Abstract
Linear chains of volcanic ocean islands are one of the most distinctive features on our planet. The longest, the Hawaiian–Emperor Chain, has been active for more than 80 million years, and is thought to have formed as the Pacific Plate moved across the Hawaiian mantle plume, the hottest and most productive of Earth's plumes. Volcanoes fed by the plume today form two adjacent trends, including Mauna Kea and Mauna Loa, that exhibit strikingly different geochemical characteristics. An extensive data set of isotopic analyses shows that lavas with these distinct characteristics have erupted in parallel along the Kea and Loa trends for at least 5 million years. Seismological data suggest that the Hawaiian mantle plume, when projected into the deep mantle, overlies the boundary between typical Pacific lower mantle and a sharply defined layer of apparently different material. This layer exhibits low seismic shear velocities and occurs on the Loa side of the plume. We conclude that the geochemical differences between the Kea and Loa trends reflect preferential sampling of these two distinct sources of deep mantle material. Similar indications of preferential sampling at the limit of a large anomalous low-velocity zone are found in Kerguelen and Tristan da Cunha basalts in the Indian and Atlantic oceans, respectively. We infer that the anomalous low-velocity zones at the core–mantle boundary are storing geochemical anomalies that are enriched in recycled material and sampled by strong mantle plumes.
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References
Davies, G. F. Role of the lithosphere in mantle convection. J. Geophys. Res. 93, 10451–10466 (1988).
Sleep, N. Hotspots and mantle plumes: Some phenomenology. J. Geophys. Res. 95, 6715–6736 (1990).
Richards, M. A., Duncan, R. A. & Courtillot, V. E. Flood basalts and hot-spot tracks: Plume heads and tails. Science 246, 103–107 (1989).
Montelli, R., Nolet, G., Dahlen, F. A. & Masters, G. A catalogue of deep mantle plumes: New results from finite-frequency tomography. Geochem. Geophys. Geosyst. 7, Q11007 (2006).
Morgan, W. J. Convection plumes in the lower mantle. Nature 230, 42–43 (1971).
Jellinek, A. & Manga, M. Links between long-lived hot spots, mantle plumes, D” and plate tectonics. Rev. Geophys. 42, RG3002 (2004).
DePaolo, D. J. & Weis, D. in Continental Scientific Drilling: A Decade of Progress, and Challenges for the Future (eds Harms, U., Koeberl, C. & Zoback, M. D.), Springer, pp. 259–288 (2007).
Tatsumoto, M. Isotopic composition of lead in oceanic basalt and its implication to mantle evolution. Earth Planet. Sci. Lett. 38, 63–87 (1978).
Zindler, A. & Hart, S. Chemical geodynamics. Annu. Rev. Earth Planet. Sci. 14, 493–571 (1986).
Sun, S. & McDonough, W. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes, in Magmatism in the Ocean Basins (eds Saunders, A. D. & Norry, M. J.) Geol. Soc. London Spec. Publ. 42, 313–345 (1989).
Hofmann, A. W. in The Mantle and the Core (ed. Carlson, R. W.), Treatise of Geochemistry Vol. 2 (eds. Holland H. D. & Turekian K. K.), 61–101 (Elsevier–Pergamon, 2003).
White, W. Oceanic island basalts and mantle plumes: the geochemical perspective. Annu. Rev. Earth Planet. Sci. 38, 133–160 (2010).
White, W. M. Sources of oceanic basalts — radiogenic isotopic evidence. Geology 13, 115–118 (1985).
Labrosse, S., Hernlund, J. W. & Coltice, N. A crystallizing dense magma ocean at the base of the Earth's mantle. Nature 450, 866–869 (2007).
Carlson, R. W., Boyet, M. Composition of the Earth's interior: the importance of early events. Phil. Trans. R. Soc. A 366, 4077–4103 (2008).
van Keken, P., Hauri, E. H. & Ballentine, C. J. Mantle mixing: The generation, preservation, and destruction of chemical heterogeneity. Annu. Rev. Earth Planet. Sci. 30, 493–525 (2002).
