Speaker: Dr. Jordan Rosenfeld
Honorary Faculty
Applied Freshwater Research Unit, BC Ministry of Environment
Hypoxia is defined as depression of dissolved oxygen levels below saturation, and can have negative impacts on plants and animals reliant on oxygen for growth and survival. Thresholds for hypoxia in marine pelagic systems have traditionally been defined as 2 mg/l or thereabouts in the academic literature. However, this is well below saturation, and well below the threshold for negative impacts on physiology, growth, and survival for many organisms. In contrast, threshold for hypoxia in freshwater and in most jurisdictional regulations are typically set at much higher values (range of 4-6 mg/l). The origin of thresholds for hypoxia in marine pelagic systems is obscure, but appears to be based on catastrophic collapse or change in community structure, while thresholds in freshwater are based on incipient impacts to individual growth or survival. Dr. Rosenfeld speculates on the origins of this discrepancy and it’s implications for management and perceptions of impact in freshwater and marine ecosystems |