Journal of Southeast Asian Earth Sciences
Permian brachiopod faunas of Western Australia: Gondwanan—Asian relationships and Permian climate☆
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Cited by (29)
Late Artinskian–Early Kungurian (Early Permian) warming and maximum marine flooding in the East Gondwana interior rift, Timor and Western Australia, and comparisons across East Gondwana
2017, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :Warming through cycles I and II of the Byro Group is indicated by (1) the disappearance of dropstones above the lower Coyrie Formation; (2) the very rare appearance of conodonts either in the upper Coyrie Formation or the Bulgadoo Shale; (3) the appearance in cycle II formations of brachiopods with “Tethyan” warm-water affinity (e.g. Demonedys, Fredericksia(?), Tornquistia, Quinquenella, Retimarginifera, Spiriferella, and Spiroelytha), some of which persisted through cycles III and IV (Archbold and Shi, 1995); and (4) the diversification of the stemless crinoid Calceolispongia in Cycles II and III (Teichert, 1991). This suggests that by the latest Artinskian–earliest Kungurian relatively warm sea conditions were present in the Southern Carnarvon Basin, compared to earlier in the late Artinskian, and may have persisted through the Kungurian.
Postglacial Early Permian (late Sakmarian-early Artinskian) shallow-marine carbonate deposition along a 2000km transect from Timor to west Australia
2014, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :The absence of any reports of Tubiphytes and fusulinids such as endothyraceans, tetrataxaceans and pseudoammodiscids in Sakmarian–early Artinskian deposits from eastern Australia, suggests that water temperatures in the East Gondwana interior-rift system were higher than those in the epeiric seas of eastern Australia. Based on marine invertebrates, but in particular the brachiopods, Archbold and Shi (1995, 1996) recognized a Westralian biogeographic province for the late Sakmarian–Artinskian comprising faunas, including warm-water elements, from the Perth, Carnarvon and Canning Basins as well as from New Guinea (West Papua), Timor, and other blocks now within southern Asia. Coeval faunas from eastern Australia were distinguished as the Austrazean Province and regarded as indicative of extremely cold-water conditions (Archbold, 2000, 2001).
Late Paleozoic middle-latitude Gondwana environment-stable isotope records from Western Australia
2013, Gondwana ResearchCitation Excerpt :Many proxies, such as faunal assemblages of brachiopods (e.g., Archbold and Shi, 1995; Shen and Shi, 2004) and plants (e.g., McLoughlin, 1993), Mg/Ca ratios of foraminifera (Nürnberg et al., 1996), Sr/Ca ratios of corals (de Villiers et al., 1995), and stable oxygen isotope compositions of carbonates and conodont apatite (Anderson and Arthur, 1983; Luz et al., 1984; Joachimski et al., 2012) have been utilized to provide varieties of paleoenvironmental information for different geological ages.
Earliest Permian brachiopod faunas of west-central Argentina: Defining the Pennsylvanian-Permian boundary in Gondwana
2010, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :On a global scale, Gondwana's lithologic and palaeontological data suggest that for this interval of time (i.e., Asselian), a climatic amelioration occurred in most parts of Gondwana, accompanied by an increase in temperature compared to glacial times (Dickins, 1978, 1996). Palaeotemperature curves for the Western Australian Permian constructed on the basis of brachiopod diversity fluctuations (Archbold and Shi, 1995, 1996), also indicate a warming trend from cold to cold temperate conditions from late Asselian to early Sakmarian (Lionia lyoni and Trigonotreta occidentalis brachiopod zones; Archbold and Shi, 1995, Fig. 2). In the west-central Argentinian basins the onset of the temperate conditions would have occurred near the end of the Pennsylvanian (Kasimovian–Gzhelian, López Gamundí et al., 1993).
Oxygen isotope values from high-latitudes: Clues for Permian sea-surface temperature gradients and Late Palaeozoic deglaciation
2008, Palaeogeography, Palaeoclimatology, PalaeoecologyEarly and Middle Permian paleoclimates of the Baoshan Block, western Yunnan, China: Insight from carbonates
2005, Journal of Asian Earth Sciences
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Contribution to IGCP Project 321.