Albarède, F. & van der Hilst, R. Zoned mantle convection. Phil. Trans. R. Soc. A 360, 2569–2592 (2002).
Willbold, M. & Stracke, A. Trace element composition of mantle end-members: Implications for recycling of oceanic and upper and lower continental crust. Geochem. Geophys. Geosyst. 7, Q04004 (2006).
Willbold, M. & Stracke, A. Formation of enriched mantle components by recycling of upper and lower continental crust. Chem. Geol. 276, 188–197 (2010).
Wilson, J. T. Evidence from islands on the spreading of the ocean floor. Can. J. Phys. 41, 863–868 (1963).
Ribe, N. & Christensen, U. The dynamical origin of Hawaiian volcanism. Earth Planet. Sci. Lett. 171, 517–531 (1999).
Wolfe, C. J. et al. Mantle shear-wave velocity structure beneath the Hawaiian hot spot. Science 326, 1388–1390 (2009).
Lenardic, A. & Jellinek, A. M. Tails of two plume types in one mantle. Geology 37, 127–130 (2009).
Richards, M. A. & Griffiths, R. W. Deflection of plumes by mantle shear flow: experimental results and a simple theory. Geophys. J. 94, 367–376 (1988).
DePaolo, D. J., Bryce, J., Dodson, A., Shuster, D. & Kennedy, B. Isotopic evolution of Mauna Loa and the chemical structure of the Hawaiian plume. Geochem. Geophys. Geosyst. 2, 1044 (2001).
Kerr, R. & Mériaux, C. Structure and dynamics of sheared mantle plumes. Geochem. Geophys. Geosyst. 5, Q12009 (2004).
Abouchami, W. et al. Lead isotopes reveal bilateral asymmetry and vertical continuity in the Hawaiian mantle plume. Nature 434, 851–856 (2005).
Ren, Z., Ingle, S., Takahashi, E., Hirano, N. & Hirata, T. The chemical structure of the Hawaiian mantle plume. Nature 436, 837–840 (2005).
Farnetani, C. G. & Hofmann, A. W. Dynamics and internal structure of the Hawaiian plume. Earth Planet. Sci. Lett. 295, 231–240 (2010).
Sharp, W. & Renne, P. The 40Ar/39Ar dating of core recovered by the Hawaii Scientific Drilling Project (phase 2), Hilo, Hawaii. Geochem. Geophys. Geosyst. 6, Q04G17 (2005).
Stolper, E. M., DePaolo, D. J. & Thomas, D. M. Deep drilling into a mantle plume volcano: the Hawaii Scientific Drilling Project. Scient. Drilling 7, 4–14 (2009).
Clague D. A., Dalrymple G. B. The Hawaiian–Emperor volcanic chain Part 1. Geologic evolution. USGS Prof. Pap. 1350, 5–54 (1987).
Garcia, M. O., Caplan-Auerbach, J., De Carlo, E. H., Kurz. M. D. & Becker, N., Geology, geochemistry and earthquake history of Loihi seamount, Hawaii's youngest volcano. Chem. Erde 66, 81–108 (2006).
Blichert-Toft, J., Weis, D., Maerschalk, C., Agranier, A. & Albarède, F. Hawaiian hot spot dynamics as inferred from the Hf and Pb isotope evolution of Mauna Kea volcano. Geochem. Geophys. Geosyst. 4, 8704 (2003).
Eisele, J., Abouchami, W., Galer, S. J. G. & Hofmann, A. W. The 320 kyr Pb isotope evolution of Mauna Kea lavas recorded in the HSDP-2 drill core. Geochem. Geophys. Geosyst. 4, 8710 (2003).
Kurz, M., Curtice, J., Lott, D. & Solow, A. Rapid helium isotopic variability in Mauna Kea shield lavas from the Hawaiian Scientific Drilling Project. Geochem. Geophys. Geosyst. 5, Q04G14 (2004).
