2021
DOI: 10.1016/j.gloplacha.2021.103428
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End-Triassic crisis and “unreefing” led to the demise of the Dachstein carbonate platform: A revised model and evidence from the Transdanubian Range, Hungary

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Cited by 7 publications
(3 citation statements)
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“…Thus, while large evolutionary events may have global signatures in the fossil record, they may also display regional epicentres due to the interactions of spatially non-random controls on diversity with diversity drivers operating at global scales. Across the TJME, reefs were widely distributed, and so their relationship with global diversity approached a global trend, rather than displaying any distinct regionalisation, with previous studies confirming the severity of the event for reefs globally 50 , 59 , 60 .…”
Section: Discussionmentioning
confidence: 55%
“…Thus, while large evolutionary events may have global signatures in the fossil record, they may also display regional epicentres due to the interactions of spatially non-random controls on diversity with diversity drivers operating at global scales. Across the TJME, reefs were widely distributed, and so their relationship with global diversity approached a global trend, rather than displaying any distinct regionalisation, with previous studies confirming the severity of the event for reefs globally 50 , 59 , 60 .…”
Section: Discussionmentioning
confidence: 55%
“…The close similarities in skeletal abundance and diversity patterns across the Triassic/Jurassic boundary between the widely separated regions (~500 km) of the Lombardy Basin and the Apennine Platform are also representative of a more general pattern across the western Tethys. This pattern of reduced animal abundance across the Triassic/Jurassic boundary followed by establishment of abiotic and microbial carbonate factories during the Early Jurassic occurred also in the Northern Calcareous Alps in Austria (McRoberts et al, 1997), the Transdanubian Range in Hungary (Pálfy et al, 2021), the central and northern Apennines of Italy (Barattolo & Romano, 2005; Brandano et al, 2016; Mancinelli et al, 2005), western Sicily (Todaro et al, 2017, 2018), Greece (Romano et al, 2008), and Turkey (Coskun Tunaboylu et al, 2014). The recovery of skeletal abundance to pre‐extinction levels in shallow‐marine environments across western Tethyan carbonate platforms occurred in upper Hettangian‐Sinemurian limestones with an increase in skeletal contribution from protists and mollusks.…”
Section: Discussionmentioning
confidence: 97%
“…The Triassic/ Jurassic boundary is marked by a subaerial exposure surface associated with a sea-level drop that can be traced across the entire Apennine Platform (Berra, 2012;Cirilli et al, 2015;Todaro et al, 2017). et al, 1997), the Transdanubian Range in Hungary (Pálfy et al, 2021), the central and northern Apennines of Italy (Barattolo & Romano, 2005;Brandano et al, 2016;Mancinelli et al, 2005), western Sicily (Todaro et al, 2017(Todaro et al, , 2018, Greece (Romano et al, 2008), and Turkey (Coskun Tunaboylu et al, 2014). The recovery of skeletal abundance to pre-extinction levels in shallow-marine environments across western Tethyan carbonate platforms occurred in upper Hettangian-Sinemurian limestones with an increase in skeletal contribution from protists and mollusks.…”
Section: I/ca Ratios Of Bulk Carbonate Samplesmentioning
confidence: 99%