000119653 001__ 119653
000119653 005__ 20230519145458.0
000119653 0247_ $$2doi$$a10.1038/s41598-021-93261-1
000119653 0248_ $$2sideral$$a126129
000119653 037__ $$aART-2021-126129
000119653 041__ $$aeng
000119653 100__ $$aLuzón C.
000119653 245__ $$aTaphonomic and spatial analyses from the Early Pleistocene site of Venta Micena 4 (Orce, Guadix-Baza Basin, southern Spain)
000119653 260__ $$c2021
000119653 5060_ $$aAccess copy available to the general public$$fUnrestricted
000119653 5203_ $$aVenta Micena is an area containing several palaeontological sites marking the beginning of the Calabrian stage (Early Pleistocene). The richness of the fossil accumulation including species of Asian, African and European origin, makes Venta Micena a key site for the the palaeoecological and palaeoenvironmental study of southern Europe during the Early Pleistocene. Thus, research has been focused on Venta Micena 3, which was originally interpreted as a single palaeosurface associated with a marshy context, in which most of the fauna was accumulated by Pachycrocuta brevirostris. Recent excavations have unearthed a new site, Venta Micena 4, located in the same stratigraphic unit (Unit C) and in close proximity to Venta Micena 3. Here we show the first analyses regarding the taphonomic and spatial nature of this new site, defining two stratigraphic boundaries corresponding to two different depositional events. Furthermore, the taphonomic analyses of fossil remains seem to indicate a different accumulative agent than Pachycrocuta, thus adding more complexity to the palaeobiological interpretation of the Venta Micena area. These results contribute to the discussion of traditional interpretations made from Venta Micena 3. © 2021, The Author(s).
000119653 540__ $$9info:eu-repo/semantics/openAccess$$aby$$uhttp://creativecommons.org/licenses/by/3.0/es/
000119653 590__ $$a4.997$$b2021
000119653 591__ $$aMULTIDISCIPLINARY SCIENCES$$b19 / 74 = 0.257$$c2021$$dQ2$$eT1
000119653 592__ $$a1.005$$b2021
000119653 593__ $$aMultidisciplinary$$c2021$$dQ1
000119653 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000119653 700__ $$aYravedra J.
000119653 700__ $$aCourtenay L.A.
000119653 700__ $$aSaarinen J.
000119653 700__ $$aBlain H.-A.
000119653 700__ $$0(orcid)0000-0001-6138-7227$$aDe Miguel D.$$uUniversidad de Zaragoza
000119653 700__ $$aViranta S.
000119653 700__ $$0(orcid)0000-0003-2487-547X$$aAzanza B.$$uUniversidad de Zaragoza
000119653 700__ $$aRodríguez-Alba J.J.
000119653 700__ $$aHerranz-Rodrigo D.
000119653 700__ $$aSerrano-Ramos A.
000119653 700__ $$aSolano J.A.
000119653 700__ $$aOms O.
000119653 700__ $$aAgustí J.
000119653 700__ $$aFortelius M.
000119653 700__ $$aJiménez-Arenas J.M.
000119653 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000119653 773__ $$g11, 1 (2021), 13977$$pSci. rep. (Nat. Publ. Group)$$tScientific reports (Nature Publishing Group)$$x2045-2322
000119653 8564_ $$s3034533$$uhttps://zaguan.unizar.es/record/119653/files/texto_completo.pdf$$yVersión publicada
000119653 8564_ $$s2326041$$uhttps://zaguan.unizar.es/record/119653/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000119653 909CO $$ooai:zaguan.unizar.es:119653$$particulos$$pdriver
000119653 951__ $$a2023-05-18-14:53:45
000119653 980__ $$aARTICLE