017-Z
Abrantes F, Meggers H, Nave S, et al. Fluxes of micro-organisms along a productivity gradient in the Canary Islands region (29°N): implications for paleoreconstructions. Deep Sea Research Part II: Topical Studies in Oceanography. 2002;49(17):3599 - 3629. doi:10.1016/S0967-0645(02)00100-5
Abrantes F, Baas J, Haflidason H, et al. Sediment fluxes along the northeastern European Margin: inferring hydrological changes between 20 and 8 kyr. Marine Geology. 1998;152(1-3):7 - 23. doi:10.1016/S0025-3227(98)00062-0
Abrantes F, Rodrigues T, Rufino M, et al. Historical Climate off the Atlantic Iberian Peninsula. Climate of the Past Discussions. 2017:1 - 40. doi:10.5194/cp-2017-39
Abrantes F. 200 000 yr diatom records from Atlantic upwelling sites reveal maximum productivity during LGM and a shift in phytoplankton community structure at 185 000 yr. Earth and Planetary Science Letters. 2000;176(1):7 - 16. doi:10.1016/S0012-821X(99)00312-X
Abrantes F, Lopes C, Rodrigues T, et al. Proxy calibration to instrumental data set: Implications for paleoceanographic reconstructions. Geochemistry, Geophysics, Geosystems. 2009;10(9):n/a - n/a. doi:10.1029/2009GC002604
Abrantes F, Alt-Epping U, Lebreiro S, Voelker AHL, Schneider R. Sedimentological record of tsunamis on shallow-shelf areas: The case of the 1969 AD and 1755 AD tsunamis on the Portuguese Shelf off Lisbon. Marine Geology. 2008;249(3-4):283 - 293. doi:10.1016/j.margeo.2007.12.004
Abrantes F, Voelker AHL, Sierro FJavier, et al. The Climate Of The Mediterranean Regionpaleoclimate Variability In The Mediterranean Region. Elsevier; 2012:1 - 86. doi:10.1016/B978-0-12-416042-2.00001-X
Abrantes F. Diatom assemblages as upwelling indicators in surface sediments off Portugal. Marine Geology. 1988;85(1):15 - 39. doi:10.1016/0025-3227(88)90082-5
Abrantes F, Lopes C, Mix A, Pisias N. Diatoms in Southeast Pacific surface sediments reflect environmental properties. Quaternary Science Reviews. 2007;26(1-2):155 - 169. doi:10.1016/j.quascirev.2006.02.022
Abrantes F, Cermeno P, Lopes C, et al. Diatoms Si uptake capacity drives carbon export in coastal upwelling systems. Biogeosciences. 2016;13(14):4099 - 4109. doi:10.5194/bg-13-4099-201610.5194/bg-13-4099-2016-supplement
Abrantes F, Voelker AHL, Sierro FJavier, et al. The Climate of the Mediterranean RegionPaleoclimate Variability in the Mediterranean Region. In: Elsevier; 2012:1 - 86. doi:10.1016/B978-0-12-416042-2.00001-X
Abrantes F, Lebreiro S, Rodrigues T, et al. Shallow-marine sediment cores record climate variability and earthquake activity off Lisbon (Portugal) for the last 2000 years. Quaternary Science Reviews. 2005;24(23-24):2477 - 2494. doi:10.1016/j.quascirev.2004.04.009
Abrantes F. A 340,000 year continental climate record from tropical Africa – news from opal phytoliths from the equatorial Atlantic. Earth and Planetary Science Letters. 2003;209(1-2):165 - 179. doi:10.1016/S0012-821X(03)00039-6
Abrantes F, Rodrigues T, Montanari B, et al. Climate of the last millennium at the southern pole of the North Atlantic Oscillation: an inner-shelf sediment record of flooding and upwelling. Climate Research. 2011;48(2):261 - 280. doi:10.3354/cr01010
Abrantes F, Gil IM. Marine Diatoms. In: Encyclopedia Of Quaternary Science. Vol. PALEOCEANOGRAPHY, BIOLOGICAL PROXIES. 2ndnd ed. Encyclopedia of Quaternary Science. Elsevier; 2013:816 - 824. doi:10.1016/B978-0-444-53643-3.00284-3