Climate variability of the last ~2700 years in the Southern Adriatic Sea: Coccolithophore evidences

New information on palaeoenvironmental conditions over the past ~2700 years in the Central Mediterranean Sea have been acquired through the high-resolution study of calcareous nannofossils preserved in the sediment core SW104-ND14Q recovered in the Southern Adriatic Sea (SAS) at 1013-m water depth....

Full description

Bibliographic Details
Published in:The Holocene
Main Authors: Cascella, Antonio, Bonomo, Sergio, Jalali, Bassem, Sicre, Marie-Alexandrine, Pelosi, Nicola, Schmidt, Sabine, Lirer, Fabrizio
Other Authors: Istituto Nazionale di Geofisica e Vulcanologia – Sezione di Pisa (INGV), Istituto Nazionale di Geofisica e Vulcanologia, Istituto di Scienze Marine Napoli (ISMAR-CNR), Istituto di Science Marine (ISMAR ), Consiglio Nazionale delle Ricerche (CNR)-Consiglio Nazionale delle Ricerche (CNR), Unité GEOGLOB, Faculté des Sciences de Sfax, Université de Sfax - University of Sfax-Université de Sfax - University of Sfax, Variabilité de l'Océan et de la Glace de mer (VOG), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Institut de Recherche pour le Développement (IRD)-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Institut de Recherche pour le Développement (IRD)-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU), Consiglio Nazionale delle Ricerche (CNR), UMR 5805 Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC), Observatoire aquitain des sciences de l'univers (OASU), Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2019
Subjects:
geo
Online Access:https://doi.org/10.1177/0959683619865600
https://hal.archives-ouvertes.fr/hal-02357284
id fttriple:oai:gotriple.eu:jyeXCrIQAeSyvHdG26hKW
record_format openpolar
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic South Adriatic Sea
central Mediterranean
reworked coccoliths
last millennia
coccolithophorid primary productivity
coccolithophores
envir
geo
spellingShingle South Adriatic Sea
central Mediterranean
reworked coccoliths
last millennia
coccolithophorid primary productivity
coccolithophores
envir
geo
Cascella, Antonio
Bonomo, Sergio
Jalali, Bassem
Sicre, Marie-Alexandrine
Pelosi, Nicola
Schmidt, Sabine
Lirer, Fabrizio
Climate variability of the last ~2700 years in the Southern Adriatic Sea: Coccolithophore evidences
topic_facet South Adriatic Sea
central Mediterranean
reworked coccoliths
last millennia
coccolithophorid primary productivity
coccolithophores
envir
geo
description New information on palaeoenvironmental conditions over the past ~2700 years in the Central Mediterranean Sea have been acquired through the high-resolution study of calcareous nannofossils preserved in the sediment core SW104-ND14Q recovered in the Southern Adriatic Sea (SAS) at 1013-m water depth. The surface water properties at this open SAS site are sensitive to atmospheric forcing (acting both at local and regional scale) and the North Ionian Sea driven inflowing waters. Our data show a relationship between reworked coccolith abundances, flood frequency across the Southern Alps and the North Atlantic Oscillation (NAO) confirming their value as indicator of runoff/precipitation. Changes in the abundance of the opportunistic (r-strategist) species Emiliania huxleyi and deep dweller taxa Florisphaera profunda were used to reconstruct the upper water column stratification and associated changes in coccolithophorid productivity. The negative correlation between reworked coccoliths and the N-Ratio (r = −0.44; p = 6−7) suggest that fresh water induced stratification is a controlling factor of the SAS coccolithophorid production. High coccolithophorid productivity levels occurred during dry periods and/or time intervals of inflowing salty and nutrient-rich Levantine Intermediate Waters favouring convection while lower levels took place during high freshwater discharge, mainly during the ‘Little Ice Age’ and two centennial scale intervals of weakest NAO around 200 BCE and 500 CE.
author2 Istituto Nazionale di Geofisica e Vulcanologia – Sezione di Pisa (INGV)
Istituto Nazionale di Geofisica e Vulcanologia
Istituto di Scienze Marine Napoli (ISMAR-CNR)
Istituto di Science Marine (ISMAR )
Consiglio Nazionale delle Ricerche (CNR)-Consiglio Nazionale delle Ricerche (CNR)
Unité GEOGLOB
Faculté des Sciences de Sfax
Université de Sfax - University of Sfax-Université de Sfax - University of Sfax
Variabilité de l'Océan et de la Glace de mer (VOG)
Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN)
Institut de Recherche pour le Développement (IRD)-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Institut de Recherche pour le Développement (IRD)-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)
Consiglio Nazionale delle Ricerche (CNR)
UMR 5805 Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC)
Observatoire aquitain des sciences de l'univers (OASU)
Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Cascella, Antonio
Bonomo, Sergio
Jalali, Bassem
Sicre, Marie-Alexandrine
Pelosi, Nicola
Schmidt, Sabine
Lirer, Fabrizio
