The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks
- Autores
- Eagle, R. A.; Eler, J. M.; Tripati, A. K.; Res, J. B.; Freitas, P. S.; Heibental, C .; Wanamaker, A. D., Jr.; Taviani, M.; Elliot, M.; Marenssi, Sergio Alfredo; Nakamura, K.; Ramirez, P.; Roy, K .
- Año de publicación
- 2013
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The shells of marine mollusks are widely used archives of past climate and ocean chemistry. Whilst the measurement of mollusk δ 18O to develop records of past climate change is a commonly used approach, it has proven challenging to develop reliable independent paleothermometers that can be used to deconvolve the contributions of temperature and fluid composition on molluscan oxygen isotope compositions. Here we investigate the temperature dependence of 13C–18O bond abundance, denoted by the measured parameter 147, in shell carbonates of bivalve mollusks and assess its potential to be a useful paleothermometer. We report measurements on cultured specimens spanning a range in water temperatures of 5 to 25 ◦C, and field collected specimens spanning a range of −1 to 29 ◦C. In addition we investigate the potential influence of carbonate saturation state on bivalve stable isotope compositions by making measurements on both calcitic and aragonitic specimens that have been cultured in seawater that is either supersaturated or undersaturated with respect to aragonite. We find a robust relationship between 147 and growth temperature. We also find that the slope of a linear regression through all the 147 data for bivalves plotted against seawater temperature is significantly shallower than previously published inorganic and biogenic carbonate calibration studies produced in our laboratory and go on to discuss the possible sources of this difference. We find that changing seawater saturation state does not have significant effect on the 147 of bivalve shell carbonate in two taxa that we examined, and we do not observe significant differences between 147-temperature relationships between calcitic and aragonitic taxa.
Fil: Eagle, R. A.. University of California; Estados Unidos. California Institute of Technology; Estados Unidos
Fil: Eler, J. M.. California Institute of Technology; Estados Unidos
Fil: Tripati, A. K.. University of California; Estados Unidos
Fil: Res, J. B.. University Of North Carolina; Estados Unidos
Fil: Freitas, P. S.. Laboratorio Nacional de Energia e Geologia; Portugal
Fil: Heibental, C .. Geomar-helmholtz Centre For Ocean Research Kiel; Alemania
Fil: Wanamaker, A. D., Jr.. University of Iowa; Estados Unidos
Fil: Taviani, M.. Consiglio Nazionale Delle Ricerche. Istituto di Scienze Marine; Italia. Woods Hole Oceanographic Institution; Estados Unidos
Fil: Elliot, M.. Universite de Nantes; Francia
Fil: Marenssi, Sergio Alfredo. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Nakamura, K.. California State University; Estados Unidos
Fil: Ramirez, P.. California State University; Estados Unidos
Fil: Roy, K .. University of California; Estados Unidos - Materia
-
STABLE ISOTOPES
PALEOTEMPERATURES
SHELLS - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/11018
Ver los metadatos del registro completo
id |
CONICETDig_f3f3fa71aa08a203a8f943ed9cf4b3d0 |
---|---|
oai_identifier_str |
oai:ri.conicet.gov.ar:11336/11018 |
network_acronym_str |
CONICETDig |
repository_id_str |
3498 |
network_name_str |
CONICET Digital (CONICET) |
spelling |
The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusksEagle, R. A.Eler, J. M.Tripati, A. K.Res, J. B.Freitas, P. S.Heibental, C .Wanamaker, A. D., Jr.Taviani, M.Elliot, M.Marenssi, Sergio AlfredoNakamura, K.Ramirez, P.Roy, K .STABLE ISOTOPESPALEOTEMPERATURESSHELLShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The shells of marine mollusks are widely used archives of past climate and ocean chemistry. Whilst the measurement of mollusk δ 18O to develop records of past climate change is a commonly used approach, it has proven challenging to develop reliable independent paleothermometers that can be used to deconvolve the contributions of temperature and fluid composition on molluscan oxygen isotope compositions. Here we investigate the temperature dependence of 13C–18O bond abundance, denoted by the measured parameter 147, in shell carbonates of bivalve mollusks and assess its potential to be a useful paleothermometer. We report measurements on cultured specimens spanning a range in water temperatures of 5 to 25 ◦C, and field collected specimens spanning a range of −1 to 29 ◦C. In addition we investigate the potential influence of carbonate saturation state on bivalve stable isotope compositions