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        <dc:title>Jurassic volcaniclastic-basaltic andesite-dolerite sequence in Tasmania: New age constraints for fossil plants from Lune River</dc:title>
        <dc:creator>Bromfield, KE</dc:creator>
        <dc:creator>Burrett, CF</dc:creator>
        <dc:creator>Leslie, RA</dc:creator>
        <dc:creator>Meffre, S</dc:creator>
        <dc:subject>260100 Geology</dc:subject>
        <dc:description>Jurassic plants excavated from a 1265 m site, at Lune River, southern Tasmania, include an araucarian&#13;
tree and numerous pteridophytes, belonging to the orders Osmundales, Filicales and Bennettitales. The&#13;
fossils occur in 2 – 3 m of immature volcanilithic sandstone beds. The sandstone consists primarily of clasts&#13;
from granitic basement rocks underlying much of southeast Tasmania and mafic clasts containing&#13;
feldspathicmicroliths, and primary, phreatomagmatic quartz crystals. Detrital zircons from the sandstones&#13;
are mostly Early Jurassic (Toarcian) in age (182+4 Ma) with minor Triassic (226 Ma), Devonian (380 –&#13;
360 Ma) and Proterozoic populations. Basaltic andesite, hereafter referred to as andesite, caps the&#13;
volcanilithic units and displays similar ratios of fluid-immobile trace elements (e.g. Zr/Nb, Ti/V), to the&#13;
Jurassic dolerite found in Tasmania, indicative of a common source. The andesites are correlated with the&#13;
Jurassic Kirkpatrick Basalts (Trans-Antarctic Mountains, Antarctica) based on their field relationships with&#13;
bounding strata, age, and distinctive similarities in major-element composition and fluid-immobile traceelement&#13;
ratios. The andesite is interpreted as an extrusive equivalent of the Tasmanian dolerite.&#13;
Importantly, drillcore from Lune River contains stoped clasts of andesite in fine-grained dolerite, indicating&#13;
that the andesite pre-dates the dolerite. Thermal alteration index of microfossils (3 – 3.3) and reflectance of&#13;
organic material within the sediments (0.54 – 0.77 Ro) resulted from contact metamorphism associated&#13;
with the emplacement of this basalt. The sedimentology and stratigraphy of the depositional environment,&#13;
plus the presence of hydrophilic pteridophytes and gymnosperms, indicates that the Toarcian&#13;
environment was temperate to warm and humid, with an abundant supply of water.</dc:description>
        <dc:date>2007-10</dc:date>
        <dc:type>Article</dc:type>
        <dc:type>PeerReviewed</dc:type>
        <dc:format>application/pdf</dc:format>
        <dc:identifier>http://eprints.utas.edu.au/6556/1/51585.pdf</dc:identifier>
        <dc:relation>http://dx.doi.org/10.1080/08120090701488297</dc:relation>
        <dc:identifier>Bromfield, KE and Burrett, CF and Leslie, RA and Meffre, S (2007) Jurassic volcaniclastic-basaltic andesite-dolerite sequence in Tasmania: New age constraints for fossil plants from Lune River. Australian Journal of Earth Sciences, 54 (7). pp. 965-974. ISSN 0812-0099</dc:identifier>
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