000032736 001__ 32736
000032736 005__ 20240109134254.0
000032736 0247_ $$2doi$$a10.1016/j.earscirev.2014.11.008
000032736 0248_ $$2sideral$$a89288
000032736 037__ $$aART-2015-89288
000032736 041__ $$aeng
000032736 100__ $$0(orcid)0000-0001-5660-1428$$aMolina, E.$$uUniversidad de Zaragoza
000032736 245__ $$aEvidence and causes of the main extinction events in the Paleogene based on extinction and survival patterns of foraminifera
000032736 260__ $$c2015
000032736 5060_ $$aAccess copy available to the general public$$fUnrestricted
000032736 5203_ $$aWe review the four main extinction events in the Paleogene, from the Cretaceous/Paleogene boundary to the Eocene/Oligocene boundary, integrating the results obtained from a study of foraminiferal assemblages with other paleontological and geological data. Different survival strategies followed by the species are described and the duration of the phases of extinction, survival, and recovery is estimated. The models and patterns of extinction of the foraminifera are highlighted. We present a range of evidence and paleo-environmental factors and analyze the possible causes of extinction. A new terminology for mass extinction events is proposed: sudden mass extinction would have happened virtually instantaneously and the process would have taken a few years or decades (Cretaceous/Paleogene boundary). Rapid mass extinction is defined as that which occurred in relatively short events, around 100 kyr (Paleocene/Eocene and Eocene/Oligocene boundaries). Slow mass extinctions are suggested to have lasted around 1 Myr (Bartonian/Priabonian transition) and may even have lasted for several million years.
000032736 536__ $$9info:eu-repo/grantAgreement/ES/MINECO/CGL2011-229121$$9info:eu-repo/grantAgreement/ES/DGA/E05$$9info:eu-repo/grantAgreement/ES/MINECO-FEDER/CGL2011-23077
000032736 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000032736 590__ $$a6.991$$b2015
000032736 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b5 / 183 = 0.027$$c2015$$dQ1$$eT1
000032736 592__ $$a3.692$$b2015
000032736 593__ $$aEarth and Planetary Sciences (miscellaneous)$$c2015$$dQ1
000032736 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000032736 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000032736 773__ $$g140 (2015), 166-181$$pEarth-sci. rev.$$tEarth-Science Reviews$$x0012-8252
000032736 8564_ $$s3423286$$uhttps://zaguan.unizar.es/record/32736/files/texto_completo.pdf$$yPostprint
000032736 8564_ $$s105960$$uhttps://zaguan.unizar.es/record/32736/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint
000032736 909CO $$ooai:zaguan.unizar.es:32736$$particulos$$pdriver
000032736 951__ $$a2024-01-09-13:32:11
000032736 980__ $$aARTICLE