Marco A. Aquino-López , Nicole K. Sanderson , Maarten Blaauw , Joan-Albert Sanchez-Cabeza , Ana Carolina Ruiz-Fernández , J. Andrés Christen
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引用次数: 0
Abstract
Accurate dating of sediment layers is vital for deciphering Earth’s environmental history. This study addresses the precision and accuracy of lead-210 (210Pb) dating models, a critical tool in sedimentary research for understanding environmental changes. Traditional Constant Rate of Supply (CRS) methods, while widely used, often struggle with accuracy, particularly in complex sedimentation scenarios. We contrast the CRS model with Plum, an advanced Bayesian approach, using simulated 210Pb profiles derived from varied sedimentation processes. Our analysis reveals that even under ideal CRS conditions, the model’s precision does not significantly improve with additional data. In the contrary, Plum consistently outperforms CRS in both accuracy and precision, even with limited data inputs. As data volume increases, Plum’s performance improves markedly, unlike CRS. The Bayesian framework effectively addresses the complexities overlooked by CRS, demonstrating its superiority in refining sediment chronologies. This paper highlights the importance of incorporating statistical advancements in sediment dating techniques. By applying refined Bayesian methods like Plum, researchers can achieve more reliable sediment chronologies, essential for robust environmental studies and unravelling complex climate histories. Our findings suggest that embracing statistical innovations in geochronology can substantially enhance our understanding of Earth’s environmental changes.
期刊介绍:
Quaternary Geochronology is an international journal devoted to the publication of the highest-quality, peer-reviewed articles on all aspects of dating methods applicable to the Quaternary Period - the last 2.6 million years of Earth history. Reliable ages are fundamental to place changes in climates, landscapes, flora and fauna - including the evolution and ecological impact of humans - in their correct temporal sequence, and to understand the tempo and mode of geological and biological processes.