Long-Term Effects of an Oil Spill on Populations of the Salt-Marsh Crab Uca pugnax

1978 ◽  
Vol 35 (5) ◽  
pp. 648-649 ◽  
Author(s):  
C. T. Krebs ◽  
K. A. Burns

A spill of fuel oil at West Falmouth, Massachusetts, in 1969 contaminated contiguous salt marshes with up to 6000 μg oil/g (ppm) of wet mud and affected local populations of the salt-marsh crab Uca pugnax. Directly related to high sediment oil content were reduced crab density, reduced ratio of females to males, reduced juvenile settlement, heavy overwinter mortality, incorporation of oil into body tissues, behavioral disorders such as locomotor impairment, and abnormal burrow construction. Concentrations of weathered fuel oil > 1000 ppm were directly toxic to adults, while those of 100–200 ppm were toxic to juveniles. Cumulative effects occurred at lower concentrations. Recovery of the marsh from this relatively small oil spill is still incomplete after 7 yr. Interpretation of the crab population data upon the basis of detailed analysis of the aromatic fraction of the fuel oil provided by Dr J. Teal, Woods Hole Oceanographic Institution, showed that recovery of the crab populations was highly correlated with the disappearance of the naphthalene fraction of the aromatics. There had been a decrease in the aromatics from 42% in 1970 to approximately 18% in 1976 in Station I surface sediments, while preliminary analyses show aromatics still high at other stations where little recovery has been observed. By 1970–71 all parent naphthalene compounds were gone in Station I surface sediments, but substituted naphthalenes were still in high concentrations. By 1972–73 dimethyl naphthalenes and C3 and C4 substituted naphthalenes remained at about 25% of original values. By 1976–77 only C3 and C4 substituted naphthalenes remained at less than one tenth of their 1973 levels. In 1972–73 the substituted naphthalenes were at high enough concentrations to prevent recruitment, as large juvenile crab settlements in 1970–73 produced no recruitment into the crab populations. By 1976–77 these toxic compounds were at low enough levels that recovery of the crab population was occurring with recruitment, and increasing density was observed in both years. High aromatic concentrations at other stations may still be inhibiting recovery at these stations. The long-term inhibition of recruitment and low population densities may have resulted from exposure to oil in the interstitial waters during the sensitive molt period and/or during the long periods of time while the crabs were overwintering in the substrate. Key words: petroleum, Uca pugnax, crab, salt-marsh, population, pollution

Science ◽  
1977 ◽  
Vol 197 (4302) ◽  
pp. 484-487 ◽  
Author(s):  
C. T. KREBS ◽  
K. A. BURNS

Microbiome ◽  
2021 ◽  
Vol 9 (1) ◽  
Author(s):  
Daniel R. Leadbeater ◽  
Nicola C. Oates ◽  
Joseph P. Bennett ◽  
Yi Li ◽  
Adam A. Dowle ◽  
...  

Abstract Background Salt marshes are major natural repositories of sequestered organic carbon with high burial rates of organic matter, produced by highly productive native flora. Accumulated carbon predominantly exists as lignocellulose which is metabolised by communities of functionally diverse microbes. However, the organisms that orchestrate this process and the enzymatic mechanisms employed that regulate the accumulation, composition and permanence of this carbon stock are not yet known. We applied meta-exo-proteome proteomics and 16S rRNA gene profiling to study lignocellulose decomposition in situ within the surface level sediments of a natural established UK salt marsh. Results Our studies revealed a community dominated by Gammaproteobacteria, Bacteroidetes and Deltaproteobacteria that drive lignocellulose degradation in the salt marsh. We identify 42 families of lignocellulolytic bacteria of which the most active secretors of carbohydrate-active enzymes were observed to be Prolixibacteracea, Flavobacteriaceae, Cellvibrionaceae, Saccharospirillaceae, Alteromonadaceae, Vibrionaceae and Cytophagaceae. These families secreted lignocellulose-active glycoside hydrolase (GH) family enzymes GH3, GH5, GH6, GH9, GH10, GH11, GH13 and GH43 that were associated with degrading Spartina biomass. While fungi were present, we did not detect a lignocellulolytic contribution from fungi which are major contributors to terrestrial lignocellulose deconstruction. Oxidative enzymes such as laccases, peroxidases and lytic polysaccharide monooxygenases that are important for lignocellulose degradation in the terrestrial environment were present but not abundant, while a notable abundance of putative esterases (such as carbohydrate esterase family 1) associated with decoupling lignin from polysaccharides in lignocellulose was observed. Conclusions Here, we identify a diverse cohort of previously undefined bacteria that drive lignocellulose degradation in the surface sediments of the salt marsh environment and describe the enzymatic mechanisms they employ to facilitate this process. Our results increase the understanding of the microbial and molecular mechanisms that underpin carbon sequestration from lignocellulose within salt marsh surface sediments in situ and provide insights into the potential enzymatic mechanisms regulating the enrichment of polyphenolics in salt marsh sediments.


