Silicon (Si) is a critical nutrient in the global ocean, essential for the growth of a wide range of organisms, including microalgae, sponges, and rhizarians. Silicifying Rhizaria were among the first protists to inhabit the ocean and, alongside sponges, dominated biogenic silica production during the Cambrian era. Despite their significance, these organisms remain poorly understood as key components of marine ecosystems. In today’s ocean, diatoms are widely recognized as the primary contributors to the Si cycle within the planktonic realm. However, recent research has uncovered that Rhizaria exhibit unexpectedly high individual Si production rates and biogenic silica content, indicating that their role in marine Si and carbon cycles may have been underestimated.
This project seeks to elucidate the process of silicification in Rhizaria and to identify the factors driving variability in silicic acid uptake. To achieve this, the work is divided into three integrated components. The first involves analyzing global transcriptomic data and individual transcriptomes of isolated Rhizaria to investigate the diversity of Si transporters. The second focuses on examining silica deposition using fluorescence markers across a wide range of Rhizaria. The third component quantifies gene expression during silicification, employing primers developed from the first component.
This interdisciplinary project leverages bioinformatics, molecular biology, and physiology, presenting a unified approach to studying plankton. Its outcomes will significantly enhance our understanding of Si transport in Rhizaria and their role in the ocean's biogeochemical Si cycle.