<mods:mods version="3.0" xsi:schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-0.xsd" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:mods="http://www.loc.gov/mods/v3"><mods:titleInfo><mods:title>Jurassic volcaniclastic-basaltic andesite-dolerite sequence in Tasmania: New age constraints for fossil plants from Lune River</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">KE</mods:namePart><mods:namePart type="family">Bromfield</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">CF</mods:namePart><mods:namePart type="family">Burrett</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">RA</mods:namePart><mods:namePart type="family">Leslie</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">S</mods:namePart><mods:namePart type="family">Meffre</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>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.</mods:abstract><mods:classification authority="lcc">260100 Geology</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">2007-10</mods:dateIssued></mods:originInfo><mods:genre>Article</mods:genre></mods:mods>