(Table S1) Age determination of sediment cores of the Azores Current System ...

In order to test the sensitivity of marine primary productivity in the midlatitude open ocean North Atlantic to changes in the Atlantic Meridional Overturning Circulation (AMOC), we investigated two spliced sediment cores from a site south of the Azores Islands at the northern rim of the North Atlan...

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Main Authors: Schwab, Christian, Kinkel, Hanno, Weinelt, M, Repschläger, Janne
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.824858
https://doi.pangaea.de/10.1594/PANGAEA.824858
id ftdatacite:10.1594/pangaea.824858
record_format openpolar
spelling ftdatacite:10.1594/pangaea.824858 2024-09-15T18:22:30+00:00 (Table S1) Age determination of sediment cores of the Azores Current System ... Schwab, Christian Kinkel, Hanno Weinelt, M Repschläger, Janne 2012 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.824858 https://doi.pangaea.de/10.1594/PANGAEA.824858 en eng PANGAEA https://dx.doi.org/10.1029/2012pa002281 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label DEPTH, sediment/rock Age, dated Age, dated standard deviation Reservoir effect/correction Age model Piston corer Calypso Corer Age, 14C AMS Age, 14C calibrated, CALIB 6.0 and Marine09 Reimer et al., 2009 GEOFAR MD168 Le Noroit Marion Dufresne 1995 Dataset dataset Supplementary Dataset 2012 ftdatacite https://doi.org/10.1594/pangaea.82485810.1029/2012pa002281 2024-07-03T13:10:33Z In order to test the sensitivity of marine primary productivity in the midlatitude open ocean North Atlantic to changes in the Atlantic Meridional Overturning Circulation (AMOC), we investigated two spliced sediment cores from a site south of the Azores Islands at the northern rim of the North Atlantic subtropical gyre. For this purpose we analyzed coccolithophore assemblages, diatom abundances, alkenones and conducted X-ray fluorescence (XRF) core scanning. During times of reduced AMOC, especially during Heinrich event 1 (H1) and the Younger Dryas, we observe a strong increase in productivity as evidenced by high coccolith accumulation rates, high alkenone concentrations/accumulation rates, high Ba/Ti-ratios, high abundances of diatoms and low abundances ofF. profunda. The increased productivity is partly caused by a more southern position of the Azores Front (AzF), and hence by a less northward extension of the subtropical gyre, as deduced from high abundances of the temperate coccolithophore species G. ... : AMS determination on monospecific planktonic foraminifera (Globigerinoides runber white or Globigerina bulloides). ... Dataset North Atlantic Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
DEPTH, sediment/rock
Age, dated
Age, dated standard deviation
Reservoir effect/correction
Age model
Piston corer
Calypso Corer
Age, 14C AMS
Age, 14C calibrated, CALIB 6.0 and Marine09 Reimer et al., 2009
GEOFAR
MD168
Le Noroit
Marion Dufresne 1995
spellingShingle Event label
DEPTH, sediment/rock
Age, dated
Age, dated standard deviation
Reservoir effect/correction
Age model
Piston corer
Calypso Corer
Age, 14C AMS
Age, 14C calibrated, CALIB 6.0 and Marine09 Reimer et al., 2009
GEOFAR
MD168
Le Noroit
Marion Dufresne 1995
Schwab, Christian
Kinkel, Hanno
Weinelt, M
Repschläger, Janne
(Table S1) Age determination of sediment cores of the Azores Current System ...
topic_facet Event label
DEPTH, sediment/rock
Age, dated
Age, dated standard deviation
Reservoir effect/correction
Age model
Piston corer
Calypso Corer
Age, 14C AMS
Age, 14C calibrated, CALIB 6.0 and Marine09 Reimer et al., 2009
GEOFAR
MD168
Le Noroit
Marion Dufresne 1995
description In order to test the sensitivity of marine primary productivity in the midlatitude open ocean North Atlantic to changes in the Atlantic Meridional Overturning Circulation (AMOC), we investigated two spliced sediment cores from a site south of the Azores Islands at the northern rim of the North Atlantic subtropical gyre. For this purpose we analyzed coccolithophore assemblages, diatom abundances, alkenones and conducted X-ray fluorescence (XRF) core scanning. During times of reduced AMOC, especially during Heinrich event 1 (H1) and the Younger Dryas, we observe a strong increase in productivity as evidenced by high coccolith accumulation rates, high alkenone concentrations/accumulation rates, high Ba/Ti-ratios, high abundances of diatoms and low abundances ofF. profunda. The increased productivity is partly caused by a more southern position of the Azores Front (AzF), and hence by a less northward extension of the subtropical gyre, as deduced from high abundances of the temperate coccolithophore species G. ... : AMS determination on monospecific planktonic foraminifera (Globigerinoides runber white or Globigerina bulloides). ...
format Dataset
author Schwab, Christian
Kinkel, Hanno
Weinelt, M
Repschläger, Janne
author_facet Schwab, Christian
Kinkel, Hanno
Weinelt, M
Repschläger, Janne
author_sort Schwab, Christian
title (Table S1) Age determination of sediment cores of the Azores Current System ...
title_short (Table S1) Age determination of sediment cores of the Azores Current System ...
title_full (Table S1) Age determination of sediment cores of the Azores Current System ...
title_fullStr (Table S1) Age determination of sediment cores of the Azores Current System ...
title_full_unstemmed (Table S1) Age determination of sediment cores of the Azores Current System ...
title_sort (table s1) age determination of sediment cores of the azores current system ...
publisher PANGAEA
publishDate 2012
url https://dx.doi.org/10.1594/pangaea.824858
https://doi.pangaea.de/10.1594/PANGAEA.824858
genre North Atlantic
Planktonic foraminifera
genre_facet North Atlantic
Planktonic foraminifera
op_relation https://dx.doi.org/10.1029/2012pa002281
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.82485810.1029/2012pa002281
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