1 research outputs found
Toxicity and Mutagenicity of Gulf of Mexico Waters During and After the Deepwater Horizon Oil Spill
The Deepwater Horizon oil spill is
unparalleled among environmental
hydrocarbon releases, because of the tremendous volume of oil, the
additional contamination by dispersant, and the oceanic depth at which
this release occurred. Here, we present data on general toxicity and
mutagenicity of upper water column waters and, to a lesser degree,
sediment porewater of the Northeastern Gulf of Mexico (NEGOM) and
west Florida shelf (WFS) at the time of the Deepwater Horizon oil
spill in 2010 and thereafter. During a research cruise in August 2010,
analysis of water collected in the NEGOM indicated that samples of
3 of 14 (21%) stations were toxic to bacteria based on the Microtox
assay, 4 of 13 (34%) were toxic to phytoplankton via the QwikLite
assay, and 6 of 14 (43%) showed DNA damaging activity using the λ-Microscreen
Prophage induction assay. The Microtox and Microscreen assays indicated
that the degree of toxicity was correlated to total petroleum hydrocarbon
concentration. Long-term monitoring of stations on the NEGOM and the
WFS was undertaken by 8 and 6 cruises to these areas, respectively.
Microtox toxicity was nearly totally absent by December 2010 in the
Northeastern Gulf of Mexico (3 of 8 cruises with one positive station).
In contrast, QwikLite toxicity assay yielded positives at each cruise,
often at multiple stations or depths, indicating the greater sensitivity
of the QwikLite assay to environmental factors. The Microscreen mutagenicity
assays indicated that certain water column samples overlying the WFS
were mutagenic at least 1.5 years after capping the Macondo well.
Similarly, sediment porewater samples taken from 1000, 1200, and 1400
m from the slope off the WFS in June 2011 were also highly genotoxic.
Our observations are consistent with a portion of the dispersed oil
from the Macondo well area advecting to the southeast and upwelling
onto the WFS, although other explanations exist. Organisms in contact
with these waters might experience DNA damage that could lead to mutation
and heritable alterations to the community pangenome. Such mutagenic
interactions might not become apparent in higher organisms for years