REASSESSMENT OF THE AGE OF BASEMENT IN THE VAVILOV BASIN DRILLED AT ODP SITE 651 (TYRRHENIAN SEA, MEDITERRANEAN)

We carried out a biostratigraphic study based on calcareous nannofossils in sediments from Ocean Drilling Program (ODP) Site 651, drilled in the basalt-floored Vavilov sub-basin of the Tyrrhenian Sea (western Mediterranean) during Leg 107. The expedition achieved its primary objective to collect ba...

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Main Authors: ISABELLA RAFFI, AMALIA NOTARO
Format: Article
Language:English
Published: Milano University Press 2025-01-01
Series:Rivista Italiana di Paleontologia e Stratigrafia
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Online Access:https://riviste.unimi.it/index.php/RIPS/article/view/22586
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author ISABELLA RAFFI
AMALIA NOTARO
author_facet ISABELLA RAFFI
AMALIA NOTARO
author_sort ISABELLA RAFFI
collection DOAJ
description We carried out a biostratigraphic study based on calcareous nannofossils in sediments from Ocean Drilling Program (ODP) Site 651, drilled in the basalt-floored Vavilov sub-basin of the Tyrrhenian Sea (western Mediterranean) during Leg 107. The expedition achieved its primary objective to collect basement samples to date the ocean crust and obtain new data for reconstructing the geological evolution of the area. Studies on the ODP Site 651 succession determined the nature of the basement and provided time constraints for tectonic and magmatic processes in the basin, but contradictory lines of evidence emerged for the age of the basalts based on radiometric ages, paleomagnetic signature and planktonic foraminifera data. In an attempt to clarify the basement age, we performed detailed sampling for calcareous nannofossil analysis to update the biostratigraphy and chronology of the sediments overlying the basement. We determined the sediment accumulation rate using reliable nannofossil biohorizons that have a robust chronology, which increases up-section from ~ 2 cm/kyr to 3.4 cm /kyr. The age of the basalt/sediment contact was obtained through extrapolation of the sedimentation rate from the deepest datable portion of the sediments down to the top of basement. The inferred age for the top of the basalt is at least 4.1-4.2 Ma and differs from previous evaluations. This age for the basalt in the Vavilov Basin basement is consistent to a reversed interval C2Ar within the Gilbert magnetochron, supporting one of the chronologies previously proposed.
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spelling doaj-art-77e7f893aa2146ab80807165c6d1a01d2025-01-08T15:45:22ZengMilano University PressRivista Italiana di Paleontologia e Stratigrafia0035-68832039-49422025-01-01131110.54103/2039-4942/22586REASSESSMENT OF THE AGE OF BASEMENT IN THE VAVILOV BASIN DRILLED AT ODP SITE 651 (TYRRHENIAN SEA, MEDITERRANEAN)ISABELLA RAFFI0AMALIA NOTARO1University of Chieti-Pescara University of Chieti-Pescara We carried out a biostratigraphic study based on calcareous nannofossils in sediments from Ocean Drilling Program (ODP) Site 651, drilled in the basalt-floored Vavilov sub-basin of the Tyrrhenian Sea (western Mediterranean) during Leg 107. The expedition achieved its primary objective to collect basement samples to date the ocean crust and obtain new data for reconstructing the geological evolution of the area. Studies on the ODP Site 651 succession determined the nature of the basement and provided time constraints for tectonic and magmatic processes in the basin, but contradictory lines of evidence emerged for the age of the basalts based on radiometric ages, paleomagnetic signature and planktonic foraminifera data. In an attempt to clarify the basement age, we performed detailed sampling for calcareous nannofossil analysis to update the biostratigraphy and chronology of the sediments overlying the basement. We determined the sediment accumulation rate using reliable nannofossil biohorizons that have a robust chronology, which increases up-section from ~ 2 cm/kyr to 3.4 cm /kyr. The age of the basalt/sediment contact was obtained through extrapolation of the sedimentation rate from the deepest datable portion of the sediments down to the top of basement. The inferred age for the top of the basalt is at least 4.1-4.2 Ma and differs from previous evaluations. This age for the basalt in the Vavilov Basin basement is consistent to a reversed interval C2Ar within the Gilbert magnetochron, supporting one of the chronologies previously proposed. https://riviste.unimi.it/index.php/RIPS/article/view/22586Calcareous nannofossils; biochronology; ODP Site 651; Tyrrhenian Sea; basement age.
spellingShingle ISABELLA RAFFI
AMALIA NOTARO
REASSESSMENT OF THE AGE OF BASEMENT IN THE VAVILOV BASIN DRILLED AT ODP SITE 651 (TYRRHENIAN SEA, MEDITERRANEAN)
Rivista Italiana di Paleontologia e Stratigrafia
Calcareous nannofossils; biochronology; ODP Site 651; Tyrrhenian Sea; basement age.
title REASSESSMENT OF THE AGE OF BASEMENT IN THE VAVILOV BASIN DRILLED AT ODP SITE 651 (TYRRHENIAN SEA, MEDITERRANEAN)
title_full REASSESSMENT OF THE AGE OF BASEMENT IN THE VAVILOV BASIN DRILLED AT ODP SITE 651 (TYRRHENIAN SEA, MEDITERRANEAN)
title_fullStr REASSESSMENT OF THE AGE OF BASEMENT IN THE VAVILOV BASIN DRILLED AT ODP SITE 651 (TYRRHENIAN SEA, MEDITERRANEAN)
title_full_unstemmed REASSESSMENT OF THE AGE OF BASEMENT IN THE VAVILOV BASIN DRILLED AT ODP SITE 651 (TYRRHENIAN SEA, MEDITERRANEAN)
title_short REASSESSMENT OF THE AGE OF BASEMENT IN THE VAVILOV BASIN DRILLED AT ODP SITE 651 (TYRRHENIAN SEA, MEDITERRANEAN)
title_sort reassessment of the age of basement in the vavilov basin drilled at odp site 651 tyrrhenian sea mediterranean
topic Calcareous nannofossils; biochronology; ODP Site 651; Tyrrhenian Sea; basement age.
url https://riviste.unimi.it/index.php/RIPS/article/view/22586
work_keys_str_mv AT isabellaraffi reassessmentoftheageofbasementinthevavilovbasindrilledatodpsite651tyrrhenianseamediterranean
AT amalianotaro reassessmentoftheageofbasementinthevavilovbasindrilledatodpsite651tyrrhenianseamediterranean