. (2016) 'Titanium stable isotope investigation of magmatic processes on the Earth and Moon.', Earth and planetary science letters., 449 . pp. 197-205. Further information on publisher's website: Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details.

No abstract

Community differentiation is a fundamental topic of the social sciences, and its prehistoric origins in Europe are typically assumed to lie among the complex, densely populated societies that developed millennia after their Neolithic predecessors. Here we present the earliest, statistically significant evidence for such differentiation among the first farmers of Neolithic Europe. By using strontium isotopic data from more than 300 early Neolithic human skeletons, we find significantly less variance in geographic signatures among males than we find among females, and less variance among burials with ground stone adzes than burials without such adzes. From this, in context with other available evidence, we infer differential land use in early Neolithic central Europe within a patrilocal kinship system.

. (2012) 'Late accretion on the earliest planetesimals revealed by the highly siderophile elements. ', Science., Further information on publisher's website: Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details.

Further information on publisher's website:http://dx.doi.org/10.1016/j.gca. 2008.11.036 Publisher's copyright statement: NOTICE: this is the author's version of a work that was accepted for publication in Geochimica et Cosmochimica Acta. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reected in this document. Changes may have been made to this work since it was submitted for publication. A denitive version was subsequently published in Geochimica et Cosmochimica Acta, 73 (5), 2009Acta, 73 (5), , 2009Acta, 73 (5), , 10.1016Acta, 73 (5), /j.gca.2008 Additional information: Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details. has not significantly changed the concentrations of the PGE, except Pd which is severely 32 depleted in gabbroic eclogites relative to gabbros (~75% loss). In contrast, basaltic eclogites 33 display significant depletion of Pt (≥60%), Pd (>85%) and Re (50-60%) compared with 34 published MORB, while Os, Ir and Ru abundances are broadly comparable. Thus, these data 35 suggest that only Pt, Pd and Re, and not Os, Ir and Ru, may be significantly fluxed into the 36 mantle wedge from mafic oceanic crust. Re-Os model ages for gabbroic and gabbroic 37 eclogite minerals are close to age estimates for igneous crystallisation and high-pressure 38 metamorphism, respectively, hence the HSE budgets can be related to both igneous and 39 metamorphic behaviour. The gabbroic budget of Os, Ir, Ru and Pd (but not Pt) is dominated 40 by sulphide, which typically hosts >90% of the Os, whereas silicates account for most of the 41Re (with up to 75% in plagioclase alone