FLUTTUAZIONI CLIMATICHE DURANTE IL QUATERNARIO NEL MAR TIRRENO, MEDITERRANEO OCCIDENTALE (CAROTA PC-19 BAN 80)

Core PC—19, recovered from the central Tyrrhenian Sea (Western Mediterranean) during cruise BAN 80, was investigated with micropaleontological and stable isotopic techniques. The time interval spans from Late Pleistocene to Holocene; the biostratigraphic framework was provided by calcareous nannofos...

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Main Authors: DONATA VIOLANTI, ELISABETTA PARISI, ELISABETTA ERBA
Format: Article in Journal/Newspaper
Language:English
Published: Milano University Press 2020
Subjects:
Online Access:https://doaj.org/article/95e2f318e9b243bf8c65e3a00522942d
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spelling ftdoajarticles:oai:doaj.org/article:95e2f318e9b243bf8c65e3a00522942d 2023-10-01T03:59:01+02:00 FLUTTUAZIONI CLIMATICHE DURANTE IL QUATERNARIO NEL MAR TIRRENO, MEDITERRANEO OCCIDENTALE (CAROTA PC-19 BAN 80) DONATA VIOLANTI ELISABETTA PARISI ELISABETTA ERBA 2020-04-01T00:00:00Z https://doaj.org/article/95e2f318e9b243bf8c65e3a00522942d EN eng Milano University Press https://riviste.unimi.it/index.php/RIPS/article/view/13232 https://doaj.org/toc/0035-6883 https://doaj.org/toc/2039-4942 0035-6883 2039-4942 https://doaj.org/article/95e2f318e9b243bf8c65e3a00522942d Rivista Italiana di Paleontologia e Stratigrafia, Vol 92, Iss 4 (2020) Climatic fluctuations Tyrrhenian Sea Quaternary Foraminifera Stable isotopes Calcareous nannofossils Geology QE1-996.5 Paleontology QE701-760 article 2020 ftdoajarticles 2023-09-03T00:38:33Z Core PC—19, recovered from the central Tyrrhenian Sea (Western Mediterranean) during cruise BAN 80, was investigated with micropaleontological and stable isotopic techniques. The time interval spans from Late Pleistocene to Holocene; the biostratigraphic framework was provided by calcareous nannofossils. Two biozones (Emiliania huxleyi and E. huxleyi Acme Zones) and two distinct biohorizons (the Gephyrocapsa caribbeanica/E. huxleyi abundance reversal and the beginning of E. huxleyi Acme) were recognized. Calcareous nannofossils confirmed to be excellent indicators of surface water mass temperatures: two warrn and five cold episodes and five low—salinity events were pointed out. Planktonic foraminifera were quantitatively analyzed: large fluctuations in abundance were pointed out and a climatic curve was constructed. Data regarding changes of deep water assemblages were provided by benthic foraminifera. Oxygen and carbon isotopic composition was measured on tests of Globigerina bulloides or Globigerinoides ruber; isotopic curves were correlated with the faunal climatic one and plotted against the biostratigraphic framework. Isotopic stages 3 and 5 and substages 5a and 5e could be identified whereas stage 1 was recognized only partially. Climatic zones W, X, Y and Z could be tentatively identified. The paleoceanographic changes evidenced by the present study are consistent with those known. for the eastern Mediterranean: thus Quaternary paleoclimatic and paleoceanographic signals had a large significance at least at regional scale. Article in Journal/Newspaper Planktonic foraminifera Directory of Open Access Journals: DOAJ Articles
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Climatic fluctuations
Tyrrhenian Sea
Quaternary
Foraminifera
Stable isotopes
Calcareous nannofossils
Geology
QE1-996.5
Paleontology
QE701-760
