000097418 001__ 97418
000097418 005__ 20230519145459.0
000097418 0247_ $$2doi$$a10.1016/j.gloplacha.2020.103372
000097418 0248_ $$2sideral$$a121797
000097418 037__ $$aART-2021-121797
000097418 041__ $$aeng
000097418 100__ $$0(orcid)0000-0002-8801-9544$$aAlegret, L.$$uUniversidad de Zaragoza
000097418 245__ $$aTurnover and stability in the deep sea: Benthic foraminifera as tracers of Paleogene global change
000097418 260__ $$c2021
000097418 5060_ $$aAccess copy available to the general public$$fUnrestricted
000097418 5203_ $$aBenthic foraminifera are the most common meiofaunal unicellular deep-sea biota, forming skeletons used as proxies for past climate change. We aim to increase understanding of past non-analog oceans and ecosystems by evaluating deep-sea benthic foraminiferal responses to global environmental changes over latest Cretaceous through Oligocene times (67–23 million years ago). Earth suffered an asteroid impact at the end of the Cretaceous (~instantaneous; 66 Ma), episodes of rapid global warming during the Paleocene-Eocene Thermal Maximum (PETM; ~56 Ma) and other hyperthermals (millennial timescales), followed by gradual, but punctuated cooling (timescales of hundred thousands of years) from a world without polar ice sheets to a world with a large Antarctic ice sheet. Here we present the first compilation of quantitative data on deep-sea foraminifera at sites in all the world''s oceans, aiming to build a first unique, uniform database that allows comparison of deep-sea faunal turnover across the uppermost Cretaceous through Paleogene. We document variability in space and time of benthic foraminiferal diversity: lack of extinction at the asteroid impact even though other marine and terrestrial groups suffered mass extinction; major extinction at the PETM followed by recovery and diversification; and gradual but fundamental turnover during gradual cooling and increase in polar ice volume (possibly linked to changes in the oceanic carbon cycle). High latitude cooling from ~45 Ma on, i.e., after the end of the Early Eocene Climate Optimum (53.2–49.2 Ma), may have made the middle Eocene a critical period of several millions of years of faunal turnover and establishment of latitudinal diversity gradients. This compilation thus illuminates the penetration of global change at very different rates into the largest and one of the most stable habitats on Earth, the deep sea with its highly diverse biota.
000097418 536__ $$9info:eu-repo/grantAgreement/ES/MINECO-FEDER/PID2019-105537RB-I00$$9info:eu-repo/grantAgreement/ES/MINECO-FEDER/CGL2017-84693-R$$9info:eu-repo/grantAgreement/ES/DGA/E33-17R
000097418 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000097418 590__ $$a4.956$$b2021
000097418 592__ $$a1.371$$b2021
000097418 594__ $$a7.9$$b2021
000097418 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b36 / 203 = 0.177$$c2021$$dQ1$$eT1
000097418 593__ $$aOceanography$$c2021$$dQ1
000097418 591__ $$aGEOGRAPHY, PHYSICAL$$b8 / 50 = 0.16$$c2021$$dQ1$$eT1
000097418 593__ $$aGlobal and Planetary Change$$c2021$$dQ1
000097418 655_4 $$ainfo:eu-repo/semantics/review$$vinfo:eu-repo/semantics/publishedVersion
000097418 700__ $$aArreguín-Rodríguez, G.J.
000097418 700__ $$0(orcid)0000-0002-4964-6035$$aTrasviña-Moreno, C.A.
000097418 700__ $$aThomas, E.
000097418 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000097418 773__ $$g196 (2021), 103372 [17 pp]$$pGlob. planet. change$$tGLOBAL AND PLANETARY CHANGE$$x0921-8181
000097418 8564_ $$s3355890$$uhttps://zaguan.unizar.es/record/97418/files/texto_completo.pdf$$yVersión publicada
000097418 8564_ $$s452939$$uhttps://zaguan.unizar.es/record/97418/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000097418 909CO $$ooai:zaguan.unizar.es:97418$$particulos$$pdriver
000097418 951__ $$a2023-05-18-14:55:03
000097418 980__ $$aARTICLE