Rhodes, J. M. & Vollinger, M. J. Composition of basaltic lavas sampled by phase-2 of the Hawaii Scientific Drilling Project: Geochemical stratigraphy and magma types, Geochem. Geophys. Geosyst. 5, Q03G13 (2004).
Bryce, J., DePaolo, D. J. & Lassiter, J. Geochemical structure of the Hawaiian plume: Sr, Nd, and Os isotopes in the 2.8 km HSDP-2 section of Mauna Kea volcano. Geochem. Geophys. Geosyst. 6, Q09G18 (2005).
Dana, D. J. Geology, Report of the United States Exploring Expedition, 1838–1842, Vol. 10 (C. Sherman, Philadelphia, 1849).
Jackson, E. D., Shaw, H. R. & Bargar, K. E. Calculated geochronology and stress field orientations along the Hawaiian chain. Earth Planet. Sci. Lett. 26, 145–155 (1975).
Lassiter, J., DePaolo, D. J. & Tatsumoto, M. Isotopic evolution of Mauna Kea volcano: Results from the initial phase of the Hawaii Scientific Drilling Project. J. Geophys. Res. 101, 11769–11780 (1996).
Abouchami, W., Galer, S. J. G. & Hofmann, A. W. High precision lead isotope systematics of lavas from the Hawaiian Scientific Drilling Project. Chem. Geol. 169, 187–209 (2000).
Clague, D. A. Hawaiian alkaline volcanism. Geol. Soc. London Spec. Pub. 30, 227–252 (1987).
Ren, Z.-Y., Tomoyuki, S., Masako, Y., Johnson, K. M. & Takahashi, E. Isotope compositions of submarine Hana Ridge lavas, Haleakala volcano, Hawaii: Implications for source compositions melting process and the structure of the Hawaiian plume. J. Petrol. 47, 255–275 (2006).
Marske, J. P., Pietruszka, A. J., Weis, D., Garcia, M. O. & Rhodes, J. M. Rapid passage of a small-scale mantle heterogeneity through the melting regions of Kilauea and Mauna Loa Volcanoes. Earth Planet. Sci. Lett. 259, 34–50 (2007).
Hanano, D., Weis, D., Scoates, J. S., Aciego, S. & DePaolo, D. J. Horizontal and vertical zoning of heterogeneities in the Hawaiian mantle plume from the geochemistry of consecutive postshield volcano pairs: Kohala-Mahukona and Mauna Kea-Hualalai. Geochem. Geophys. Geosyst. 11, Q01004 (2010).
Xu, G. et al. Geochemical characteristics of West Molokai shield- and postshield-stage lavas: Constraints on Hawaiian plume models. Geochem. Geophys. Geosyst. 8, Q08G21 (2007).
Tanaka, R., Makishima, A. & Nakamura, E. Hawaiian double volcanic chain triggered by an episodic involvement of recycled material: Constraints from temporal Sr-Nd–Hf–Pb isotopic trend of the Loa-type volcanoes. Earth Planet. Sci. Lett. 265, 450–465 (2008).
Robinson, J. & Eakins, B. Calculated volumes of individual shield volcanoes at the young end of the Hawaiian Ridge. J. Volcanol. Geotherm. Res. 151, 309–317 (2006).
Garcia, M. O., Hulsebosch, T. P. & Rhodes, J. M. in Mauna Loa Revealed: Structure, Composition, History, and Hazards (eds. Rhodes, J. M. & Lockwood, J. P.), Geophys. Monogr. Ser. 92. American Geophysical Union, Washington, DC, pp. 219–239 (1995).
Jicha, B., Rhodes, J. M., Singer, B. S., Vollinger, M. J., Garcia, M. O. 40Ar/39Ar geochronology of submarine Mauna Loa volcano, Hawaii. American Geophysical Union, Fall Meeting, abstract #V43F-2328 (2009).
Wanless, V. D. et al. Submarine radial vents on Mauna Loa Volcano, Hawaii. Geochem. Geophys. Geosyst. 7, Q05001 (2006).
