Data from: Degradation of internal organic matter is the main control on pteropod shell dissolution after death

The potential for preservation of thecosome pteropods is thought to be largely governed by the chemical stability of their delicate aragonitic shells in seawater. However, sediment trap studies have found that significant carbonate dissolution can occur above the carbonate saturation horizon. Here w...

Full description

Bibliographic Details
Main Authors: Oakes, Rosie L., Peck, Victoria L., Manno, Clara, Bralower, Timothy J.
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2019
Subjects:
Online Access:https://doi.org/10.5061/dryad.8ts30t5
id ftzenodo:oai:zenodo.org:4973649
record_format openpolar
spelling ftzenodo:oai:zenodo.org:4973649 2024-09-15T17:46:09+00:00 Data from: Degradation of internal organic matter is the main control on pteropod shell dissolution after death Oakes, Rosie L. Peck, Victoria L. Manno, Clara Bralower, Timothy J. 2019-05-09 https://doi.org/10.5061/dryad.8ts30t5 unknown Zenodo https://doi.org/10.1029/2019GB006223 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.8ts30t5 oai:zenodo.org:4973649 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode taphonomy Limacina helicina antarctica Modern decay pteropod Holocene info:eu-repo/semantics/other 2019 ftzenodo https://doi.org/10.5061/dryad.8ts30t510.1029/2019GB006223 2024-07-26T21:53:53Z The potential for preservation of thecosome pteropods is thought to be largely governed by the chemical stability of their delicate aragonitic shells in seawater. However, sediment trap studies have found that significant carbonate dissolution can occur above the carbonate saturation horizon. Here we present the results from experiments conducted on two cruises to the Scotia Sea to directly test whether the breakdown of the organic pteropod body influences shell dissolution. We find that, on the timescales of three to thirteen days, the oxidation of organic matter within the shells of dead pteropods is a stronger driver of shell dissolution than the saturation state of seawater. Three to four days after death, shells became milky white and nano‐SEM images reveal smoothing of internal surface features and increased shell porosity, both indicative of aragonite dissolution. These findings have implications for the interpretation of the condition of pteropod shells from sediment traps and the fossil record, as well as for understanding the processes controlling particulate carbonate export from the surface ocean. Ambient seawater (omega 1.40) - live File contains 5 folders with the reconstructed CT data (*.DICOM format) and scan set-up information (*.pca format) for the 5 live specimens of L.helicina antarctica incubated for 13 days in ambient seawater (omega aragonite = 1.40) 1) Ambient seawater (omega 1.40) - live.zip Ambient seawater (omega 1.40) - decay File contains 5 folders with the reconstructed CT data (*.DICOM format) and scan set-up information (*.pca format) for the 5 decaying specimens of L.helicina antarctica incubated for 13 days in ambient seawater (omega aragonite = 1.40) 2) Ambient seawater (omega 1.40) - decay.zip Slightly undersaturated seawater (omega 0.89) - decay File contains 5 folders with the reconstructed CT data (*.DICOM format) and scan set-up information (*.pca format) for the 5 decaying specimens of L.helicina antarctica incubated for 13 days in seawater adjusted to an aragonite ... Other/Unknown Material Antarc* Antarctica Limacina helicina Scotia Sea Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic taphonomy
Limacina helicina antarctica
Modern
decay
pteropod
Holocene
spellingShingle taphonomy
Limacina helicina antarctica
Modern
decay
pteropod
Holocene
Oakes, Rosie L.
Peck, Victoria L.
Manno, Clara
Bralower, Timothy J.
Data from: Degradation of internal organic matter is the main control on pteropod shell dissolution after death
topic_facet taphonomy
Limacina helicina antarctica
Modern
decay
pteropod
Holocene
description The potential for preservation of thecosome pteropods is thought to be largely governed by the chemical stability of their delicate aragonitic shells in seawater. However, sediment trap studies have found that significant carbonate dissolution can occur above the carbonate saturation horizon. Here we present the results from experiments conducted on two cruises to the Scotia Sea to directly test whether the breakdown of the organic pteropod body influences shell dissolution. We find that, on the timescales of three to thirteen days, the oxidation of organic matter within the shells of dead pteropods is a stronger driver of shell dissolution than the saturation state of seawater. Three to four days after death, shells became milky white and nano‐SEM images reveal smoothing of internal surface features and increased shell porosity, both indicative of aragonite dissolution. These findings have implications for the interpretation of the condition of pteropod shells from sediment traps and the fossil record, as well as for understanding the processes controlling particulate carbonate export from the surface ocean. Ambient seawater (omega 1.40) - live File contains 5 folders with the reconstructed CT data (*.DICOM format) and scan set-up information (*.pca format) for the 5 live specimens of L.helicina antarctica incubated for 13 days in ambient seawater (omega aragonite = 1.40) 1) Ambient seawater (omega 1.40) - live.zip Ambient seawater (omega 1.40) - decay File contains 5 folders with the reconstructed CT data (*.DICOM format) and scan set-up information (*.pca format) for the 5 decaying specimens of L.helicina antarctica incubated for 13 days in ambient seawater (omega aragonite = 1.40) 2) Ambient seawater (omega 1.40) - decay.zip Slightly undersaturated seawater (omega 0.89) - decay File contains 5 folders with the reconstructed CT data (*.DICOM format) and scan set-up information (*.pca format) for the 5 decaying specimens of L.helicina antarctica incubated for 13 days in seawater adjusted to an aragonite ...
format Other/Unknown Material
author Oakes, Rosie L.
Peck, Victoria L.
Manno, Clara
Bralower, Timothy J.
author_facet Oakes, Rosie L.
Peck, Victoria L.
Manno, Clara
Bralower, Timothy J.
author_sort Oakes, Rosie L.
title Data from: Degradation of internal organic matter is the main control on pteropod shell dissolution after death
title_short Data from: Degradation of internal organic matter is the main control on pteropod shell dissolution after death
title_full Data from: Degradation of internal organic matter is the main control on pteropod shell dissolution after death
title_fullStr Data from: Degradation of internal organic matter is the main control on pteropod shell dissolution after death
title_full_unstemmed Data from: Degradation of internal organic matter is the main control on pteropod shell dissolution after death
title_sort data from: degradation of internal organic matter is the main control on pteropod shell dissolution after death
publisher Zenodo
publishDate 2019
url https://doi.org/10.5061/dryad.8ts30t5
genre Antarc*
Antarctica
Limacina helicina
Scotia Sea
genre_facet Antarc*
Antarctica
Limacina helicina
Scotia Sea
op_relation https://doi.org/10.1029/2019GB006223
https://zenodo.org/communities/dryad
https://doi.org/10.5061/dryad.8ts30t5
oai:zenodo.org:4973649
op_rights info:eu-repo/semantics/openAccess
Creative Commons Zero v1.0 Universal
https://creativecommons.org/publicdomain/zero/1.0/legalcode
op_doi https://doi.org/10.5061/dryad.8ts30t510.1029/2019GB006223
_version_ 1810494130479955968