by making measurements on both calcitic and aragonitic specimens that have been cultured in seawater that is either supersaturated or undersaturated with respect to aragonite. We find a robust relationship between 147 and growth temperature. We also find that the slope of a linear regression through all the 147 data for bivalves plotted against seawater temperature is significantly shallower than previously published inorganic and biogenic carbonate calibration studies produced in our laboratory and go on to discuss the possible sources of this difference. We find that changing seawater saturation state does not have significant effect on the 147 of bivalve shell carbonate in two taxa that we examined, and we do not observe significant differences between 147-temperature relationships between calcitic and aragonitic taxa.Fil: Eagle, R. A.. University of California; Estados Unidos. California Institute of Technology; Estados UnidosFil: Eler, J. M.. California Institute of Technology; Estados UnidosFil: Tripati, A. K.. University of California; Estados UnidosFil: Res, J. B.. University Of North Carolina; Estados UnidosFil: Freitas, P. S.. Laboratorio Nacional de Energia e Geologia; PortugalFil: Heibental, C .. Geomar-helmholtz Centre For Ocean Research Kiel; AlemaniaFil: Wanamaker, A. D., Jr.. University of Iowa; Estados UnidosFil: Taviani, M.. Consiglio Nazionale Delle Ricerche. Istituto di Scienze Marine; Italia. Woods Hole Oceanographic Institution; Estados UnidosFil: Elliot, M.. Universite de Nantes; FranciaFil: Marenssi, Sergio Alfredo. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Nakamura, K.. California State University; Estados UnidosFil: Ramirez, P.. California State University; Estados UnidosFil: Roy, K .. University of California; Estados UnidosCopernicus Publications2013-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/11018Eagle, R. A.; Eler, J. M.; Tripati, A. K.; Res, J. B.; Freitas, P. S.; et al.; The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks; Copernicus Publications; Biogeosciences; 10; 5-2013; 4591-46061726-41701726-4189enginfo:eu-repo/semantics/altIdentifier/url/http://www.biogeosciences.net/10/4591/2013/info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:46:15Zoai:ri.conicet.gov.ar:11336/11018instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 09:46:16.02CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks |
title |
The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks |
spellingShingle |
The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks Eagle, R. A. STABLE ISOTOPES PALEOTEMPERATURES SHELLS |
title_short |
The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks |
title_full |
The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks |
title_fullStr |
The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks |
title_full_unstemmed |
The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks |
title_sort |
The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks |
dc.creator.none.fl_str_mv |
Eagle, R. A. Eler, J. M. Tripati, A. K. Res, J. B. Freitas, P. S. Heibental, C . Wanamaker, A. D., Jr. Taviani, M. Elliot, M. Marenssi, Sergio Alfredo Nakamura, K. Ramirez, P. Roy, K . |
author |
Eagle, R. A. |
author_facet |
Eagle, R. A. Eler, J. M. Tripati, A. K. Res, J. B. Freitas, P. S. Heibental, C . Wanamaker, A. D., Jr. Taviani, M. Elliot, M. Marenssi, Sergio Alfredo Nakamura, K. Ramirez, P. Roy, K . |
author_role |
author |
author2 |
Eler, J. M. Tripati, A. K. Res, J. B. Freitas, P. S. Heibental, C . Wanamaker, A. D., Jr. Taviani, M. Elliot, M. Marenssi, Sergio Alfredo Nakamura, K. Ramirez, P. Roy, K . |
author2_role |
author author author author author author author author author author author author |
dc.subject.none.fl_str_mv |
STABLE ISOTOPES PALEOTEMPERATURES SHELLS |
topic |
STABLE ISOTOPES PALEOTEMPERATURES SHELLS |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The shells of marine mollusks are widely used archives of past climate and ocean chemistry. Whilst the measurement of mollusk δ 18O to develop records of past climate change is a commonly used approach, it has proven challenging to develop reliable independent paleothermometers that can be used to deconvolve the contributions of temperature and fluid composition on molluscan oxygen isotope compositions. Here we investigate the temperature dependence of 13C–18O bond abundance, denoted by the measured parameter 147, in shell carbonates of bivalve mollusks and assess its potential to be a useful paleothermometer. We report measurements on cultured specimens spanning a range in water temperatures of 5 to 25 ◦C, and field collected specimens