Mariana serpentinite mud volcanism exhumes subducted seamount materials: Implications for the origin of life

Patricia Fryer; C. Geoffrey Wheat; Trevor Williams; Kevin Johnson; Christopher Kelley; Elmar Albers; John W. Shervais; Walter Kurz; Jeffrey Ryan; Barbara A. Bekins; Baptiste Debret; Jianghong Deng; Yanhui Dong; Philip Eickenbusch; Emanuelle Frery; Yuji Ichiyama; Raymond Johnston; Richard Kevorkian; Vitor Magalhaes; Simone Mantovanelli; Walter Menapace; Catriona D. Menzies; Katsuyoshi Michibayashi; Craig Moyer; Kelli Mullane; Jung-Woo Park; Roy Price; Olivier Sissmann; Shino Suzuki; Ken Takai; Bastien Walter; Rui Zhang; Diva Amon; Deborah Glickson; Shirley Pomponi

doi:10.1098/rsta.2018.0425

Mariana serpentinite mud volcanism exhumes subducted seamount materials: Implications for the origin of life

Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences

By: Patricia Fryer, C. Geoffrey Wheat, Trevor Williams, Kevin Johnson, Christopher Kelley, Elmar Albers, John W. Shervais, Walter Kurz, Jeffrey Ryan, Barbara A. Bekins, Baptiste Debret, Jianghong Deng, Yanhui Dong, Philip Eickenbusch, Emanuelle Frery, Yuji Ichiyama, Raymond Johnston, Richard Kevorkian, Vitor Magalhaes, Simone Mantovanelli, Walter Menapace, Catriona D. Menzies, Katsuyoshi Michibayashi, Craig Moyer, Kelli Mullane, Jung-Woo Park, Roy Price, Olivier Sissmann, Shino Suzuki, Ken Takai, Bastien Walter, Rui Zhang, Diva Amon, Deborah Glickson, and Shirley Pomponi

https://doi.org/10.1098/rsta.2018.0425

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Abstract

The subduction of seamounts and ridge features at convergent plate boundaries plays an important role in the deformation of the overriding plate and influences geochemical cycling and associated biological processes. Active serpentinization of forearc mantle and serpentinite mud volcanism on the Mariana forearc (between the trench and active volcanic arc) provides windows on subduction processes. Here, we present (1) the first observation of an extensive exposure of an undeformed Cretaceous seamount currently being subducted at the Mariana Trench inner slope; (2) vertical deformation of the forearc region related to subduction of Pacific Plate seamounts and thickened crust; (3) recovered Ocean Drilling Program and International Ocean Discovery Program cores of serpentinite mudflows that confirm exhumation of various Pacific Plate lithologies, including subducted reef limestone; (4) petrologic, geochemical and paleontological data from the cores that show that Pacific Plate seamount exhumation covers greater spatial and temporal extents; (5) the inference that microbial communities associated with serpentinite mud volcanism may also be exhumed from the subducted plate seafloor and/or seamounts; and (6) the implications for effects of these processes with regard to evolution of life.

Additional publication details
Publication type	Article
Publication Subtype	Journal Article
Title	Mariana serpentinite mud volcanism exhumes subducted seamount materials: Implications for the origin of life
Series title	Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
DOI	10.1098/rsta.2018.0425
Volume	378
Issue	2165
Year Published	2020
Language	English
Publisher	The Royal Society Publishing
Contributing office(s)	WMA - Earth System Processes Division
Description	20180425, 28 p.
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