spellingShingle Climatic fluctuations
Tyrrhenian Sea
Quaternary
Foraminifera
Stable isotopes
Calcareous nannofossils
Geology
QE1-996.5
Paleontology
QE701-760
DONATA VIOLANTI
ELISABETTA PARISI
ELISABETTA ERBA
FLUTTUAZIONI CLIMATICHE DURANTE IL QUATERNARIO NEL MAR TIRRENO, MEDITERRANEO OCCIDENTALE (CAROTA PC-19 BAN 80)
topic_facet Climatic fluctuations
Tyrrhenian Sea
Quaternary
Foraminifera
Stable isotopes
Calcareous nannofossils
Geology
QE1-996.5
Paleontology
QE701-760
description Core PC—19, recovered from the central Tyrrhenian Sea (Western Mediterranean) during cruise BAN 80, was investigated with micropaleontological and stable isotopic techniques. The time interval spans from Late Pleistocene to Holocene; the biostratigraphic framework was provided by calcareous nannofossils. Two biozones (Emiliania huxleyi and E. huxleyi Acme Zones) and two distinct biohorizons (the Gephyrocapsa caribbeanica/E. huxleyi abundance reversal and the beginning of E. huxleyi Acme) were recognized. Calcareous nannofossils confirmed to be excellent indicators of surface water mass temperatures: two warrn and five cold episodes and five low—salinity events were pointed out. Planktonic foraminifera were quantitatively analyzed: large fluctuations in abundance were pointed out and a climatic curve was constructed. Data regarding changes of deep water assemblages were provided by benthic foraminifera. Oxygen and carbon isotopic composition was measured on tests of Globigerina bulloides or Globigerinoides ruber; isotopic curves were correlated with the faunal climatic one and plotted against the biostratigraphic framework. Isotopic stages 3 and 5 and substages 5a and 5e could be identified whereas stage 1 was recognized only partially. Climatic zones W, X, Y and Z could be tentatively identified. The paleoceanographic changes evidenced by the present study are consistent with those known. for the eastern Mediterranean: thus Quaternary paleoclimatic and paleoceanographic signals had a large significance at least at regional scale.
format Article in Journal/Newspaper
author DONATA VIOLANTI
ELISABETTA PARISI
ELISABETTA ERBA
author_facet DONATA VIOLANTI
ELISABETTA PARISI
ELISABETTA ERBA
author_sort DONATA VIOLANTI
title FLUTTUAZIONI CLIMATICHE DURANTE IL QUATERNARIO NEL MAR TIRRENO, MEDITERRANEO OCCIDENTALE (CAROTA PC-19 BAN 80)
title_short FLUTTUAZIONI CLIMATICHE DURANTE IL QUATERNARIO NEL MAR TIRRENO, MEDITERRANEO OCCIDENTALE (CAROTA PC-19 BAN 80)
title_full FLUTTUAZIONI CLIMATICHE DURANTE IL QUATERNARIO NEL MAR TIRRENO, MEDITERRANEO OCCIDENTALE (CAROTA PC-19 BAN 80)
title_fullStr FLUTTUAZIONI CLIMATICHE DURANTE IL QUATERNARIO NEL MAR TIRRENO, MEDITERRANEO OCCIDENTALE (CAROTA PC-19 BAN 80)
title_full_unstemmed FLUTTUAZIONI CLIMATICHE DURANTE IL QUATERNARIO NEL MAR TIRRENO, MEDITERRANEO OCCIDENTALE (CAROTA PC-19 BAN 80)
title_sort fluttuazioni climatiche durante il quaternario nel mar tirreno, mediterraneo occidentale (carota pc-19 ban 80)
publisher Milano University Press
publishDate 2020
url https://doaj.org/article/95e2f318e9b243bf8c65e3a00522942d
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source Rivista Italiana di Paleontologia e Stratigrafia, Vol 92, Iss 4 (2020)
op_relation https://riviste.unimi.it/index.php/RIPS/article/view/13232
https://doaj.org/toc/0035-6883
https://doaj.org/toc/2039-4942
0035-6883
2039-4942
https://doaj.org/article/95e2f318e9b243bf8c65e3a00522942d
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