Auxiliary Material for Paper 2011GC003617 Domains of depleted mantle: New evidence from hafnium and neodymium isotopes Vincent J. M. Salters National High Magnetic Field Laboratory and Department of Earth, Ocean and Atmospheric Sciences, Florida State University, Tallahassee, Florida, USA Soumen Mallick National High Magnetic Field Laboratory and Department of Earth, Ocean and Atmospheric Sciences, Florida State University, Tallahassee, Florida, USA Now at Department of Earth and Ocean Sciences, University of South Carolina, Columbia, South Carolina, USA Stanley R. Hart Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA Charles E. Langmuir Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts, USA Andreas Stracke Max-Planck-Institut fuer Chemie, Postfach Mainz, Germany Institute of Geochemistry and Petrology, ETH Zurich, Zurich, Switzerland Now at Instituet fuer Mineralogie, Westfaelische Wilhelms Universitaet, Muenster, Germany Salters, V. J. M., S. Mallick, S. R. Hart, C. E. Langmuir, and A. Stracke (2011), Domains of depleted mantle: New evidence from hafnium and neodymium isotopes, Geochem. Geophys. Geosyst., 12, Q08001, doi:10.1029/2011GC003617. Introduction: Auxiliary material consists of one large data table with the Hf and Nd isotopic compositions of the mid-ocean ridge basalts and ocean island basalts. The ridge basalts also have their latitude and longitude indicated. Additional material also includes one map with the ridge segments where Hf and Nd isotopes are correlated. These locations include data presented in this paper as well as literature data. 1. 2011gc003617-ds01.xls Data Set S1. The Hf and Nd isotopic compositions of the mid-ocean ridge basalts and ocean island basalts. The ridge basalts also have their latitude and longitude indicated. 2. 2011gc003617-fs01.png Figure S1. Distribution of locations of mid ocean ridge basalts which show correlation between Hf and Nd isotopic compositions. It should be noted that density of available data is an important factor controlling where correlation between isotope systems can be observed. Locations are listed in Table 1.