Carbon and Oxygen Isotope Records from Tridacna derasa Shells: Toward Establishing a Reliable Proxy for Sea Surface Environments
We report the carbon (δ13C) and oxygen (δ18O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The high-resolution δ13C profiles of samples from the inner shell layer on cross-sections fall within similar narrow ranges and display no regular variations o...
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| Published in | PloS one Vol. 11; no. 6; p. e0157659 |
|---|---|
| Main Authors | , , , , |
| Format | Journal Article |
| Language | English |
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United States
Public Library of Science
21.06.2016
Public Library of Science (PLoS) |
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| Abstract | We report the carbon (δ13C) and oxygen (δ18O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The high-resolution δ13C profiles of samples from the inner shell layer on cross-sections fall within similar narrow ranges and display no regular variations or trends, such as an ontogenetic trend or abrupt short-term drops likely to be related to reproductive activity. This suggests that the calcification site of this species is not likely affected by photosynthetic CO2 uptake or CO2 incorporation during respiration. The δ18O profiles show distinct seasonal cycles. The intraspecific variability in the δ18O values is small in parts of the shell precipitated in the adult stage, but is not negligible in the juvenile and senescent stages. The differences in the monthly and seasonally resolved δ18O values among shells are less than 0.51‰ and 0.76‰, respectively. The shell δ18O values are nearly identical or close to the δ18O values for aragonite precipitated in oxygen isotope equilibrium with ambient seawater (δ18OEA). The largest differences between the shell δ18O and δ18OEA values calculated from the monthly and seasonally resolved data correspond to an overestimate of the seawater temperature by as much as 1.7°C and 2.3°C, respectively. However, these differences are smaller in the adult stage (<0.25‰) than in the other stages. This small difference allows an accurate reconstruction of the seawater temperature with an error of <1.1°C. Consequently, we recommend that multiple shell records be obtained because of the non-negligible intraspecific variations in their δ18O values. Growth banding, composed of alternating narrow white bands and wide light-grey bands, is discernible on cross-sections of the inner shell layer. The δ18Oshell data indicate that they were formed in winter and the other seasons, respectively. |
|---|---|
| AbstractList | We report the carbon (δ
13
C) and oxygen (δ
18
O) isotope records of three modern
Tridacna derasa
shells from Ishigaki-jima, southwestern Japan. The high-resolution δ
13
C profiles of samples from the inner shell layer on cross-sections fall within similar narrow ranges and display no regular variations or trends, such as an ontogenetic trend or abrupt short-term drops likely to be related to reproductive activity. This suggests that the calcification site of this species is not likely affected by photosynthetic CO
2
uptake or CO
2
incorporation during respiration. The δ
18
O profiles show distinct seasonal cycles. The intraspecific variability in the δ
18
O values is small in parts of the shell precipitated in the adult stage, but is not negligible in the juvenile and senescent stages. The differences in the monthly and seasonally resolved δ
18
O values among shells are less than 0.51‰ and 0.76‰, respectively. The shell δ
18
O values are nearly identical or close to the δ
18
O values for aragonite precipitated in oxygen isotope equilibrium with ambient seawater (δ
18
O
EA
). The largest differences between the shell δ
18
O and δ
18
O
EA
values calculated from the monthly and seasonally resolved data correspond to an overestimate of the seawater temperature by as much as 1.7°C and 2.3°C, respectively. However, these differences are smaller in the adult stage (<0.25‰) than in the other stages. This small difference allows an accurate reconstruction of the seawater temperature with an error of <1.1°C. Consequently, we recommend that multiple shell records be obtained because of the non-negligible intraspecific variations in their δ
18
O values. Growth banding, composed of alternating narrow white bands and wide light-grey bands, is discernible on cross-sections of the inner shell layer. The δ
18
O
shell
