Slit-band gastropods (Pleurotomariida) from the Upper Triassic St. Cassian Formation and their diversity dynamics in the Triassic

Zootaxa ◽  
2021 ◽  
Vol 5042 (1) ◽  
pp. 1-165
Author(s):  
BARAN KARAPUNAR ◽  
ALEXANDER NÜTZEL
Keyword(s):  
Marine Invertebrate ◽  
Type Specimens ◽  
Gastropod Species ◽  
Generic Level ◽  
Cassian Formation ◽  
Extinction Event ◽  
Mass Extinction Event ◽  
Permian Mass Extinction ◽  
The 19Th Century ◽  
Diversity Dynamics

The St. Cassian Formation, Italy, has yielded the most diverse marine invertebrate fauna known from the Triassic. A quarter of all described Triassic gastropod species has been reported from this formation. Most of the gastropod species from the St. Cassian Formation were erected in the 19th century and many of them are known only from their original figures and descriptions. The failure to study type specimens resulted in many erroneous identifications by subsequent authors. Here, we revise the slit band gastropods (Pleurotomariida) from the St. Cassian Formation—one of the major groups present in this formation. A total of 77 nominate Pleurotomariida species belonging to 29 genera and 11 families are present in the St. Cassian Formation which comprises approximately 14 % of the total nominate gastropod species of that formation. In addition, we revise several taxa that had been wrongly assigned to Pleurotomariida. As other gastropod clades, Pleurotomariida experienced a major extinction at the end-Permian mass extinction event. As in the Late Palaeozoic, their relative abundance in gastropod faunas continued to be 30 % in some Anisian faunas but decreased to 5–10 % afterwards. Their diversification at generic level became interrupted by an extinction event within the Carnian, probably by the Carnian Pluvial Event. As a result of their sluggish recovery compared to the other gastropod groups, their species diversity decreased from 26 % during the Permian to 18 % during the Triassic.                 Type specimens of the following genera are studied: Proteomphalus, Rhaphistomella, Temnotropis, Kittlidiscus, Stuorella, Schizogonium, Wortheniella, Bandelium, Lancedellia, Rinaldoella, Pseudowortheniella, Paleunema, Ampezzalina, Bandelastraea, Cheilotomona, Pseudoscalites, Delphinulopsis, and Cochlearia.                 Nine new pleurotomariidan genera are erected: Amplitomaria, Pseudoananias, Lineacingulum, Pressulasphaera, Cancellotomaria, Acutitomaria, Lineaetomaria, Nodocingulum, and Striacingulum.                 Eight new species are described: Schizogonium undae, Acutitomaria kustatscherae, Wortheniella klipsteini, Wortheniella paolofedelei, Rinaldoella tornata, Nodocingulum ernstkittli, Nodocingulum? turris, and Laubella subsulcata.                 Eoworthenia frydai is a new replacement name for Worthenia rarissima Barrande.  

scholarly journals Subsequent biotic crises delayed marine recovery following the late Permian mass extinction event in northern Italy

PLoS ONE ◽  
2017 ◽  
Vol 12 (3) ◽  
pp. e0172321 ◽  
Author(s):  
William J. Foster ◽  
Silvia Danise ◽  
Gregory D. Price ◽  
Richard J. Twitchett
Keyword(s):  
Mass Extinction ◽  
Northern Italy ◽  
Late Permian ◽  
Extinction Event ◽  
Mass Extinction Event ◽  
Permian Mass Extinction

Rapid marine recovery after the end-Permian mass-extinction event in the absence of marine anoxia

Geology ◽  
2004 ◽  
Vol 32 (9) ◽  
pp. 805 ◽  
Author(s):  
R.J. Twitchett ◽  
L. Krystyn ◽  
A. Baud ◽  
J.R. Wheeley ◽  
S. Richoz
Keyword(s):  
Mass Extinction ◽  
Extinction Event ◽  
Mass Extinction Event ◽  
Permian Mass Extinction

Earliest Silurian faunal survival and recovery after the end Ordovician glaciation: evidence from the brachiopods

2007 ◽  
Vol 98 (3-4) ◽  
pp. 291-301 ◽  
Author(s):  
L. Robin M. Cocks ◽  
Rong Jia-yu
Keyword(s):  
Global Warming ◽  
Recovery Rate ◽  
Mass Extinction ◽  
Ice Age ◽  
Benthic Assemblages ◽  
Ice Cap ◽  
Extinction Event ◽  
Mass Extinction Event ◽  
Permian Mass Extinction ◽  
Ecological Recovery

ABSTRACTEarliest Silurian (basal Llandovery) brachiopod faunas are surveyed and listed from around the globe, and divided between Lower Rhuddanian and Upper Rhuddanian occurrences. 60 genera are known from the Lower Rhuddanian within 20 superfamilies and there are 87 genera in 25 superfamilies in the Upper Rhuddanian. The 29 areas surveyed span the globe, both latitudinally and longitudinally. Only six superfamilies are Lazarus taxa which are known both from the Ordovician and Middle Llandovery (Aeronian) and later rocks but have not been recorded from the Rhuddanian. These are surprising results, since many previous studies have inferred that the Rhuddanian was a time of very sparse faunas. The global warming that followed the latest Ordovician (Hirnantian) ice age did not proceed quickly, with an ice-cap probably present through at least the Llandovery. There is a marked absence of Lower Rhuddanian bioherms even at low palaeolatitudes; however, the ecological recovery rate was far faster than that following the end-Permian mass extinction event. The partitioning of the Rhuddanian shelf faunas into well-defined benthic assemblages progressed slowly over the interval.

