4.1 Article

Development of the early Cambrian oryctocephalid trilobite Oryctocarella duyunensis from western Hunan, China

Journal

JOURNAL OF PALEONTOLOGY
Volume 95, Issue 4, Pages 777-792

Publisher

CAMBRIDGE UNIV PRESS
DOI: 10.1017/jpa.2020.111

Keywords

-

Categories

Funding

  1. National Key Research and Development Program [2017YFC0603101]
  2. Natural Science Foundation of China [42072021, 41890844, 41890840, 41621003, 41330101, 41521061, 41290260]
  3. 111 Project [D17013]
  4. Ministry of Science and Technology of China [2015FY310100]
  5. National Commission on Stratigraphy of China [DD20160120-04]
  6. key project of the State Key Laboratory of Continental Dynamics [201210128]
  7. IGCP 668 project The Stratigraphic and Magmatic History of Early Paleozoic Equatorial Gondwana and its Associated Evolutionary Dynamics
  8. Strategic Priority Research Program of Chinese Academy of Sciences [XDB26000000]
  9. Shaanxi Provincial Education Department [17JK0762]
  10. Shaanxi Natural Science Basic Research Project [2018JM4038]
  11. Key Scientific and Technological Innovation Team Project in Shaanxi Province
  12. US National Science Foundation [EAR-1849963]
  13. Fulbright Academic and Professional Excellence Award [2019 APE-R/107]

Ask authors/readers for more resources

Abundant articulated specimens of the oryctocarine trilobite Oryctocarella duyunensis from the lower Cambrian Balang Formation in western Hunan Province, South China, allow the description of all meraspid degrees. The study shows progressive and gradual change in overall form during meraspid growth, with variation in the number of pygidial segments. A model based on degree-based ontogenetic staging is more likely to explain the growth pattern observed, compared to a model based on the number of thoracic and pygidial segments.
Abundant articulated specimens of the oryctocarine trilobite Oryctocarella duyunensis from the lower Cambrian (Stage 4, Series 2) Balang Formation at the Bulin section in western Hunan Province, South China, permit the description of all meraspid degrees. The maximum number of thoracic segments observed in this collection is 11. Meraspid growth was accompanied by progressive and gradual change in overall form, and this animal showed an homonymously segmented trunk with variation in the number of pygidial segments during ontogeny. Such variation permits a variety of plausible explanations, but a model of successive instars defined by the number of thoracic segments, and in suborder by the number of pygidial segments, is highly unlikely to explain the growth pattern because it would result in the loss of trunk segments between some instars. Degree-based ontogenetic staging is compatible with the variation observed.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.1
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available