data indicate that they were formed in winter and the other seasons, respectively. We report the carbon (δ 13 C) and oxygen (δ 18 O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The high-resolution δ 13 C profiles of samples from the inner shell layer on cross-sections fall within similar narrow ranges and display no regular variations or trends, such as an ontogenetic trend or abrupt short-term drops likely to be related to reproductive activity. This suggests that the calcification site of this species is not likely affected by photosynthetic CO 2 uptake or CO 2 incorporation during respiration. The δ 18 O profiles show distinct seasonal cycles. The intraspecific variability in the δ 18 O values is small in parts of the shell precipitated in the adult stage, but is not negligible in the juvenile and senescent stages. The differences in the monthly and seasonally resolved δ 18 O values among shells are less than 0.51‰ and 0.76‰, respectively. The shell δ 18 O values are nearly identical or close to the δ 18 O values for aragonite precipitated in oxygen isotope equilibrium with ambient seawater (δ 18 O EA ). The largest differences between the shell δ 18 O and δ 18 O EA values calculated from the monthly and seasonally resolved data correspond to an overestimate of the seawater temperature by as much as 1.7°C and 2.3°C, respectively. However, these differences are smaller in the adult stage (<0.25‰) than in the other stages. This small difference allows an accurate reconstruction of the seawater temperature with an error of <1.1°C. Consequently, we recommend that multiple shell records be obtained because of the non-negligible intraspecific variations in their δ 18 O values. Growth banding, composed of alternating narrow white bands and wide light-grey bands, is discernible on cross-sections of the inner shell layer. The δ 18 O shell data indicate that they were formed in winter and the other seasons, respectively. We report the carbon ([delta].sup.13 C) and oxygen ([delta].sup.18 O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The high-resolution [delta].sup.13 C profiles of samples from the inner shell layer on cross-sections fall within similar narrow ranges and display no regular variations or trends, such as an ontogenetic trend or abrupt short-term drops likely to be related to reproductive activity. This suggests that the calcification site of this species is not likely affected by photosynthetic CO.sub.2 uptake or CO.sub.2 incorporation during respiration. The [delta].sup.18 O profiles show distinct seasonal cycles. The intraspecific variability in the [delta].sup.18 O values is small in parts of the shell precipitated in the adult stage, but is not negligible in the juvenile and senescent stages. The differences in the monthly and seasonally resolved [delta].sup.18 O values among shells are less than 0.51â° and 0.76â°, respectively. The shell [delta].sup.18 O values are nearly identical or close to the [delta].sup.18 O values for aragonite precipitated in oxygen isotope equilibrium with ambient seawater ([delta].sup.18 O.sub.EA). The largest differences between the shell [delta].sup.18 O and [delta].sup.18 O.sub.EA values calculated from the monthly and seasonally resolved data correspond to an overestimate of the seawater temperature by as much as 1.7°C and 2.3°C, respectively. However, these differences are smaller in the adult stage (<0.25â°) than in the other stages. This small difference allows an accurate reconstruction of the seawater temperature with an error of <1.1°C. Consequently, we recommend that multiple shell records be obtained because of the non-negligible intraspecific variations in their [delta].sup.18 O values. Growth banding, composed of alternating narrow white bands and wide light-grey bands, is discernible on cross-sections of the inner shell layer. The [delta].sup.18 O.sub.shell data indicate that they were formed in winter and the other seasons, respectively. We report the carbon (δ13C) and oxygen (δ18O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The high-resolution δ13C profiles of samples from the inner shell layer on cross-sections fall within similar narrow ranges and display no regular variations or trends, such as an ontogenetic trend or abrupt short-term drops likely to be related to reproductive activity. This suggests that the calcification site of this species is not likely affected by photosynthetic CO2 uptake or CO2 incorporation during respiration. The δ18O profiles show distinct seasonal cycles. The intraspecific variability in the δ18O values is small in parts of the shell precipitated in the adult stage, but is not negligible in the juvenile and senescent stages. The differences in the monthly and seasonally resolved δ18O values among shells are less than 0.51‰ and 0.76‰, respectively. The shell δ18O values are nearly identical or close to the δ18O values for aragonite precipitated in oxygen isotope equilibrium with ambient seawater (δ18OEA). The largest differences between the shell δ18O and δ18OEA values calculated from the monthly and seasonally resolved data correspond to an overestimate of the seawater temperature by as much as 1.7°C and 2.3°C, respectively. However, these differences are smaller in the adult stage (<0.25‰) than in the other stages. This small