Late Ordovician (Katian) linguliform microbrachiopods from north‐eastern Yunnan, South China

2021 ◽  
Author(s):  
Di Chen ◽  
Bing Huang ◽  
Wen‐Jie Li ◽  
Rong‐Yu Li ◽  
Jia‐Yu Rong
Keyword(s):  
South China ◽  
Late Ordovician ◽  
North Eastern

Early Sandbian (Late Ordovician) conodonts from the Yenwashan Formation, western Zhejiang, South China

2009 ◽  
Vol 33 (2) ◽  
pp. 133-161 ◽  
Author(s):  
Yong Yi Zhen ◽  
Yuandong Zhang ◽  
Ian G. Percival
Keyword(s):  
South China ◽  
Late Ordovician

Corallite increase in the Late Ordovician coral Agetolites, and its taxonomic implication

2019 ◽  
Vol 93 (5) ◽  
pp. 839-855
Author(s):  
Ning Sun ◽  
Robert J. Elias ◽  
Dong-Jin Lee
Keyword(s):  
South China ◽  
Typical Feature ◽  
Late Ordovician ◽  
Growth Characteristics ◽  
Taxonomic Position ◽  
Phylogenetic Relation ◽  
Axial Mode ◽  
Rugose Corals ◽  
Lateral Mode ◽  
Tabulate Corals

AbstractAgetolites is a problematic Late Ordovician genus possessing traits of both tabulate and rugose corals. The presence of numerous mural pores has often been considered to indicate a relation to tabulates, although an affinity to rugosans has also been proposed, based mainly on well-developed septa that alternate in length. To further consider the taxonomic position of Agetolites, growth characteristics of coralla representing three species from the Xiazhen Formation in South China are documented and assessed, focusing on modes of corallite increase. Three major modes of increase are recognized. By far the most common mode involves the development of an offset from a connective mural pore, without a clear relationship to a particular parent corallite. This mode of increase is usually associated with corner pores, but in one case occurs at a wall pore. The lateral mode of increase, which is relatively uncommon, is a typical feature in corallites along the boundary of intergrowths with stromatoporoids. The axial mode of increase is rare, occurring during rejuvenation of a damaged corallite or during regeneration following termination of a corallite. The mode of corallite increase that is characteristic of Agetolites, involving a connective mural pore and occurring without evidence of a particular parent, supports the interpretation that this genus is not a rugosan or a typical favositid tabulate. Mural pores are unknown in rugosans, and offsets arise from distinct parent corallites in favositids. The Ordovician genus Lichenaria, considered a representative of the most primitive stock of tabulate corals, shows the closest similarities with types of increase in Agetolites. Certain aspects of lateral and axial increase in Agetolites are comparable to features in a few more genera of Ordovician tabulates, further supporting a tabulate affinity. The phylogenetic relation of Agetolites to those and other tabulate genera, however, remains unresolved.

Late Ordovician trilobites from the Mayatas Formation, Atansor area, north-central Kazakhstan

2016 ◽  
Vol 107 (1) ◽  
pp. 33-52
Author(s):  
L. M. E. McCobb ◽  
L. E. Popov
Keyword(s):  
South China ◽  
Deep Water ◽  
New Genus ◽  
Late Ordovician ◽  
Active Margin ◽  
North Central ◽  
Area North

ABSTRACTTwo trilobite faunas of Late Ordovician (Katian) age are described from the Mayatas Formation in the Stepnyak region of north-central Kazakhstan. The older, oligotaxic fauna derives from flanks of a carbonate build-up, and is dominated by numerous Sphaerexochus specimens. Amphilichas is also relatively common, with Pliomerina and indeterminate asaphids present as rare components. The overlying unit of siliceous argillites contains a different assemblage, representing the raphiophorid biofacies and comprising seven genera. The poorly preserved fauna is dominated by blind trilobites (a new genus of trinucleid, the three-segmented raphiophorid Pseudampyxina, Malongullia?, Lonchodomas and Arthrorhachis) and at least two species of large-eyed Telephina, suggesting that they occupied the disphotic zone in deep water offshore. A single cranidium of the odontopleurid Primaspis is also present. The trinucleid, Iputaspis stepnyakensis gen. et sp. nov., has an unusual pit arrangement, with E1 and E2 aligned in sulci and all I arcs irregularly arranged. The Atansor area is located within the Stepnyak tectonostratigraphical unit, which probably represented an Ordovician active margin of the Kalmykkol–Kokchetav Microplate. Some of the genera represented in the faunas have affinities with Australia and South China and, also, there is a possible link to European peri-Gondwana.

Late Ordovician brachiopod biofacies of the Girvan district, SW Scotland

2000 ◽  
Vol 91 (3-4) ◽  
pp. 471-477 ◽  
Author(s):  
David A. T. Harper
Keyword(s):  
South China ◽  
Deep Water ◽  
Late Ordovician ◽  
Outer Shelf ◽  
Tectonic Events ◽  
Environmental Fluctuations ◽  
Laurentian Margin

ABSTRACTDiverse and abundant brachiopod faunas, associated with unstable outer shelf and slope environments, occur through the Upper Ardmillan Group (upper Caradoc–upper Ashgill) in the Girvan district of SW Scotland. Representatives of the deep-water Foliomena fauna occur intermittently throughout the group, appearing in both the Whitehouse and Drummuck subgroups. This distinctive assemblage of small, thin-shelled brachiopods, including Dedzetina, Christiania, Cyclospira and Foliomena itself, first appeared in South China during the early Caradoc but had colonised the Laurentian margins by the late Caradoc. Within the upper Caradoc–lower Ashgill Whitehouse Subgroup, the Foliomena fauna is interbedded with a variety of other less cosmopolitan deep-water assemblages including the Onniella–Skenidioides and Lingulella–Trimurellina associations. Shallower-water environments in the middle Ashgill Lower Drummuck Subgroup hosted the Fardenia–Eopholidostrophia association in sands, and the Christiania-Leptaena association in muds and silts. The remarkable Lady Burn Starfish Beds in the upper part of the group contain a variety of brachiopod-dominated assemblages including the Eochonetes and Plaesiomys-Schizophorella associations, transported from various shelf locations, within a very diverse mid-Ashgill biota. Nevertheless, elements of the Foliomena fauna persisted to near the top of the Drummuck Subgroup, occurring as rare assemblages in more muddy and silty facies. The upper Ashgill High Mains Formation contains abundant elements of the terminal Ordovician Hirnantia fauna including Eostropheodonta, Hindella and Hirnantia itself, but also some taxa more typical of the Laurentian Edgewood Province. As a whole, the changing brachiopod biofacies monitor environmental fluctuations, on part of the Laurentian margin, driven by mainly eustatic and tectonic events.

DID VOLCANISM TRIGGER THE LATE ORDOVICIAN MASS EXTINCTION? MERCURY DATA FROM SOUTH CHINA

2016 ◽  
Author(s):  
David S. Jones ◽  
◽  
Anna M. Martini ◽  
Kunio Kaiho
Keyword(s):  
South China ◽  
Mass Extinction ◽  
Late Ordovician

Late Ordovician–Early Silurian chitinozoans from north-eastern and western Illinois, USA

2010 ◽  
Vol 159 (1-2) ◽  
pp. 81-93 ◽  
Author(s):  
Anthony Butcher ◽  
Donald G. Mikulic ◽  
Joanne Kluessendorf
Keyword(s):  
Late Ordovician ◽  
North Eastern
Sign in / Sign up

Export Citation Format

Share Document