dc.contributor.author
Alba, David M.
dc.contributor.author
Casanovas i Vilar, Isaac
dc.contributor.author
Garcés Crespo, Miguel
dc.contributor.author
Robles, Josep Maria
dc.date.issued
2016-12-12T07:04:30Z
dc.date.issued
2018-01-31T23:01:26Z
dc.date.issued
2016-12-12T07:04:35Z
dc.identifier
https://hdl.handle.net/2445/104582
dc.description.abstract
More than ten years of paleontological fieldwork during the enlargement of the Can Mata Landfill (Abocador de Can Mata [ACM]), in els Hostalets de Pierola (Vallès-Penedès Basin, NE Iberian Peninsula) led to the recovery of >60,000 Miocene vertebrate remains. The huge sampling effort (due to continuous surveillance of heavy machinery digging activity, coupled with manual excavation and screen-washing of sediments) enabled generally rare faunal elements such as pliopithecoid and hominoid primates to be found. Thanks to detailed litho-, bio- and magnetostratigraphic controls, accurate dating is possible for all the recovered primate remains from 19 of the 235 localities defined along the 234 m-thick composite stratigraphic sequence of the ACM. Here we report updated estimated (interpolated) ages for these paleontological localities and review the timing of the primate succession in this area. Our results indicate that the whole ACM sequence is late Aragonian in age (MN6 and MN7+8) and includes seven magnetozones that are correlated to subchrons C5Ar.1r to C5r.2r (ca. 12.6 to 11.4 Ma). Great apes (dryopithecines) are first recorded at 12.4-12.3 Ma, but most of the finds (Anoiapithecus, Pierolapithecus and Dryopithecus) cluster between 12.0 and 11.9 Ma, followed by some indeterminate dryopithecine remains between 11.7 and 11.6 Ma. Pliopithecoids first appear at 12.1 Ma, being subsequently represented by Pliopithecus between 11.9 and 11.7 Ma. The small-bodied hominoid Pliobates is the youngest ACM primate, with an estimated age of 11.6 Ma. Although these primates probably overlapped in time, their co-occurrence is recorded only twice, at 11.9 Ma (a dryopithecine with Pliopithecus) and at 11.6 Ma (a dryopithecine with Pliobates). The rare co-occurrence between great apes and small-bodied catarrhines might be attributable to sampling biases and/or to presumed diverging ecological preferences of these groups. In the future, more detailed analyses of the fauna recovered from the long and densely-sampled ACM sequence will hopefully throw new light on this long-standing, unresolved question.
dc.format
application/pdf
dc.format
application/pdf
dc.publisher
Elsevier B.V.
dc.relation
Versió postprint del document publicat a: https://doi.org/10.1016/j.jhevol.2016.09.012
dc.relation
Journal of Human Evolution, 2017, vol. 102, p. 12-20
dc.relation
https://doi.org/10.1016/j.jhevol.2016.09.012
dc.rights
cc-by-nc-nd (c) Elsevier B.V., 2017
dc.rights
http://creativecommons.org/licenses/by-nc-nd/3.0/es
dc.rights
info:eu-repo/semantics/openAccess
dc.source
Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)
dc.subject
Hostalets de Pierola (Catalunya)
dc.subject
Primats fòssils
dc.subject
Paleomagnetisme
dc.subject
Magnetoestratigrafia
dc.subject
Hostalets de Pierola (Catalonia)
dc.subject
Primates, Fossil
dc.subject
Paleomagnetism
dc.subject
Magnetostratigraphy
dc.title
Ten years in the dump: An updated review of the Miocene primate-bearing localities from Abocador de Can Mata (NE Iberian Peninsula)
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/acceptedVersion