Fossil evidence unveils an early Cambrian origin for Bryozoa

Bryozoans (also known as ectoprocts or moss animals) are aquatic, dominantly sessile, filter-feeding lophophorates that construct an organic or calcareous modular colonial (clonal) exoskeleton 1 – 3 . The presence of six major orders of bryozoans with advanced polymorphisms in lower Ordovician rocks...

Full description

Saved in:
Bibliographic Details
Published inNature (London) Vol. 599; no. 7884; pp. 251 - 255
Main Authors Zhang, Zhiliang, Zhang, Zhifei, Ma, Junye, Taylor, Paul D., Strotz, Luke C., Jacquet, Sarah M., Skovsted, Christian B., Chen, Feiyang, Han, Jian, Brock, Glenn A.
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group UK 11.11.2021
Nature Publishing Group
Subjects
Online AccessGet full text
ISSN0028-0836
1476-4687
1476-4687
DOI10.1038/s41586-021-04033-w

Cover

More Information
Summary:Bryozoans (also known as ectoprocts or moss animals) are aquatic, dominantly sessile, filter-feeding lophophorates that construct an organic or calcareous modular colonial (clonal) exoskeleton 1 – 3 . The presence of six major orders of bryozoans with advanced polymorphisms in lower Ordovician rocks strongly suggests a Cambrian origin for the largest and most diverse lophophorate phylum 2 , 4 – 8 . However, a lack of convincing bryozoan fossils from the Cambrian period has hampered resolution of the true origins and character assembly of the earliest members of the group. Here we interpret the millimetric, erect, bilaminate, secondarily phosphatized fossil Protomelission gatehousei 9 from the early Cambrian of Australia and South China as a potential stem-group bryozoan. The monomorphic zooid capsules, modular construction, organic composition and simple linear budding growth geometry represent a mixture of organic Gymnolaemata and biomineralized Stenolaemata character traits, with phylogenetic analyses identifying P. gatehousei as a stem-group bryozoan. This aligns the origin of phylum Bryozoa with all other skeletonized phyla in Cambrian Age 3, pushing back its first occurrence by approximately 35 million years. It also reconciles the fossil record with molecular clock estimations of an early Cambrian origination and subsequent Ordovician radiation of Bryozoa following the acquisition of a carbonate skeleton 10 – 13 . Interpretation of the early Cambrian fossil Protomelission gatehousei 9 as a potential stem-group bryozoan realigns the fossil record with molecular clock estimations of the origins of Bryozoa.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 14
content type line 23
ISSN:0028-0836
1476-4687
1476-4687
DOI:10.1038/s41586-021-04033-w