δ 18 O and δ 13 C of planktonic foraminifer Globigerinoides ruber: Effects of test size sampling and laboratory treatment

The effects of test size sampling and ultrasonic cleaning on stable oxygen (delta O-18) and carbon (delta C-13) isotopes of planktonic foraminifera (Globigerinoides ruber) were evaluated in this study. The G. ruber tests observed under the scanning electron microscope show that shells can be complet...

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Published in:Palaeoworld
Main Authors: Xu, Ye, Li, Bao-Hua
Format: Report
Language:English
Published: ELSEVIER 2024
Subjects:
Online Access:http://ir.nigpas.ac.cn/handle/332004/43543
https://doi.org/10.1016/j.palwor.2023.01.012
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record_format openpolar
spelling ftchinacscnigpas:oai:ir.nigpas.ac.cn:332004/43543 2024-06-23T07:56:16+00:00 δ 18 O and δ 13 C of planktonic foraminifer Globigerinoides ruber: Effects of test size sampling and laboratory treatment Xu, Ye Li, Bao-Hua 2024-03-01 http://ir.nigpas.ac.cn/handle/332004/43543 https://doi.org/10.1016/j.palwor.2023.01.012 英语 eng ELSEVIER PALAEOWORLD http://ir.nigpas.ac.cn/handle/332004/43543 doi:10.1016/j.palwor.2023.01.012 Cleaning method test size stable isotope planktonic foraminifera Globigerinoides ruber ISOTOPIC COMPOSITION STABLE-ISOTOPES DIFFERENTIAL DISSOLUTION CORE-TOPS SURFACE CARBON TEMPERATURE OXYGEN FRACTIONATION CYCLES Paleontology 期刊论文 2024 ftchinacscnigpas https://doi.org/10.1016/j.palwor.2023.01.012 2024-05-27T23:37:00Z The effects of test size sampling and ultrasonic cleaning on stable oxygen (delta O-18) and carbon (delta C-13) isotopes of planktonic foraminifera (Globigerinoides ruber) were evaluated in this study. The G. ruber tests observed under the scanning electron microscope show that shells can be completely cleaned only through cracking and ultrasonic cleaning. We found that there is no statistically significant effect of cleaning on obtaining more stable and reliable delta O-18 values of G. ruber, suggesting cracking and ultrasonic cleaning may be unnecessary before isotope analysis. Five size ranges were chosen to investigate the delta O-18 and delta C-13 differences in test size. The results show that there is a positive correlation between the delta C-13 value and test size. No obvious delta O-18 difference is observed for the size range from 150 mu m to 355 mu m, though a stronger delta O-18 depletion exists for the coarser fraction (> 355 mu m). To obtain more consistent and accurate stable isotopes, and considering the size-linked delta C-13, it is recommended to select the 200-355 mu m size fraction of G. ruber with the size range as narrow as possible. (c) 2023 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved. Report Planktonic foraminifera Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences) Palaeoworld 33 1 257 266
institution Open Polar
collection Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences)
op_collection_id ftchinacscnigpas
language English
topic Cleaning method
test size
stable isotope
planktonic foraminifera
Globigerinoides ruber
ISOTOPIC COMPOSITION
STABLE-ISOTOPES
DIFFERENTIAL DISSOLUTION
CORE-TOPS
SURFACE
CARBON
TEMPERATURE
OXYGEN
FRACTIONATION
CYCLES
Paleontology
spellingShingle Cleaning method
test size
stable isotope
planktonic foraminifera
Globigerinoides ruber
ISOTOPIC COMPOSITION
STABLE-ISOTOPES
DIFFERENTIAL DISSOLUTION
CORE-TOPS
SURFACE
CARBON
TEMPERATURE
OXYGEN
FRACTIONATION
CYCLES
Paleontology
Xu, Ye
Li, Bao-Hua
δ 18 O and δ 13 C of planktonic foraminifer Globigerinoides ruber: Effects of test size sampling and laboratory treatment
topic_facet Cleaning method
test size
stable isotope
planktonic foraminifera
Globigerinoides ruber
ISOTOPIC COMPOSITION
STABLE-ISOTOPES
DIFFERENTIAL DISSOLUTION
CORE-TOPS
SURFACE
CARBON
TEMPERATURE
OXYGEN
FRACTIONATION
CYCLES
Paleontology
description The effects of test size sampling and ultrasonic cleaning on stable oxygen (delta O-18) and carbon (delta C-13) isotopes of planktonic foraminifera (Globigerinoides ruber) were evaluated in this study. The G. ruber tests observed under the scanning electron microscope show that shells can be completely cleaned only through cracking and ultrasonic cleaning. We found that there is no statistically significant effect of cleaning on obtaining more stable and reliable delta O-18 values of G. ruber, suggesting cracking and ultrasonic cleaning may be unnecessary before isotope analysis. Five size ranges were chosen to investigate the delta O-18 and delta C-13 differences in test size. The results show that there is a positive correlation between the delta C-13 value and test size. No obvious delta O-18 difference is observed for the size range from 150 mu m to 355 mu m, though a stronger delta O-18 depletion exists for the coarser fraction (> 355 mu m). To obtain more consistent and accurate stable isotopes, and considering the size-linked delta C-13, it is recommended to select the 200-355 mu m size fraction of G. ruber with the size range as narrow as possible. (c) 2023 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
format Report
author Xu, Ye
Li, Bao-Hua
author_facet Xu, Ye
Li, Bao-Hua
author_sort Xu, Ye
title δ 18 O and δ 13 C of planktonic foraminifer Globigerinoides ruber: Effects of test size sampling and laboratory treatment
title_short δ 18 O and δ 13 C of planktonic foraminifer Globigerinoides ruber: Effects of test size sampling and laboratory treatment
title_full δ 18 O and δ 13 C of planktonic foraminifer Globigerinoides ruber: Effects of test size sampling and laboratory treatment
title_fullStr δ 18 O and δ 13 C of planktonic foraminifer Globigerinoides ruber: Effects of test size sampling and laboratory treatment
title_full_unstemmed δ 18 O and δ 13 C of planktonic foraminifer Globigerinoides ruber: Effects of test size sampling and laboratory treatment
title_sort δ 18 o and δ 13 c of planktonic foraminifer globigerinoides ruber: effects of test size sampling and laboratory treatment
publisher ELSEVIER
publishDate 2024
url http://ir.nigpas.ac.cn/handle/332004/43543
https://doi.org/10.1016/j.palwor.2023.01.012
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation PALAEOWORLD
http://ir.nigpas.ac.cn/handle/332004/43543
doi:10.1016/j.palwor.2023.01.012
op_doi https://doi.org/10.1016/j.palwor.2023.01.012
container_title Palaeoworld
container_volume 33
container_issue 1
container_start_page 257
op_container_end_page 266
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