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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Online Access: | http://hdl.handle.net/2122/12437 https://doi.org/10.1016/j.revmic.2018.05.001 |
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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 |
container_start_page |
81 |
op_container_end_page |
96 |
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1766271574364651520 |