Temperature-Regulated Turnover Of Chromophoric Dissolved Organic Matter In Global Dark Marginal Basins

Oceanic absorption of heat generated by greenhouse gas emissions has resulted in warming of the dark ocean (>200 m) that contains a large refractory DOM (RDOM) pool. However, changes in microbially mediated production and degradation dynamics for RDOM components in response to warming of dark marginal basins remain unclear. Herein, we integrated data from the dark South China, Mediterranean and Japan Seas (temperature range: 0.09-15.1 degrees C) to demonstrate that in situ production efficiency of two ubiquitous humic-like fluorophores increased at higher dark ocean temperature, whereas chromophores at a wavelength of 325 nm (a(CDOM)(325)) changed from production to degradation at higher temperature. Increased oxygen consumption and a reduction of labile substrates in future warmer dark ocean environments may initiate the final degradation of some semi-refractory components, thereby increasing the recalcitrance of RDOM, but decreasing the DOM inventory in dark basins and creating a positive feedback to rising atmospheric CO2.