author_facet Cascella, Antonio
Bonomo, Sergio
Jalali, Bassem
Sicre, Marie-Alexandrine
Pelosi, Nicola
Schmidt, Sabine
Lirer, Fabrizio
author_sort Cascella, Antonio
title Climate variability of the last ~2700 years in the Southern Adriatic Sea: Coccolithophore evidences
title_short Climate variability of the last ~2700 years in the Southern Adriatic Sea: Coccolithophore evidences
title_full Climate variability of the last ~2700 years in the Southern Adriatic Sea: Coccolithophore evidences
title_fullStr Climate variability of the last ~2700 years in the Southern Adriatic Sea: Coccolithophore evidences
title_full_unstemmed Climate variability of the last ~2700 years in the Southern Adriatic Sea: Coccolithophore evidences
title_sort climate variability of the last ~2700 years in the southern adriatic sea: coccolithophore evidences
publisher HAL CCSD
publishDate 2019
url https://doi.org/10.1177/0959683619865600
https://hal.archives-ouvertes.fr/hal-02357284
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Hyper Article en Ligne - Sciences de l'Homme et de la Société
ISSN: 0959-6836
EISSN: 1477-0911
The holocene
The holocene, London: Sage, 2019, 160 (12), pp.095968361986560. ⟨10.1177/0959683619865600⟩
op_relation hal-02357284
doi:10.1177/0959683619865600
WOS: 000480078600001
10670/1.7bw6pa
hal-02189322
10670/1.z0mzv0
https://hal.archives-ouvertes.fr/hal-02357284
op_rights undefined
other
op_doi https://doi.org/10.1177/0959683619865600
container_title The Holocene
container_volume 30
container_issue 1
container_start_page 53
op_container_end_page 64
_version_ 1766132681403269120
spelling fttriple:oai:gotriple.eu:jyeXCrIQAeSyvHdG26hKW 2023-05-15T17:34:00+02:00 Climate variability of the last ~2700 years in the Southern Adriatic Sea: Coccolithophore evidences Cascella, Antonio Bonomo, Sergio Jalali, Bassem Sicre, Marie-Alexandrine Pelosi, Nicola Schmidt, Sabine Lirer, Fabrizio Istituto Nazionale di Geofisica e Vulcanologia – Sezione di Pisa (INGV) Istituto Nazionale di Geofisica e Vulcanologia Istituto di Scienze Marine Napoli (ISMAR-CNR) Istituto di Science Marine (ISMAR ) Consiglio Nazionale delle Ricerche (CNR)-Consiglio Nazionale delle Ricerche (CNR) Unité GEOGLOB Faculté des Sciences de Sfax Université de Sfax - University of Sfax-Université de Sfax - University of Sfax Variabilité de l'Océan et de la Glace de mer (VOG) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Institut de Recherche pour le Développement (IRD)-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Institut de Recherche pour le Développement (IRD)-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU) Consiglio Nazionale delle Ricerche (CNR) UMR 5805 Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) 2019-07-31 https://doi.org/10.1177/0959683619865600 https://hal.archives-ouvertes.fr/hal-02357284 en eng HAL CCSD London: Sage hal-02357284 doi:10.1177/0959683619865600 WOS: 000480078600001 10670/1.7bw6pa hal-02189322 10670/1.z0mzv0 https://hal.archives-ouvertes.fr/hal-02357284 undefined other Hyper Article en Ligne - Sciences de l'Homme et de la Société ISSN: 0959-6836 EISSN: 1477-0911 The holocene The holocene, London: Sage, 2019, 160 (12), pp.095968361986560. ⟨10.1177/0959683619865600⟩ South Adriatic Sea central Mediterranean reworked coccoliths last millennia coccolithophorid primary productivity coccolithophores envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2019 fttriple https://doi.org/10.1177/0959683619865600 2023-01-22T17:34:22Z New information on palaeoenvironmental conditions over the past ~2700 years in the Central Mediterranean Sea have been acquired through the high-resolution study of calcareous nannofossils preserved in the sediment core SW104-ND14Q recovered in the Southern Adriatic Sea (SAS) at 1013-m water depth. The surface water properties at this open SAS site are sensitive to atmospheric forcing (acting both at local and regional scale) and the North Ionian Sea driven inflowing waters. Our data show a relationship between reworked coccolith abundances, flood frequency across the Southern Alps and the North Atlantic Oscillation (NAO) confirming their value as indicator of runoff/precipitation. Changes in the abundance of the opportunistic (r-strategist) species Emiliania huxleyi and deep dweller taxa Florisphaera profunda were used to reconstruct the upper water column stratification and associated changes in coccolithophorid productivity. The negative correlation between reworked coccoliths and the N-Ratio (r = −0.44; p = 6−7) suggest that fresh water induced stratification is a controlling factor of the SAS coccolithophorid production. High coccolithophorid productivity levels occurred during dry periods and/or time intervals of inflowing salty and nutrient-rich Levantine Intermediate Waters favouring convection while lower levels took place during high freshwater discharge, mainly during the ‘Little Ice Age’ and two centennial scale intervals of weakest NAO around 200 BCE and 500 CE. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Unknown The Holocene 30 1 53 64