scholarly journals Paterimitra pyramidalisfrom South Australia: scleritome, shell structure and evolution of a lower Cambrian stem group brachiopod

Palaeontology ◽  
2013 ◽  
Vol 57 (2) ◽  
pp. 417-446 ◽  
Author(s):  
Cecilia M. Larsson ◽  
Christian B. Skovsted ◽  
Glenn A. Brock ◽  
Uwe Balthasar ◽  
Timothy P. Topper ◽  
...  
2020 ◽  
Author(s):  
Sarah M. Jacquet ◽  
◽  
April A. Miller ◽  
Laura Speir ◽  
Tara Selly ◽  
...  

2014 ◽  
Vol 88 (2) ◽  
pp. 359-366 ◽  
Author(s):  
Guoxiang Li ◽  
Zhifei Zhang ◽  
Hong Hua ◽  
Huining Yang

The early Cambrian calcareous skeletal fossilApistoconchaConway Morris is characterized by its two valves having posterior teeth and internal umbonal cavities. It has been reported from lower Cambrian Botomian-equivalent carbonate rocks in Australia, Mongolia, and Greenland. Here we report a new occurrence ofApistoconchain the lower Cambrian Xinji Formation of Luonan, southeast Shaanxi Province, North China Platform. Based on material (five ventral and four dorsal valves) from the Xinji Formation,Apistoconchacf.aphelesis systematically described and the taxonomic affinity ofApistoconchais discussed. The shell ofApistoconchapossesses an ‘antero-posterior’ plane of bilateral symmetry, and its two valves apparently articulated in life, although the tooth-like structures and pits show little resemblance to the teeth and sockets, respectively, of bivalved shells of rhynchonelliform brachiopods or pelecypods.Apistoconchacannot be assigned to the crown groups of either brachiopods or mollusks, even though functional morphological analysis indicates thatApistoconchamay be a ‘stem-group brachiopod’. UnlikeApistoconcha, the morphologically similarTianzhushanellaLiu is known only from a single type of valve lacking posterior teeth and pits.Tianzhushanellamay represent either a univalved animal or a bivalved animal, the other valve of which has not yet been identified. Even though bothApistoconchaandTianzhushanellamay represent stem-group brachiopods, they probably correspond to different stages of brachiopod evolution. Thus assignment ofApistoconchaandTianzhushanellato the same family (Tianzhushanellidae) may obscure their phylogenic implications.


2011 ◽  
Vol 58 (3) ◽  
pp. 243-257 ◽  
Author(s):  
J. G. Gehling ◽  
J. B. Jago ◽  
J. R. Paterson ◽  
D. C. García-Bellido ◽  
G. D. Edgecombe

Author(s):  
Artem Kouchinsky ◽  
Lars Holmer ◽  
Galina Ushatinskaya ◽  
Michael Steiner
Keyword(s):  

Palaeontology ◽  
2010 ◽  
Vol 53 (2) ◽  
pp. 377-402 ◽  
Author(s):  
JOHN R. PATERSON ◽  
GREGORY D. EDGECOMBE ◽  
DIEGO C. GARCÍA-BELLIDO ◽  
JAMES B. JAGO ◽  
JAMES G. GEHLING

2011 ◽  
Vol 56 (2) ◽  
pp. 385-400 ◽  
Author(s):  
Gregory D. Edgecombe ◽  
Diego C. García-Bellido ◽  
John R. Paterson

2018 ◽  
Vol 2 (2) ◽  
pp. 213-222 ◽  
Author(s):  
James G. Gehling ◽  
Mary L. Droser

Predation is one of the most fundamental ecological and evolutionary drivers in modern and ancient ecosystems. Here, we report the discovery of evidence of the oldest scavenging of shallowly buried bodies of iconic soft-bodied members of the Ediacara Biota by cryptic seafloor mat-burrowing animals that produced the furrow and levee trace fossil, Helminthoidichnites isp. These mat-burrowers were probably omnivorous, stem-group bilaterians that largely grazed on microbial mats but when following mats under thin sands, they actively scavenged buried Dickinsonia, Aspidella, Funisia and other elements of the Ediacara Biota. These traces of opportunistic scavengers of dead animals from the Ediacaran of South Australia represent a fundamental ecological innovation and a possible pathway to the evolution of macrophagous predation in the Cambrian. While the Ediacaran oceans may have had oxygen levels too low to support typical large predators, the Helminthoidichnites maker lived in and grazed on microbial mats, which may have provided a localized source of oxygen.


Lithos ◽  
2018 ◽  
Vol 318-319 ◽  
pp. 219-229 ◽  
Author(s):  
Gaëlle Lamarque ◽  
Jérôme Bascou ◽  
René-Pierre Ménot ◽  
Jean-Louis Paquette ◽  
Simon Couzinié ◽  
...  

1997 ◽  
Vol 71 (1) ◽  
pp. 22-32 ◽  
Author(s):  
Derek E. G. Briggs ◽  
Christopher Nedin

Most of the specimens ofMyoscolex atelesGlaessner, 1979, the most abundant soft-bodied taxon in the Big Gully fauna from the Lower Cambrian Emu Bay Shale of South Australia, preserveonlythe phosphatized trunk muscles, in striking contrast to the organic residues that characterize other Burgess-Shale-type biotas. This is the oldest phosphatized muscle tissue and the first thus far reported from the Cambrian. The extent of phosphatization implies a source in addition to the animal itself, and this is reflected in high levels of phosphate in the Big Gully sequence compared to other shales. The apparent anomaly posed by the extensive preservation of labile muscle tissue as opposed to the more decay resistant cuticle is explained by the role of bacterial processes in the preservation of soft tissues. New specimens ofMyoscolexreveal a variable number of trunk somites with possible tergites, and flap-like appendages. There is evidence for at least three eyes on the head, and a proboscis may have been present. An annelid affinity is rejected andMyoscolexis reinterpreted as anOpabinia-likeanimal with possible affinities with the arachnomorph arthropods.


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