Rhodes, J. M. & Hart, S. R. in Mauna Loa Revealed: Structure, Composition, History, and Hazards (eds Rhodes, J. M. & Lockwood, J. P.), Geophys. Monogr. Ser. 92. 263–288 (American Geophysical Union, 1995).
Greene, A. R. et al. Low-productivity Hawaiian volcanism between Kaua'i and O'ahu. Geochem. Geophys. Geosyst. 11, Q0AC08 (2010).
Kimura, J., Sisson, T., Nakano, N., Coombs, M. & Lipman, P. Isotope geochemistry of early Kilauea magmas from the submarine Hilina bench: The nature of the Hilina mantle component. J. Volcanol. Geotherm. Res. 151, 51–72 (2006).
Chen, C., Frey, F. A., Garcia, M. O., Dalrymple, G. & Hart, S. R. The tholeiite to alkalic basalt transition at Haleakala Volcano, Maui, Hawaii. Contrib. Mineral. Petrol. 106, 183–200 (1991).
Gaffney, A., Nelson, B. & Blichert-Toft, J. Geochemical constraints on the role of oceanic lithosphere in intra-volcano heterogeneity at West Maui, Hawaii. J. Petrol. 45, 1663–1687 (2004).
Blichert-Toft, J., Frey, F. A. & Albarède, F. Hf isotope evidence for pelagic sediments in the source of Hawaiian basalts. Science 285, 879–882 (1999).
Garcia, M. O. et al. Petrology, geochemistry and geochronology of Kaua'i lavas over 4.5 Myr: implications for the origin of rejuvenated volcanism and the evolution of the Hawaiian plume. J. Petrol. 51, 1507–1540 (2010).
Garnero, E. J. & McNamara, A. Structure and dynamics of Earth's lower mantle. Science 320, 626–628 (2008).
Thorne, M., Grand, S. & Garnero, E. Geographic correlation between hot spots and deep mantle lateral shear-wave velocity gradients. Phys. Earth Planet. Inter. 176, 47–63 (2004).
Burke, K., Steinberger, B., Torsvik, T. H. & Smethurst, M. A. Plume generation zones at the margins of large low shear velocity provinces on the core–mantle boundary. Earth Planet. Sci. Lett. 265, 49–60 (2008).
Ritsema, J., van Heijst, H. & Woodhouse, J. Complex shear wave velocity structure imaged beneath Africa and Iceland. Science 286, 1925–1928 (1999).
Mégnin, C. & Romanowicz, B. The shear velocity structure of the mantle from the inversion of body, surface, and higher modes waveforms. Geophys. J. Int. 143, 709–728 (2000).
To, A., Fukao, Y. & Tsuboi, S. Evidence for a thick and localized ultra low shear velocity zone at the base of the mantle beneath the central Pacific. Phys. Earth Planet. Inter. 184, 119–133 (2011).
Garnero, E. Heterogeneity of the lowermost mantle. Annu. Rev. Earth Planet. Sci. 28, 509–537 (2000).
Ishii, M. & Tromp, J. Normal-mode and free-air gravity constraints on lateral variations in velocity and density of Earth's mantle. Science 285, 1231–1236 (1999).
Tarduno, J. et al. The Emperor Seamounts: Southward motion of the Hawaiian hotspot plume in Earth's mantle. Science 301, 1064–1069 (2003).
Wolfe, C. J. et al. Mantle P-wave velocity structure beneath the Hawaiian hotspot. Earth Planet. Sci. Lett. 303, 267–280 (2011).
Richards, M. A. & Griffiths, R. W. Thermal entrainment by deflected mantle plumes. Nature 342, 900–902 (1989).
Kerr, R. C. & Lister, J. R. Rise and deflection of mantle plume tails. Geochem. Geophys. Geosyst. 9, Q10004 (2008).
Blichert-Toft, J. & Albarède, F. Mixing of isotopic heterogeneities in the Mauna Kea plume conduit. Earth Planet. Sci. Lett. 282, 190–200 (2009).
