Ancient lithospheric source for quaternary lavas in hispaniola

Ancient lithospheric source for quaternary lavas in hispaniola


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ABSTRACT Fragments of ancient continental lithosphere, entrained in the shallow oceanic mantle, have been found in a number of locations in the Southern Hemisphere1,2,3,4, including rare arc


settings5. Lavas erupted in these locations exhibit Pb isotopic characteristics that are similar to the so-called enriched mantle 1 reservoir1, one of the end-members that define the


isotopic composition of the Earth’s mantle. However, no lavas with isotopic signatures resembling enriched mantle 1 have been identified in the Caribbean region. Here we present isotopic


analyses for mafic-alkaline lavas from Quaternary volcanic centres in Hispaniola. We identify unusual isotopic characteristics indicating the presence of a mantle component similar to


enriched mantle 1 beneath Hispaniola. Furthermore, we find evidence for an involvement of this mantle component in the genesis of spatially associated calk-alkaline lavas. On the basis of


these isotopic systematics we estimate that the mafic-alkaline lavas are derived from an ancient lithospheric fragment with affinities to the supercontinent Gondwana. We conclude that the


fragment originated from the Grenvillian terranes of Central America and Mexico, which also have affinities to Gondwana6, indicating that Hispaniola interacted tectonically with these


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support SIMILAR CONTENT BEING VIEWED BY OTHERS ACCRETION OF “YOUNG” PHANEROZOIC SUBCONTINENTAL LITHOSPHERIC MANTLE TRIGGERED BY BACK-ARC EXTENSION—THE CASE OF THE IVREA-VERBANO ZONE Article


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Scholar  Download references ACKNOWLEDGEMENTS This work would not be possible without the initial field and laboratory studies of P. Vespucci and W. Wertz. Fieldwork by J.F.L. was funded by


the National Science Foundation Latin American Cooperative Program and Dirección General de Minería and assisted by geology students from the Universidad Catolica Madre y Maestra. Special


thanks to P. Mueller for comments on earlier versions of the manuscript and for introducing G.D.K. to Precambrian geology. G.D.K. was supported by a grant from the National Science


Foundation during the early stages of this work. We would like to thank the editor, H. Langenberg, for handling of the manuscript and two anonymous reviewers for providing comments. AUTHOR


INFORMATION Author notes * Adam R. Goss & Ricardo Arévalo Jr Present address: Present addresses: ExxonMobil Development Company, Angola/Congo DEV-GP6-755, Houston, Texas 77060, USA,


AUTHORS AND AFFILIATIONS * Department of Geological Sciences, University of Florida, Gainesville, Florida, 32611, USA George D. Kamenov, Michael R. Perfit & Adam R. Goss * Department of


Earth and Environmental Science, The George Washington University, Washington DC 20052, USA John F. Lewis * Department of Geology, University of Maryland, College Park, Maryland 20742, USA


Ricardo Arévalo Jr * Department of Geography and Geology, University of Nebraska at Omaha, Omaha, Nebraska 68182, USA Robert D. Shuster * Planetary Environments Laboratory, NASA Goddard


Space Flight Center, Mail Code 699.0, Greenbelt, Maryland 20771, USA, Ricardo Arévalo Jr Authors * George D. Kamenov View author publications You can also search for this author inPubMed 


Google Scholar * Michael R. Perfit View author publications You can also search for this author inPubMed Google Scholar * John F. Lewis View author publications You can also search for this


author inPubMed Google Scholar * Adam R. Goss View author publications You can also search for this author inPubMed Google Scholar * Ricardo Arévalo Jr View author publications You can also


search for this author inPubMed Google Scholar * Robert D. Shuster View author publications You can also search for this author inPubMed Google Scholar CONTRIBUTIONS G.D.K., M.R.P. and


J.F.L. wrote the paper; M.R.P. and J.F.L. collected the samples and G.D.K., M.R.P., R.A., R.D.S and A.R.G. carried out the analyses. All authors provided scientific input during the data


interpretation and manuscript preparation. CORRESPONDING AUTHORS Correspondence to George D. Kamenov, Adam R. Goss or Ricardo Arévalo Jr. ETHICS DECLARATIONS COMPETING INTERESTS The authors


declare no competing financial interests. SUPPLEMENTARY INFORMATION SUPPLEMENTARY INFORMATION Supplementary Information (PDF 887 kb) RIGHTS AND PERMISSIONS Reprints and permissions ABOUT


THIS ARTICLE CITE THIS ARTICLE Kamenov, G., Perfit, M., Lewis, J. _et al._ Ancient lithospheric source for Quaternary lavas in Hispaniola. _Nature Geosci_ 4, 554–557 (2011).


https://doi.org/10.1038/ngeo1203 Download citation * Received: 04 April 2011 * Accepted: 08 June 2011 * Published: 10 July 2011 * Issue Date: August 2011 * DOI:


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