Age significance of U-Th-Pb zircon data from early Archaean rocks of west Greenland - a reassessment based on combined ion-microprobe and imaging studies

The geochronological evolution of early Archaean Amitsoq gneisses from sout hern West Greenland is reassessed here using the well-established cathodolu minescence imaging method both to reveal previously undocumented complex zi rcon growth histories and to control positioning of ion-microprobe U-Th-Pb analyses. Several of the gneisses typically contain zircon grains with grea ter than or equal to 3.8 Ga cores of igneous origin, mostly completely mant led by growth banded magmatic zircon at ca. 3.65 Ga and in turn partly mant led by late Archaean metamorphic overgrowths at ca. 2.7 Ga. The greater tha n or equal to 3.8 Ga cores are regarded as inherited, with apparent dates r anging down to ca. 3.65 Ga reflecting differential Pb loss. This contrasts with published views interpreting greater than or equal to 3.8 Ga dates as emplacement ages of the host rock to the zircons, with all younger ages rep resenting later Pb loss and/or metamorphic recrystallisation. Two of the an alysed gneisses have discordant relationships to metasedimentary enclaves c ontaining accessory apatite with graphite inclusions whose C-isotope ratios have been considered as biogenic in origin. The present data show that the minimum age of the enclaves is 3.65 Ga and not 3.85 Ga as previously claim ed. This has important implications for the current debate on the possibili ty of temporal overlap of earliest life with a bolide impact scenario termi nating at greater than or equal to 3.8 Ga (as on the moon). We also discuss the implication of the discovery of highly complex internal structures in Amitsoq gneiss zircons for the interpretation of published, zircon derived Lu-Hf information. (C) 1999 Elsevier Science B.V. All rights reserved.