BRACHIOPODS FROM THE BYRD GROUP (CAMBRIAN SERIES 2, STAGE 4) CENTRAL TRANSANTARCTIC MOUNTAINS, EAST ANTARCTICA: BIOSTRATIGRAPHY, PHYLOGENY AND SYSTEMATICS

• Published in: Papers in Palaeontology
• Main Authors: Claybourn, Thomas M., Skovsted, Christian B., Holmer, Lars E., Pan, Bing, Myrow, Paul M., Topper, Timothy P., Brock, Glenn A.
• Format: Report
• Language: English
• Published: WILEY 2020
• Subjects: brachiopods; East Antarctica; Cambrian Series 2; Biostratigraphy; Palaeobiogeography; cladistics; 3 GORGES AREA; ROSS OROGEN; ACROTRETOID BRACHIOPODS; ORDINAL CLASSIFICATION; LINGULATE BRACHIOPODS; SHUIJINGTUO FORMATION; DELAMERIAN OROGENY; SOUTH-AUSTRALIA; SHELLY FOSSILS; AMADEUS BASIN; Paleontology; Transantarctic Mountains; Byrd; Antarc*; Antarctica
• Online Access: http://ir.nigpas.ac.cn/handle/332004/31438; https://doi.org/10.1002/spp2.1295

Brachiopods from Cambrian Series 2, Stage 4 carbonate strata of the Byrd Group in the Central Transantarctic Mountains, East Antarctica, are described for the first time. These include six Ungulate, one paterinate and one rhynchonelliform taxon, including the new 'Ungulate brachiopod Pliatrmus wildi gen. et sp. nov. The biostratigraphy correlates closely to the brachiopods recently reported from the Xinji Formation (Shuiyu section) in North China, as well as brachiopods recovered from the Dailyatia odyssei Zone across the Arrowie Basin of South Australia. These findings also support the previously identified close palaeobiogeography of these regions. The first unambiguous example of the acrotretid brachiopod Eohadrotreta zhenbaensis Li & Holmer outside South China is also identified in the context of its ontogenetic stages. Well-preserved specimens of the acrotheloid Schizopholis yorkensis (Holmer & Ushatinskaya) facilitate a new reconstruction of its musculature and visceral region. These data are synthesized into a new cladistic analysis that resolves Acrotheloidea as a well-supported monophyletic Glade and supports previous hypotheses of a morphocline in acrotheloid evolution.