Further processing options
available via online resource

High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods

Saved in:

Bibliographic Details
Journal Title: The Journal of Geology
Authors and Corporations: Rodland, David L., Kowalewski, Michał, Dettman, David L., Flessa, Karl W., Atudorei, Viorel, Sharp, Zachary D.
In: The Journal of Geology, 111, 2003, 4, p. 441-453
Type of Resource: E-Article
Language: English
published:
author_facet Rodland, David L.
Kowalewski, Michał
Dettman, David L.
Flessa, Karl W.
Atudorei, Viorel
Sharp, Zachary D.
Rodland, David L.
Kowalewski, Michał
Dettman, David L.
Flessa, Karl W.
Atudorei, Viorel
Sharp, Zachary D.
author Rodland, David L.
Kowalewski, Michał
Dettman, David L.
Flessa, Karl W.
Atudorei, Viorel
Sharp, Zachary D.
spellingShingle Rodland, David L.
Kowalewski, Michał
Dettman, David L.
Flessa, Karl W.
Atudorei, Viorel
Sharp, Zachary D.
The Journal of Geology
High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
author_sort rodland, david l.
spelling Rodland, David L. Kowalewski, Michał Dettman, David L. Flessa, Karl W. Atudorei, Viorel Sharp, Zachary D. 0022-1376 1537-5269 The University of Chicago Press https://www.jstor.org/stable/10.1086/375283 <label>Abstract</label> <p>Laser ablation and silver phosphate procedures were used to measure the oxygen isotope composition in organophosphatic shells of lingulid brachiopods at a variety of scales: within valves, between valves from the same individual, between individuals collected at the same location at the same time, between localities, and between modern and fossil specimens. Specimens included modern lingulids from several patches in the northern Gulf of California (Mexico) and the Gulf of Nicoya (Costa Rica), and fossil specimens from the lower Triassic Dinwoody Formation. All specimens display a high degree of intrashell variability, frequently exceeding 4‰. This variability is not symmetrical within the shell, does not appear to reflect growth bands, and is not consistent with a published lingulid phosphate‐oxygen isotope thermometer. Shells analyzed using silver phosphate preparations have variability similar (&gt;3.5‰) to that of shells analyzed using the laser ablation technique, ruling out the influence of organic carbon contamination. We interpret this variation as primary, representing a vital effect, possibly the result of enzymatic fractionation near mantle canals and muscle scars or in vivo mineralogical changes in shell composition. In contrast, oxygen isotope analysis of carbonate from these shells is repeatable and appears to represent equilibrium values. Although oxygen isotope analyses from laser ablation and silver phosphate methods indicate that the phosphate in lingulid valves is an unreliable recorder of oxygen isotope ratios in seawater, it may be possible to derive paleoclimate data from the carbonate fraction.</p> High‐Resolution Analysis of δ<sup>18</sup>O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods The Journal of Geology
doi_str_mv 10.1086/375283
facet_avail Online
format ElectronicArticle
fullrecord {"finc.format":"ElectronicArticle","finc.mega_collection":["sid-55-col-jstoras6","JSTOR Arts \u0026 Sciences VI Archive"],"finc.id":"ai-55-aHR0cHM6Ly93d3cuanN0b3Iub3JnL3N0YWJsZS8xMC4xMDg2LzM3NTI4Mw","finc.record_id":"10.1086/375283","finc.source_id":"55","ris.type":"EJOUR","rft.atitle":"High‐Resolution Analysis of δ\u003csup\u003e18\u003c/sup\u003eO in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods","rft.epage":"453","rft.genre":"article","rft.issn":["0022-1376","1537-5269"],"rft.issue":"4","rft.jtitle":"The Journal of Geology","rft.tpages":"12","rft.pages":"441-453","rft.pub":["The University of Chicago Press"],"rft.date":"2003-07-01","x.date":"2003-07-01T00:00:00Z","rft.spage":"441","rft.volume":"111","abstract":"\u003clabel\u003eAbstract\u003c/label\u003e\n \u003cp\u003eLaser ablation and silver phosphate procedures were used to measure the oxygen isotope composition in organophosphatic shells of lingulid brachiopods at a variety of scales: within valves, between valves from the same individual, between individuals collected at the same location at the same time, between localities, and between modern and fossil specimens. Specimens included modern lingulids from several patches in the northern Gulf of California (Mexico) and the Gulf of Nicoya (Costa Rica), and fossil specimens from the lower Triassic