spanning a range of −1 to 29 ◦C. In addition we investigate the potential influence of carbonate saturation state on bivalve stable isotope compositions by making measurements on both calcitic and aragonitic specimens that have been cultured in seawater that is either supersaturated or undersaturated with respect to aragonite. We find a robust relationship between 147 and growth temperature. We also find that the slope of a linear regression through all the 147 data for bivalves plotted against seawater temperature is significantly shallower than previously published inorganic and biogenic carbonate calibration studies produced in our laboratory and go on to discuss the possible sources of this difference. We find that changing seawater saturation state does not have significant effect on the 147 of bivalve shell carbonate in two taxa that we examined, and we do not observe significant differences between 147-temperature relationships between calcitic and aragonitic taxa. Fil: Eagle, R. A.. University of California; Estados Unidos. California Institute of Technology; Estados Unidos Fil: Eler, J. M.. California Institute of Technology; Estados Unidos Fil: Tripati, A. K.. University of California; Estados Unidos Fil: Res, J. B.. University Of North Carolina; Estados Unidos Fil: Freitas, P. S.. Laboratorio Nacional de Energia e Geologia; Portugal Fil: Heibental, C .. Geomar-helmholtz Centre For Ocean Research Kiel; Alemania Fil: Wanamaker, A. D., Jr.. University of Iowa; Estados Unidos Fil: Taviani, M.. Consiglio Nazionale Delle Ricerche. Istituto di Scienze Marine; Italia. Woods Hole Oceanographic Institution; Estados Unidos Fil: Elliot, M.. Universite de Nantes; Francia Fil: Marenssi, Sergio Alfredo. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Nakamura, K.. California State University; Estados Unidos Fil: Ramirez, P.. California State University; Estados Unidos Fil: Roy, K .. University of California; Estados Unidos |
description |
The shells of marine mollusks are widely used archives of past climate and ocean chemistry. Whilst the measurement of mollusk δ 18O to develop records of past climate change is a commonly used approach, it has proven challenging to develop reliable independent paleothermometers that can be used to deconvolve the contributions of temperature and fluid composition on molluscan oxygen isotope compositions. Here we investigate the temperature dependence of 13C–18O bond abundance, denoted by the measured parameter 147, in shell carbonates of bivalve mollusks and assess its potential to be a useful paleothermometer. We report measurements on cultured specimens spanning a range in water temperatures of 5 to 25 ◦C, and field collected specimens spanning a range of −1 to 29 ◦C. In addition we investigate the potential influence of carbonate saturation state on bivalve stable isotope compositions by making measurements on both calcitic and aragonitic specimens that have been cultured in seawater that is either supersaturated or undersaturated with respect to aragonite. We find a robust relationship between 147 and growth temperature. We also find that the slope of a linear regression through all the 147 data for bivalves plotted against seawater temperature is significantly shallower than previously published inorganic and biogenic carbonate calibration studies produced in our laboratory and go on to discuss the possible sources of this difference. We find that changing seawater saturation state does not have significant effect on the 147 of bivalve shell carbonate in two taxa that we examined, and we do not observe significant differences between 147-temperature relationships between calcitic and aragonitic taxa. |
publishDate |
2013 |
dc.date.none.fl_str_mv |
2013-05 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/11018 Eagle, R. A.; Eler, J. M.; Tripati, A. K.; Res, J. B.; Freitas, P. S.; et al.; The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks; Copernicus Publications; Biogeosciences; 10; 5-2013; 4591-4606 1726-4170 1726-4189 |
url |
http://hdl.handle.net/11336/11018 |
identifier_str_mv |
Eagle, R. A.; Eler, J. M.; Tripati, A. K.; Res, J. B.; Freitas, P. S.; et al.; The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks; Copernicus Publications; Biogeosciences; 10; 5-2013; 4591-4606 1726-4170 1726-4189 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://www.biogeosciences.net/10/4591/2013/ |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Copernicus Publications |
publisher.none.fl_str_mv |
Copernicus Publications |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
_version_ |
1842268781014941696 |
score |
13.13397 |