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    (Table 1) Sample descriptions and geochemistry for core material at DSDP Holes 64-479 and 64-480

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    Laminated and nonlaminated sediments from Holes 480 and 479 have been analyzed for potential differences in the composition of organic matter. Their lipid composition is very similar and indicates a primary autochthonous microbial origin and some influx of allochthonous higher-plant detritus. The nonlaminated sections contain relatively more terrigenous plant wax detritus versus autochthonous residues and a much greater amount of perylene than the laminated sections

    (Table 2) Carbon isotope composition of CH4 and CO2 at DSDP Leg 64 Holes

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    Empty cells and samples 64-474A-40-3, 64-477-7-1, 64-478-33-3, 64-480-21-2, 64-481A-9-5 and 64-481A-22-6 were insufficient for determination
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