Late Wuchiapingian (Late Dzhulfian, early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon, central–eastern Peloponnesus, Greece)

2002 ◽  
Vol 334 (12) ◽  
pp. 925-931 ◽  
Author(s):  
Emmanuel Skourtsos ◽  
Daniel Vachard ◽  
Alexandra Zambetakis-Lekkas ◽  
Rossana Martini ◽  
Louisette Zaninetti
1993 ◽  
Vol 5 (4) ◽  
pp. 409-410 ◽  
Author(s):  
J. A. Webb ◽  
C. R. Fielding

The East Antarctic Craton contains only one substantial outcrop of Palaeozoic–Mesozoic strata between 0° and 150°E; this lies in Mac. Robertson Land, on the eastern margin of the northern Prince Charles Mountains. These rocks are known as the Amery Group (Mond 1972, McKelvey & Stephenson 1990) and comprise dominantly fluviatile sandstones, with subordinate shales, coals and conglomerates. The lower formations of the Amery Group, the Radok Conglomerate and Bainmedart Coal Measures, contain a diverse Stage 5 palynomorph assemblage indicating a Baigendzhinian–Tatarian age (late Early–Late Permian, hereafter abbreviated as mid–Late Permian; Dibner 1978).


1989 ◽  
Vol 37 ◽  
pp. 205-211
Author(s):  
Lars Stemmerik ◽  
Mordeckai Magaritz

Isotope data from Late Palaeozoic limestones of the Wandel Sea Basin in eastern North Greenland show a variation of b13C from 0.0 %o to 5.7 %o vs PDB. Carbonates depleted in 13C occur in the basal part of lower Moscovian, upper Moscovian and middle Gzhelian transgressive sequences. 13C enriched limestones occur later in the cycles. The most 13C enriched limestones occur in the youngest (late Early Permian-early Late Permian) part of the sequence in Amdrup Land. The isotopic data is believed to represent changes in the global carbon cycle. Thus 13C enriched carbonates correlate to periods of burial of organic carbon mostly as coal, while 13C depleted carbonates formed as the result of erosion and oxidation of organic carbon during sea-level low stands.


2018 ◽  
Vol 58 ◽  
pp. 58-70 ◽  
Author(s):  
Borhan Bagherpour ◽  
Hugo Bucher ◽  
Elke Schneebeli-Hermann ◽  
Torsten Vennemann ◽  
Massimo Chiaradia ◽  
...  

2007 ◽  
Vol 252 (1-2) ◽  
pp. 239-258 ◽  
Author(s):  
Wan Yang ◽  
Yiqun Liu ◽  
Qiao Feng ◽  
Jinyan Lin ◽  
Dingwu Zhou ◽  
...  

2015 ◽  
Vol 424 ◽  
pp. 140-147 ◽  
Author(s):  
Haijun Song ◽  
Paul B. Wignall ◽  
Jinnan Tong ◽  
Huyue Song ◽  
Jing Chen ◽  
...  

2012 ◽  
Vol 279 (1736) ◽  
pp. 2180-2187 ◽  
Author(s):  
Roland B. Sookias ◽  
Richard J. Butler ◽  
Roger B. J. Benson

A major macroevolutionary question concerns how long-term patterns of body-size evolution are underpinned by smaller scale processes along lineages. One outstanding long-term transition is the replacement of basal therapsids (stem-group mammals) by archosauromorphs, including dinosaurs, as the dominant large-bodied terrestrial fauna during the Triassic (approx. 252–201 million years ago). This landmark event preceded more than 150 million years of archosauromorph dominance. We analyse a new body-size dataset of more than 400 therapsid and archosauromorph species spanning the Late Permian–Middle Jurassic. Maximum-likelihood analyses indicate that Cope's rule (an active within-lineage trend of body-size increase) is extremely rare, despite conspicuous patterns of body-size turnover, and contrary to proposals that Cope's rule is central to vertebrate evolution. Instead, passive processes predominate in taxonomically and ecomorphologically more inclusive clades, with stasis common in less inclusive clades. Body-size limits are clade-dependent, suggesting intrinsic, biological factors are more important than the external environment. This clade-dependence is exemplified by maximum size of Middle–early Late Triassic archosauromorph predators exceeding that of contemporary herbivores, breaking a widely-accepted ‘rule’ that herbivore maximum size greatly exceeds carnivore maximum size. Archosauromorph and dinosaur dominance occurred via opportunistic replacement of therapsids following extinction, but were facilitated by higher archosauromorph growth rates.


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