DISCUSSION OF SAMPLING STRATEGY
Communal and Composite Geochemical Samples
Glass Samples
Fresh glass is important for determining the chemical
composition of magmas because it is unaffected by mineral
accumulation and posteruption alteration. Glass is also usually
chemically homogenous so that chemical analyses made with
microbeam techniques are applicable to the bulk sample. Fresh
glass from flow and pillow margins and from hyaloclastites were
identified under the binocular microscope during the routine
description of the cores. The locations of most of the pieces that
contain glass are given in Table 4. A subset of ~50 glasses was
sampled on board ship for a coordinated effort to obtain a wide
variety of analyses on the same samples (Table 4). Glass chips and
thin sections will be analyzed first by electron microprobe for 10
major elements (Si, Al, Fe, Mg, Ca, Na, K, P, Ti, and Mn). This
will determine how many different compositions are present in the
cores. Based on the major element analyses, selected thin sections
and chips will be distributed among the other investigators who
wish to conduct laser and ion beam microanalyses and water
measurements by Fourier transform infrared spectroscopy. Also,
based on the major elements, samples will be distributed for mass
spectroscopy for heavy isotopes, halogens, Li, and B. Some samples
were distributed on board the ship for magnetic intensity
measurements, and additional samples will be distributed after
thin-section billets are cut from the samples. Thin sections
examined for evidence of microbial activity (Fisk) will also be
measured for the relative chemical and microbial alteration
(Staudigel).
Analysis of Logs
An important aspect of the construction of a reference site
involves integrating the geophysical and chemical logs with the
core information to create a complete crustal section. In the case
of the basement logging at Site 801, of particular interest is
determining the relative proportions of interflow material, thick
flows, and thin sheet flows or pillows. The strategy involves an
integration of the FMS logs, geochemical data, and core lithology
data for the Hole 801C basement. The porosity-sensitive logs
(resistivity, velocity, density, and neutron porosity) will be
studied for Hole 801C to characterize very old oceanic crust
formed at a very fast spreading rate. In addition, a modeling
study of the temperature log in Hole 801C will be undertaken to
further constrain the porosity/permeability of basement.
Given the interest in the magnetic reversal history of Jurassic
ocean crust, the magnetic logs will be used to establish the
magnetic polarity stratigraphy of Hole 801C basement from the log
data and to construct a model of the surface magnetic field using
the various polarity intervals as input.
Paleomagnetic and Paleointensity Analysis
A number of the fresh glass samples from flow and pillow margins
and from hyaloclastites were distributed on board the ship for
magnetic intensity measurements.
Microbiology
The majority of the microbiology data will be generated in
shore-based studies. The major efforts will be to determine
community composition by DNA extraction, in situ hybridization,
characterization of microbes isolated from enrichment cultures,
and culturing of microbes from samples maintained at in situ
pressure. Culturing at high pressure and at 1 atm will be done at
different shore-based laboratories. These studies will be
coordinated with additional study of igneous rocks, veins, and
sediment from which biological samples were collected. Rock
samples will be examined by scanning electron microscope for
microbes and microbial alteration textures. The amount of
microbial vs. chemical alteration will be measured in thin
sections, and the types and compositions of secondary minerals
will be determined by electron microprobe. The lithology of
sediments used for cultures and ATP measurements will be
determined from smear slides.