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North Atlantic drift sediments constrain Eocene tidal dissipation and the evolution of the Earth-Moon system. <i>Paleoceanography and Paleoclimatology 38(2)</i>: e2022PA004555. <a href=\"https://dx.doi.org/10.1029/2022PA004555\" target=\"_blank\">https://dx.doi.org/10.1029/2022PA004555</a>","AutID":329743,"MonDate":null,"AnaDate":2023,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":363540,"RR":"<b>Davis, C.V.; Shaw, J.O.; D'haenens, S.; Thomas, E.; Hull, P.M.</b> (2022). Photosymbiont associations persisted in planktic foraminifera during early Eocene hyperthermals at Shatsky Rise (Pacific Ocean). <i>PLoS One 17(9)</i>: e0267636. <a href=\"https://dx.doi.org/10.1371/journal.pone.0267636\" target=\"_blank\">https://dx.doi.org/10.1371/journal.pone.0267636</a>","AutID":329743,"MonDate":null,"AnaDate":2022,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":361772,"RR":"<b>Pearson, P.N.; John, E.; Wade, B.S.; D'haenens, S.; Lear, C.H.</b> (2022). 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Atlantic deep-sea cherts associated with Eocene hyperthermal events. <i>Paleoceanography and Paleoclimatology 34(2)</i>: 287-299. <a href=\"https://dx.doi.org/10.1029/2018PA003503\" target=\"_blank\">https://dx.doi.org/10.1029/2018PA003503</a>","AutID":129308,"MonDate":null,"AnaDate":2019,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":295474,"RR":"<b>Arreguin-Rodriguez, G.J.; Thomas, E.; D'haenens, S.; Speijer, R.P.; Alegret, L.</b> (2018). Early Eocene deep-sea benthic foraminiferal faunas: recovery from the Paleocene Eocene Thermal Maximum extinction in a greenhouse world. <i>PLoS One 13(2)</i>: e0193167. <a href=\"https://dx.doi.org/10.1371/journal.pone.0193167\" target=\"_blank\">https://dx.doi.org/10.1371/journal.pone.0193167</a>","AutID":329743,"MonDate":null,"AnaDate":2018,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":285445,"RR":"<b>Bornemann, A.; D'haenens, S.; Norris, R.D.; Speijer, R.P.</b> (2016). The demise of the early Eocene greenhouse - Decoupled deep and surface water cooling in the eastern North Atlantic. <i>Global Planet. Change 145</i>: 130-140. <a href=\"https://dx.doi.org/10.1016/j.gloplacha.2016.08.010\" target=\"_blank\">https://dx.doi.org/10.1016/j.gloplacha.2016.08.010</a>","AutID":154196,"MonDate":null,"AnaDate":2016,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":257068,"RR":"<b>Deprez, A.; Tesseur, S.; Stassen, P.; D'haenens, S.; Steurbaut, E.; King, C.; Claeys, P.; Speijer, R.P.</b> (2015). Early Eocene environmental development in the northern Peri-Tethys (Aktulagay, Kazakhstan) based on benthic foraminiferal assemblages and stable isotopes (O, C). <i>Mar. Micropaleontol. 115</i>: 59-71. <a href=\"https://dx.doi.org/10.1016/j.marmicro.2014.11.003\" target=\"_blank\">https://dx.doi.org/10.1016/j.marmicro.2014.11.003</a>","AutID":154196,"MonDate":null,"AnaDate":2015,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":247010,"RR":"<b>Bornemann, A; Norris, D; Lyman, A; D'haenens, S.; Groeneveld, J; Rohl, U; Farley, A; Speijer, R.P.</b> (2014). Persistent environmental change after the Paleocene-Eocene Thermal Maximum in the eastern North Atlantic. <i>Earth Planet. Sci. Lett. 394</i>: 70-81. <a href=\"http://dx.doi.org/10.1016/j.epsl.2014.03.017\" target=\"_blank\">dx.doi.org/10.1016/j.epsl.2014.03.017</a>","AutID":154196,"MonDate":null,"AnaDate":2014,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":247011,"RR":"<b>D'haenens, S.; Bornemann, A; Claeys, P.; Rohl, U; Steurbaut, E.; Speijer, R.P.</b> (2014). A transient deep-sea circulation switch during Eocene Thermal Maximum 2. <i>Paleoceanography 29(5)</i>: 370-388. <a href=\"http://dx.doi.org/10.1002/2013PA002567\" target=\"_blank\">dx.doi.org/10.1002/2013PA002567</a>","AutID":154196,"MonDate":null,"AnaDate":2014,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":220186,"RR":"<b>D'haenens, S.; Bornemann, A.; Stassen, P.; Speijer, R.P.</b> (2012). Multiple early Eocene benthic foraminiferal assemblage and d<sup>13</sup>C fluctuations at DSDP Site 401 (Bay of Biscay — NE Atlantic). <i>Mar. Micropaleontol. 88-89</i>: 15-35. <a href=\"http://dx.doi.org/10.1016/j.marmicro.2012.02.006\" target=\"_blank\">http://dx.doi.org/10.1016/j.marmicro.2012.02.006</a>","AutID":154196,"MonDate":null,"AnaDate":2012,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":220286,"RR":"<b>D'haenens, S.; Bornemann, A.; Roose, K.; Claeys, P.; Speijer, R.P.</b> (2012). Stable isotope paleoecology (d<sup>13</sup>C and d<sup>18</sup>O) of early Eocene <i>Zeauvigerina aegyptiaca</i> from the North Atlantic (DSDP Site 401). <i>Austrian J. Earth Sci. 105(1)</i>: 179-188","AutID":162060,"MonDate":null,"AnaDate":2012,"PeerRev":1,"outputType":"1_A1","OpenAcc":1}],"Abstr":[{"BRefID":365114,"RR":"<b>De Vleeschouwer, D.; Penman, D.; D'haenens, S.; Wu, F.; Westerhold, T.; Vahlenkamp, M.; Cappelli, C.; Agnini, C.; Kordesch, W.; King, D.; van der Ploeg, R.; Pälike, H.; Kirtland-Turner, S.; Wilson, P.; Norris, R.D.; Zachos, J.C.; Bohaty, S.; Hull, P.</b> (2023). North Atlantic drift sediments constrain Eocene tidal dissipation and the evolution of the Earth-Moon system, <b><i>in</i></b>: <i>EGU General Assembly 2023. Vienna, Austria & Online, 23–28 April 2023.</i> pp. EGU23-12739. <a href=\"https://dx.doi.org/10.5194/egusphere-egu23-12739\" target=\"_blank\">https://dx.doi.org/10.5194/egusphere-egu23-12739</a>","AutID":533549,"MonDate":null,"AnaDate":2023,"PeerRev":0,"outputType":"6_Abstr","OpenAcc":1},{"BRefID":324828,"RR":"<b>D'haenens, S.; Bornemann, A.; Speijer, R.P.</b> (2012). The PETM and ETM2: reset buttons for benthic ecosystem evolution?, <b><i>in</i></b>: Devleeschouwer, X. <i>et al.</i> <i>Abstract Book. 4<sup>th</sup> International Geologica Belgica Meeting 2012, September 11-14, Brussels, Belgium.</i> pp. 40","AutID":154196,"MonDate":null,"AnaDate":2012,"PeerRev":0,"outputType":"6_Abstr","OpenAcc":1},{"BRefID":202773,"RR":"<b>D'haenens, S.; Bornemann, A.; Stassen, P.; Speijer, R.P.</b> (2011). 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