Coupled atmospheric and marine palaeoclimatic reconstruction for the last 35 ka in the Sele Plain–Gulf of Salerno area (southern Italy)
International audience Planktonic foraminifera and pollen data from core GNS84-C106 (Gulf of Salerno, Tyrrhenian Sea) were analysed through the Modern Analogue Technique, Constrained Cluster Analysis and relative variation biplots. A long period of mild climate, centred around 25 ka BP, is evident i...
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Online Access: | https://hal.archives-ouvertes.fr/halsde-00469800 https://doi.org/10.1016/j.quaint.2008.05.006 |
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ftccsdartic:oai:HAL:halsde-00469800v1 2023-05-15T18:01:03+02:00 Coupled atmospheric and marine palaeoclimatic reconstruction for the last 35 ka in the Sele Plain–Gulf of Salerno area (southern Italy) Di Donato, Valentino Esposito, Paola Russo-Erniolli, Elda Scarano, Arianna Cheddadi, Rachid Departimento di Scienze della Terra Napoli Università degli studi di Napoli Federico II Institut des Sciences de l'Evolution de Montpellier (UMR ISEM) École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement IRD : UR226 2008-11 https://hal.archives-ouvertes.fr/halsde-00469800 https://doi.org/10.1016/j.quaint.2008.05.006 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quaint.2008.05.006 halsde-00469800 https://hal.archives-ouvertes.fr/halsde-00469800 doi:10.1016/j.quaint.2008.05.006 ISSN: 1040-6182 Quaternary International https://hal.archives-ouvertes.fr/halsde-00469800 Quaternary International, Elsevier, 2008, 190, pp.146-157. ⟨10.1016/j.quaint.2008.05.006⟩ GRANDE DI MONTICCHIO TYRRHENIAN SEA RADIOCARBON CALIBRATION CLIMATE VARIABILITY COMPOSITIONAL DATA POLLEN HOLOCENE TEMPERATURE ATLANTIC RECORDS [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2008 ftccsdartic https://doi.org/10.1016/j.quaint.2008.05.006 2021-11-21T04:44:09Z International audience Planktonic foraminifera and pollen data from core GNS84-C106 (Gulf of Salerno, Tyrrhenian Sea) were analysed through the Modern Analogue Technique, Constrained Cluster Analysis and relative variation biplots. A long period of mild climate, centred around 25 ka BP, is evident in both marine and continental reconstructions. The cooling phase from 17 to 14.7 ka BP, correlated to the H1 Heinrich event, is indicated by a sea surface temperature (SST) decrease, which roughly coincides with the cold-arid phase identified by annual and January temperatures. A rapid increase in atmospheric temperatures and precipitation, culminating at 13.8 ka BP, marks the BA cronozone. The corresponding increase in summer and winter SSTs, of 11 and 6.5 °C, respectively, occurred over 600 years. The beginning of the YD, centred around 12.5 ka BP, is marked by a decrease in summer and winter SSTs of, respectively, 4.5 and 3.5 °C in one century. The atmospheric evidence of the YD is primarily reflected in low January temperatures, reaching −6 °C, the lowest values ever experienced in the analysed time interval. The Late Glacial–Holocene transition is clearly recorded in both the continental and marine realms. From 11.5 to 9 ka BP, atmospheric temperatures record a period of substantial stability followed by a drop at 8.9 ka BP, which chronologically fall within the first RCC event (9–8 ka BP) of Mayewski et al. [2004. Holocene climate variability. Quaternary Research 62, 243–255], in correspondence with a phase of relatively high seasonality, indicated by foraminifera. Article Outline Article in Journal/Newspaper Planktonic foraminifera Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Quaternary International 190 1 146 157 |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
GRANDE DI MONTICCHIO TYRRHENIAN SEA RADIOCARBON CALIBRATION CLIMATE VARIABILITY COMPOSITIONAL DATA POLLEN HOLOCENE TEMPERATURE ATLANTIC RECORDS [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
GRANDE DI MONTICCHIO TYRRHENIAN SEA RADIOCARBON CALIBRATION CLIMATE VARIABILITY COMPOSITIONAL DATA POLLEN HOLOCENE TEMPERATURE ATLANTIC RECORDS [SDE.MCG]Environmental Sciences/Global Changes Di Donato, Valentino Esposito, Paola Russo-Erniolli, Elda Scarano, Arianna Cheddadi, Rachid Coupled atmospheric and marine palaeoclimatic reconstruction for the last 35 ka in the Sele Plain–Gulf of Salerno area (southern Italy) |
