Lestari W, Al-Suwaidi A, Fox C, Vajda V, Hennhoefer D
Sci Rep. 2024; 14(1):9742.
PMID: 38679621
PMC: 11056376.
DOI: 10.1038/s41598-024-60088-5.
Didier G, Laurin M
PeerJ. 2021; 9:e12577.
PMID: 34966586
PMC: 8667717.
DOI: 10.7717/peerj.12577.
Zhang H, Zhang F, Chen J, Erwin D, Syverson D, Ni P
Sci Adv. 2021; 7(47):eabh1390.
PMID: 34788084
PMC: 8597993.
DOI: 10.1126/sciadv.abh1390.
Viglietti P, Benson R, Smith R, Botha J, Kammerer C, Skosan Z
Proc Natl Acad Sci U S A. 2021; 118(17).
PMID: 33875588
PMC: 8092562.
DOI: 10.1073/pnas.2017045118.
Botha J
PeerJ. 2020; 8:e10408.
PMID: 33282563
PMC: 7694564.
DOI: 10.7717/peerj.10408.
Effects of taphonomic deformation on geometric morphometric analysis of fossils: a study using the dicynodont (Therapsida, Anomodontia).
Kammerer C, Deutsch M, Lungmus J, Angielczyk K
PeerJ. 2020; 8:e9925.
PMID: 33083110
PMC: 7547620.
DOI: 10.7717/peerj.9925.
Altered fluvial patterns in North China indicate rapid climate change linked to the Permian-Triassic mass extinction.
Zhu Z, Liu Y, Kuang H, Benton M, Newell A, Xu H
Sci Rep. 2019; 9(1):16818.
PMID: 31727990
PMC: 6856103.
DOI: 10.1038/s41598-019-53321-z.
Effect of climate change on distribution of species of common horned frogs in South America.
Vieira K, Montenegro P, Santana G, Vieira W
PLoS One. 2018; 13(9):e0202813.
PMID: 30208067
PMC: 6135375.
DOI: 10.1371/journal.pone.0202813.
A geochemical view into continental palaeotemperatures of the end-Permian using oxygen and hydrogen isotope composition of secondary silica in chert rubble breccia: Kaibab Formation, Grand Canyon (USA).
Kenny R
Geochem Trans. 2018; 19(1):2.
PMID: 29340852
PMC: 5770344.
DOI: 10.1186/s12932-017-0047-y.
An early geikiid dicynodont from the Assemblage Zone (late Permian) of South Africa.
Kammerer C, Smith R
PeerJ. 2017; 5:e2913.
PMID: 28168104
PMC: 5289114.
DOI: 10.7717/peerj.2913.
Boreal earliest Triassic biotas elucidate globally depauperate hard substrate communities after the end-Permian mass extinction.
Zaton M, Niedzwiedzki G, Blom H, Kear B
Sci Rep. 2016; 6:36345.
PMID: 27821855
PMC: 5099577.
DOI: 10.1038/srep36345.
Provincialization of terrestrial faunas following the end-Permian mass extinction.
Sidor C, Vilhena D, Angielczyk K, Huttenlocker A, Nesbitt S, Peecook B
Proc Natl Acad Sci U S A. 2013; 110(20):8129-33.
PMID: 23630295
PMC: 3657826.
DOI: 10.1073/pnas.1302323110.
Recent progress in paleontological methods for dating the Tree of Life.
Laurin M
Front Genet. 2012; 3:130.
PMID: 22811696
PMC: 3395881.
DOI: 10.3389/fgene.2012.00130.
Delayed recovery of non-marine tetrapods after the end-Permian mass extinction tracks global carbon cycle.
Irmis R, Whiteside J
Proc Biol Sci. 2011; 279(1732):1310-8.
PMID: 22031757
PMC: 3282377.
DOI: 10.1098/rspb.2011.1895.
The Triassic dicynodont Kombuisia (Synapsida, Anomodontia) from Antarctica, a refuge from the terrestrial Permian-Triassic mass extinction.
Frobisch J, Angielczyk K, Sidor C
Naturwissenschaften. 2009; 97(2):187-96.
PMID: 19956920
DOI: 10.1007/s00114-009-0626-6.
Global taxonomic diversity of anomodonts (tetrapoda, therapsida) and the terrestrial rock record across the Permian-Triassic boundary.
Frobisch J
PLoS One. 2008; 3(11):e3733.
PMID: 19011684
PMC: 2581439.
DOI: 10.1371/journal.pone.0003733.
Trophic network models explain instability of Early Triassic terrestrial communities.
Roopnarine P, Angielczyk K, Wang S, Hertog R
Proc Biol Sci. 2007; 274(1622):2077-86.
PMID: 17609191
PMC: 2706195.
DOI: 10.1098/rspb.2007.0515.