Assessing the impacts of oil-associated marine snow formation and sedimentation during and after the Deepwater Horizon oil spill. (March 2016)

• Record Type: Journal Article
• Authors: Daly, Kendra L.; Passow, Uta; Chanton, Jeffrey; Hollander, David
• Is Part Of: Anthropocene. Volume 13(2016)
• Page Start: 18
• Page End: 33
• Publication Date: 2016-03
• Subjects: Deepwater Horizon oil spill -- Gulf of Mexico -- Marine oil snow -- MOSSFA -- Bacteria -- Plankton; Nature -- Effect of human beings on -- Periodicals; Human ecology -- Periodicals; 304.2
• DOI: 10.1016/j.ancene.2016.01.006
• Languages: English
• ISSNs: 2213-3054

Abstract

Highlights: A significant fraction of DWH oil was transported to depth via sinking oil-associated marine snow (MOS), which formed in surface waters. MOS formation and sedimentation was influenced by plankton dynamics and river discharge of nutrients and suspended minerals. Sedimented oil on the seafloor impacted benthic organisms and sediment bio-geochemistry. Baseline time-series data and model development are urgently needed for all levels of ecosystems in regions of hydrocarbon extraction. Emergency responders should consider oil sedimentation processes when planning oil spill mitigation strategies. Abstract: The Deepwater Horizon oil spill was the largest in US history, unprecedented for the depth and volume of oil released, the amount of dispersants applied, and the unexpected, protracted sedimentation of oil-associated marine snow (MOS) to the seafloor. Marine snow formation, incorporation of oil, and subsequent gravitational settling to the seafloor (i.e., MOSSFA: Marine Oil Snow Sedimentation and Flocculent Accumulation) was a significant pathway for the distribution and fate of oil, accounting for as much as 14% of the total oil released. Long residence times of oil on the seafloor will result in prolonged exposure by benthic organisms and economically important fish. Bioaccumulation of hydrocarbons into the food web also has been documented. Major surface processes governing the MOSSFA event included an elevated and extended Mississippi River discharge, which enhanced phytoplankton production and suspended particle concentrations, zooplankton grazing, and enhanced microbial mucus formation. Previous reports indicated that MOS sedimentation also occurred during the Tsesis and Ixtoc-I oil spills; thus, MOSSFA events may occur during future oil spills, particularly since 85% of global deep-water oil exploration sites are adjacent to deltaic systems. We provide a conceptual framework of MOSSFA processes and identify data gaps to help guide current research and to improve our ability to predict MOSSFA events under different environmental conditions. Baseline time-series data and model development are urgently needed for all levels of ecosystems in regions of hydrocarbon extraction to prepare for and respond to future oil spills and to understand the impacts of oil spills on the environment.