{"database":"biostudies-literature","file_versions":[],"scores":null,"additional":{"submitter":["Barkley AE"],"funding":["NSF","NSF (NSF)","Storke Endowment of the Department of Earth and Environmental Sciences, Columbia University","G. Unger Vetlesen Foundation","G. Unger Vetlesen Foundation (The G. Unger Vetlesen Foundation)","Swiss NSF Postdoctoral Fellowship","Lamont Postdoctoral Fellowship"],"pagination":["e2402120121"],"full_dataset_link":["https://www.ebi.ac.uk/biostudies/studies/S-EPMC11295081"],"repository":["biostudies-literature"],"omics_type":["Unknown"],"volume":["121(31)"],"pubmed_abstract":["Disentangling inputs of aeolian dust, ice-rafted debris (IRD), and eroded continental detritus delivered by ocean currents to marine sediments provide important insights into Earth System processes and climate. This study uses Sr-Nd-Pb isotope ratios of the continent-derived (lithogenic) fraction in deep-sea core TN057-6 from the subantarctic Southern Ocean southwest of Africa over the past 150,000 y to identify source regions and quantify their relative contributions and fluxes utilizing a mixing model set in a Bayesian framework. The data are compared with proxies from parallel core Ocean Drilling Program Site 1090 and newly presented data from potential South America aeolian dust source areas (PSAs), allowing for an integrated investigation into atmospheric, oceanic, and cryospheric dyn"],"journal":["Proceedings of the National Academy of Sciences of the United States of America"],"pubmed_title":["Patagonian dust, Agulhas Current, and Antarctic ice-rafted debris contributions to the South Atlantic Ocean over the past 150,000 years."],"pmcid":["PMC11295081"],"funding_grant_id":["OCE 0823507","NA","OPP 1204050"],"pubmed_authors":["Koffman BG","Anderson RF","Goldstein SL","Winckler G","Middleton JL","Calabozo F","Cai Y","Longman J","Kaplan MR","Barkley AE","Recasens C","Bolge L"],"additional_accession":[]},"is_claimable":false,"name":"Patagonian dust, Agulhas Current, and Antarctic ice-rafted debris contributions to the South Atlantic Ocean over the past 150,000 years.","description":"Disentangling inputs of aeolian dust, ice-rafted debris (IRD), and eroded continental detritus delivered by ocean currents to marine sediments provide important insights into Earth System processes and climate. This study uses Sr-Nd-Pb isotope ratios of the continent-derived (lithogenic) fraction in deep-sea core TN057-6 from the subantarctic Southern Ocean southwest of Africa over the past 150,000 y to identify source regions and quantify their relative contributions and fluxes utilizing a mixing model set in a Bayesian framework. The data are compared with proxies from parallel core Ocean Drilling Program Site 1090 and newly presented data from potential South America aeolian dust source areas (PSAs), allowing for an integrated investigation into atmospheric, oceanic, and cryospheric dyn","dates":{"release":"2024-01-01T00:00:00Z","publication":"2024 Jul","modification":"2026-06-02T20:00:50.177Z","creation":"2025-04-03T23:36:37.507Z"},"accession":"S-EPMC11295081","cross_references":{"pubmed":["39042680"],"doi":["10.1073/pnas.2402120121"]}}