A sedimentary DNA record of the Atacama Trench reveals biodiversity changes in the most productive marine ecosystem.
Autor: | Rivera Rosas DE; Marine Science Program, Biological and Environmental Science and Engineering Division (BESE), King Abdullah University of Science and Technology (KAUST), Thuwal, Kingdom of Saudi Arabia., Geraldi NR; Nature Metrics, Guildford, UK., Glud RN; Danish Center for Hadal Research (HADAL) and Nordcee, Department of Biology, University of Southern Denmark, Odense M, Denmark.; Tokyo University of Marine Science and Technology, Tokyo, Japan.; Danish Institute for Advanced Study (DIAS), University of Southern Denmark, Odense M, Denmark., Oguri K; Danish Center for Hadal Research (HADAL) and Nordcee, Department of Biology, University of Southern Denmark, Odense M, Denmark.; Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan., Haond SA; UMR MARBEC, University of Montpellier, IRD, Ifremer, CNRS, Sète, France., Duarte CM; Marine Science Program, Biological and Environmental Science and Engineering Division (BESE), King Abdullah University of Science and Technology (KAUST), Thuwal, Kingdom of Saudi Arabia. |
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Jazyk: | angličtina |
Zdroj: | Global change biology [Glob Chang Biol] 2024 Jul; Vol. 30 (7), pp. e17412. |
DOI: | 10.1111/gcb.17412 |
Abstrakt: | The hadopelagic environment remains highly understudied due to the inherent difficulties in sampling at these depths. The use of sediment environmental DNA (eDNA) can overcome some of these restrictions as settled and preserved DNA represent an archive of the biological communities. We use sediment eDNA to assess changes in the community within one of the world's most productive open-ocean ecosystems: the Atacama Trench. The ecosystems around the Atacama Trench have been intensively fished and are affected by climate oscillations, but the understanding of potential impacts on the marine community is limited. We sampled five sites using sediment cores at water depths from 2400 to ~8000 m. The chronologies of the sedimentary record were determined using 210 Pb (Global Change Biology© 2024 The Author(s). Global Change Biology published by John Wiley & Sons Ltd.) |
Databáze: | MEDLINE |
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