1987 ◽  
Vol 1987 (1) ◽  
pp. 445-449 ◽  
Author(s):  
Steve K. Alexander ◽  
James W. Webb

ABSTRACT A single spill of crude oil in a salt marsh is generally considered to have limited biological effects. A crude oil spill in Dickinson Bayou (in the Galveston Bay system of Texas) in January 1984 provided the opportunity to test this hypothesis in salt marshes exposed to varying amounts of oil. Growth of Spartina alterniflora was unaffected in light to moderately oiled sediments (less than 5 mg oil/g sediment). However, growth was significantly reduced in sediments with high oil content (5 to 51 mg/g) through 18 months. Erosion of shoreline areas with high oil content was evident by 16 months and continued through 32 months. These results demonstrate the adverse effect of high concentrations of crude oil in salt marsh sediments. Each crude oil spill must be evaluated individually with regard to the likelihood of significant accumulation of oil in sediments before a decision is made regarding a cleanup response.


2005 ◽  
Vol 2005 (1) ◽  
pp. 869-872 ◽  
Author(s):  
Chuck Getter ◽  
Jacqui Michel ◽  
Miles Hayes

ABSTRACT Our team completed a broad multidisciplinary survey in 2003 characterizing several thousand transects along 850 km of oil-impacted shoreline to determine the impacts of the 1991 oil spill on the Saudi Arabian Gulf from the western end of Abu Ali Island to the Kuwait border. Salt marshes and tidal flats there form a very significant portion of the oil-impacted coastline. These habitats were heavily oiled in 1991 and significant loss of biological communities was reported then. Although a large scale response effort followed the spill, the size of the spill overwhelmed it. The overwhelming majority of the spill site is remote and will likely receive little or no cleanup and/or restoration effort. After completing the survey, we conducted an ecological survey at two selected salt marsh transects using line-intercept and quadrat counts counting macrovegetation and intertidal macroepibenthos within one impacted (recovering) and one unoiled (comparison) transect. The objective of our paper is to present useful highlights regarding the nature of the recovery of intertidal macroepibenthos and the vegetation associated with salt marshes. A continuing impact to key species and their assemblages is documented and discussed. We conclude that while recovery has progressed from initial reports of significant damages in 1991–1993 the overall recovery of the salt marshes is far from complete. Some areas of considerable size and importance show little or no sign of recovery. In summary, the oil spill of 1991 was arguably the largest coastal spill in history. Long-term effects are widespread, appear to be profoundly large-scale, and in some cases salt marshes show little sign of natural recovery.


2001 ◽  
Vol 2001 (1) ◽  
pp. 399-403 ◽  
Author(s):  
Mark G. Carls ◽  
Ron Heintz ◽  
Adam Moles ◽  
Stanley D. Rice ◽  
Jeffrey W. Short

ABSTRACT Immediate damage from an oil spill is usually obvious (oiled birds, oiled shoreline), but long-term damage to either fauna or habitat is more subtle, difficult to measure, difficult to evaluate, and hence often controversial. The question is, are too many of response decisions such as dispersant use or shoreline cleanup based on short-term acute toxicity models? Have long-term damage scenarios been discounted because of the inherent difficulty in deriving definitive answers? Experience with the Exxon Valdez oil spill is shedding new light on the potential for long-term damage. Government-funded studies demonstrated that oil persists in certain habitats for extended periods of time, such as the intertidal reaches of salmon streams, in soft sediments underlying mussel beds, and on cobble beaches armored with large boulders. Observation of long-term persistence of oil in some habitats is not new, but an increasing number of studies indicate that fauna may be chronically and significantly exposed to oil in these habitats. The toxic components in oil responsible for much of the long-term effects are believed to be the larger 3- and 4-ring polyaromatic hydrocarbons (PAHs) that can induce cellular and genetic effects rather than the narcotic monoaromatic hydrocarbons (MAHs) responsible for acute mortalities. Observation of long-term persistence of Exxon Valdez oil, coupled with adverse effects on sensitive life stages, leads to the conclusion that strategies based on minimizing acute mortalities immediately following a spill probably do not provide adequate protection against long-term damage. When making environmental decisions in response to a spill (prevention measures or restoration measures), more weight should probably be given to long-term issues rather than discounting their significance. Total environmental cost is the sum of short-term damage and long-term damage, and long term-damage to habitats and sensitive life stages probably needs more consideration even though it is very difficult to evaluate and compare to the relatively obvious acute issues.


