Frequency and dynamics of millennial-scale variability during Marine Isotope Stage 19: Insights from the Sulmona Basin (central Italy)
International audience Among past interglacial periods, Marine Isotope Stage (MIS) 19 is particularly interesting because its orbital geometry is very similar to that of the present interglacial. Here we present a high-resolution (sub-centennial) multiproxy record covering the ca. 790-770 ka interva...
Published in: | Quaternary Science Reviews |
---|---|
Main Authors: | , , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2019
|
Subjects: | |
Online Access: | https://hal.science/hal-03329520 https://hal.science/hal-03329520/document https://hal.science/hal-03329520/file/Regattieri%20et%20al%202019.pdf https://doi.org/10.1016/j.quascirev.2019.04.024 |
id |
ftceafr:oai:HAL:hal-03329520v1 |
---|---|
record_format |
openpolar |
institution |
Open Polar |
collection |
HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) |
op_collection_id |
ftceafr |
language |
English |
topic |
Stable isotope geochemistry interglacial variability central Italy lacustrine succession MIS 19 [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry |
spellingShingle |
Stable isotope geochemistry interglacial variability central Italy lacustrine succession MIS 19 [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry Regattieri, Eleonora Giaccio, Biagio Mannella, Giorgio Zanchetta, Giovanni Nomade, Sebastien Tognarelli, Andrea Perchiazzi, Natale Vogel, Hendrik Boschi, Chiara Drysdale, Russell Neil Wagner, Bernd Gemelli, Maurizio Tzedakis, Polichronis Frequency and dynamics of millennial-scale variability during Marine Isotope Stage 19: Insights from the Sulmona Basin (central Italy) |
topic_facet |
Stable isotope geochemistry interglacial variability central Italy lacustrine succession MIS 19 [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry |
description |
International audience Among past interglacial periods, Marine Isotope Stage (MIS) 19 is particularly interesting because its orbital geometry is very similar to that of the present interglacial. Here we present a high-resolution (sub-centennial) multiproxy record covering the ca. 790-770 ka interval, i.e. the interglacial MIS 19c and the ensuing glacial inception of MIS 19b, from a lacustrine sediment sequence retrieved from the Sulmona Basin (central Italy). The record has an independent chronology based on radiometric dating of six volcanic ash layers, and the resulting age model has a mean associated uncertainty of ±2.6 kyr. Variations in sediment geochemistry and mineralogy are interpreted in terms of past hydrological and temperature changes. Several millennial and sub-millennial events of reduced precipitation are well expressed. Comparisons with continental and marine records from the mid-latitude and sub-polar North Atlantic suggest a broad spatial expression for the observed events. Events occurring within the interglacial are not clearly associated with changes in marine proxies in the Iberian Margin, although similarities with the record from the sub-polar North Atlantic can be recognized and tentatively linked to changes in local hydrography having a downstream effect amplified by changes in atmospheric circulation. During the glacial inception, changes in the Sulmona record are coherent with changes in North Atlantic records, with drier events likely associated with meltwater-induced intervals of AMOC weakening. An event at ca. 785.6 ka may also reflect oceanic changes caused by freshwater discharges from residual ice-sheets and an outburst flood, similar to the 8.2 ka event in the Holocene. |
author2 |
Dipartimento di Scienze della Terra Pisa University of Pisa - Università di Pisa Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Paléocéanographie (PALEOCEAN) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Oeschger Centre for Climate Change Research (OCCR) Universität Bern = University of Bern = Université de Berne (UNIBE) CNR Istituto di Geoscienze e Georisorse Pisa (IGG-CNR) National Research Council of Italy University of Melbourne Universität zu Köln = University of Cologne Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Environmental Change Research Centre University College of London London (UCL) |
format |
Article in Journal/Newspaper |
author |
Regattieri, Eleonora Giaccio, Biagio Mannella, Giorgio Zanchetta, Giovanni Nomade, Sebastien Tognarelli, Andrea Perchiazzi, Natale Vogel, Hendrik Boschi, Chiara Drysdale, Russell Neil Wagner, Bernd Gemelli, Maurizio Tzedakis, Polichronis |
author_facet |
Regattieri, Eleonora Giaccio, Biagio Mannella, Giorgio Zanchetta, Giovanni Nomade, Sebastien Tognarelli, Andrea Perchiazzi, Natale Vogel, Hendrik Boschi, Chiara Drysdale, Russell Neil Wagner, Bernd Gemelli, Maurizio Tzedakis, Polichronis |
author_sort |
Regattieri, Eleonora |
title |
Frequency and dynamics of millennial-scale variability during Marine Isotope Stage 19: Insights from the Sulmona Basin (central Italy) |
title_short |
Frequency and dynamics of millennial-scale variability during Marine Isotope Stage 19: Insights from the Sulmona Basin (central Italy) |
title_full |
Frequency and dynamics of millennial-scale variability during Marine Isotope Stage 19: Insights from the Sulmona Basin (central Italy) |
