3. SITE 1071
Position: 39°22.9446′N, 72°43.6830′W Start hole: 1300 hr, 23 June 1997 End hole: 0355 hr, 24 June 1997 Time on hole: 14.92 hr Seafloor (drill pipe measurement from rig floor, mbrf): 99.4 Total depth (drill pipe measurement from rig floor, mbrf): 151.3 Distance between rig floor and sea level (m): 11.2 Water depth (drill pipe measurement from sea level, m): 88.2 Penetration (mbsf): 51.9 Coring totals: Type: APC Number: 7 Cored: 36.3 m Recovered: 27.75 m (76.45%)
Occurrence and Formation of Dolomite in Organic-Rich Continental Margin Sediments
Dolomite is presently forming throughout a large part of the oceans in continental margin marine sediments accumulating at rates less than 500 m/m.y. and having organic carbon contents greater than 0.5 wt. %. At higher sedimentation rates, the dolomite content of the sediments is greatly diluted. At lower organic carbon content, the porewater chemistry precludes dolomite formation. The reactants for dolomite formation have the following sources: magnesium supplied from overlying seawater, calcium supplied by the dissolution of calcium carbonate, and carbon supplied from carbonate dissolution and organic carbon oxidation. The rate of dolomite formation appears to be limited by the rate of calcium carbonate dissolution. This rate can be quantitatively calculated from the magnesium diffusional and advective fluxes. Conversely, in ancient sediments the depth and timing of dolomite formation can be calculated from the amount of dolomite and the sedimentation rate. In dolomite-rich sediments these calculations demonstrate that most of the dolomite formed within a few tens of meters of the sea floor within the zone of microbial sulfate reduction. Such dolomites have ne ative values of ^dgr13C. Dolomite in dolomite-poor sediments may form at greater burial depth, below the zone of sulfate reduction, resulting in positive values of ^dgr13C. The distribution coefficient of strontium in dolomite has been determined to have an average value of 0.06. Using this value, predicted strontium contents for submarine dolomites range from 150 ppm in dolomite-rich sections to 1,290 ppm in dolomite-poor sections.
Late Oligocene transgression of middle Atlantic Coastal Plain
The subsurface Piney Point Formation of the coastal plain of Maryland, Delaware, and New Jersey contains planktonic foraminifera of late Oligocene age. The transgressive Piney Point Formation was deposited in inner to middle shelf environments on an eroded Eocene surface. The disconformity that separates the Piney Point from the Eocene formations below resulted from a major lowering of global sea level in early Oligocene time. This eustatic regression correlates with severe climatic changes noted elsewhere in the geologic record of this time.