{"title":"海洋科学中的铍同位素:了解洋流和冰动力学","authors":"Yusuke Yokoyama, Adam D. Sproson","doi":"10.1146/annurev-marine-040224-033226","DOIUrl":null,"url":null,"abstract":"The Earth's climate has been kept under Goldilocks conditions because a variety of feedback systems maintain the atmospheric <jats:italic>p</jats:italic>CO<jats:sub>2</jats:sub> within a narrow range. The ocean, as a large reservoir of carbon compared with the atmosphere, plays a key role in the climate system, and studying ocean process can help us better understand this system. Cosmogenic nuclides produced in the atmosphere and their ratio to a terrestrial counterpart can provide detailed depictions of Earth surface process, and they have therefore been utilized widely since it became possible to measure them with accelerator mass spectrometry. Beryllium isotopes (<jats:sup>10</jats:sup>Be<jats:inline-formula> <jats:tex-math>$/$</jats:tex-math> </jats:inline-formula> <jats:sup>9</jats:sup>Be) are one of the most useful isotope systems for this purpose. In this article, we summarize recent developments in beryllium isotope chemistry and the isotopes’ relation to ocean current and ice sheet dynamics as well as weathering in relation to long-term climate.","PeriodicalId":55508,"journal":{"name":"Annual Review of Marine Science","volume":"26 1","pages":""},"PeriodicalIF":18.9000,"publicationDate":"2025-07-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Beryllium Isotopes in Marine Science: Understanding Ocean Current and Ice Dynamics\",\"authors\":\"Yusuke Yokoyama, Adam D. Sproson\",\"doi\":\"10.1146/annurev-marine-040224-033226\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The Earth's climate has been kept under Goldilocks conditions because a variety of feedback systems maintain the atmospheric <jats:italic>p</jats:italic>CO<jats:sub>2</jats:sub> within a narrow range. The ocean, as a large reservoir of carbon compared with the atmosphere, plays a key role in the climate system, and studying ocean process can help us better understand this system. Cosmogenic nuclides produced in the atmosphere and their ratio to a terrestrial counterpart can provide detailed depictions of Earth surface process, and they have therefore been utilized widely since it became possible to measure them with accelerator mass spectrometry. Beryllium isotopes (<jats:sup>10</jats:sup>Be<jats:inline-formula> <jats:tex-math>$/$</jats:tex-math> </jats:inline-formula> <jats:sup>9</jats:sup>Be) are one of the most useful isotope systems for this purpose. In this article, we summarize recent developments in beryllium isotope chemistry and the isotopes’ relation to ocean current and ice sheet dynamics as well as weathering in relation to long-term climate.\",\"PeriodicalId\":55508,\"journal\":{\"name\":\"Annual Review of Marine Science\",\"volume\":\"26 1\",\"pages\":\"\"},\"PeriodicalIF\":18.9000,\"publicationDate\":\"2025-07-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Annual Review of Marine Science\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1146/annurev-marine-040224-033226\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Annual Review of Marine Science","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1146/annurev-marine-040224-033226","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Beryllium Isotopes in Marine Science: Understanding Ocean Current and Ice Dynamics
The Earth's climate has been kept under Goldilocks conditions because a variety of feedback systems maintain the atmospheric pCO2 within a narrow range. The ocean, as a large reservoir of carbon compared with the atmosphere, plays a key role in the climate system, and studying ocean process can help us better understand this system. Cosmogenic nuclides produced in the atmosphere and their ratio to a terrestrial counterpart can provide detailed depictions of Earth surface process, and they have therefore been utilized widely since it became possible to measure them with accelerator mass spectrometry. Beryllium isotopes (10Be$/$9Be) are one of the most useful isotope systems for this purpose. In this article, we summarize recent developments in beryllium isotope chemistry and the isotopes’ relation to ocean current and ice sheet dynamics as well as weathering in relation to long-term climate.
期刊介绍:
The Annual Review of Marine Science, published since 2009, offers a comprehensive overview of the field. It covers various disciplines, including coastal and blue water oceanography (biological, chemical, geological, and physical), ecology, conservation, and technological advancements related to the marine environment. The journal's transition from gated to open access through Annual Reviews' Subscribe to Open program ensures that all articles are available under a CC BY license, promoting wider accessibility and dissemination of knowledge.