difference allows an accurate reconstruction of the seawater temperature with an error of <1.1°C. Consequently, we recommend that multiple shell records be obtained because of the non-negligible intraspecific variations in their δ18O values. Growth banding, composed of alternating narrow white bands and wide light-grey bands, is discernible on cross-sections of the inner shell layer. The δ18Oshell data indicate that they were formed in winter and the other seasons, respectively. We report the carbon (δ13C) and oxygen (δ18O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The high-resolution δ13C profiles of samples from the inner shell layer on cross-sections fall within similar narrow ranges and display no regular variations or trends, such as an ontogenetic trend or abrupt short-term drops likely to be related to reproductive activity. This suggests that the calcification site of this species is not likely affected by photosynthetic CO2 uptake or CO2 incorporation during respiration. The δ18O profiles show distinct seasonal cycles. The intraspecific variability in the δ18O values is small in parts of the shell precipitated in the adult stage, but is not negligible in the juvenile and senescent stages. The differences in the monthly and seasonally resolved δ18O values among shells are less than 0.51‰ and 0.76‰, respectively. The shell δ18O values are nearly identical or close to the δ18O values for aragonite precipitated in oxygen isotope equilibrium with ambient seawater (δ18OEA). The largest differences between the shell δ18O and δ18OEA values calculated from the monthly and seasonally resolved data correspond to an overestimate of the seawater temperature by as much as 1.7°C and 2.3°C, respectively. However, these differences are smaller in the adult stage (<0.25‰) than in the other stages. This small difference allows an accurate reconstruction of the seawater temperature with an error of <1.1°C. Consequently, we recommend that multiple shell records be obtained because of the non-negligible intraspecific variations in their δ18O values. Growth banding, composed of alternating narrow white bands and wide light-grey bands, is discernible on cross-sections of the inner shell layer. The δ18Oshell data indicate that they were formed in winter and the other seasons, respectively. We report the carbon ([delta]13C) and oxygen ([delta]18O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The high-resolution [delta]13C profiles of samples from the inner shell layer on cross-sections fall within similar narrow ranges and display no regular variations or trends, such as an ontogenetic trend or abrupt short-term drops likely to be related to reproductive activity. This suggests that the calcification site of this species is not likely affected by photosynthetic CO2 uptake or CO2 incorporation during respiration. The [delta]18O profiles show distinct seasonal cycles. The intraspecific variability in the [delta]18O values is small in parts of the shell precipitated in the adult stage, but is not negligible in the juvenile and senescent stages. The differences in the monthly and seasonally resolved [delta]18O values among shells are less than 0.51ppt and 0.76ppt, respectively. The shell [delta]18O values are nearly identical or close to the [delta]18O values for aragonite precipitated in oxygen isotope equilibrium with ambient seawater ([delta]18OEA). The largest differences between the shell [delta]18O and [delta]18OEA values calculated from the monthly and seasonally resolved data correspond to an overestimate of the seawater temperature by as much as 1.7 degree C and 2.3 degree C, respectively. However, these differences are smaller in the adult stage (<0.25ppt) than in the other stages. This small difference allows an accurate reconstruction of the seawater temperature with an error of <1.1 degree C. Consequently, we recommend that multiple shell records be obtained because of the non-negligible intraspecific variations in their [delta]18O values. Growth banding, composed of alternating narrow white bands and wide light-grey bands, is discernible on cross-sections of the inner shell layer. The [delta]18Oshell data indicate that they were formed in winter and the other seasons, respectively. |
| Audience | Academic |
| Author | Iryu, Yasufumi Takayanagi, Hideko Yamanashi, Junpei Asami, Ryuji Isaji, Ayaka |
| AuthorAffiliation | University of California, UNITED STATES 3 Department of Earth Science, Faculty of Science, University of the Ryukyus, 1 Senbaru, Nishihara, Okinawa, Japan 2 Department of Earth & Planetary Sciences, Graduate School of Environmental Studies, Nagoya University, Furo-cho, Chikusa-ku, Nagoya, Japan 1 Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Aobayama, Sendai, Japan |
