000048348 001__ 48348
000048348 005__ 20200221144142.0
000048348 0247_ $$2doi$$a10.3140/bull.geosci.1569
000048348 0248_ $$2sideral$$a94044
000048348 037__ $$aART-2016-94044
000048348 041__ $$aeng
000048348 100__ $$0(orcid)0000-0003-1536-3069$$aJiménez-Sánchez, A.$$uUniversidad de Zaragoza
000048348 245__ $$aNew bryozoans from the upper ordovician of morocco and their place in the temperate-to-cool water meditterranean province
000048348 260__ $$c2016
000048348 5060_ $$aAccess copy available to the general public$$fUnrestricted
000048348 5203_ $$aA new study of the Upper Ordovician bryozoans belonging to the families Aisenvergiidae, Amplexoporidae, Arthrostylidae, Enalloporidae, Halloporidae, Heterotrypidae, Mesotrypidae, Ptilodictyidae, Rhinidictyidae and Trematoporidae from the eastern Anti-Atlas of Morocco is presented here. These bryozoans come from the calcarenitic levels of the Khabt-el-Hajar Formation, upper Katian, where for the first time the orders Fenestrata and Cryptostomata are described in this formation. This fauna inhabited an upper offshore environment and represent high-energy deposits, typical of a shore face environment, as well as storm-induced deposits. A total of 15 species included in 13 genera, 10 of them only identified in the calcarenitic levels of the Khabt-el-Hajar Formation, and two incertae sedis taxa are described. A new species, Trematopora vesiculata, is defined. An update of the Upper Ordovician bryozoan presence/absence database, including the 22 genera described in total in the Khabt-el-Hajar Formation, has been carried out. The augmented database has been analysed with two multivariate statistical techniques: detrended correspondence analysis (DCA) and principal coordinate analysis (PCO), in order to assess the palaeogeographic affinity of this fauna, and the results show that Moroccan bryozoans, in spite of belonging to the fauna developed in the highest latitudes during the upper Katian, have a clear Mediterranean affinity.
000048348 536__ $$9info:eu-repo/grantAgreement/ES/DGA/E17$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2012-39471
000048348 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc$$uhttp://creativecommons.org/licenses/by-nc/3.0/es/
000048348 590__ $$a1.175$$b2016
000048348 591__ $$aPALEONTOLOGY$$b32 / 53 = 0.604$$c2016$$dQ3$$eT2
000048348 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b136 / 188 = 0.723$$c2016$$dQ3$$eT3
000048348 592__ $$a0.501$$b2016
000048348 593__ $$aEnvironmental Science (miscellaneous)$$c2016$$dQ2
000048348 593__ $$aEarth and Planetary Sciences (miscellaneous)$$c2016$$dQ2
000048348 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000048348 700__ $$aErnst, A.
000048348 700__ $$aVennin, E.
000048348 700__ $$0(orcid)0000-0002-7270-300X$$aVillas, E.$$uUniversidad de Zaragoza
000048348 7102_ $$12000$$2685$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Petrología y Geoquímica
000048348 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000048348 773__ $$g91, 1 (2016), 23-50$$pBULLETIN OF GEOSCIENCES$$tBULLETIN OF GEOSCIENCES$$x1214-1119
000048348 8564_ $$s8026911$$uhttps://zaguan.unizar.es/record/48348/files/texto_completo.pdf$$yVersión publicada
000048348 8564_ $$s110991$$uhttps://zaguan.unizar.es/record/48348/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000048348 909CO $$ooai:zaguan.unizar.es:48348$$particulos$$pdriver
000048348 951__ $$a2020-02-21-13:05:39
000048348 980__ $$aARTICLE