1997 ◽  
Vol 1997 (1) ◽  
pp. 1040-1041 ◽  
Author(s):  
Sally C. Levings ◽  
Stephen D. Garrity ◽  
Edward S. Van Vleet ◽  
Dana L. Wetzel

ABSTRACT More than 300,000 gallons of refined petroleum products were discharged near the entrance to Tampa Bay, Florida on August 10, 1993. Floating slicks and sunken oil patty (no. 6 fuel oil) subsequently entered Boca Ciega Bay through John's Pass and washed or stranded on four mangrove keys inside the pass. Between one and two years after the spill, surviving red mangroves showed graded negative responses to oil in 4 of 4 measures of shoot growth and production. Sublethal, long-term effects of oil spills may be more common than reported, but detection requires detailed data on species-specific growth and production patterns with respect to oiling.


2014 ◽  
Vol 2014 (1) ◽  
pp. 1985-1999 ◽  
Author(s):  
Scott Zengel ◽  
Nicolle Rutherford ◽  
Brittany Bernik ◽  
Zachary Nixon ◽  
Jacqueline Michel

ABSTRACT The Deepwater Horizon oil spill resulted in persistent heavy oiling in salt marshes, particularly in northern Barataria Bay, Louisiana. Oiling conditions and several ecological variables were compared among reference plots and three types of heavily oiled plots located along a continuous shoreline area in northern Barataria Bay: oiled control plots, mechanical treatment plots, and mechanical treatment plots coupled with vegetation planting (Spartina alterniflora). Data were collected more than three years following initial oiling and two years following cleanup treatments and planting. Salt marsh oiling and associated impacts were apparent across all oiling/treatment classes relative to reference conditions. Mechanical treatment with planting showed the most improvement in oiling conditions and was also effective in re-establishing vegetation cover and plant species composition similar to reference conditions, in contrast to the oiled controls and mechanical treatment plots without planting. Marsh periwinkle (Littoraria irrorata) recovery was limited across all oiling/treatment classes relative to reference. Impacts to fiddler crabs (Uca spp.) were also documented in the heavily oiled plots. Positive influences of mechanical treatment and planting on macroinvertebrate recovery were observed; however, invertebrate recovery may lag the return of Spartina alterniflora by several years. Vegetation planting should be considered as a spill response and emergency restoration option for heavily oiled salt marshes where vegetation impacts are substantial, natural recovery may be lacking or delayed, intensive cleanup treatments are used, or where marsh shorelines are at risk of erosion.


The supertanker Amoco Cadiz wrecked on the coast of northern Brittany in April 1978. The resulting spill of 223000 t of crude oil polluted some 360 km of rocky or sandy shores, salt marshes and estuaries. An immediate mortality impact was observed. Populations of bivalves, periwinkles, limpets, peracarid crustaceans, heart urchins and sea birds were the most severely affected. Populations of polychaete worms, large crustaceans and coastal fishes were less affected. Three to six generations (5—10 years for bivalves but up to 60 years for birds) may be necessary before populations retrieve their stable age distribution. Delayed effects on mortality, growth and recruitment were still observed up to 3 years after the spill. Estuarine flat fishes and mullets had reduced growth, fecundity and recruitment; they were affected by fin rot disease. Populations of clams and nematodes in the meiofauna declined one year after the spill. Weathered oil is still present in low-energy areas. Species with short life cycles tend to replace long-lived species. A fauna of cirratulid and capitellid polychaete worms now prevails in sandy to m uddy areas. For several clam populations, recruitment remains unstable. Three years after the spill it is still premature to decide how long it will take before populations and ecosystems reach their former or new equilibria.


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