000077054 001__ 77054
000077054 005__ 20221020131654.0
000077054 0247_ $$2doi$$a10.4202/app.00520.2018
000077054 0248_ $$2sideral$$a109623
000077054 037__ $$aART-2018-109623
000077054 041__ $$aeng
000077054 100__ $$aZamora, S.
000077054 245__ $$aEnvironmental distribution of post-Palaeozoic crinoids from the Iberian and south-Pyrenean basins, NE Spain
000077054 260__ $$c2018
000077054 5060_ $$aAccess copy available to the general public$$fUnrestricted
000077054 5203_ $$aPost-Palaeozoic crinoids from northeast Spain ranging from the Ladinian (Middle Triassic) to the Ilerdian (lower Ypresian, early Eocene) are documented. Here we provide the first attempt to reconstruct the environmental distribution of these crinoids based on relatively complete material (mostly cups). Triassic forms are dominated by encrinids from outer carbonate ramps. Late Jurassic crinoids are dominated by cyrtocrinids, comatulids, millericrinids, and isocrinids, occurring either on sponge mounds and meadows or on soft substrates within middle to outer carbonate ramps. Aptian (Early Cretaceous) forms include nearly complete isocrinids which are found in extremely shallow environments represented by bioclastic carbonates and interspersed oyster-rich layers. Other Aptian occurrences come from more distal and deep environments and are composed solely of comatulids. Albian forms are dominated by cyrtocrinids and isocrinids associated with coral reefs. Late Cretaceous and Eocene crinoids include mostly bourgueticrinids (Comatulida) that are found either in outer ramp facies or associated with mid-ramp reef complexes. The later corresponds to one of the shallowest occurrence of bourgueticrinids in the Cenozoic. The palaeoecological data for fossil crinoids of northeast Spain contributes to reconstructing the history of the bathymetric distribution of articulate crinoids, supporting the idea that stalked crinoids were able to inhabit a wide range of shallow marine environments in the late Mesozoic and early Cenozoic.
000077054 536__ $$9info:eu-repo/grantAgreement/ES/DGA/E18-17R$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2015-64422-P$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2017-87631
000077054 540__ $$9info:eu-repo/semantics/openAccess$$aby$$uhttp://creativecommons.org/licenses/by/3.0/es/
000077054 590__ $$a1.639$$b2018
000077054 591__ $$aPALEONTOLOGY$$b17 / 56 = 0.304$$c2018$$dQ2$$eT1
000077054 592__ $$a0.764$$b2018
000077054 593__ $$aPaleontology$$c2018$$dQ1
000077054 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000077054 700__ $$0(orcid)0000-0002-2430-7424$$aAurell, M.$$uUniversidad de Zaragoza
000077054 700__ $$aVeitch, M.
000077054 700__ $$aSaulsbury, J.
000077054 700__ $$aLópez-Horgue, M.A.
000077054 700__ $$0(orcid)0000-0002-9532-6972$$aFerratges, F.A.$$uUniversidad de Zaragoza
000077054 700__ $$0(orcid)0000-0003-0063-8752$$aArz, J.A.$$uUniversidad de Zaragoza
000077054 700__ $$aBaumiller, T.K.
000077054 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000077054 7102_ $$12000$$2280$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Estratigrafía
000077054 773__ $$g63, 4 (2018), 779-794$$pActa Palaeontol. Pol.$$tActa Palaeontologica Polonica$$x0567-7920
000077054 8564_ $$s649134$$uhttps://zaguan.unizar.es/record/77054/files/texto_completo.pdf$$yVersión publicada
000077054 8564_ $$s104036$$uhttps://zaguan.unizar.es/record/77054/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000077054 909CO $$ooai:zaguan.unizar.es:77054$$particulos$$pdriver
000077054 951__ $$a2022-10-20-13:05:50
000077054 980__ $$aARTICLE