Dinwoody Formation. All specimens display a high degree of intrashell variability, frequently exceeding 4‰. This variability is not symmetrical within the shell, does not appear to reflect growth bands, and is not consistent with a published lingulid phosphate‐oxygen isotope thermometer. Shells analyzed using silver phosphate preparations have variability similar (\u0026gt;3.5‰) to that of shells analyzed using the laser ablation technique, ruling out the influence of organic carbon contamination. We interpret this variation as primary, representing a vital effect, possibly the result of enzymatic fractionation near mantle canals and muscle scars or in vivo mineralogical changes in shell composition. In contrast, oxygen isotope analysis of carbonate from these shells is repeatable and appears to represent equilibrium values. Although oxygen isotope analyses from laser ablation and silver phosphate methods indicate that the phosphate in lingulid valves is an unreliable recorder of oxygen isotope ratios in seawater, it may be possible to derive paleoclimate data from the carbonate fraction.\u003c/p\u003e","authors":[{"rft.aulast":"Rodland","rft.aufirst":"David L."},{"rft.aulast":"Kowalewski","rft.aufirst":"Michał"},{"rft.aulast":"Dettman","rft.aufirst":"David L."},{"rft.aulast":"Flessa","rft.aufirst":"Karl W."},{"rft.aulast":"Atudorei","rft.aufirst":"Viorel"},{"rft.aulast":"Sharp","rft.aufirst":"Zachary D."}],"doi":"10.1086/375283","languages":["eng"],"url":["https://www.jstor.org/stable/10.1086/375283"],"version":"0.9","x.labels":["DE-D13","DE-15"]}
id ai-55-aHR0cHM6Ly93d3cuanN0b3Iub3JnL3N0YWJsZS8xMC4xMDg2LzM3NTI4Mw
institution DE-D13
DE-15
imprint The University of Chicago Press, 2003
imprint_str_mv The University of Chicago Press, 2003
issn 0022-1376
1537-5269
issn_str_mv 0022-1376
1537-5269
language English
mega_collection JSTOR Arts & Sciences VI Archive
match_str rodland2003highresolutionanalysisofd18ointhebiogenicphosphateofmodernandfossillingulidbrachiopods
publishDateSort 2003
publisher The University of Chicago Press
record_id 10.1086/375283
recordtype is
record_format is
series The Journal of Geology
source_id 55
title High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_unstemmed High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_full High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_fullStr High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_full_unstemmed High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_short High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_sort high‐resolution analysis of δ18o in the biogenic phosphate of modern and fossil lingulid brachiopods
url https://www.jstor.org/stable/10.1086/375283
https://doi.org/10.1086/375283
publishDate 2003
physical 441-453
description Abstract Laser ablation and silver phosphate procedures were used to measure the oxygen isotope composition in organophosphatic shells of lingulid brachiopods at a variety of scales: within valves, between valves from the same individual, between individuals collected at the same location at the same time, between localities, and between modern and fossil specimens. Specimens included modern lingulids from several patches in the northern Gulf of California (Mexico) and the Gulf of Nicoya (Costa Rica), and fossil specimens from the lower Triassic Dinwoody Formation. All specimens display a high degree of intrashell variability, frequently exceeding 4‰. This variability is not symmetrical within the shell, does not appear to reflect growth bands, and is not consistent with a published lingulid phosphate‐oxygen isotope thermometer. Shells analyzed using silver phosphate preparations have variability similar (&gt;3.5‰) to that of shells analyzed using the laser ablation technique, ruling out the influence of organic carbon contamination. We interpret this variation as primary, representing a vital effect, possibly the result of enzymatic fractionation near mantle canals and muscle scars or in vivo mineralogical changes in shell composition. In contrast, oxygen isotope analysis of carbonate from these shells is repeatable and appears to represent equilibrium values. Although oxygen isotope analyses from laser ablation and silver phosphate methods indicate that the phosphate in lingulid valves is an unreliable recorder of oxygen isotope ratios in seawater, it may be possible to derive paleoclimate data from the carbonate fraction.