title_fullStr |
Frequency and dynamics of millennial-scale variability during Marine Isotope Stage 19: Insights from the Sulmona Basin (central Italy) |
title_full_unstemmed |
Frequency and dynamics of millennial-scale variability during Marine Isotope Stage 19: Insights from the Sulmona Basin (central Italy) |
title_sort |
frequency and dynamics of millennial-scale variability during marine isotope stage 19: insights from the sulmona basin (central italy) |
publisher |
HAL CCSD |
publishDate |
2019 |
url |
https://hal.science/hal-03329520 https://hal.science/hal-03329520/document https://hal.science/hal-03329520/file/Regattieri%20et%20al%202019.pdf https://doi.org/10.1016/j.quascirev.2019.04.024 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-03329520 Quaternary Science Reviews, 2019, 214, pp.28-43. ⟨10.1016/j.quascirev.2019.04.024⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2019.04.024 hal-03329520 https://hal.science/hal-03329520 https://hal.science/hal-03329520/document https://hal.science/hal-03329520/file/Regattieri%20et%20al%202019.pdf doi:10.1016/j.quascirev.2019.04.024 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.quascirev.2019.04.024 |
container_title |
Quaternary Science Reviews |
container_volume |
214 |
container_start_page |
28 |
op_container_end_page |
43 |
_version_ |
1810461352214396928 |
spelling |
ftceafr:oai:HAL:hal-03329520v1 2024-09-15T18:22:03+00:00 Frequency and dynamics of millennial-scale variability during Marine Isotope Stage 19: Insights from the Sulmona Basin (central Italy) Regattieri, Eleonora Giaccio, Biagio Mannella, Giorgio Zanchetta, Giovanni Nomade, Sebastien Tognarelli, Andrea Perchiazzi, Natale Vogel, Hendrik Boschi, Chiara Drysdale, Russell Neil Wagner, Bernd Gemelli, Maurizio Tzedakis, Polichronis Dipartimento di Scienze della Terra Pisa University of Pisa - Università di Pisa Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Paléocéanographie (PALEOCEAN) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Oeschger Centre for Climate Change Research (OCCR) Universität Bern = University of Bern = Université de Berne (UNIBE) CNR Istituto di Geoscienze e Georisorse Pisa (IGG-CNR) National Research Council of Italy University of Melbourne Universität zu Köln = University of Cologne Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Environmental Change Research Centre University College of London London (UCL) 2019 https://hal.science/hal-03329520 https://hal.science/hal-03329520/document https://hal.science/hal-03329520/file/Regattieri%20et%20al%202019.pdf https://doi.org/10.1016/j.quascirev.2019.04.024 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2019.04.024 hal-03329520 https://hal.science/hal-03329520 https://hal.science/hal-03329520/document https://hal.science/hal-03329520/file/Regattieri%20et%20al%202019.pdf doi:10.1016/j.quascirev.2019.04.024 info:eu-repo/semantics/OpenAccess ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-03329520 Quaternary Science Reviews, 2019, 214, pp.28-43. ⟨10.1016/j.quascirev.2019.04.024⟩ Stable isotope geochemistry interglacial variability central Italy lacustrine succession MIS 19 [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry info:eu-repo/semantics/article Journal articles 2019 ftceafr https://doi.org/10.1016/j.quascirev.2019.04.024 2024-07-29T23:36:00Z International audience Among past interglacial periods, Marine Isotope Stage (MIS) 19 is particularly interesting because its orbital geometry is very similar to that of the present interglacial. Here we present a high-resolution (sub-centennial) multiproxy record covering the ca. 790-770 ka interval, i.e. the interglacial MIS 19c and the ensuing glacial inception of MIS 19b, from a lacustrine sediment sequence retrieved from the Sulmona Basin (central Italy). The record has an independent chronology based on radiometric dating of six volcanic ash layers, and the resulting age model has a mean associated uncertainty of ±2.6 kyr. Variations in sediment geochemistry and mineralogy are interpreted in terms of past hydrological and temperature changes. Several millennial and sub-millennial events of reduced precipitation are well expressed. Comparisons with continental and marine records from the mid-latitude and sub-polar North Atlantic suggest a broad spatial expression for the observed events. Events occurring within the interglacial are not clearly associated with changes in marine proxies in the Iberian Margin, although similarities with the record from the sub-polar North Atlantic can be recognized and tentatively linked to changes in local hydrography having a downstream effect amplified by changes in atmospheric circulation. During the glacial inception, changes in the Sulmona record are coherent with changes in North Atlantic records, with drier events likely associated with meltwater-induced intervals of AMOC weakening. An event at ca. 785.6 ka may also reflect oceanic changes caused by freshwater discharges from residual ice-sheets and an outburst flood, similar to the 8.2 ka event in the Holocene. Article in Journal/Newspaper North Atlantic HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) Quaternary Science Reviews 214 28 43 |