Zhijie Xu, Xiaoyu Zhang, Kongyang Zhu, Mu Huang, Miao Yu, Zheng Li, Zhongrong Qiu, Yanfang Lu
{"title":"化石与现代鱼齿元素组成、87Sr/86Sr-143Nd/144Nd对比及深海沉积物稀土元素富集意义","authors":"Zhijie Xu, Xiaoyu Zhang, Kongyang Zhu, Mu Huang, Miao Yu, Zheng Li, Zhongrong Qiu, Yanfang Lu","doi":"10.3389/fmars.2025.1534727","DOIUrl":null,"url":null,"abstract":"Fossil fish teeth are important carriers of rare earth elements (REEs) in deep-sea sediments. Meanwhile, <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr-<jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd in these fossils have been widely used in paleoceanography. However, when and how REEs enter the fish teeth remains ambiguous, which hinders elucidating the enrichment mechanism of REEs in deep-sea sediments, and the effectiveness of <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr-<jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd in paleoceanography is doubted. This study examined the contents of REEs, major and trace elements, and <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr-<jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd in modern fish teeth and in fossil fish teeth from deep-sea sediments. The results indicated that elemental geochemical properties and a redox environment are the main factors controlling their enrichment process in fish teeth. At least three categories of trace elements are classified during two different stages (physiological process of living fish and post-deposition of fossils): (1) elements of Type I mainly belong to IA, IIA, IIIA, IVA, and transition group with active chemical properties, entering into the fish teeth during life; (2) Type II represents elements from the IA, VA, transition elements, and Actinides groups, and are enriched uninterruptedly from the living fish teeth to the post-deposition fossils with variable valences under different redox conditions; (3) Type III are elements accumulated only after deposition under oxidizing or suboxidizing and are members of Lanthanides and rare dispersed elements groups with a large atomic radius and strong chemical activity. The distinctly different enrichment processes of Sr and Nd, <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr, and <jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd in fossil fish teeth may represent different material sources and should be cautiously employed in paleoceanography. The continuous rehabilitation of <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr in fossil fish teeth after deposition would change the original <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr of seawater recorded near fish teeth but the content of Sr remains unchanged. As for <jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd, when Nd enters the fossils after deposition, the exchange of 143Nd/144Nd between particles and pore liquid gradually ceases due to the saturation of the isomorphism lattice. <jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd of fossil fish teeth may provide more information about deep seawater at the seawater-sediment interface. This study elucidates the enrichment mechanism of REEs in deep-sea sediments and the cautious utilization of <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr and <jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd of fossils is a prerequisite.","PeriodicalId":12479,"journal":{"name":"Frontiers in Marine Science","volume":"18 1","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2025-04-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Comparison of elemental composition and 87Sr/86Sr-143Nd/144Nd between fossil and modern fish teeth and the significance of the enrichment of REE in deep-sea sediments\",\"authors\":\"Zhijie Xu, Xiaoyu Zhang, Kongyang Zhu, Mu Huang, Miao Yu, Zheng Li, Zhongrong Qiu, Yanfang Lu\",\"doi\":\"10.3389/fmars.2025.1534727\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Fossil fish teeth are important carriers of rare earth elements (REEs) in deep-sea sediments. Meanwhile, <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr-<jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd in these fossils have been widely used in paleoceanography. However, when and how REEs enter the fish teeth remains ambiguous, which hinders elucidating the enrichment mechanism of REEs in deep-sea sediments, and the effectiveness of <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr-<jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd in paleoceanography is doubted. This study examined the contents of REEs, major and trace elements, and <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr-<jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd in modern fish teeth and in fossil fish teeth from deep-sea sediments. The results indicated that elemental geochemical properties and a redox environment are the main factors controlling their enrichment process in fish teeth. At least three categories of trace elements are classified during two different stages (physiological process of living fish and post-deposition of fossils): (1) elements of Type I mainly belong to IA, IIA, IIIA, IVA, and transition group with active chemical properties, entering into the fish teeth during life; (2) Type II represents elements from the IA, VA, transition elements, and Actinides groups, and are enriched uninterruptedly from the living fish teeth to the post-deposition fossils with variable valences under different redox conditions; (3) Type III are elements accumulated only after deposition under oxidizing or suboxidizing and are members of Lanthanides and rare dispersed elements groups with a large atomic radius and strong chemical activity. The distinctly different enrichment processes of Sr and Nd, <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr, and <jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd in fossil fish teeth may represent different material sources and should be cautiously employed in paleoceanography. The continuous rehabilitation of <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr in fossil fish teeth after deposition would change the original <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr of seawater recorded near fish teeth but the content of Sr remains unchanged. As for <jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd, when Nd enters the fossils after deposition, the exchange of 143Nd/144Nd between particles and pore liquid gradually ceases due to the saturation of the isomorphism lattice. <jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd of fossil fish teeth may provide more information about deep seawater at the seawater-sediment interface. This study elucidates the enrichment mechanism of REEs in deep-sea sediments and the cautious utilization of <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr and <jats:sup>143</jats:sup>Nd/<jats:sup>144</jats:sup>Nd of fossils is a prerequisite.