000070783 001__ 70783
000070783 005__ 20200221144237.0
000070783 0247_ $$2doi$$a10.1344/GeologicaActa2016.14.2.2
000070783 0248_ $$2sideral$$a105989
000070783 037__ $$aART-2016-105989
000070783 041__ $$aeng
000070783 100__ $$aMoreno-Dominguez, R.
000070783 245__ $$aFirst record of the mangrove palm Nypa from the northeastern Ebro Basin, Spain: with taphonomic criteria to evaluate the drifting duration
000070783 260__ $$c2016
000070783 5060_ $$aAccess copy available to the general public$$fUnrestricted
000070783 5203_ $$aFossil fruits pertaining to the mangrove palm genus Nypa STECK, (Arecaceae, Arecales) were collected from a new plant-bearing assemblage in the Arguis Formation (Fm.), northeastern Ebro Basin (Arguis, Huesca Province, Spain). This formation is Bartonian to early Priabonian in age and comprises pro-delta and carbonate platform deposits. The new assemblage consists of nine specimens of fossil Nypa fruits and one monocotyledon leaf fragment. Over half of these fossil fruits are nearly-complete (i.e. with preserved mesocarps) while the other represent endocarps. From the point of view of morphology and size they resemble other European records of this genus. The type of remain preserved (fruits or endocarps), presence of abrasion, Teredo borings and sedimentary facies provide criteria to infer contrasting lengths of transport (drifting). However, they indicate in all cases that these fossil fruits were afloat in seawater for a considerable time. The discovery of Nypa fruits suggests a tropical-subtropical climate in the area, as well as the presence of a coastal environment and littoral forests during deposition. This interpretation corroborates previous findings from the nearby Eocene outcrops of the Catalan Central Depression (Eastern Pyrenees range).
000070783 536__ $$9info:eu-repo/grantAgreement/ES/MINECO/CGL2015-69805-P
000070783 540__ $$9info:eu-repo/semantics/openAccess$$aby-sa$$uhttp://creativecommons.org/licenses/by-sa/3.0/es/
000070783 590__ $$a0.86$$b2016
000070783 591__ $$aGEOLOGY$$b27 / 47 = 0.574$$c2016$$dQ3$$eT2
000070783 592__ $$a0.54$$b2016
000070783 593__ $$aGeology$$c2016$$dQ2
000070783 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000070783 700__ $$aCascales-Minana, B.
000070783 700__ $$0(orcid)0000-0002-0903-3605$$aFerrer, J.$$uUniversidad de Zaragoza
000070783 700__ $$aDiez, J.B.
000070783 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000070783 773__ $$g14, 2 (2016), 101-111$$pGeol. acta$$tGEOLOGICA ACTA$$x1695-6133
000070783 8564_ $$s1203506$$uhttps://zaguan.unizar.es/record/70783/files/texto_completo.pdf$$yVersión publicada
000070783 8564_ $$s94709$$uhttps://zaguan.unizar.es/record/70783/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000070783 909CO $$ooai:zaguan.unizar.es:70783$$particulos$$pdriver
000070783 951__ $$a2020-02-21-13:21:09
000070783 980__ $$aARTICLE