Early Miocene volcanic activity and paleoenvironment conditions recorded in tephra layers of the AND-2A core (southern McMurdo Sound, Antarctica)

• Published in: Geosphere
• Main Authors: Di Roberto, A., Del Carlo, P., Rocchi, S., Panter, K. S.
• Other Authors: Di Roberto, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia, Del Carlo, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia, Rocchi, S.; Dipartimento di Scienze della Terra, Università di Pisa, Pisa, Italy, Panter, K. S.; Department of Geology, Bowling Green State University, Bowling Green, OH, 43403, USA, Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia, Dipartimento di Scienze della Terra, Università di Pisa, Pisa, Italy, Department of Geology, Bowling Green State University, Bowling Green, OH, 43403, USA
• Format: Article in Journal/Newspaper
• Language: English
• Published: Geological Society of America 2012
• Subjects: Antarctica; Volcaniclastic sediments; Paleoenvironment; Mt. Morning; Victoria Land Basin; 02. Cryosphere::02.03. Ice cores::02.03.05. Paleoclimate; 04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating; processes; transport; 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks; Antarctic; McMurdo Sound; Ross Sea; The Antarctic; Victoria Land; Antarc*
• Online Access: http://hdl.handle.net/2122/8254; https://doi.org/10.1130/GES00754.1

The ANtarctic geological DRILLing program (ANDRILL) successfully recovered 1138.54 m of core from drillhole, AND-2A, in the Ross Sea sediments (Antarctica). The core is composed of terrigenous claystones, siltstones, sandstones, conglomerates, breccias, and diamictites with abundant volcanic material. In this work we present sedimentological, morphoscopic, petrographic, and geochemical data on pyroclasts recovered from core AND-2A, which provide insights on eruption styles, volcanic sources, and environments of deposition. One pyroclastic fall deposit, 12 resedimented volcaniclastic deposits and 14 volcanogenic sedimentary deposits record a history of intense explosive volcanic activity in southern Victoria Land during the Early Miocene. Tephra were ejected during Subplinian and Plinian eruptions fed by trachytic to rhyolitic magmas and during Strombolian to Hawaiian eruptions fed by basaltic to mugearitic magmas in submarine/subglacial to subaerial environments. The long-lived Mt. Morning eruptive centre, located c. 80 km south of the drillsite, was recognized as the probable volcanic source for these products on the basis of volcanological, geochemical, and age constraints. The study of tephra in the AND-2A core provides important paleoenvironment information by revealing that the deposition of primary and moderately reworked tephra occurred in a proglacial setting under generally open water marine conditions. Published 1342-1355 3.7. Dinamica del clima e dell'oceano JCR Journal partially_open