1. Shallow ocean deoxygenation drove trilobite turnover during the late Cambrian SPICE event.
- Author
-
Aihua Yang, Bo Chen, Zhixin Sun, Tostevin, Rosalie, Tianchen He, Xi Chen, Jitao Chen, Miao Lu, Chunlin Hu, Shengxian Du, Jun Chen, Wenjun Jiao, and Maoyan Zhu
- Subjects
- *
HYPOXIA (Water) , *TRILOBITES , *ANOXIC waters , *DEOXYGENATION , *CARBON isotopes , *OCEAN - Abstract
The spread of marine anoxia is believed to have played a key role in the development of the SPICE (Steptoean Positive Carbon Isotope Excursion) event and the end-Marjuman extinction in the late Cambrian (∼497.5 m.y. ago), but their cause-and-effect relationship is poorly constrained. Here we present an integrated analysis of carbonate δ13C, cerium anomalies (Ce/Ce*), and genus-level diversity data of trilobites from the North China Platform. Our results show tightly coupled changes between the SPICE, an increase in Ce/Ce*, and a trilobite turnover event, which we interpret as indicating enhanced productivity and organic remineralization, leading to the development of low-oxygen conditions in shallowwater settings. This study therefore establishes a direct link between local ecological stress and trilobite turnover during the global SPICE event. Furthermore, the presence of low-oxygen rather than fully anoxic conditions during the peak of the SPICE event could explain the nature of the end-Marjuman crisis, which was characterized by the replacement of shallowwater fauna by deeper-water counterparts that were potentially more tolerant of hypoxia. [ABSTRACT FROM AUTHOR]
- Published
- 2024
- Full Text
- View/download PDF