Wilkes Land Late Pleistocene diatom age model: From bio-events to quantitative biostratigraphy

A new method merges conventional and quantitative biostratigraphic approaches, supported by magnetic polarity data, to develop a chronological framework for sediment core MD03-2595 retrieved on the continental rise off Wilkes Land, East Antarctica before proceeding to paleoceanographic and paleoclim...

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Published in:Revue de Micropaléontologie
Main Authors: Tolotti, R., Bárcena, M.A., Macrì, Patrizia, Caburlotto, A., Bonci, Maria Cristina, De Santis, Laura, Donda, Federica, Corradi, Nicola, Crosta, X.
Other Authors: #PLACEHOLDER_PARENT_METADATA_VALUE#, Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:http://hdl.handle.net/2122/12437
https://doi.org/10.1016/j.revmic.2018.05.001
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spelling ftingv:oai:www.earth-prints.org:2122/12437 2023-05-15T14:01:37+02:00 Wilkes Land Late Pleistocene diatom age model: From bio-events to quantitative biostratigraphy Tolotti, R. Bárcena, M.A. Macrì, Patrizia Caburlotto, A. Bonci, Maria Cristina De Santis, Laura Donda, Federica Corradi, Nicola Crosta, X. #PLACEHOLDER_PARENT_METADATA_VALUE# Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia 2018 http://hdl.handle.net/2122/12437 https://doi.org/10.1016/j.revmic.2018.05.001 en eng Revue de Micropaléontologie /61 (2018) http://hdl.handle.net/2122/12437 doi:10.1016/j.revmic.2018.05.001 restricted Late Pleistocene Quantitative Biostratigraphy Matuyama-Brunhes Transition Mid Pleistocene Transition 04.04. Geology article 2018 ftingv https://doi.org/10.1016/j.revmic.2018.05.001 2022-07-29T06:07:44Z A new method merges conventional and quantitative biostratigraphic approaches, supported by magnetic polarity data, to develop a chronological framework for sediment core MD03-2595 retrieved on the continental rise off Wilkes Land, East Antarctica before proceeding to paleoceanographic and paleoclimatic analysis. This combined method helped to identify climatic cycles, highlight stratigraphic discontinuities and reworking, and assess regional sedimentological and diatom biostratigraphic evolution. Core MD03-2595 spans the last 0.8 Ma, from the Mid Pleistocene Transition (MPT) to the Early Holocene. A hiatus including Marine Isotope Stages (MIS) 19, 18 and 17 was identified, and a decreasing trend in sediment accumulation rates from MIS 16 to the Holocene was observed. This quantitative diatom biostratigraphic dataset, placed in its own sedimentological and paleomagnetic context, provides new information regarding the paleobiogeographic distribution and ecological responses of biostratigraphically significant diatom species, such as Thalassiosira elliptipora and T. fasciculata, for the Matuyama–Brunhes (M–B) transition, and Actinocyclus ingens, Hemidiscus karstenii and Rouxia spp. for the middle and late Pleistocene diatom biozonation. Published 81-96 1A. Geomagnetismo e Paleomagnetismo N/A or not JCR Article in Journal/Newspaper Antarc* Antarctica East Antarctica Wilkes Land Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) East Antarctica Wilkes Land ENVELOPE(120.000,120.000,-69.000,-69.000) Revue de Micropaléontologie 61 2 81 96
institution Open Polar
collection Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia)
op_collection_id ftingv
language English
topic Late Pleistocene
Quantitative Biostratigraphy
Matuyama-Brunhes Transition
Mid Pleistocene Transition
04.04. Geology
spellingShingle Late Pleistocene
Quantitative Biostratigraphy
Matuyama-Brunhes Transition
Mid Pleistocene Transition
04.04. Geology
Tolotti, R.
Bárcena, M.A.
Macrì, Patrizia
Caburlotto, A.
Bonci, Maria Cristina
De Santis, Laura
Donda, Federica
Corradi, Nicola
Crosta, X.
Wilkes Land Late Pleistocene diatom age model: From bio-events to quantitative biostratigraphy
topic_facet Late Pleistocene
Quantitative Biostratigraphy
Matuyama-Brunhes Transition
Mid Pleistocene Transition
04.04. Geology
description A new method merges conventional and quantitative biostratigraphic approaches, supported by magnetic polarity data, to develop a chronological framework for sediment core MD03-2595 retrieved on the continental rise off Wilkes Land, East Antarctica before proceeding to paleoceanographic and paleoclimatic analysis. This combined method helped to identify climatic cycles, highlight stratigraphic discontinuities and reworking, and assess regional sedimentological and diatom biostratigraphic evolution. Core MD03-2595 spans the last 0.8 Ma, from the Mid Pleistocene Transition (MPT) to the Early Holocene. A hiatus including Marine Isotope Stages (MIS) 19, 18 and 17 was identified, and a decreasing trend in sediment accumulation rates from MIS 16 to the Holocene was observed. This quantitative diatom biostratigraphic dataset, placed in its own sedimentological and paleomagnetic context, provides new information regarding the paleobiogeographic distribution and ecological responses of biostratigraphically significant diatom species, such as Thalassiosira elliptipora and T. fasciculata, for the Matuyama–Brunhes (M–B) transition, and Actinocyclus ingens, Hemidiscus karstenii and Rouxia spp. for the middle and late Pleistocene diatom biozonation. Published 81-96 1A. Geomagnetismo e Paleomagnetismo N/A or not JCR
author2 #PLACEHOLDER_PARENT_METADATA_VALUE#
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia
format Article in Journal/Newspaper
author Tolotti, R.
Bárcena, M.A.
Macrì, Patrizia
Caburlotto, A.
Bonci, Maria Cristina
De Santis, Laura
Donda, Federica
Corradi, Nicola
Crosta, X.
author_facet Tolotti, R.
Bárcena, M.A.
Macrì, Patrizia
Caburlotto, A.
Bonci, Maria Cristina
De Santis, Laura
Donda, Federica
Corradi, Nicola
Crosta, X.
author_sort Tolotti, R.
title Wilkes Land Late Pleistocene diatom age model: From bio-events to quantitative biostratigraphy
title_short Wilkes Land Late Pleistocene diatom age model: From bio-events to quantitative biostratigraphy
title_full Wilkes Land Late Pleistocene diatom age model: From bio-events to quantitative biostratigraphy
title_fullStr Wilkes Land Late Pleistocene diatom age model: From bio-events to quantitative biostratigraphy
title_full_unstemmed Wilkes Land Late Pleistocene diatom age model: From bio-events to quantitative biostratigraphy
title_sort wilkes land late pleistocene diatom age model: from bio-events to quantitative biostratigraphy
publishDate 2018
url http://hdl.handle.net/2122/12437
https://doi.org/10.1016/j.revmic.2018.05.001
long_lat ENVELOPE(120.000,120.000,-69.000,-69.000)
geographic East Antarctica
Wilkes Land
geographic_facet East Antarctica
Wilkes Land
genre Antarc*
Antarctica
East Antarctica
Wilkes Land
genre_facet Antarc*
Antarctica
East Antarctica
Wilkes Land
op_relation Revue de Micropaléontologie
/61 (2018)
http://hdl.handle.net/2122/12437
doi:10.1016/j.revmic.2018.05.001
op_rights restricted
op_doi https://doi.org/10.1016/j.revmic.2018.05.001
container_title Revue de Micropaléontologie
container_volume 61
container_issue 2
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