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G-Cubed: Geochemistry, Geophysics, Geosystems; an electronic journal of the Earth sciences

 

Keywords

  • 40Ar/39Ar geochronology
  • seamounts
  • guyots
  • submarine alteration
  • Pacific plate
  • hot spots

Index Terms

  • Geochemistry: Geochronology
  • Marine Geology and Geophysics: Plate tectonics
  • Tectonophysics: Dynamics, convection currents and mantle plumes
Abstract
Cited By
 

Abstract

Implications of a nonlinear 40Ar/39Ar age progression along the Louisville seamount trail for models of fixed and moving hot spots

Anthony A. P. Koppers

Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093-0225, USA

Robert A. Duncan

College of Oceanic and Atmospheric Sciences, Oregon State University, 104 Ocean Administration Building, Corvallis, OR 97331-5503, USA

Bernhard Steinberger

IFREE, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima-cho, Yokosuka-shi, Kanagawa 237-0061, Japan

The Louisville seamount trail has been recognized as one of the key examples of hot spot volcanism, comparable to the classic volcanic Hawaiian-Emperor lineaments. The published total fusion 40Ar/39Ar data of Watts et al. [1988] showed an astonishing linear age progression, firmly establishing Louisville as a fixed hot spot in the South Pacific mantle. We report new 40Ar/39Ar ages based on high-resolution incremental heating 40Ar/39Ar dating for the same group of samples, showing a marked increase in both precision and accuracy. One of the key findings in our reexamination is that the age progression is not linear after all. The new data show a significantly decreased “apparent” plate velocity for the Louisville seamount trail older than 62 Ma but confirm the linear trend between 47 Ma and the present day (although based on only three samples over 2150 km). The most recent volcanic activity in the Louisville seamount trail has now been dated at 1.11 ± 0.04 Ma for the most southeastern seamount located at 50°26′S and 139°09′W. These results indicate that the Louisville age progression should be interpreted on the basis of both plate and hot spot motion. In this paper we examine our new results in conjunction with the numerical mantle flow models of Steinberger et al. [2004] that also predict marked deviations from simple linear age progressions. With these models we can achieve a good fit to the geometry of both the Hawaiian and Louisville seamount trails and their age progressions as well as the ∼15° paleolatitudinal shift observed by Tarduno et al. [2003] for the Hawaiian hot spot between 80 and 47 Ma. If the model is restricted to Pacific hot spots only, we can improve the fit to the nonlinear age trend for the Louisville seamount trail by allowing an additional rotation change of the Pacific plate around 62 Ma and by decreasing the initiation age of the Louisville plume from 120 to 90 Ma. This improved model features a significant eastward hot spot motion of ∼5° between 80 and 30 Ma for the Louisville hot spot, which is quite dissimilar to the southward motion of the Hawaiian hot spot during the same time interval, followed by a minor ∼2° latitudinal shift over the last 30 Myr. If hot spot tracks are considered globally, the age trend observed for the oldest part of the Louisville seamount trail does not entirely follow the numerical model predictions. This may indicate some remaining inaccuracies in the global plate circuit, but it may also indicate that the Louisville hot spot experienced a motion somewhat different than in the numerical model: faster in the interval between 62 and 47 Ma but slower before that.

Received 3 December 2003; accepted 30 April 2004; published 19 June 2004.

Citation: Koppers, A. A. P., R. A. Duncan, and B. Steinberger (2004), Implications of a nonlinear 40Ar/39Ar age progression along the Louisville seamount trail for models of fixed and moving hot spots, Geochem. Geophys. Geosyst., 5, Q06L02, doi:10.1029/2003GC000671.

Cited By

Duncan, Robert A. (2004), Radiometric ages for basement rocks from the Emperor Seamounts, ODP Leg 197, Geochem Geophys Geosyst, 5, Q08L03, doi:10.1029/2004GC000704.

Koppers, Anthony A. P., Hubert Staudigel, Jason Phipps Morgan, and Robert A. Duncan (2007), Nonlinear 40Ar/39Ar age systematics along the Gilbert Ridge and Tokelau Seamount Trail and the timing of the Hawaii-Emperor Bend, Geochem Geophys Geosyst, 8, Q06L13, doi:10.1029/2006GC001489.

Koppers, Anthony A.P., Jamie A. Russell, Matthew G. Jackson, Jasper Konter, Hubert Staudigel, and Stanley R. Hart (2008), Samoa reinstated as a primary hotspot trail, Geol, 36(6), 435, doi:10.1130/G24630A.1.

Steinberger, Bernhard, Rupert Sutherland, and Richard J. O'Connell (2004), Prediction of Emperor-Hawaii seamount locations from a revised model of global plate motion and mantle flow, Appl Opt, 430(6996), 167, doi:10.1038/nature02660.

Steinberger, B., and M. Antretter (2006), Conduit diameter and buoyant rising speed of mantle plumes: Implications for the motion of hot spots and shape of plume conduits, Geochem Geophys Geosyst, 7, Q11018, doi:10.1029/2006GC001409.

Steinberger, Bernhard, and Carmen Gaina (2007), Plate-tectonic reconstructions predict part of the Hawaiian hotspot track to be preserved in the Bering Sea, Geol, 35(5), 407, doi:10.1130/G23383A.1.

Torsvik, Trond H., R. Dietmar Müller, Rob Van der Voo, Bernhard Steinberger, and Carmen Gaina (2008), Global plate motion frames: Toward a unified model, Rev Geophys, 46, RG3004, doi:10.1029/2007RG000227.

Vlastélic, Ivan (2005), Initiation of a plume-ridge interaction in the South Pacific recorded by high-precision Pb isotopes along Hollister Ridge, Geochem Geophys Geosyst, 6, Q05011, doi:10.1029/2004GC000902.

Wessel, Paul, Yasushi Harada, and Loren W. Kroenke (2006), Toward a self-consistent, high-resolution absolute plate motion model for the Pacific, Geochem Geophys Geosyst, 7, Q03L12, doi:10.1029/2005GC001000.

Wessel, Paul, and Loren W. Kroenke (2008), Pacific absolute plate motion since 145 Ma: An assessment of the fixed hot spot hypothesis, J Geophys Res, 113, B06101, doi:10.1029/2007JB005499.

Wessel, Paul (2008), Hotspotting: Principles and properties of a plate tectonic Hough transform, Geochem Geophys Geosyst, 9, Q08004, doi:10.1029/2008GC002058.