\",\"PeriodicalId\":12479,\"journal\":{\"name\":\"Frontiers in Marine Science\",\"volume\":\"18 1\",\"pages\":\"\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2025-04-07\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Frontiers in Marine Science\",\"FirstCategoryId\":\"99\",\"ListUrlMain\":\"https://doi.org/10.3389/fmars.2025.1534727\",\"RegionNum\":2,\"RegionCategory\":\"生物学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"MARINE & FRESHWATER BIOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Frontiers in Marine Science","FirstCategoryId":"99","ListUrlMain":"https://doi.org/10.3389/fmars.2025.1534727","RegionNum":2,"RegionCategory":"生物学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"MARINE & FRESHWATER BIOLOGY","Score":null,"Total":0}
Comparison of elemental composition and 87Sr/86Sr-143Nd/144Nd between fossil and modern fish teeth and the significance of the enrichment of REE in deep-sea sediments
Fossil fish teeth are important carriers of rare earth elements (REEs) in deep-sea sediments. Meanwhile, 87Sr/86Sr-143Nd/144Nd in these fossils have been widely used in paleoceanography. However, when and how REEs enter the fish teeth remains ambiguous, which hinders elucidating the enrichment mechanism of REEs in deep-sea sediments, and the effectiveness of 87Sr/86Sr-143Nd/144Nd in paleoceanography is doubted. This study examined the contents of REEs, major and trace elements, and 87Sr/86Sr-143Nd/144Nd in modern fish teeth and in fossil fish teeth from deep-sea sediments. The results indicated that elemental geochemical properties and a redox environment are the main factors controlling their enrichment process in fish teeth. At least three categories of trace elements are classified during two different stages (physiological process of living fish and post-deposition of fossils): (1) elements of Type I mainly belong to IA, IIA, IIIA, IVA, and transition group with active chemical properties, entering into the fish teeth during life; (2) Type II represents elements from the IA, VA, transition elements, and Actinides groups, and are enriched uninterruptedly from the living fish teeth to the post-deposition fossils with variable valences under different redox conditions; (3) Type III are elements accumulated only after deposition under oxidizing or suboxidizing and are members of Lanthanides and rare dispersed elements groups with a large atomic radius and strong chemical activity. The distinctly different enrichment processes of Sr and Nd, 87Sr/86Sr, and 143Nd/144Nd in fossil fish teeth may represent different material sources and should be cautiously employed in paleoceanography. The continuous rehabilitation of 87Sr/86Sr in fossil fish teeth after deposition would change the original 87Sr/86Sr of seawater recorded near fish teeth but the content of Sr remains unchanged. As for 143Nd/144Nd, when Nd enters the fossils after deposition, the exchange of 143Nd/144Nd between particles and pore liquid gradually ceases due to the saturation of the isomorphism lattice. 143Nd/144Nd of fossil fish teeth may provide more information about deep seawater at the seawater-sediment interface. This study elucidates the enrichment mechanism of REEs in deep-sea sediments and the cautious utilization of 87Sr/86Sr and 143Nd/144Nd of fossils is a prerequisite.
期刊介绍:
Frontiers in Marine Science publishes rigorously peer-reviewed research that advances our understanding of all aspects of the environment, biology, ecosystem functioning and human interactions with the oceans. Field Chief Editor Carlos M. Duarte at King Abdullah University of Science and Technology Thuwal is supported by an outstanding Editorial Board of international researchers. This multidisciplinary open-access journal is at the forefront of disseminating and communicating scientific knowledge and impactful discoveries to researchers, academics, policy makers and the public worldwide.
With the human population predicted to reach 9 billion people by 2050, it is clear that traditional land resources will not suffice to meet the demand for food or energy, required to support high-quality livelihoods. As a result, the oceans are emerging as a source of untapped assets, with new innovative industries, such as aquaculture, marine biotechnology, marine energy and deep-sea mining growing rapidly under a new era characterized by rapid growth of a blue, ocean-based economy. The sustainability of the blue economy is closely dependent on our knowledge about how to mitigate the impacts of the multiple pressures on the ocean ecosystem associated with the increased scale and diversification of industry operations in the ocean and global human pressures on the environment. Therefore, Frontiers in Marine Science particularly welcomes the communication of research outcomes addressing ocean-based solutions for the emerging challenges, including improved forecasting and observational capacities, understanding biodiversity and ecosystem problems, locally and globally, effective management strategies to maintain ocean health, and an improved capacity to sustainably derive resources from the oceans.