Magnetostratigraphic Chronology of a Cenozoic Sequence From DSDP Site 274, Ross Sea, Antarctica

• Published in: Frontiers in Earth Science
• Main Authors: Jovane, Luigi, Florindo, Fabio, Wilson, Gary, de Almeida Pecchiai Saldanha Leone, Stephanie, Hassan, Muhammad Bin, Rodelli, Daniel, Cortese, Giuseppe
• Other Authors: Fundação de Amparo à Pesquisa do Estado de São Paulo
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Frontiers Media SA 2020
• Subjects: Antarctic; Ross Sea; The Antarctic; Victoria Land; Antarc*; Antarctica; Ice Sheet
• Online Access: http://dx.doi.org/10.3389/feart.2020.563453; https://www.frontiersin.org/articles/10.3389/feart.2020.563453/full

New paleomagnetic results from the late Eocene-Middle Miocene samples from Deep Sea Drilling Project Site 274, cored during Leg 28 on the continental rise off Victoria Land, Ross Sea, provide a chronostratigraphic framework for an existing paleoclimate archive during a key period of Antarctic climate and ice sheet evolution. Based on this new age model, the cored late Eocene-Middle Miocene sequence covers an interval of almost 20 Myr (from ∼35 to ∼15 Ma). Biostratigraphic constraints allow a number of possible correlations with the Geomagnetic Polarity Time Scale. Regardless of correlation, average interval sediment accumulation rates above 260 mbsf are ∼6 cm/kyr with the record punctuated by a number of unconformities. Below 260 mbsf (across the Eocene/Oligocene boundary) interval, sedimentation accumulation rates are closer to ∼1 cm/kyr. A major unconformity identified at ∼180 mbsf represents at least 9 Myr accounting for the late Oligocene and Early Miocene and represent non-deposition and/or erosion due to intensification of Antarctic Circumpolar Current activity. Significant fluctuations in grain size and magnetic properties observed above the unconformity at 180 mbsf, in the Early Miocene portion of this sedimentary record, reflect cyclical behavior in glacial advance and retreat from the continent. Similar glacial cyclicity has already been identified in other Miocene sequences recovered in drill cores from the Antarctic margin.