topic_facet |
GRANDE DI MONTICCHIO TYRRHENIAN SEA RADIOCARBON CALIBRATION CLIMATE VARIABILITY COMPOSITIONAL DATA POLLEN HOLOCENE TEMPERATURE ATLANTIC RECORDS [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience Planktonic foraminifera and pollen data from core GNS84-C106 (Gulf of Salerno, Tyrrhenian Sea) were analysed through the Modern Analogue Technique, Constrained Cluster Analysis and relative variation biplots. A long period of mild climate, centred around 25 ka BP, is evident in both marine and continental reconstructions. The cooling phase from 17 to 14.7 ka BP, correlated to the H1 Heinrich event, is indicated by a sea surface temperature (SST) decrease, which roughly coincides with the cold-arid phase identified by annual and January temperatures. A rapid increase in atmospheric temperatures and precipitation, culminating at 13.8 ka BP, marks the BA cronozone. The corresponding increase in summer and winter SSTs, of 11 and 6.5 °C, respectively, occurred over 600 years. The beginning of the YD, centred around 12.5 ka BP, is marked by a decrease in summer and winter SSTs of, respectively, 4.5 and 3.5 °C in one century. The atmospheric evidence of the YD is primarily reflected in low January temperatures, reaching −6 °C, the lowest values ever experienced in the analysed time interval. The Late Glacial–Holocene transition is clearly recorded in both the continental and marine realms. From 11.5 to 9 ka BP, atmospheric temperatures record a period of substantial stability followed by a drop at 8.9 ka BP, which chronologically fall within the first RCC event (9–8 ka BP) of Mayewski et al. [2004. Holocene climate variability. Quaternary Research 62, 243–255], in correspondence with a phase of relatively high seasonality, indicated by foraminifera. Article Outline |
author2 |
Departimento di Scienze della Terra Napoli Università degli studi di Napoli Federico II Institut des Sciences de l'Evolution de Montpellier (UMR ISEM) École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement IRD : UR226 |
format |
Article in Journal/Newspaper |
author |
Di Donato, Valentino Esposito, Paola Russo-Erniolli, Elda Scarano, Arianna Cheddadi, Rachid |
author_facet |
Di Donato, Valentino Esposito, Paola Russo-Erniolli, Elda Scarano, Arianna Cheddadi, Rachid |
author_sort |
Di Donato, Valentino |
title |
Coupled atmospheric and marine palaeoclimatic reconstruction for the last 35 ka in the Sele Plain–Gulf of Salerno area (southern Italy) |
title_short |
Coupled atmospheric and marine palaeoclimatic reconstruction for the last 35 ka in the Sele Plain–Gulf of Salerno area (southern Italy) |
title_full |
Coupled atmospheric and marine palaeoclimatic reconstruction for the last 35 ka in the Sele Plain–Gulf of Salerno area (southern Italy) |
title_fullStr |
Coupled atmospheric and marine palaeoclimatic reconstruction for the last 35 ka in the Sele Plain–Gulf of Salerno area (southern Italy) |
title_full_unstemmed |
Coupled atmospheric and marine palaeoclimatic reconstruction for the last 35 ka in the Sele Plain–Gulf of Salerno area (southern Italy) |
title_sort |
coupled atmospheric and marine palaeoclimatic reconstruction for the last 35 ka in the sele plain–gulf of salerno area (southern italy) |
publisher |
HAL CCSD |
publishDate |
2008 |
url |
https://hal.archives-ouvertes.fr/halsde-00469800 https://doi.org/10.1016/j.quaint.2008.05.006 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
ISSN: 1040-6182 Quaternary International https://hal.archives-ouvertes.fr/halsde-00469800 Quaternary International, Elsevier, 2008, 190, pp.146-157. ⟨10.1016/j.quaint.2008.05.006⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quaint.2008.05.006 halsde-00469800 https://hal.archives-ouvertes.fr/halsde-00469800 doi:10.1016/j.quaint.2008.05.006 |
op_doi |
https://doi.org/10.1016/j.quaint.2008.05.006 |
container_title |
Quaternary International |
container_volume |
190 |
container_issue |
1 |
container_start_page |
146 |
op_container_end_page |
157 |
_version_ |
1766170381447593984 |