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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Cambridge University Press (CUP)
1980
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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 |
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Open Polar |
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Cambridge University Press |
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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 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 |
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 |
container_volume |
13 |
container_issue |
1 |
container_start_page |
65 |
op_container_end_page |
74 |
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1809898100676886528 |