Blake, S. & Campbell, I. The dynamics of magma-mixing during flow in volcanic conduits. Contrib. Mineral. Petrol. 94, 72–81 (1986).
Lister, J. Long-wavelength instability of a line plume. J. Fluid Mechanics 175, 413–428 (1987).
Cao, Q., der Hilst, van, R., de Hoop, M. & Shim, S. Seismic imaging of transition zone discontinuities suggests hot mantle west of Hawaii. Science 332, 1068–1071 (2011).
Olson, P. & Yuen, D. A. Thermochemical plumes and mantle phase transitions. J. Geophys. Res. 87, 3993–4002 (1982).
Hirose, K. Phase transitions in pyrolitic mantle around 670-km depth: Implications for upwelling of plumes from the lower mantle. J. Geophys. Res. 107, B42078 (2002).
Boschi, L., Becker, T. & Steinberger, B. Mantle plumes: Dynamic models and seismic images. Geochem. Geophys. Geosyst. 8, Q10006 (2007).
Bercovici, D. & Mahoney, J. Double flood basalts and plume head separation at the 660 kilometer discontinuity. Science 266, 1367–1369 (1994).
Kumagai, I. & Kurita, K. On the fate of mantle plumes at density interfaces. Earth Planet. Sci. Lett. 179, 63–71 (2000).
Lister, J. & Kerr, R. C. The propagation of two-dimensional and axisymmetric viscous gravity currents at a fluid interface. J. Fluid Mechanics 203, 215–249 (1989).
Steinberger, B., Sutherland, R. & O'Connell, R. J. Prediction of Emperor–Hawaii seamount locations from a revised model of global plate motion and mantle flow. Nature 430, 167–173 (2004).
Garnero, E., Lay, T. & McNamara, A. in Plates, Plumes, and Planetary Processes (eds Foulger, G. R. & Jurdy, D. M.), Geol. Soc. Am. Spec. Paper 430, 79–101 (2007).
Idehara, K. Structural heterogeneity of an ultra-low-velocity zone beneath the Philippine Islands: Implications for core–mantle chemical interactions induced by massive partial melting at the bottom of the mantle. Phys. Earth Planet. Inter. 184, 80–90 (2011).
McNamara, A., Garnero, E. & Rost, S. Tracking deep mantle reservoirs with ultra-low velocity zones. Earth Planet. Sci. Lett. 299, 1–9 (2010).
Williams, Q., Revenaugh, J. & Garnero, E. A correlation between ultra-low basal velocities in the mantle and hot spots. Science 281, 546–549 (1998).
Rost, S., Garnero, E., Williams, Q. & Manga, M. Seismological constraints on a possible plume root at the core–mantle boundary. Nature 435, 666–669 (2005).
Nomura, R. et al. Spin crossover and iron-rich silicate melt in the Earth's deep mantle. Nature 473, 199–202 (2011).
Hernlund, J. W. & Jellinek, A. M. Dynamics and structure of a stirred partially molten ultralow-velocity zone. Earth Planet. Sci. Lett. 296, 1–8 (2010).
Maclennan, J. Lead isotope variability in olivine-hosted melt inclusions from Iceland. Geochim. Cosmochim. Acta 72, 4159–4176 (2008).
Hewitt, I. J. Modelling melting rates in upwelling mantle. Earth Planet. Sci. Lett. 300, 264–274 (2010).
Williams, Q. & Garnero, E. J. Seismic evidence for partial melt at the base of the mantle, Science 273, 1528–1530 (1996).
Brandon, A. D. & Walker, R. J. The debate over core–mantle interaction. Earth Planet. Sci. Lett. 232, 211–225 (2005).
Murphy, D. T., Brandon, A. D., Debaille, V., Burgess, R. & Ballentine, C. J. In search of a hidden long-term isolated sub-chondritic 142Nd/144Nd reservoir in the deep mantle: Implications for the Nd isotope systematics of the Earth. Geochim. Cosmochim. Acta 74, 738–750 (2010).
