Early recovery of sponge framework reefs after Cambrian archaeocyath extinction: Zhangxia Formation (early Cambrian Series 3), Shandong, North China
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- 作者：Jeong-Hyun Leea ; jeonghyunlee@cnu.ac.kr" class="auth_mail" title="E-mail the corresponding author ; Jongsun Hongb ; bulgeun@korea.ac.kr" class="auth_mail" title="E-mail the corresponding author ; Suk-Joo Chohb ; sjchoh@korea.ac.kr" class="auth_mail" title="E-mail the corresponding author ; Dong-Jin Leec ; d ; djlee@andong.ac.kr" class="auth_mail" title="E-mail the corresponding author ; Jusun Wooe ; jusunwoo@kopri.re.kr" class="auth_mail" title="E-mail the corresponding author ; Robert Ridingf ; rriding@utk.edu" class="auth_mail" title="E-mail the corresponding author
- 关键词：Cambrian ; Metazoan-microbial reef ; Sponge ; Rankenella ; Reef framework
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：1 September 2016
- 年：2016
- 卷：457
- 期：Complete
- 页码：269-276
- 全文大小：2774 K
文摘
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Lithistid sponges mutually attached and formed reef framework in the middle Cambrian.
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Their structure is similar to those of archaeocyath reefs and Early Ordovician reefs.
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Lithistid sponge-microbial reefs were widespread throughout the mid-late Cambrian.
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Framework-building metazoans recovered within ~ 5 Myr of the archaeocyath reef decline.