collection sid-55-col-jstoras6
container_issue 4
container_start_page 441
container_title The Journal of Geology
container_volume 111
format_de105 Article, E-Article
format_de14 Article, E-Article
format_de15 Article, E-Article
format_de520 Article, E-Article
format_de540 Article, E-Article
format_dech1 Article, E-Article
format_ded117 Article, E-Article
format_degla1 E-Article
format_del152 Buch
format_del189 Article, E-Article
format_dezi4 Article
format_dezwi2 Article, E-Article
format_finc Article, E-Article
format_nrw Article, E-Article
_version_ 1808781408801390595
geogr_code not assigned
last_indexed 2024-08-30T03:26:11.374Z
geogr_code_person not assigned
openURL url_ver=Z39.88-2004&ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fvufind.svn.sourceforge.net%3Agenerator&rft.title=High%E2%80%90Resolution+Analysis+of+%CE%B418O+in+the+Biogenic+Phosphate+of+Modern+and+Fossil+Lingulid+Brachiopods&rft.date=2003-07-01&genre=article&rft_id=info%3Adoi%2F10.1086%2F375283&issn=1537-5269&volume=111&issue=4&spage=441&epage=453&pages=441-453&jtitle=The+Journal+of+Geology&atitle=High%E2%80%90Resolution+Analysis+of+%CE%B4%3Csup%3E18%3C%2Fsup%3EO+in+the+Biogenic+Phosphate+of+Modern+and+Fossil+Lingulid+Brachiopods&aulast=Sharp&aufirst=Zachary%C2%A0D.&rft.language%5B0%5D=eng
SOLR
_version_ 1808781408801390595
author Rodland, David L., Kowalewski, Michał, Dettman, David L., Flessa, Karl W., Atudorei, Viorel, Sharp, Zachary D.
author_facet Rodland, David L., Kowalewski, Michał, Dettman, David L., Flessa, Karl W., Atudorei, Viorel, Sharp, Zachary D., Rodland, David L., Kowalewski, Michał, Dettman, David L., Flessa, Karl W., Atudorei, Viorel, Sharp, Zachary D.
author_sort rodland, david l.
collection sid-55-col-jstoras6
container_issue 4
container_start_page 441
container_title The Journal of Geology
container_volume 111
description Abstract Laser ablation and silver phosphate procedures were used to measure the oxygen isotope composition in organophosphatic shells of lingulid brachiopods at a variety of scales: within valves, between valves from the same individual, between individuals collected at the same location at the same time, between localities, and between modern and fossil specimens. Specimens included modern lingulids from several patches in the northern Gulf of California (Mexico) and the Gulf of Nicoya (Costa Rica), and fossil specimens from the lower Triassic Dinwoody Formation. All specimens display a high degree of intrashell variability, frequently exceeding 4‰. This variability is not symmetrical within the shell, does not appear to reflect growth bands, and is not consistent with a published lingulid phosphate‐oxygen isotope thermometer. Shells analyzed using silver phosphate preparations have variability similar (&gt;3.5‰) to that of shells analyzed using the laser ablation technique, ruling out the influence of organic carbon contamination. We interpret this variation as primary, representing a vital effect, possibly the result of enzymatic fractionation near mantle canals and muscle scars or in vivo mineralogical changes in shell composition. In contrast, oxygen isotope analysis of carbonate from these shells is repeatable and appears to represent equilibrium values. Although oxygen isotope analyses from laser ablation and silver phosphate methods indicate that the phosphate in lingulid valves is an unreliable recorder of oxygen isotope ratios in seawater, it may be possible to derive paleoclimate data from the carbonate fraction.
