{"title":"基于高分辨率耳石 δ18O 图谱和流体力学模型的鱼类洄游史简易可视化技术","authors":"Tatsuya Sakamoto","doi":"10.1002/lol2.10434","DOIUrl":null,"url":null,"abstract":"Oxygen‐stable isotope (<jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O) in otoliths has been useful to infer marine fish migrations. However, because otolith <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O is affected by two parameters, temperature and <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O of ambient water, its interpretation becomes challenging when neither of them is constant. Here, I describe a simple method using hydrodynamic models to visualize potential migration histories from high‐resolution otolith <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O chronologies. By predicting the distribution of potential otolith <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O, that is, otolith <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O isoscape from modeled temperature and salinity distributions and comparing these with observed values, possible fish locations can be inferred. The demonstration of sardine juveniles in the western North Pacific region reproduced their seasonal northward migrations accurately. The predicted locations were consistent with the results of sampling surveys of eggs and juveniles and correctly approached the point where fish were caught. The methodological recommendations and the successful demonstration in this study may help in planning future sclerochronology research using carbonate <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O values.","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":null,"pages":null},"PeriodicalIF":5.1000,"publicationDate":"2024-10-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Simple visualization of fish migration history based on high‐resolution otolith δ18O profiles and hydrodynamic models\",\"authors\":\"Tatsuya Sakamoto\",\"doi\":\"10.1002/lol2.10434\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Oxygen‐stable isotope (<jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O) in otoliths has been useful to infer marine fish migrations. However, because otolith <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O is affected by two parameters, temperature and <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O of ambient water, its interpretation becomes challenging when neither of them is constant. Here, I describe a simple method using hydrodynamic models to visualize potential migration histories from high‐resolution otolith <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O chronologies. By predicting the distribution of potential otolith <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O, that is, otolith <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O isoscape from modeled temperature and salinity distributions and comparing these with observed values, possible fish locations can be inferred. The demonstration of sardine juveniles in the western North Pacific region reproduced their seasonal northward migrations accurately. The predicted locations were consistent with the results of sampling surveys of eggs and juveniles and correctly approached the point where fish were caught. The methodological recommendations and the successful demonstration in this study may help in planning future sclerochronology research using carbonate <jats:italic>δ</jats:italic><jats:sup>18</jats:sup>O values.\",\"PeriodicalId\":18128,\"journal\":{\"name\":\"Limnology and Oceanography Letters\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":5.1000,\"publicationDate\":\"2024-10-05\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Limnology and Oceanography Letters\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://doi.org/10.1002/lol2.10434\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"LIMNOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Limnology and Oceanography Letters","FirstCategoryId":"93","ListUrlMain":"https://doi.org/10.1002/lol2.10434","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"LIMNOLOGY","Score":null,"Total":0}
Simple visualization of fish migration history based on high‐resolution otolith δ18O profiles and hydrodynamic models
Oxygen‐stable isotope (δ18O) in otoliths has been useful to infer marine fish migrations. However, because otolith δ18O is affected by two parameters, temperature and δ18O of ambient water, its interpretation becomes challenging when neither of them is constant. Here, I describe a simple method using hydrodynamic models to visualize potential migration histories from high‐resolution otolith δ18O chronologies. By predicting the distribution of potential otolith δ18O, that is, otolith δ18O isoscape from modeled temperature and salinity distributions and comparing these with observed values, possible fish locations can be inferred. The demonstration of sardine juveniles in the western North Pacific region reproduced their seasonal northward migrations accurately. The predicted locations were consistent with the results of sampling surveys of eggs and juveniles and correctly approached the point where fish were caught. The methodological recommendations and the successful demonstration in this study may help in planning future sclerochronology research using carbonate δ18O values.
期刊介绍:
Limnology and Oceanography Letters (LO-Letters) serves as a platform for communicating the latest innovative and trend-setting research in the aquatic sciences. Manuscripts submitted to LO-Letters are expected to present high-impact, cutting-edge results, discoveries, or conceptual developments across all areas of limnology and oceanography, including their integration. Selection criteria for manuscripts include their broad relevance to the field, strong empirical and conceptual foundations, succinct and elegant conclusions, and potential to advance knowledge in aquatic sciences.