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Review of Research on Early Cambrian Phosphatized Quadrapyrgites

Journal

ACTA GEOLOGICA SINICA-ENGLISH EDITION
Volume 89, Issue 4, Pages 1398-1405

Publisher

WILEY-BLACKWELL
DOI: 10.1111/1755-6724.12535

Keywords

SSFs; Quadrapyrgites; Meishucunian; Ontogenetic Sequence; Shaanxi province

Funding

  1. National Natural Science Foundation of China [41072012]
  2. State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences [113115, 20132107]
  3. Central University Fund [CHD2012ZD017]
  4. College Students' Innovative Entrepreneurial Training Program of Chang'an University [201510710060, 201510710056, 201510710179]

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The metazoan Quadrapyrgites consists, from proximal to distal ends, of an oral area, a cone, a collar, and an apex from the Early Cambrian Fortunian Stage in Xixiang Zhangjiagou section, southern Shaanxi Province, South China. Three morphological types of the apex, the most characteristic feature of the taxon, are identified from hundreds of Quadrapyrgites specimens. The Quadrapyrgites growth zone is situated at the oral end, where 12 terminal lobes are generated, uplifted, enlarged, and evaginated to form a crest; A one-by-one of crest number from 2 to 13 has been recognized. The unique growth pattern and ontogenetic sequence refute a cubozoan or cycloneuralian affinity for Olivooides and Quadrapyrgites, and instead defend a coronate scyphozoan hypothesis. An embryonic development and ontogenetic sequence with embryo and crest is constructed.

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