Despite its significance, the full extent of these environmental changes and the ways they interacted remained poorly resolved. The new analysis addresses this gap by combining precisely dated strata with independent records of sea level and biodiversity. Time series analysis of the sedimentary archives revealed a distinct rhythm of approximately 2 million years that aligns with cycles in reconstructed sea-level fluctuations and biodiversity dynamics.

Most strikingly, the researchers found that sea-level changes preceded shifts in benthic species richness by about 70,000 years. This lag links astronomically driven eustatic oscillations, meaning global changes in sea level, to marine redox fluctuations and concurrent biodiversity turnover. The finding connects orbital forcing to ocean chemistry and biological change during this critical interval of Earth history, with sea-level variation operating as a leading signal ahead of the ecological response recorded in seafloor-dwelling communities.

The results offer pivotal constraints on ocean-climate interactions during the Cambrian and provide insight into Earth system resilience to extreme climatic and biogeochemical perturbations.

Subject of Research: Coupled sea-level and biodiversity dynamics during the Cambrian SPICE event

Article Title: Coupled sea-level and biodiversity dynamics during the Cambrian SPICE event

Article References: Wang, M., Shi, Y., Yang, A., Zhang, H., Zhang, X., Wu, Y., Shi, Y., Liu, J., Wei, R., Jin, Z., & Li, M. (2026). Coupled sea-level and biodiversity dynamics during the Cambrian SPICE event. Nature Communications. https://doi.org/10.1038/s41467-026-78601-x

Image Credits: AI Generated

DOI: 10.1038/s41467-026-78601-x

Keywords: Cambrian, SPICE event, carbon isotope excursion, astrochronology, sea level, biodiversity, marine anoxia, North China Block, ocean-climate interactions, Coupled, sea-level, dynamics