Migration Route of <i>Sthenoteuthis oualaniensis</i> in the South China Sea Based on Statolith Trace Element Information

<i>Sthenoteuthis oualaniensis</i> (Lesson, 1830) is a pelagic species with a complex population structure and wide migration range. The trace elements in statoliths are effective indicators for reconstructing the life history of an individual. In this study, the trace elements in statoli...

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Main Authors: Jiangtao Fan, Zhou Fang, Shengwei Ma, Peng Zhang, Xue Feng, Zuozhi Chen
Format: Article
Language:English
Published: MDPI AG 2023-09-01
Series:Animals
Subjects:
Online Access:https://www.mdpi.com/2076-2615/13/18/2811
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author Jiangtao Fan
Zhou Fang
Shengwei Ma
Peng Zhang
Xue Feng
Zuozhi Chen
author_facet Jiangtao Fan
Zhou Fang
Shengwei Ma
Peng Zhang
Xue Feng
Zuozhi Chen
author_sort Jiangtao Fan
collection DOAJ
description <i>Sthenoteuthis oualaniensis</i> (Lesson, 1830) is a pelagic species with a complex population structure and wide migration range. The trace elements in statoliths are effective indicators for reconstructing the life history of an individual. In this study, the trace elements in statoliths were determined via laser ablation inductively coupled plasma mass spectrometry, and a multiple regression tree (MRT) model was used to trace the migration of <i>S. oualaniensis</i> and identify its potential habitats in the South China Sea. Na, Mg, Fe, Sr, and Ba were the effective trace elements, with significant differences found among stocks (<i>p</i> < 0.05). The MRT was divided into five clusters representing five life history stages. The Mg:Ca and Sr:Ca ratios decreased initially and increased thereafter, and the Mg:Ca, Sr:Ca, and Ba:Ca ratios differed significantly among the stages of the life history in each stock (<i>p</i> < 0.05). The hatching water temperatures for the winter and summer–autumn spawning populations were 28.05–28.88 °C (temperature at 25 m) and 27.15–27.92 °C (temperature at 25 m). The winter stock hatched in the southern South China Sea, and the larvae then migrated northwest during the summer monsoon. The summer–autumn stocks hatched in the northern South China Sea, and the larvae migrated southward under the mesoscale closed anticyclonic circulation in the northern South China Sea. These results provide insight into the migration of <i>S. oualaniensis</i> in the South China Sea.
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spelling doaj.art-fe7f0ad1a13d424fb9467a75af6821ae2023-11-19T09:13:57ZengMDPI AGAnimals2076-26152023-09-011318281110.3390/ani13182811Migration Route of <i>Sthenoteuthis oualaniensis</i> in the South China Sea Based on Statolith Trace Element InformationJiangtao Fan0Zhou Fang1Shengwei Ma2Peng Zhang3Xue Feng4Zuozhi Chen5South China Sea Fisheries Research Institute, Guangzhou 510300, ChinaCollege of Marine Sciences, Shanghai Ocean University, Shanghai 201306, ChinaSouth China Sea Fisheries Research Institute, Guangzhou 510300, ChinaSouth China Sea Fisheries Research Institute, Guangzhou 510300, ChinaSouth China Sea Fisheries Research Institute, Guangzhou 510300, ChinaSouth China Sea Fisheries Research Institute, Guangzhou 510300, China<i>Sthenoteuthis oualaniensis</i> (Lesson, 1830) is a pelagic species with a complex population structure and wide migration range. The trace elements in statoliths are effective indicators for reconstructing the life history of an individual. In this study, the trace elements in statoliths were determined via laser ablation inductively coupled plasma mass spectrometry, and a multiple regression tree (MRT) model was used to trace the migration of <i>S. oualaniensis</i> and identify its potential habitats in the South China Sea. Na, Mg, Fe, Sr, and Ba were the effective trace elements, with significant differences found among stocks (<i>p</i> < 0.05). The MRT was divided into five clusters representing five life history stages. The Mg:Ca and Sr:Ca ratios decreased initially and increased thereafter, and the Mg:Ca, Sr:Ca, and Ba:Ca ratios differed significantly among the stages of the life history in each stock (<i>p</i> < 0.05). The hatching water temperatures for the winter and summer–autumn spawning populations were 28.05–28.88 °C (temperature at 25 m) and 27.15–27.92 °C (temperature at 25 m). The winter stock hatched in the southern South China Sea, and the larvae then migrated northwest during the summer monsoon. The summer–autumn stocks hatched in the northern South China Sea, and the larvae migrated southward under the mesoscale closed anticyclonic circulation in the northern South China Sea. These results provide insight into the migration of <i>S. oualaniensis</i> in the South China Sea.https://www.mdpi.com/2076-2615/13/18/2811South China Sea<i>Sthenoteuthis oualaniensis</i>statolithtrace elementmigration route
spellingShingle Jiangtao Fan
Zhou Fang
Shengwei Ma
Peng Zhang
Xue Feng
Zuozhi Chen
Migration Route of <i>Sthenoteuthis oualaniensis</i> in the South China Sea Based on Statolith Trace Element Information
Animals
South China Sea
<i>Sthenoteuthis oualaniensis</i>
statolith
trace element
migration route
title Migration Route of <i>Sthenoteuthis oualaniensis</i> in the South China Sea Based on Statolith Trace Element Information
title_full Migration Route of <i>Sthenoteuthis oualaniensis</i> in the South China Sea Based on Statolith Trace Element Information
title_fullStr Migration Route of <i>Sthenoteuthis oualaniensis</i> in the South China Sea Based on Statolith Trace Element Information
title_full_unstemmed Migration Route of <i>Sthenoteuthis oualaniensis</i> in the South China Sea Based on Statolith Trace Element Information
title_short Migration Route of <i>Sthenoteuthis oualaniensis</i> in the South China Sea Based on Statolith Trace Element Information
title_sort migration route of i sthenoteuthis oualaniensis i in the south china sea based on statolith trace element information
topic South China Sea
<i>Sthenoteuthis oualaniensis</i>
statolith
trace element
migration route
url https://www.mdpi.com/2076-2615/13/18/2811
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