doi_str_mv 10.1086/375283
facet_avail Online
format ElectronicArticle
format_de105 Article, E-Article
format_de14 Article, E-Article
format_de15 Article, E-Article
format_de520 Article, E-Article
format_de540 Article, E-Article
format_dech1 Article, E-Article
format_ded117 Article, E-Article
format_degla1 E-Article
format_del152 Buch
format_del189 Article, E-Article
format_dezi4 Article
format_dezwi2 Article, E-Article
format_finc Article, E-Article
format_nrw Article, E-Article
geogr_code not assigned
geogr_code_person not assigned
id ai-55-aHR0cHM6Ly93d3cuanN0b3Iub3JnL3N0YWJsZS8xMC4xMDg2LzM3NTI4Mw
imprint The University of Chicago Press, 2003
imprint_str_mv The University of Chicago Press, 2003
institution DE-D13, DE-15
issn 0022-1376, 1537-5269
issn_str_mv 0022-1376, 1537-5269
language English
last_indexed 2024-08-30T03:26:11.374Z
match_str rodland2003highresolutionanalysisofd18ointhebiogenicphosphateofmodernandfossillingulidbrachiopods
mega_collection JSTOR Arts & Sciences VI Archive
physical 441-453
publishDate 2003
publishDateSort 2003
publisher The University of Chicago Press
record_format is
record_id 10.1086/375283
recordtype is
series The Journal of Geology
source_id 55
spelling Rodland, David L. Kowalewski, Michał Dettman, David L. Flessa, Karl W. Atudorei, Viorel Sharp, Zachary D. 0022-1376 1537-5269 The University of Chicago Press https://www.jstor.org/stable/10.1086/375283 <label>Abstract</label> <p>Laser ablation and silver phosphate procedures were used to measure the oxygen isotope composition in organophosphatic shells of lingulid brachiopods at a variety of scales: within valves, between valves from the same individual, between individuals collected at the same location at the same time, between localities, and between modern and fossil specimens. Specimens included modern lingulids from several patches in the northern Gulf of California (Mexico) and the Gulf of Nicoya (Costa Rica), and fossil specimens from the lower Triassic Dinwoody Formation. All specimens display a high degree of intrashell variability, frequently exceeding 4‰. This variability is not symmetrical within the shell, does not appear to reflect growth bands, and is not consistent with a published lingulid phosphate‐oxygen isotope thermometer. Shells analyzed using silver phosphate preparations have variability similar (&gt;3.5‰) to that of shells analyzed using the laser ablation technique, ruling out the influence of organic carbon contamination. We interpret this variation as primary, representing a vital effect, possibly the result of enzymatic fractionation near mantle canals and muscle scars or in vivo mineralogical changes in shell composition. In contrast, oxygen isotope analysis of carbonate from these shells is repeatable and appears to represent equilibrium values. Although oxygen isotope analyses from laser ablation and silver phosphate methods indicate that the phosphate in lingulid valves is an unreliable recorder of oxygen isotope ratios in seawater, it may be possible to derive paleoclimate data from the carbonate fraction.</p> High‐Resolution Analysis of δ<sup>18</sup>O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods The Journal of Geology
spellingShingle Rodland, David L., Kowalewski, Michał, Dettman, David L., Flessa, Karl W., Atudorei, Viorel, Sharp, Zachary D., The Journal of Geology, High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_full High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_fullStr High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_full_unstemmed High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_short High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
title_sort high‐resolution analysis of δ18o in the biogenic phosphate of modern and fossil lingulid brachiopods
title_unstemmed High‐Resolution Analysis of δ18O in the Biogenic Phosphate of Modern and Fossil Lingulid Brachiopods
url https://www.jstor.org/stable/10.1086/375283, https://doi.org/10.1086/375283