Revising chronological uncertainties in marine archives using global anthropogenic signals: a case study on the oceanic 13C Suess effect

Marine sediments are excellent archives for reconstructing past changes in climate and ocean circulation. Overlapping with instrumental records, they hold the potential to elucidate natural variability and contextualize current changes. Yet, dating uncertainties of traditional approaches (e.g., up t...

Full description

Bibliographic Details
Published in:Geochronology
Main Authors: Irvalı, Nil, Ninnemann, Ulysses S., Olsen, Are, Rose, Neil L., Thornalley, David J. R., Mjell, Tor L., Counillon, François
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/gchron-6-449-2024
https://gchron.copernicus.org/articles/6/449/2024/
id ftcopernicus:oai:publications.copernicus.org:gchron116311
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:gchron116311 2024-09-15T18:23:25+00:00 Revising chronological uncertainties in marine archives using global anthropogenic signals: a case study on the oceanic 13C Suess effect Irvalı, Nil Ninnemann, Ulysses S. Olsen, Are Rose, Neil L. Thornalley, David J. R. Mjell, Tor L. Counillon, François 2024-08-05 application/pdf https://doi.org/10.5194/gchron-6-449-2024 https://gchron.copernicus.org/articles/6/449/2024/ eng eng doi:10.5194/gchron-6-449-2024 https://gchron.copernicus.org/articles/6/449/2024/ eISSN: 2628-3719 Text 2024 ftcopernicus https://doi.org/10.5194/gchron-6-449-2024 2024-08-12T14:05:16Z Marine sediments are excellent archives for reconstructing past changes in climate and ocean circulation. Overlapping with instrumental records, they hold the potential to elucidate natural variability and contextualize current changes. Yet, dating uncertainties of traditional approaches (e.g., up to ± 30–50 years for the last 2 centuries) pose major challenges for integrating the shorter instrumental records with these extended marine archives. Hence, robust sediment chronologies are crucial, and most existing age model constraints do not provide sufficient age control, particularly for the 20th century, which is the most critical period for comparing proxy records to historical changes. Here we propose a novel chronostratigraphic approach that uses anthropogenic signals such as the oceanic 13 C Suess effect and spheroidal carbonaceous fly-ash particles to reduce age model uncertainties in high-resolution marine archives. As a test, we apply this new approach to a marine sediment core located at the Gardar Drift, in the subpolar North Atlantic, and revise the previously published age model for this site. We further provide a refined estimate of regional reservoir corrections and uncertainties for Gardar Drift. Text North Atlantic Copernicus Publications: E-Journals Geochronology 6 3 449 463
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Marine sediments are excellent archives for reconstructing past changes in climate and ocean circulation. Overlapping with instrumental records, they hold the potential to elucidate natural variability and contextualize current changes. Yet, dating uncertainties of traditional approaches (e.g., up to ± 30–50 years for the last 2 centuries) pose major challenges for integrating the shorter instrumental records with these extended marine archives. Hence, robust sediment chronologies are crucial, and most existing age model constraints do not provide sufficient age control, particularly for the 20th century, which is the most critical period for comparing proxy records to historical changes. Here we propose a novel chronostratigraphic approach that uses anthropogenic signals such as the oceanic 13 C Suess effect and spheroidal carbonaceous fly-ash particles to reduce age model uncertainties in high-resolution marine archives. As a test, we apply this new approach to a marine sediment core located at the Gardar Drift, in the subpolar North Atlantic, and revise the previously published age model for this site. We further provide a refined estimate of regional reservoir corrections and uncertainties for Gardar Drift.
format Text
author Irvalı, Nil
Ninnemann, Ulysses S.
Olsen, Are
Rose, Neil L.
Thornalley, David J. R.
Mjell, Tor L.
Counillon, François
spellingShingle Irvalı, Nil
Ninnemann, Ulysses S.
Olsen, Are
Rose, Neil L.
Thornalley, David J. R.
Mjell, Tor L.
Counillon, François
Revising chronological uncertainties in marine archives using global anthropogenic signals: a case study on the oceanic 13C Suess effect
author_facet Irvalı, Nil
Ninnemann, Ulysses S.
Olsen, Are
Rose, Neil L.
Thornalley, David J. R.
Mjell, Tor L.
Counillon, François
author_sort Irvalı, Nil
title Revising chronological uncertainties in marine archives using global anthropogenic signals: a case study on the oceanic 13C Suess effect
title_short Revising chronological uncertainties in marine archives using global anthropogenic signals: a case study on the oceanic 13C Suess effect
title_full Revising chronological uncertainties in marine archives using global anthropogenic signals: a case study on the oceanic 13C Suess effect
title_fullStr Revising chronological uncertainties in marine archives using global anthropogenic signals: a case study on the oceanic 13C Suess effect
title_full_unstemmed Revising chronological uncertainties in marine archives using global anthropogenic signals: a case study on the oceanic 13C Suess effect
title_sort revising chronological uncertainties in marine archives using global anthropogenic signals: a case study on the oceanic 13c suess effect
publishDate 2024
url https://doi.org/10.5194/gchron-6-449-2024
https://gchron.copernicus.org/articles/6/449/2024/
genre North Atlantic
genre_facet North Atlantic
op_source eISSN: 2628-3719
op_relation doi:10.5194/gchron-6-449-2024
https://gchron.copernicus.org/articles/6/449/2024/
op_doi https://doi.org/10.5194/gchron-6-449-2024
container_title Geochronology
container_volume 6
container_issue 3
container_start_page 449
op_container_end_page 463
_version_ 1810463618783772672