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Changing sediment supply during glacial-interglacial intervals in the North Atlantic revealed by particle size characterization and environmental magnetism

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Autor(es):
Leone, Stephanie ; Palcu, Dan, V ; Srivastava, Priyeshu ; Bin Hassan, Muhammad ; Muraszko, Joy R. ; Jovane, Luigi
Número total de Autores: 6
Tipo de documento: Artigo Científico
Fonte: GLOBAL AND PLANETARY CHANGE; v. 220, p. 14-pg., 2023-01-05.
Resumo

The Pliocene-Pleistocene transition is characterized by an abundance of Ice-Rafted Debris (IRD) in the North Atlantic basin. One of the regions affected by IRD during this period is the Gardar Drift, where the DSDP Leg 94 Hole 611A is located. This region received sediments from different sources during the glacial and interglacial intervals (e.g., Iceland and Greenland). We analyzed grain size and particle-size specific magnetic properties of sediments for their provenance characterization between-2.64 and 2.52 Ma. Our results show that major proportion of bulk sediments during both glacial and interglacial periods were made up of basaltic-rich Icelandic sediments, whereas only during intense glacial periods (Marine Isotope Stages 100 and 104), a small proportion of non-basaltic sand compositions were identified, possibly sourced from Greenland and other non-basaltic provenance. The non-basaltic sand fractions during the intense glacial periods were likely supplied as IRDs. In addition, a new level of coarse lithics (38 pcs. of >1 mm) composed of different rocks types (e.g., basalt, granite, granodiorite etc.) were identified in DSDP 611A Hole during the end of MIS 104 glacial period. The coarse lithic fragments showed distinctive magnetic properties than rest of the particle sizes and were classified as Iceberg-Rafted Debris (IBRD). Overall, our results show that higher sand percentage was found during the intense glacial episodes, and their magnetic grain size analysis could help in distinguishing their provenance. We elaborate that particle size specific magnetic measurements of sand fractions could help in rapidly characterizing the glacial episodes in the subpolar North Atlantic. (AU)

Processo FAPESP: 18/20733-6 - Análise paleomagnética nos arquivos sedimentares de oceanos e mares epicontinentais para estudar estratificação dos oceanos e anoxia
Beneficiário:Dan Valentin Palcu Rollier
Modalidade de apoio: Bolsas no Brasil - Pós-Doutorado
Processo FAPESP: 17/04821-0 - Análise magnetostratigráfica de depósitos de ferromanganês
Beneficiário:Muhammad Bin Hassan
Modalidade de apoio: Bolsas no Brasil - Doutorado Direto
Processo FAPESP: 19/11364-0 - Investigando a acidificação dos oceanos durante o final do Maastrichtiano e início do Daniano a partir de seções marinhas do Brasil e da Índia: Implicações para o impacto versus o papel do vulcanismo na extinção em massa do limite do Cretáceo-Paleogeno.
Beneficiário:Priyeshu Srivastava
Modalidade de apoio: Bolsas no Brasil - Pós-Doutorado
Processo FAPESP: 16/24946-9 - Mudanças do nível do mar e o Sistema Monçônico Global: avaliação através de testemunhos marinhos no Brasil
Beneficiário:Luigi Jovane
Modalidade de apoio: Auxílio à Pesquisa - Programa de Pesquisa sobre Mudanças Climáticas Globais - Temático