• journal_title：Journal of Sedimentary Research
• Contributor：Michael H. Bothner ; E. C. Spiker ; P. P. Johnson ; R. R. Rendigs ; P. J. Aruscavage
• Publisher：SEPM Society for Sedimentary Geology
• Date：1981-
• Format：text/html
• Language：en
• Identifier：10.1306/212F7C70-2B24-11D7-8648000102C1865D
• journal_abbrev：Journal of Sedimentary Research
• issn：1527-1404
• volume：51
• issue：1
• firstpage：281
• section：Articles

An area of fine-grained sediment approximately 170 km x 74 km in size, located in water depths between 60 m and 150 m, south of Martha's Vineyard, Mass., is a site of modern sediment deposition. The ¹⁴ C ages systematically increase with sediment depth from about 1,300 years B.P. at the surface to 8,000-10,000 years B.P. at the depth of maximum core penetration. The old age for the surface sediments probably results from a combination of deposition of old carbon and faunal mixing. In the finest sediments, the sedimentation rates were approximately 130 cm/1,000 yrs when deposition began and have decreased to about 25 cm/1,000 yrs. The decreasing sedimentation rate reflects a diminishing source of fine sediments, which presumably came from the Georges Bank and Nantucket Shoals area. Inventories of excess ²¹⁰ Pb in undisturbed cores average 70 dpm/cm ² (disintegrations per minute per square centimeter), more than two times higher than the flux of ²¹⁰ Pb from the atmosphere and from ²²⁶ Ra decay in the overlying water. This additional influx of ²¹⁰ Pb either must be with new fine-grained sediment material or from solutions that are stripped of their ²¹⁰ Pb by particulates in the bottom nepheloid layer. Stable Pb concentrations in surface sediments are about 28 ppm, as much as two times higher than concentrations at depth. The high accumulation rates, ²¹⁰ Pb inventories, and trace-metal profiles imply that this area is a modern sink for fine-grained sediments and for pollutants associated with particulate matter in the water column. To our knowledge, this is the only site of present-day natural deposition on the Continental Shelf off the eastern United States, exclusive of the Gulf of Maine. Because the net currents on the outer half of this Continental Shelf flow from northeast to southwest, this fine-grained deposit may receive its sediments and possible contaminants from the Nantucket Shoals and Georges Bank regions.