Marine Biopolymer Dynamics, Gel Formation, and Carbon Cycling in the Ocean

Much like our own body, our planet is a macroscale dynamic system equipped with a complex set of compartmentalized controls that have made life and evolution possible on earth. Many of these global autoregulatory functions take place in the ocean; paramount among those is its role in global carbon cycling. Understanding the dynamics of organic carbon transport in the ocean remains among the most critical, urgent, and least acknowledged challenges to modern society. Dissolved in seawater is one of the earth's largest reservoirs of reduced organic carbon, reaching similar to 700 billion tons. It is composed of a polydisperse collection of marine biopolymers (MBP), that remain in reversible assembled <-> dissolved equilibrium forming hydrated networks of marine gels (MG). MGs are among the least understood aspects of marine carbon dynamics. Despite the polymer nature of this gigantic pool of material, polymer physics theory has only recently been applied to study MBP dynamics and gel formation in the ocean. There is a great deal of descriptive phenomenology, rich in classifications, and significant correlations. Still missing, however, is the guide of robust physical theory to figure out the fundamental nature of the supramolecular interactions taking place in seawater that turn out to be critical to understanding carbon transport in the ocean.

Automated summary

Similar to our body, the planet is a macroscopic dynamic system with compartmentalized controls that have enabled life and evolution. The transport of organic carbon in the ocean, forming marine gels, is a critical but often overlooked challenge. Understanding the fundamental nature of the molecular interactions in seawater is essential for comprehending carbon transport dynamics in the ocean.