{"refrec":{"BRefID":261071,"RR":"<b>Vellekoop, J.; Esmeray-Senlet, S.; Miller, K.G.; Browning, J.V.; Sluijs, A.; van de Schootbrugge, B.; Sinninghe Damsté, J.S.; Brinkhuis, H.</b> (2016). Evidence for Cretaceous-Paleogene boundary bolide “impact winter” conditions from New Jersey, USA. <i>Geology (Boulder Colo.) 44(8)</i>: 619-622. <a href=\"https://dx.doi.org/10.1130/G37961.1\" target=\"_blank\">https://dx.doi.org/10.1130/G37961.1</a>","BEntID":253089,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geology (Boulder Colo.) 44(8)</i>: 619-622. <a href=\"https://dx.doi.org/10.1130/G37961.1\" target=\"_blank\">https://dx.doi.org/10.1130/G37961.1</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vellekoop, J.; Esmeray-Senlet, S.; Miller, K.G.; Browning, J.V.; Sluijs, A.; van de Schootbrugge, B.; Sinninghe Damsté, J.S.; Brinkhuis, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vellekoop, J. <i>et al.</i>","Englishabstract":"Abrupt and short-lived “impact winter” conditions have commonly been implicated as the main mechanism leading to the mass extinction at the Cretaceous-Paleogene (K-Pg) boundary (ca. 66 Ma), marking the end of the reign of the non-avian dinosaurs. However, so far only limited evidence has been available for such a climatic perturbation. Here we perform high-resolution TEX86 organic paleothermometry on three shallow cores from the New Jersey paleoshelf, (northeastern USA) to assess the impact-provoked climatic perturbations immediately following the K-Pg impact and to place these short-term events in the context of long-term climate evolution. We provide evidence of impact-provoked, severe climatic cooling immediately following the K-Pg impact. This so-called “impact winter” occurred superimposed on a long-term cooling trend that followed a warm phase in the latest Cretaceous. 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