Research paperAnatomically preserved Glossopteris leaves from the Bowen and Sydney basins, Australia
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Cited by (35)
How similar are the venation and cuticular characters of Glossopteris, Sagenopteris and Anthrophyopsis?
2023, Review of Palaeobotany and PalynologyEnvironmental change in the late Permian of Queensland, NE Australia: The warmup to the end-Permian Extinction
2022, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :The Black Alley Shale and equivalent units (Burngrove Formation and upper Fort Cooper Coal Measures) host rich plant macrofossil assemblages, commonly preserved as impressions in association with tuff beds or as permineralized peats. The Glossopteris flora reaches peak expression in the Bowen Basin within these units: at least 33 glossopterid leaf and fructification taxa have been recognized (Rigby, 1972, 1978a; Gould and Delevoryas, 1977; McLoughlin, 1988, 1990a, 1990b, 1992, 1994a, 1994b, 1995, 2012, 2016; Pigg and McLoughlin, 1997; McLoughlin et al., 2018; Nishida et al., 2007, 2013). Other gymnosperms remain sparse, but sphenophyte and fern remains are common, although of modest diversity.
Late Permian soil-forming paleoenvironments on Gondwana: A review
2022, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :Comparisons of paleosols along lateral transects, where applicable, and appropriate sampling density are highly recommended for future work in paleoclimate reconstructions (Dzombak et al., 2021). Upper Permian Lopingian floras on Gondwana were dominated by a sole arborescent gymnospermous taxa, the glossopterids, and numerous forms of understory vegetation in the form of ferns, lycopsids, sphenopsids, and bryophytes (Cúneo et al., 1993; Pigg and Taylor, 1993; Pigg and McLoughlin, 1997; Iannuzzi, 2010; Prevec et al., 2010; McLoughlin, 2011; Schwendemann et al., 2010; Ryberg et al., 2012). The floral diversity of Gondwanan ecosystems was generally lower than in other floral realms (Angara, Euramerica, Cathaysia) throughout the Permian (Rees, 2002; Fig. 7A).
Palaeoenvironments, flora, and organic carbon and nitrogen isotope changes across the non-marine Permian-Triassic boundary at Wybung Head, Australia
2019, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :Under the glossopterid canopy, an understory flora consisted of ferns, equisetopsids, and lycopsids along with occasional hygrophytic algae like, Botryococcus sp. (Figs. 5 and 6). The glossopterid dominated palaeovegetation at Wybung Head is also present elsewhere in the Sydney Basin and in the Bowen Basin (Michaelsen, 2002; Lindström and McLoughlin, 2007; Montañez et al., 2007; Pigg and McLaughlin, 1997; Benton and Newell, 2014; Van de Wetering et al., 2013a, 2013b). The dominance of opaque phytoclast in the entire sequence indicates deposition under oxic conditions, especially in the sediments above the Birdie Coal, caused by fluctuating water tables, high energy and desiccating conditions.
Leaf Venation Density and Calculated Physiological Characteristics of Fossil Leaves From the Permian of Gondwana
2018, Transformative Paleobotany: Papers to Commemorate the Life and Legacy of Thomas N. TaylorGlossopterid Plant Remains in Permineralization: What Do They Tell Us?
2018, Transformative Paleobotany: Papers to Commemorate the Life and Legacy of Thomas N. Taylor