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.
How to do a p-descent on an elliptic curve
In this paper, we describe an algorithm that reduces the computation of the (full) p-Selmer group of an elliptic curve E over a number field to standard number field computations such as determining the (p-torsion of) the S-class group and a basis of the S-units modulo pth powers for a suitable set S of primes. In particular, we give a result reducing this set S of 'bad primes' to a very small set, which in many cases only contains the primes above p. As of today, this provides a feasible algorithm for performing a full 3-descent on an elliptic curve over Q, but the range of our algorithm will certainly be enlarged by future improvements in computational algebraic number theory. When the Galois module structure of E[p] is favorable, simplifications are possible and p-descents for larger p are accessible even today. To demonstrate how the method works, several worked examples are included.