| AuthorAffiliation_xml | – name: University of California, UNITED STATES – name: 1 Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Aobayama, Sendai, Japan – name: 2 Department of Earth & Planetary Sciences, Graduate School of Environmental Studies, Nagoya University, Furo-cho, Chikusa-ku, Nagoya, Japan – name: 3 Department of Earth Science, Faculty of Science, University of the Ryukyus, 1 Senbaru, Nishihara, Okinawa, Japan |
| Author_xml | – sequence: 1 givenname: Junpei surname: Yamanashi fullname: Yamanashi, Junpei organization: Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Aobayama, Sendai, Japan – sequence: 2 givenname: Hideko surname: Takayanagi fullname: Takayanagi, Hideko organization: Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Aobayama, Sendai, Japan – sequence: 3 givenname: Ayaka surname: Isaji fullname: Isaji, Ayaka organization: Department of Earth & Planetary Sciences, Graduate School of Environmental Studies, Nagoya University, Furo-cho, Chikusa-ku, Nagoya, Japan – sequence: 4 givenname: Ryuji surname: Asami fullname: Asami, Ryuji organization: Department of Earth Science, Faculty of Science, University of the Ryukyus, 1 Senbaru, Nishihara, Okinawa, Japan – sequence: 5 givenname: Yasufumi orcidid: 0000-0002-6099-0662 surname: Iryu fullname: Iryu, Yasufumi organization: Institute of Geology and Paleontology, Graduate School of Science, Tohoku University, Aobayama, Sendai, Japan |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/27327430$$D View this record in MEDLINE/PubMed |
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| Copyright | COPYRIGHT 2016 Public Library of Science 2016 Yamanashi et al. This is an open access article distributed under the terms of the Creative Commons Attribution License: http://creativecommons.org/licenses/by/4.0/ (the “License”), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License. 2016 Yamanashi et al 2016 Yamanashi et al |
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| DOI | 10.1371/journal.pone.0157659 |
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| Issue | 6 |
| Language | English |
| License | This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Creative Commons Attribution License |
| LinkModel | DirectLink |
| MergedId | FETCHMERGED-LOGICAL-a865t-a3ce78b13935a22e9b996a7ca8493b0ecfe1072ab4c81861e52bab40a101a8733 |
| Notes | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 Competing Interests: The authors have declared that no competing interests exist. Conceived and designed the experiments: HT RA YI. Performed the experiments: JY HT AI. Analyzed the data: JY HT RA YI. Contributed reagents/materials/analysis tools: YI. Wrote the paper: JY HT RA YI. |
| ORCID | 0000-0002-6099-0662 |
| OpenAccessLink | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4915723/ |
| PMID | 27327430 |
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| PublicationDate | 2016-06-21 |
| PublicationDateYYYYMMDD | 2016-06-21 |
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| PublicationYear | 2016 |
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| Snippet | We report the carbon (δ13C) and oxygen (δ18O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The... We report the carbon ([delta].sup.13 C) and oxygen ([delta].sup.18 O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern... We report the carbon ([delta]13C) and oxygen ([delta]18O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The... We report the carbon (δ 13 C) and oxygen (δ 18 O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The... We report the carbon (δ 13 C) and oxygen (δ 18 O) isotope records of three modern Tridacna derasa shells from Ishigaki-jima, southwestern Japan. The... |
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| SubjectTerms | Analysis Animal Shells - chemistry Animals Aragonite Archives & records Banding Biology and Life Sciences Bivalvia Bivalvia - chemistry Calcification Carbon Carbon - analysis Carbon dioxide Carbon Isotopes Chemical analysis Climate Climate change Coral reefs Cross sections Earth Sciences Geography Geology Growth models Islands Isotopes Japan Medicine and Health Sciences Metabolism Mollusca Mytilus edulis Oceans and Seas Ontogeny Oxygen Oxygen - analysis Oxygen Isotopes Paleontology Photosynthesis Physical Sciences Salinity Science Seasonal variability Seawater Shells Studies Surface Properties Temperature Tridacna derasa Water analysis |
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| Title | Carbon and Oxygen Isotope Records from Tridacna derasa Shells: Toward Establishing a Reliable Proxy for Sea Surface Environments |
| URI | https://www.ncbi.nlm.nih.gov/pubmed/27327430 https://www.proquest.com/docview/1798776880/abstract/ https://search.proquest.com/docview/1799213391 https://search.proquest.com/docview/1808629677 https://pubmed.ncbi.nlm.nih.gov/PMC4915723 https://doaj.org/article/b95286df153448ae94da385f9de26360 http://dx.doi.org/10.1371/journal.pone.0157659 |
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