Found 49 results
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Variability of the North Atlantic Current during the last 2000 years based on shelf bottom water and sea surface temperatures along an open ocean/shallow marine transect in western Europe. The Holocene. 2006;16(7):1017 - 1029. doi:10.1177/0959683606hl991rp
Unexpected weak seasonal climate in the western Mediterranean region during MIS 31, a high-insolation forced interglacial. Quaternary Science Reviews. 2017;161:1 - 17. doi:10.1016/j.quascirev.2017.02.013
Twentieth-century warming and hydrographical changes in the Tagus Prodelta, eastern North Atlantic. The Holocene. 2009;19(3):369 - 380. doi:10.1177/0959683608101388
. Temperature and productivity changes off the western Iberian margin during the last 150 ky. Quaternary Science Reviews. 2010;29(5-6):680 - 695. doi:10.1016/j.quascirev.2009.11.013
. Suspended particulate matter in the Mediterranean water at the Gulf of Cadiz and off the southwest coast of the Iberian Peninsula. Deep Sea Research Part II: Topical Studies in Oceanography. 2002;49(19):4245 - 4261. doi:10.1016/S0967-0645(02)00153-4
. 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
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
. Sediment instability on the Portuguese continental margin under abrupt glacial climate changes (last 60kyr). Quaternary Science Reviews. 2009;28(27-28):3211 - 3223. doi:10.1016/j.quascirev.2009.08.007
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
Reply to comment received from A. E. Carlson et al. regarding “The deglaciation over Laurentian Fan: History of diatoms, IRD, ice and fresh water” by Gil et al. (2015), Quaternary Science Reviews 129, 57–67. Quaternary Science Reviews. 2016;139:166 - 169. doi:10.1016/j.quascirev.2016.03.001
. A reference time scale for Site U1385 (Shackleton Site) on the SW Iberian Margin. Global and Planetary Change. 2015;133:49 - 64. doi:10.1016/j.gloplacha.2015.07.002
Proxy calibration to instrumental data set: Implications for paleoceanographic reconstructions. Geochemistry, Geophysics, Geosystems. 2009;10(9):n/a - n/a. doi:10.1029/2009GC002604
Provenance of organic matter and nutrient conditions on a river- and upwelling influenced shelf: A case study from the Portuguese Margin. Marine Geology. 2007;243(1-4):169 - 179. doi:10.1016/j.margeo.2007.04.016
. Planktonic foraminifera from modern sediments reflect upwelling patterns off Iberia: Insights from a regional transfer function. Marine Micropaleontology. 2008;66(3-4):135 - 164. doi:10.1016/j.marmicro.2007.09.003
Planktic foraminiferal responses to orbital scale oceanographic changes off the western Iberian margin over the last 900kyr: Results from IODP site U1391. Global and Planetary Change. 2015;135:47 - 56. doi:10.1016/j.gloplacha.2015.10.002
. Physical, chemical and sedimentological aspects of the Mediterranean outflow off Iberia. Deep Sea Research Part II: Topical Studies in Oceanography. 2002;49(19):4163 - 4177. doi:10.1016/S0967-0645(02)00148-0
Past circulation along the western Iberian margin: a time slice vision from the Last Glacial to the Holocene. Quaternary Science Reviews. 2014;106:316 - 329. doi:10.1016/j.quascirev.2014.09.001
Paleoproductivity variations related to climatic conditions in the Alboran Sea (western Mediterranean) during the last glacial–interglacial transition: the diatom record. Palaeogeography, Palaeoclimatology, Palaeoecology. 2001;167(3-4):337 - 357. doi:10.1016/S0031-0182(00)00246-7
. Mediterranean outflow strengthening during northern hemisphere coolings: A salt source for the glacial Atlantic?. Earth and Planetary Science Letters. 2006;245(1-2):39 - 55. doi:10.1016/j.epsl.2006.03.014
. 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
. The Late Pleistocene-Holocene sedimentary evolution of the Sines Contourite Drift (SW Portuguese Margin): A multiproxy approach. Sedimentary Geology. 2020;407:105737. doi:10.1016/j.sedgeo.2020.105737
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
. Iberian Margin sea surface temperature during MIS 15 to 9 (580–300 ka): Glacial suborbital variability versus interglacial stability. Paleoceanography. 2011;26(1). doi:10.1029/2010PA001927
. Hydrographic conditions along the western Iberian margin during marine isotope stage 2. Geochemistry, Geophysics, Geosystems. 2009;10(12):n/a - n/a. doi:10.1029/2009GC002605
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