Volcanic resurfacing and the early terrestrial crust: Zircon U-Pb and REE constraints from the Isua Greenstone Belt, southern West Greenland

The oldest known bona fide succession of elastic metasediments Occurs in the Isua Greenstone Belt. SW Greenland and consists of a variety of mica schists and rare metaconglomerates. The metasediments are in direct contact with a felsic metavolcanic lithology that has previously been dated to 3.71 Ga. Based on trace element geochemical data for 30 metasediments, we selected the six samples with highest Zr concentrations for zircon extraction. These samples all yielded very few or no zircon, Those extracted from mica schists yielded ion probe U/Pb ages between 3.70 and 3,71 Ga. One metaconglomerate sample yielded just a single zircon of 3.74 Ga age. The mica schist hosted zircons have U/Pb ages. Th/U ratios, REE patterns and Eu anomalies indistinguishable from zircon in the adjacent 3.71 Ga felsic metavolcanic unit. Trace element modelling requires the bulk of material in the metasediments to be derived from variably weathered mafic lithologies but some metasediments contain substantial contribution from more evolved source lithologies. The paucity of zircon in the mica schists is thus explained by incorporation of material from largely zircon-free volcanic lithologies. The absence of older zircon in the mica schists and the preponderance of mafic source material imply intense, mainly basaltic resurfacing of the early Earth. The implications of this process are discussed, Thermal considerations suggest that horizontal growth of Hadean crust by addition of mafic ultramafic lavas must have triggered self-reorganisation of the protocrust by remelting. Reworking oft Hadean crust may have been aided by burial of hydrated (weathered) metabasalt due to semi-continuous addition of new voluminous basalt Outpouring,;, This process Causes a bias towards eruption of Zr-saturated partial melts at the surface with O-isotope corn posit ion,, potentially different from the mantle. The oldest zircons hosted in sediments would have been buried to substantial depth or formed in plutons that crystallised at some depth from which it took hundreds of millions of years for them to be exhumed and incorporated into much younger sediments. (C) 2005 Elsevier B.V.All rights reserved.

Rho and smooth muscle cell phenotype

Smooth muscle cell (SMC) phenotypic modulation from the mature ’contractile’ to a less differentiated ’synthetic’ phenotype involves not only altered expression but also a reorganisation of contractile and cytoskeletal proteins. Objective: To investigate the role of RhoA, a known regulator of the actin cytoskeleton, in SMC phenotypic regulation. Methods: Rho transcription (RT-PCR), expression (Western analysis) and activation (membrane translocation or Rho ’pull-down’ assay) was investigated in cultured rabbit aortic SMC during phenotypic modulation, and under the influence of known SM-regulatory proteins (thrombin, heparin and TGF- β). Rho’s effect on cell morphology was examined by transient transfection of ’synthetic’ state SMC with either constitutively active Rho (Val14RhoA) or its inhibitor, C3 transferase. Results: RhoA transcription was elevated in the first 3 days of primary culture, and protein expression peaked at 2 days post-confluence when SMC return to a more ’contractile’ state. However, RhoA showed augmented activation at three time-points in primary culture: the transition point when SMCs enter logarithmic growth and are highly motile, upon reaching quiescence, and when they return to a more ’contractile’ state. Thrombin, heparin and TGF-β activated RhoA in ’synthetic’ state SMCs. Transfection with Val14RhoA caused a dramatic decrease in SMC size and a reorganization of cytoskeletal proteins, reminiscent of the ’contractile’ phenotype. Specific inhibition of endogenous Rho by C3 transferase resulted in an almost complete loss of contractile proteins. Conclusion: These data indicate that Rho is an important determining factor of SMC functional state.