{"refrec":{"BRefID":220187,"RR":"<b>Stassen, P.; Thomas, E.; Speijer, R.P.</b> (2012). Restructuring outer neritic foraminiferal assemblages in the aftermath of the Paleocene-Eocene thermal maximum. <i>J. Micropalaeontol. 31(1)</i>: 89-93. <a href=\"https://dx.doi.org/10.1144/0262-821X11-026\" target=\"_blank\">https://dx.doi.org/10.1144/0262-821X11-026</a>","BEntID":211919,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>J. Micropalaeontol. 31(1)</i>: 89-93. <a href=\"https://dx.doi.org/10.1144/0262-821X11-026\" target=\"_blank\">https://dx.doi.org/10.1144/0262-821X11-026</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Stassen, P.; Thomas, E.; Speijer, R.P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Stassen, P. <i>et al.</i>","Englishabstract":"Deep-sea benthic foraminiferal faunas underwent severe extinction during the Paleocene–Eocene thermal maximum (PETM), but less is known about neritic environments. 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