The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal
Seasonal changes in temperature and habitat migration both leave large imprints on the stable oxygen isotope composition (818O) of planktonic foraminiferal tests, but little is known about how much the depth habitat change affects the calcite 818O on seasonal timescales, potentially introducing nume...
Published in: | Geochimica et Cosmochimica Acta |
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Online Access: | http://ir.nigpas.ac.cn/handle/332004/40858 https://doi.org/10.1016/j.gca.2022.04.014 |
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ftchinacscnigpas:oai:ir.nigpas.ac.cn:332004/40858 2023-05-15T18:00:45+02:00 The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal Yu, Zhoufei Li, Baohua Li, Hongliang Zhang, Jingling Chen, Jianfang 2022-06-15 http://ir.nigpas.ac.cn/handle/332004/40858 https://doi.org/10.1016/j.gca.2022.04.014 英语 eng PERGAMON-ELSEVIER SCIENCE LTD GEOCHIMICA ET COSMOCHIMICA ACTA http://ir.nigpas.ac.cn/handle/332004/40858 doi:10.1016/j.gca.2022.04.014 Sediment trap Planktonic foraminifera Stable oxygen isotope Seasonal variation Depth migration SOUTH CHINA SEA VERTICAL-DISTRIBUTION SEDIMENT TRAPS DELTA-O-18 TEMPERATURE PACIFIC VARIABILITY SURFACE BASIN MG/CA Geochemistry & Geophysics 期刊论文 2022 ftchinacscnigpas https://doi.org/10.1016/j.gca.2022.04.014 2022-07-22T00:11:05Z Seasonal changes in temperature and habitat migration both leave large imprints on the stable oxygen isotope composition (818O) of planktonic foraminiferal tests, but little is known about how much the depth habitat change affects the calcite 818O on seasonal timescales, potentially introducing numerous errors to the study of seasonality applied individual foraminifera. In this study, two time series sediment trap moorings deployed in the northern South China Sea (SCS) from July 2012 to April 2013 and southern SCS (upwelling area) from April to October 2014 were used to infer seasonal calcification depth variations for four commonly used planktonic foraminiferal species, Globigerinoides ruber, Trilobatus sacculifer, without a sac-like final chamber, Pulleniatina obliquiloculata and Neogloboquadrina dutertrei by analyzing their test 818O values. The findings demonstrate that planktonic foraminifera deposit their tests shallower in the winter and during cold water upwelling activity, and deeper in the summer, with a changing seasonal depth habitat for all species that tends to follow the isothermals. More importantly, we devised a new approach for quantifying the effect of seasonal calcification depth changes on the 818O signature of planktonic foraminiferal tests. After applying this method to our trap site and nine other published global sediment trap sites, the results show that foraminiferal seasonal 818O signal is strongly distorted (amplified or damped) by seasonal variations in their habitat depth, particularly for the species living in low latitude, attributed to the strong vertical temperature gradient relative to the seasonal temperature change at a given water depth. Surface water species that live in the homogeneous mixed layer may be able to provide the most comprehensive seasonality information. (c) 2022 Elsevier Ltd. All rights reserved. Report Planktonic foraminifera Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences) Pacific Geochimica et Cosmochimica Acta 327 34 52 |
institution |
Open Polar |
collection |
Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences) |
op_collection_id |
ftchinacscnigpas |
language |
English |
topic |
Sediment trap Planktonic foraminifera Stable oxygen isotope Seasonal variation Depth migration SOUTH CHINA SEA VERTICAL-DISTRIBUTION SEDIMENT TRAPS DELTA-O-18 TEMPERATURE PACIFIC VARIABILITY SURFACE BASIN MG/CA Geochemistry & Geophysics |
spellingShingle |
Sediment trap Planktonic foraminifera Stable oxygen isotope Seasonal variation Depth migration SOUTH CHINA SEA VERTICAL-DISTRIBUTION SEDIMENT TRAPS DELTA-O-18 TEMPERATURE PACIFIC VARIABILITY SURFACE BASIN MG/CA Geochemistry & Geophysics Yu, Zhoufei Li, Baohua Li, Hongliang Zhang, Jingling Chen, Jianfang The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal |
topic_facet |
Sediment trap Planktonic foraminifera Stable oxygen isotope Seasonal variation Depth migration SOUTH CHINA SEA VERTICAL-DISTRIBUTION SEDIMENT TRAPS DELTA-O-18 TEMPERATURE PACIFIC VARIABILITY SURFACE BASIN MG/CA Geochemistry & Geophysics |
description |
Seasonal changes in temperature and habitat migration both leave large imprints on the stable oxygen isotope composition (818O) of planktonic foraminiferal tests, but little is known about how much the depth habitat change affects the calcite 818O on seasonal timescales, potentially introducing numerous errors to the study of seasonality applied individual foraminifera. In this study, two time series sediment trap moorings deployed in the northern South China Sea (SCS) from July 2012 to April 2013 and southern SCS (upwelling area) from April to October 2014 were used to infer seasonal calcification depth variations for four commonly used planktonic foraminiferal species, Globigerinoides ruber, Trilobatus sacculifer, without a sac-like final chamber, Pulleniatina obliquiloculata and Neogloboquadrina dutertrei by analyzing their test 818O values. The findings demonstrate that planktonic foraminifera deposit their tests shallower in the winter and during cold water upwelling activity, and deeper in the summer, with a changing seasonal depth habitat for all species that tends to follow the isothermals. More importantly, we devised a new approach for quantifying the effect of seasonal calcification depth changes on the 818O signature of planktonic foraminiferal tests. After applying this method to our trap site and nine other published global sediment trap sites, the results show that foraminiferal seasonal 818O signal is strongly distorted (amplified or damped) by seasonal variations in their habitat depth, particularly for the species living in low latitude, attributed to the strong vertical temperature gradient relative to the seasonal temperature change at a given water depth. Surface water species that live in the homogeneous mixed layer may be able to provide the most comprehensive seasonality information. (c) 2022 Elsevier Ltd. All rights reserved. |
format |
Report |
author |
Yu, Zhoufei Li, Baohua Li, Hongliang Zhang, Jingling Chen, Jianfang |
author_facet |
Yu, Zhoufei Li, Baohua Li, Hongliang Zhang, Jingling Chen, Jianfang |
author_sort |
Yu, Zhoufei |
title |
The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal |
title_short |
The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal |
title_full |
The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal |
title_fullStr |
The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal |
title_full_unstemmed |
The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal |
title_sort |
influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal |
publisher |
PERGAMON-ELSEVIER SCIENCE LTD |
publishDate |
2022 |
url |
http://ir.nigpas.ac.cn/handle/332004/40858 https://doi.org/10.1016/j.gca.2022.04.014 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
GEOCHIMICA ET COSMOCHIMICA ACTA http://ir.nigpas.ac.cn/handle/332004/40858 doi:10.1016/j.gca.2022.04.014 |
op_doi |
https://doi.org/10.1016/j.gca.2022.04.014 |
container_title |
Geochimica et Cosmochimica Acta |
container_volume |
327 |
container_start_page |
34 |
op_container_end_page |
52 |
_version_ |
1766169965690355712 |