Distinct activity phases during the recent geologic history of a Gulf of Mexico mud volcano |
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| Authors: | IR MacDonald MB Peccini |
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| Institution: | 1. Department Physical and Environmental Sciences, Texas A&M University – Corpus Christi, 6300 Ocean Dr., HR121, Corpus Christi, TX 78412, USA;2. I.M. Systems Group/NOAA Fisheries, 1315 East-West Highway, Silver Spring, MD 20910, USA |
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| Abstract: | Laser line scan imaging and chirp sub-bottom profiling were used to detail the morphology of a submarine mud volcano and brine-filled crater at 652 m water depth in the northern Gulf of Mexico. The mud volcano has a relief of 6 m and a basal diameter of about 80 m. The feature comprises a central, brine-filled crater (253 m2) surrounded by a continuous bed of methanotrophic mussels (Bathymodiolus childressi) covering 434 m2 and a patchy bed covering an additional 214 m2 of the periphery. The brine pool was mostly <2 m deep, but there were two holes of >28 m and 12 m deep, respectively at the northern end of the pool which emitted continual streams of small clear bubbles. Sub-bottom profiles indicated three distinct strata beneath the present surface of the mud volcano. Integration of 17 profiles shows that the mud volcano has been built in at least three successive stages: the lowest stage deposited 35,400 m3, while the middle and upper stages deposited 7700 and 20,400 m3, respectively. Piston cores were taken at the northern edge of the mussel bed and a site ∼100 m southwest of the pool. Mussel and lucinid shells were recovered from the closer core, lucinid shells from the distant core. A mussel shell from 3.4 m sub-bottom had a Δ14C age of 16.2 ka. Mixture of modern carbon with “carbon dead” reservoir material would produce actual ages ∼2 ka less than the radiocarbon ages. |
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| Keywords: | Mud volcano Brine pool Seep mussel Radiocarbon age Eruption Bathymodiolus childressi Laser line scan Sub-bottom profile |
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