Vidal, V. & Bonneville, A. Variations of the Hawaiian hot spot activity revealed by variations in the magma production rate. J. Geophys. Res. 109, B03104 (2004).
Huang, S., Hall, P. S. & Jackson, M. G. Geochemical zoning of volcanic chains associated with Pacific hotspots. Nature Geosci. http://dx.doi.org/10.1038/ngeo1263 (2011).
Weis, D., Bassias, Y., Gautier, I. & Mennessier, J. Dupal anomaly in existence 115 Ma ago — evidence from isotopic study of the Kerguelen Plateau (South Indian Ocean). Geochim. Cosmochim. Acta 53, 2125–2131 (1989).
Ni, S., Tan, E., Gurnis, M. & Helmberger, D. V. Sharp sides to the African super plume. Science 296, 1850–1852 (2002).
Hart, S. R. A large-scale isotope anomaly in the Southern Hemisphere mantle, Nature 309, 753–757 (1984).
Wen, L. A compositional anomaly at the Earth's core-mantle boundary as an anchor to the relatively slowly moving surface hotspots and as source to the DUPAL anomaly. Earth Planet. Sci. Lett. 246, 138–148 (2006).
Regelous, M., Hofmann, A. W., Abouchami, W. & Galer, S. J. G. Geochemistry of lavas from the Emperor Seamounts, and the geochemical evolution of Hawaiian magmatism from 85 to 42 Ma. J. Petrol. 44, 113–140 (2003).
US Geological Survey. Bathymetric map of the Hawaiian Islands (2003), available at http://geopubs.wr.usgs.gov/i-map/i2809.
Geochemistry of Rocks of the Oceans and Continents (GEOROC) database, available at http://georoc.mpch-mainz.gwdg.de/georoc/.
Trusdell, F. A. & Lockwood, J. P. Geologic Maps of the Northeast Flank of, Central-Southeast Flank of, Southern Mauna Loa Volcano, Island of Hawai'i, Hawai'i: US Geological Survey SIM 2932-A, SIM 2932-B, SIM 2932-C respectively, scale 1:50,000 (in the press).
Grand, S. P. Mantle shear-wave tomography and the fate of subducted slabs. Phil. Trans. R. Soc. A 360, 2475–2491 (2002).
Steinberger, B. Plumes in a convecting mantle: Models and observations for individual hotspots. J. Geophys. Res. 105, 11127–11152 (2000).
Bréger, L. & Romanowicz, B. Three-dimensional structure at the base of the mantle beneath the central Pacific. Science 282, 718–720 (1998).
Acknowledgements
We thank D. DePaolo, A. Hofmann, D. Hanano, A. Greene, I. Nobre Silva, C. Farnetani, F. Albarède and numerous PCIGR graduate students for discussions and insights into mantle geochemistry. We thank C. Maerschalk (ULB), B. Kieffer and J. Barling (PCIGR, UBC) for helping to produce the data. We thank S. Sparks, VGP President, for inviting D.W. to give the Daly Lecture at Fall AGU 2010. Financial support was provided by the Belgian Fonds National de la Recherche Scientifique (FNRS), NSERC Discovery Grants to D.W., J.S.S. and A.M.J., and NSF grants to M.O.G. and J.M.R. A.M.J. also acknowledges support from the Canadian Institute for Advanced Research. Correspondence and requests for materials should be addressed to D.W.
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D.W. acquired the data, compiled the literature data, conceived the idea for the paper and developed the conceptual model with A.M.J. D.W. wrote the paper, together with A.M.J and J.S.S. All authors discussed the results and the model, and contributed to the manuscript. M.O.G. and J.M.R. also wrote the proposals, led the expeditions and organized the sampling on Hawai'i and shared their knowledge and data on these islands.
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Weis, D., Garcia, M., Rhodes, J. et al. Role of the deep mantle in generating the compositional asymmetry of the Hawaiian mantle plume. Nature Geosci 4, 831–838 (2011). https://doi.org/10.1038/ngeo1328
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