Marine microgels.

The ocean plays a critical role in global carbon cycling: it handles half of the global primary production, yielding the world's largest stock of reduced organic carbon (ROC) that supports one of the world's largest biomasses. However, the mechanisms whereby ROC becomes mineralized remain unresolved. This review focuses on laboratory and field observations that dissolved organic carbon (DOC) self-assembles, forming self-assembled microgels (SAGs). Self-assembly has approximately10% yield, generating an estimated global seawater SAG budget of approximately 10(16) g C. Transects at depths of 10-4,000 m reveal concentrations of approximately 10(6) to approximately 3 x 10(12) SAG L(-1), respectively, forming an estimated ROC stock larger than the global marine biomass. Because hydrogels have approximately 1% solids (10 g L(-1)), whereas seawater DOC reaches approximately 10(-3) g L(-1), SAGs contain approximately 10(4) more bacterial substrate than seawater. Thus, microgels represent an unsuspected and huge micron-level ocean patchiness that could profoundly influence the passage of DOC through the microbial loop, with ramifications that may scale to global cycles of bioactive elements.