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Both these signatures in the sedimentary record are determined by orbital cycles influencing glacial variability on the one hand and northern African monsoon intensity on the other hand. In this paper, we use the intermediate-complexity model CLIMBER-2 to simulate African climate during the Plio-Pleistocene between 3.2 and 2.3 million years ago (Ma) and compare our simulations with the sedimentary records of marine sediment cores from ODP Site 659 (Atlantic Ocean) and ODP Site 967 (Mediterranean). In this study we will show for the first time an extended Ti-Al record of Site 967 down to 3.2 Ma."},"dsDescriptionDate":{"typeName":"dsDescriptionDate","multiple":false,"typeClass":"primitive","value":"2021-01-20"}}]},{"typeName":"subject","multiple":true,"typeClass":"controlledVocabulary","value":["Earth and Environmental Sciences"]},{"typeName":"keyword","multiple":true,"typeClass":"compound","value":[{"keywordValue":{"typeName":"keywordValue","multiple":false,"typeClass":"primitive","value":"climate, Africa, sediments, Mediterranean, orbit"}}]},{"typeName":"publication","multiple":true,"typeClass":"compound","value":[{"publicationCitation":{"typeName":"publicationCitation","multiple":false,"typeClass":"primitive","value":"Bas de Boer, Marit Peters, and Lucas J. Lourens.\r\nThe transient impact of the African monsoon on Plio-Pleistocene Mediterranean sediments.\r\nClimate of the Past, 2021."},"publicationIDType":{"typeName":"publicationIDType","multiple":false,"typeClass":"controlledVocabulary","value":"doi"},"publicationIDNumber":{"typeName":"publicationIDNumber","multiple":false,"typeClass":"primitive","value":"10.5194/cp-2020-97"},"publicationURL":{"typeName":"publicationURL","multiple":false,"typeClass":"primitive","value":"https://doi.org/10.5194/cp-2020-97"}}]},{"typeName":"notesText","multiple":false,"typeClass":"primitive","value":"Paper is accepted, but final publication depends on data availability."},{"typeName":"depositor","multiple":false,"typeClass":"primitive","value":"Boer, de, Bas"},{"typeName":"dateOfDeposit","multiple":false,"typeClass":"primitive","value":"2021-01-20"}]},"dansDataVaultMetadata":{"displayName":"Data Vault Metadata","name":"dansDataVaultMetadata","fields":[{"typeName":"dansDataversePid","multiple":false,"typeClass":"primitive","value":"doi:10.34894/HD6E9I"},{"typeName":"dansDataversePidVersion","multiple":false,"typeClass":"primitive","value":"1.0"},{"typeName":"dansBagId","multiple":false,"typeClass":"primitive","value":"urn:uuid:ce7a0597-25d7-4f41-ab42-e0e3daebce76"},{"typeName":"dansNbn","multiple":false,"typeClass":"primitive","value":"urn:nbn:nl:ui:13-2268e613-e5bf-4dc6-9872-54f8a5e9ec67"}]}},"files":[{"label":"deBoer_CP_2021_model_output_and_data.xlsx","restricted":false,"version":1,"datasetVersionId":3394,"dataFile":{"id":47546,"persistentId":"","filename":"deBoer_CP_2021_model_output_and_data.xlsx","contentType":"application/vnd.openxmlformats-officedocument.spreadsheetml.sheet","friendlyType":"MS Excel Spreadsheet","filesize":636594,"storageIdentifier":"surf://store:1771f3928cf-b0ec96e21340","rootDataFileId":-1,"checksum":{"type":"SHA-1","value":"d4307dff27da1f90b2c0c7089f144da3d211afb8"},"tabularData":false,"creationDate":"2021-01-20","publicationDate":"2021-01-20","lastUpdateTime":"2021-01-20T09:58:56Z","fileAccessRequest":false}}]}}}