Magnetostratigraphy and Pliocene-Pleistocene Boundary in Italy

Abstract Analysis of some sedimentary series near Rome and comparison with other series in northern and southern Italy give evidence that Arctica islandica , considered a marker species for the beginning of the Pleistocene, appears during the Réunion paleomagnetic event (about 2 my ago). A period of...

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Published in:Quaternary Research
Main Authors: Arias, Claudio, Azzaroli, Augusto, Bigazzi, Giulio, Bonadonna, Francescopaolo
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1980
Subjects:
Online Access:http://dx.doi.org/10.1016/0033-5894(80)90082-4
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spelling crcambridgeupr:10.1016/0033-5894(80)90082-4 2024-09-09T19:28:48+00:00 Magnetostratigraphy and Pliocene-Pleistocene Boundary in Italy Arias, Claudio Azzaroli, Augusto Bigazzi, Giulio Bonadonna, Francescopaolo 1980 http://dx.doi.org/10.1016/0033-5894(80)90082-4 http://api.elsevier.com/content/article/PII:0033589480900824?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589480900824?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400015258 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 13, issue 1, page 65-74 ISSN 0033-5894 1096-0287 journal-article 1980 crcambridgeupr https://doi.org/10.1016/0033-5894(80)90082-4 2024-07-24T04:03:48Z Abstract Analysis of some sedimentary series near Rome and comparison with other series in northern and southern Italy give evidence that Arctica islandica , considered a marker species for the beginning of the Pleistocene, appears during the Réunion paleomagnetic event (about 2 my ago). A period of erosion, called the Aullan erosional phase, is evident in the lower part of the late Villafranchian (= early Pleistocene, Olivola faunal unit). Article in Journal/Newspaper Arctica islandica Cambridge University Press Quaternary Research 13 1 65 74
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Analysis of some sedimentary series near Rome and comparison with other series in northern and southern Italy give evidence that Arctica islandica , considered a marker species for the beginning of the Pleistocene, appears during the Réunion paleomagnetic event (about 2 my ago). A period of erosion, called the Aullan erosional phase, is evident in the lower part of the late Villafranchian (= early Pleistocene, Olivola faunal unit).
format Article in Journal/Newspaper
author Arias, Claudio
Azzaroli, Augusto
Bigazzi, Giulio
Bonadonna, Francescopaolo
spellingShingle Arias, Claudio
Azzaroli, Augusto
Bigazzi, Giulio
Bonadonna, Francescopaolo
Magnetostratigraphy and Pliocene-Pleistocene Boundary in Italy
author_facet Arias, Claudio
Azzaroli, Augusto
Bigazzi, Giulio
Bonadonna, Francescopaolo
author_sort Arias, Claudio
title Magnetostratigraphy and Pliocene-Pleistocene Boundary in Italy
title_short Magnetostratigraphy and Pliocene-Pleistocene Boundary in Italy
title_full Magnetostratigraphy and Pliocene-Pleistocene Boundary in Italy
title_fullStr Magnetostratigraphy and Pliocene-Pleistocene Boundary in Italy
title_full_unstemmed Magnetostratigraphy and Pliocene-Pleistocene Boundary in Italy
title_sort magnetostratigraphy and pliocene-pleistocene boundary in italy
publisher Cambridge University Press (CUP)
publishDate 1980
url http://dx.doi.org/10.1016/0033-5894(80)90082-4
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genre Arctica islandica
genre_facet Arctica islandica
op_source Quaternary Research
volume 13, issue 1, page 65-74
ISSN 0033-5894 1096-0287
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1016/0033-5894(80)90082-4
container_title Quaternary Research
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op_container_end_page 74
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