Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series
Biweekly sediment trap samples and concurrent hydrographic measurements collected between March 2005 and October 2008 from the Cariaco Basin, Venezuela, are used to assess the relationship between [CO32?] and the area densities (?A) of two species of planktonic foraminifera (Globigerinoides ruber (p...
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Language: | English |
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2013
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ftsouthampton:oai:eprints.soton.ac.uk:355634 2023-07-30T04:06:26+02:00 Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series Marshall, Brittney J. Thunell, Robert C. Henehan, Michael J. Astor, Yrene Wejnert, Katherine E. 2013-06 https://eprints.soton.ac.uk/355634/ English eng Marshall, Brittney J., Thunell, Robert C., Henehan, Michael J., Astor, Yrene and Wejnert, Katherine E. (2013) Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series. Paleoceanography, 28 (2), 363-376. (doi:10.1002/palo.20034 <http://dx.doi.org/10.1002/palo.20034>). Article PeerReviewed 2013 ftsouthampton https://doi.org/10.1002/palo.20034 2023-07-09T21:48:22Z Biweekly sediment trap samples and concurrent hydrographic measurements collected between March 2005 and October 2008 from the Cariaco Basin, Venezuela, are used to assess the relationship between [CO32?] and the area densities (?A) of two species of planktonic foraminifera (Globigerinoides ruber (pink) and Globigerinoides sacculifer). Calcification temperatures were calculated for each sample using species-appropriate oxygen isotope (?18O) temperature equations that were then compared to monthly temperature profiles taken at the study site in order to determine calcification depth. Ambient [CO32?] was determined for these calcification depths using alkalinity, pH, temperature, salinity, and nutrient concentration measurements taken during monthly hydrographic cruises. The ?A, which is representative of calcification efficiency, is determined by dividing individual foraminiferal shell weights (±0.43 µg) by their associated silhouette areas and taking the sample average. The results of this study show a strong correlation between ?A and ambient [CO32?] for both G. ruber and G. sacculifer (R2?=?0.89 and 0.86, respectively), confirming that [CO32?] has a pronounced effect on the calcification of these species. Though the ?A for both species reveal a highly significant (p?<?0.001) relationship with ambient [CO32?], linear regression reveals that the extent to which [CO32?] influences foraminiferal calcification is species specific. Hierarchical regression analyses indicate that other environmental parameters (temperature and [PO43?]) do not confound the use of G. ruber and G. sacculifer ?A as a predictor for [CO32?]. This study suggests that G. ruber and G. sacculifer ?A can be used as reliable proxies for past surface ocean [CO32?]. Article in Journal/Newspaper Planktonic foraminifera University of Southampton: e-Prints Soton Paleoceanography 28 2 363 376 |
institution |
Open Polar |
collection |
University of Southampton: e-Prints Soton |
op_collection_id |
ftsouthampton |
language |
English |
description |
Biweekly sediment trap samples and concurrent hydrographic measurements collected between March 2005 and October 2008 from the Cariaco Basin, Venezuela, are used to assess the relationship between [CO32?] and the area densities (?A) of two species of planktonic foraminifera (Globigerinoides ruber (pink) and Globigerinoides sacculifer). Calcification temperatures were calculated for each sample using species-appropriate oxygen isotope (?18O) temperature equations that were then compared to monthly temperature profiles taken at the study site in order to determine calcification depth. Ambient [CO32?] was determined for these calcification depths using alkalinity, pH, temperature, salinity, and nutrient concentration measurements taken during monthly hydrographic cruises. The ?A, which is representative of calcification efficiency, is determined by dividing individual foraminiferal shell weights (±0.43 µg) by their associated silhouette areas and taking the sample average. The results of this study show a strong correlation between ?A and ambient [CO32?] for both G. ruber and G. sacculifer (R2?=?0.89 and 0.86, respectively), confirming that [CO32?] has a pronounced effect on the calcification of these species. Though the ?A for both species reveal a highly significant (p?<?0.001) relationship with ambient [CO32?], linear regression reveals that the extent to which [CO32?] influences foraminiferal calcification is species specific. Hierarchical regression analyses indicate that other environmental parameters (temperature and [PO43?]) do not confound the use of G. ruber and G. sacculifer ?A as a predictor for [CO32?]. This study suggests that G. ruber and G. sacculifer ?A can be used as reliable proxies for past surface ocean [CO32?]. |
format |
Article in Journal/Newspaper |
author |
Marshall, Brittney J. Thunell, Robert C. Henehan, Michael J. Astor, Yrene Wejnert, Katherine E. |
spellingShingle |
Marshall, Brittney J. Thunell, Robert C. Henehan, Michael J. Astor, Yrene Wejnert, Katherine E. Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series |
author_facet |
Marshall, Brittney J. Thunell, Robert C. Henehan, Michael J. Astor, Yrene Wejnert, Katherine E. |
author_sort |
Marshall, Brittney J. |
title |
Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series |
title_short |
Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series |
title_full |
Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series |
title_fullStr |
Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series |
title_full_unstemmed |
Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series |
title_sort |
planktonic foraminiferal area density as a proxy for carbonate ion concentration: a calibration study using the cariaco basin ocean time series |
publishDate |
2013 |
url |
https://eprints.soton.ac.uk/355634/ |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
Marshall, Brittney J., Thunell, Robert C., Henehan, Michael J., Astor, Yrene and Wejnert, Katherine E. (2013) Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series. Paleoceanography, 28 (2), 363-376. (doi:10.1002/palo.20034 <http://dx.doi.org/10.1002/palo.20034>). |
op_doi |
https://doi.org/10.1002/palo.20034 |
container_title |
Paleoceanography |
container_volume |
28 |
container_issue |
2 |
container_start_page |
363 |
op_container_end_page |
376 |
_version_ |
1772819028699512832 |