Natural and unnatural oil slicks in the Gulf of Mexico.

When wind speeds are 2-10 m s-1, reflective contrasts in the ocean surface make oil slicks visible to synthetic aperture radar (SAR) under all sky conditions. Neural network analysis of satellite SAR images quantified the magnitude and distribution of surface oil in the Gulf of Mexico from persistent, natural seeps and from the Deepwater Horizon (DWH) discharge. This analysis identified 914 natural oil seep zones across the entire Gulf of Mexico in pre-2010 data. Their ∼0.1 µm slicks covered an aggregated average of 775 km2. Assuming an average volume of 77.5 m3 over an 8-24 h lifespan per oil slick, the floating oil indicates a surface flux of 2.5-9.4 × 104 m3 yr-1. Oil from natural slicks was regionally concentrated: 68%, 25%, 7%, and <1% of the total was observed in the NW, SW, NE, and SE Gulf, respectively. This reflects differences in basin history and hydrocarbon generation. SAR images from 2010 showed that the 87 day DWH discharge produced a surface-oil footprint fundamentally different from background seepage, with an average ocean area of 11,200 km2 (SD 5028) and a volume of 22,600 m3 (SD 5411). Peak magnitudes of oil were detected during equivalent, ∼14 day intervals around 23 May and 18 June, when wind speeds remained <5 m s-1. Over this interval, aggregated volume of floating oil decreased by 21%; area covered increased by 49% (p < 0.1), potentially altering its ecological impact. The most likely causes were increased applications of dispersant and surface burning operations.

Asphalt volcanism and chemosynthetic life in the Campeche Knolls, Gulf of Mexico.

In the Campeche Knolls, in the southern Gulf of Mexico, lava-like flows of solidified asphalt cover more than 1 square kilometer of the rim of a dissected salt dome at a depth of 3000 meters below sea level. Chemosynthetic tubeworms and bivalves colonize the sea floor near the asphalt, which chilled and contracted after discharge. The site also includes oil seeps, gas hydrate deposits, locally anoxic sediments, and slabs of authigenic carbonate. Asphalt volcanism creates a habitat for chemosynthetic life that may be widespread at great depth in the Gulf of Mexico.

Chemosynthetic mussels at a brine-filled pockmark in the northern gulf of Mexico.

A large (540 square meters) bed of Bathymodiolus n. sp. (Mytilidae: Bivalvia) rings a pool of hypersaline (121.35 practical salinity units) brine at a water depth of 650 meters on the continental slope south of Louisiana. The anoxic brine (dissolved oxygen

12alpha- and 7alpha-hydroxysteroid dehydrogenase activities from Fusobacterium spp.

On screening fecal organisms for hydroxysteroid dehydrogenase activities applicable to bile acid metabolism studies, we have isolated a gram negative "Bacteroides-like" anaerobe which yields both 12alpha- and 7alpha-hydroxysteroid dehydrogenase (HSDH) activities in cell-free preparation. At the optimal harvest time of 36 hours, approximately 4500 units 12alpha-HSDH and 360 units 7alpha-HSDH were produced per 10(10) viable cells. The two enzymes appear to be separate entities in the basis of their stabilities on freezing, and prolonged storage at room temperature and elution volumes on Sephadex G 200. Thin layer chromatography studies on oxidation products confirmed the respective sites of oxidation to be the 12alpha-OH and 7alpha-OH position. No 3alpha-OH oriented activity was measurable. Preliminary kinetic studies of the 12alpha-HSDH revealed a broad pH curve with optimal activity at pH 9.5. Michaelis constants for glycodeoxycholate and NADP were estimated at 1.5 x 10(-4)M and 3.3 x 10(-5)M respectively.