Seamounts off the West Antarctic margin: A case for non-hotspot driven intraplate volcanism

• Published in: Gondwana Research
• Main Authors: Kipf, Andrea, Hauff, Folkmar, Werner, Reinhard, Gohl, K., van den Bogaard, Paul, Hoernle, Kaj A., Maicher, Doris, Klügel, A.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2014
• Subjects: Amundsen Sea; Antarctic; Byrd; De Gerlache; De Gerlache Seamounts; Gerlache; Marie Byrd Land; New Zealand; Pacific; Peter I Island; The Antarctic; Antarc*; Antarctica
• Online Access: https://oceanrep.geomar.de/id/eprint/21843/; https://oceanrep.geomar.de/id/eprint/21843/1/Kipf%20et%20al_GR_Accepted.pdf; https://oceanrep.geomar.de/id/eprint/21843/14/Kipf.pdf; https://doi.org/10.1016/j.gr.2013.06.013

Highlights: • Marie Byrd Seamounts (MBS) formed off Antarctica at 65-56 Ma in an extensional regime • MBS originate from HIMU-type mantle attached at the base of the Antarctic lithosphere • Continental insulation flow transferred HIMU mantle into the oceanic mantle New radiometric age and geochemical data of volcanic rocks from the guyot-type Marie Byrd Seamounts (MBS) and the De Gerlache Seamounts and Peter I Island (Amundsen Sea) are presented. 40Ar/39Ar ages of the shield phase of three MBS are Early Cenozoic (65 to 56 Ma) and indicate formation well after creation of the Pacific-Antarctic Ridge. A Pliocene age (3.0 Ma) documents a younger phase of volcanism at one MBS and a Pleistocene age (1.8 Ma) for the submarine base of Peter I Island. Together with published data, the new age data imply that Cenozoic intraplate magmatism occurred at distinct time intervals in spatially confined areas of the Amundsen Sea, excluding an origin through a fixed mantle plume. Peter I Island appears strongly influenced by an EMII type mantle component that may reflect shallow mantle recycling of a continental raft during the final breakup of Gondwana. By contrast the Sr-Nd-Pb-Hf isotopic compositions of the MBS display a strong affinity to a HIMU type mantle source. On a regional scale the isotopic signatures overlap with those from volcanics related to the West Antarctic Rift System, and Cretaceous intraplate volcanics in and off New Zealand. We propose reactivation of the HIMU material, initially accreted to the base of continental lithosphere during the pre-rifting stage of Marie Byrd Land/Zealandia to explain intraplate volcanism in the Amundsen Sea in the absence of a long-lived hotspot. We propose continental insulation flow as the most plausible mechanism to transfer the sub-continental accreted plume material into the shallow oceanic mantle. Crustal extension at the southern boundary of the Bellingshausen Plate from about 74 to 62 Ma may have triggered adiabatic rise of the HIMU material from the base of Marie Byrd ...