{"title":"极地硅藻在过渡带中消失","authors":"Natalia Llopis Monferrer","doi":"10.1038/s41561-024-01620-0","DOIUrl":null,"url":null,"abstract":"The intense, efficient transfer of organic carbon from the surface to the deep Southern Ocean make it a key component of the global carbon cycle. Observations show that this process isn’t always driven by sinking diatom skeletons, which often don’t make it past the mid-depth twilight zone, challenging the understanding of how climate change may impact the region.","PeriodicalId":19053,"journal":{"name":"Nature Geoscience","volume":"18 1","pages":"5-6"},"PeriodicalIF":15.7000,"publicationDate":"2024-12-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Polar diatoms fade in the twilight zone\",\"authors\":\"Natalia Llopis Monferrer\",\"doi\":\"10.1038/s41561-024-01620-0\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The intense, efficient transfer of organic carbon from the surface to the deep Southern Ocean make it a key component of the global carbon cycle. Observations show that this process isn’t always driven by sinking diatom skeletons, which often don’t make it past the mid-depth twilight zone, challenging the understanding of how climate change may impact the region.\",\"PeriodicalId\":19053,\"journal\":{\"name\":\"Nature Geoscience\",\"volume\":\"18 1\",\"pages\":\"5-6\"},\"PeriodicalIF\":15.7000,\"publicationDate\":\"2024-12-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Nature Geoscience\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.nature.com/articles/s41561-024-01620-0\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Nature Geoscience","FirstCategoryId":"89","ListUrlMain":"https://www.nature.com/articles/s41561-024-01620-0","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
The intense, efficient transfer of organic carbon from the surface to the deep Southern Ocean make it a key component of the global carbon cycle. Observations show that this process isn’t always driven by sinking diatom skeletons, which often don’t make it past the mid-depth twilight zone, challenging the understanding of how climate change may impact the region.
期刊介绍：
Nature Geoscience is a monthly interdisciplinary journal that gathers top-tier research spanning Earth Sciences and related fields.
The journal covers all geoscience disciplines, including fieldwork, modeling, and theoretical studies.
Topics include atmospheric science, biogeochemistry, climate science, geobiology, geochemistry, geoinformatics, remote sensing, geology, geomagnetism, paleomagnetism, geomorphology, geophysics, glaciology, hydrology, limnology, mineralogy, oceanography, paleontology, paleoclimatology, paleoceanography, petrology, planetary science, seismology, space physics, tectonics, and volcanology.
Nature Geoscience upholds its commitment to publishing significant, high-quality Earth Sciences research through fair, rapid, and rigorous peer review, overseen by a team of full-time professional editors.
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