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Found 45 results
Autor Título Tipo [ Ano(Asc)]
Filtros: Autor é Voelker, A.H.L.  [Clear All Filters]
2018
Voelker AHL, Jiménez-Espejo FJ, Bahr A, et al. Data report: IODP Site U1387: the revised splice between Sections U1387B-18X-3 and U1387C-8R-3 (>171.6 mcd). In: Stow DAV, Hernández-Molina FJ, Zarikian CAAlvarez, eds. Proceedings Of The Integrated Ocean Drilling Program. Vol. 339. Proceedings of the Integrated Ocean Drilling Program. Tokyo: International Ocean Discovery Program; 2018:1-11. doi:10.2204/iodp.proc.339.204.2018
Cavaleiro C, Voelker AHL, Stoll H, et al. Insolation forcing of coccolithophore productivity in the North Atlantic during the Middle Pleistocene. Quaternary Science Reviews. 2018;191:318 - 336. doi:10.1016/j.quascirev.2018.05.027
2017
Rodrigues T, Alonso-García M, Hodell DA, et al. A 1-Ma record of sea surface temperature and extreme cooling events in the North Atlantic: A perspective from the Iberian Margin. Quaternary Science Reviews. 2017;172:118 - 130. doi:10.1016/j.quascirev.2017.07.004
Ventura C, Abrantes F, Loureiro I, Voelker AHL. Data report: diatom and silicoflagellate records of marine isotope Stages 25-27 at IODP Site U1387, Faro Drift. In: Stow DAV, Hernández-Molina FJ, Zarikian CAAlvarez, , eds. Proceedings Of The Integrated Ocean Drilling Program, Volume 339. Proceedings of the Integrated Ocean Drilling Program, Volume 339. Tokyo: Integrated Ocean Drilling Program Management International, Inc.; 2017. doi:10.2204/iodp.proc.339.202.2017
Andrews JT, Dunhill G, Vogt C, Voelker AHL. Denmark Strait during the Late Glacial Maximum and Marine Isotope Stage 3: Sediment sources and transport processes. Marine Geology. 2017;390:181 - 198. doi:10.1016/j.margeo.2017.07.003
Rebotim A, Voelker AHL, Jonkers L, et al. Factors controlling the depth habitat of planktonic foraminifera in the subtropical eastern North Atlantic. Biogeosciences. 2017;14(4):827 - 859. doi:10.5194/bg-14-827-2017
García-Gallardo Á, Grunert P, Voelker AHL, Mendes I, Piller WE. Re-evaluation of the “elevated epifauna” as indicator of Mediterranean Outflow Water in the Gulf of Cadiz using stable isotopes (δ 13 C, δ 18 O). Global and Planetary Change. 2017;155:78 - 97. doi:10.1016/j.gloplacha.2017.06.005
Oliveira D, Goñi MFernanda S, Naughton F, et al. 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