scholarly journals The main stage of recovery after the end-Permian mass extinction: taxonomic rediversification and ecologic reorganization of marine level-bottom communities during the Middle Triassic

PeerJ ◽  
2021 ◽  
Vol 9 ◽  
pp. e11654
Author(s):  
Evelyn Friesenbichler ◽  
Michael Hautmann ◽  
Hugo Bucher
Keyword(s):  
Mass Extinction ◽  
Middle Triassic ◽  
Biotic Interactions ◽  
Trophic Relationships ◽  
Lag Phase ◽  
Early Triassic ◽  
Bottom Communities ◽  
Extinction Event ◽  
Mass Extinction Event ◽  
Permian Mass Extinction

The recovery of marine life from the end-Permian mass extinction event provides a test-case for biodiversification models in general, but few studies have addressed this episode in its full length and ecological context. This study analyses the recovery of marine level-bottom communities from the end-Permian mass extinction event over a period of 15 Ma, with a main focus on the previously neglected main phase during the Middle Triassic. Our analyses are based on faunas from 37 lithological units representing different environmental settings, ranging from lagoons to inner, mid- and outer ramps. Our dataset comprises 1562 species, which belong to 13 higher taxa and 12 ecological guilds. The diversification pattern of most taxa and guilds shows an initial Early Triassic lag phase that is followed by a hyperbolic diversity increase during the Bithynian (early middle Anisian) and became damped later in the Middle Triassic. The hyperbolic diversity increase is not predicted by models that suggest environmental causes for the initial lag phase. We therefore advocate a model in which diversification is primarily driven by the intensity of biotic interactions. Accordingly, the Early Triassic lag phase represents the time when the reduced species richness in the wake of the end-Permian mass extinction was insufficient for stimulating major diversifications, whereas the Anisian main diversification event started when self-accelerating processes became effective and stopped when niche-crowding prevented further diversification. Biotic interactions that might drive this pattern include interspecific competition but also habitat construction, ecosystem engineering and new options for trophic relationships. The latter factors are discussed in the context of the resurgence of large carbonate platforms, which occurred simultaneously with the diversification of benthic communities. These did not only provide new hardground habitats for a variety of epifaunal taxa, but also new options for grazing gastropods that supposedly fed from microalgae growing on dasycladaceans and other macroalgae. Whereas we do not claim that changing environmental conditions were generally unimportant for the recovery of marine level-bottom communities, we note that their actual role can only be assessed when tested against predictions of the biotic model.

scholarly journals Late Toarcian marine gastropods from the Cleveland Basin, UK: systematics, palaeobiogeography and contribution to biotic recovery from the early Toarcian extinction event

2019 ◽  
Author(s):  
Mariel Ferrari ◽  
Crispin TS Little ◽  
Jed W Atkinson
Keyword(s):  
Mass Extinction ◽  
Taxonomic Composition ◽  
The Other ◽  
Gastropod Species ◽  
Marine Gastropods ◽  
Potential Explanation ◽  
Biotic Recovery ◽  
Extinction Event ◽  
Sandstone Formation ◽  
Mass Extinction Event

As part of a study to evaluate the recovery from the early Toarcian extinction event in the Cleveland Basin, 477 new gastropod specimens were collected from mid-late Toarcian rocks of the Ravenscar section, North Yorkshire, UK. The gastropods were preserved in two modes: 1) specimens preserved with recrystallized shells, mainly in the Whitby Mudstone Formation, but also some in the Blea Wyke Sandstone Formation; 2) specimens preserved as external moulds in mineralized patches of shells in the Yellow Sandstone Member. The fossil assemblage comprised fifteen species, of which three are new: Katosira? bicarinata sp. nov., Turritelloidea stepheni sp. nov. and Striactaenonina elegans sp. nov. Four species are described in open nomenclature, as Tricarilda? sp. Jurilda sp., Cylindrobullina sp. and Cossmannina sp. The other species have previously been described: Coelodiscus minutus (Schübler in Zieten), Procerithium quadrilineatum (Römer), Pseudokatosira undulata (Benz in von Zieten), Palaeorissoina aff. acuminata (Gründel), Pietteia unicarinata (Hudleston), Globularia cf. canina (Hudleston), Striactaeonina cf. richterorum Schulbert & Nützel, Striactaenonina aff. tenuistriata (Hudleston) and Sulcoactaeon sedgvici (Phillips). Most of these species are the earliest records of their respective genera and show palaeobiogeographical connections with contemporary gastropod associations from other regions of Europe and South America. The taxonomic composition of the late Toarcian Cleveland Basin gastropod assemblage differs substantially from the faunas of the late Pliensbachian and early Toarcian Tenuicostatum Zone, showing the strong effect of the early Toarcian mass extinction event on the marine gastropod communities in the basin. Only a few gastropod species are shared between the late Toarcian faunas and the much more diverse Aalenian gastropod faunas in the Cleveland Basin, suggesting there was a facies control on gastropod occurrences at that time. This is also a potential explanation for the taxonomic differences between the late Toarcian gastropod faunas in the Cleveland Basin and those in France, and Northern and Southern Germany.

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