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                <gco:CharacterString>&amp;lt;p&amp;gt;See Platform deployments for cruise specific documentation&amp;lt;/p&amp;gt;

from Cruise: TT041 &lt;pre&gt;  &lt;b&gt;PI:&lt;/b&gt;              Warren Prell
  &lt;b&gt;of:&lt;/b&gt;              Brown University
  &lt;b&gt;dataset:&lt;/b&gt;         Sediment Composition
  &lt;b&gt;dates:&lt;/b&gt;           November 1994 and May 1995
  &lt;b&gt;location:&lt;/b&gt;        N: 17.812  S: 10.0345  W: 57.5058  E: 65.0852
  &lt;b&gt;project/cruise:&lt;/b&gt;  Arabian Sea
  &lt;b&gt;ship:&lt;/b&gt;            R/V Thomas Thompson

  &lt;a href=&quot;http://usjgofs.whoi.edu/PI-NOTES/arabian/Prell_sed_comp.html&quot;&gt;&lt;b&gt;PI Notes and Methodology&lt;/b&gt;&lt;/a&gt;

  
  Some additional undocumented information was submitted 
  with this data and is available for download as Excel files:
  -- &lt;a href=&quot;http://usjgofs.whoi.edu/PI-NOTES/arabian/Prell/TN041_047_cores.xls&quot;&gt;core meta data&lt;/a&gt;
  -- &lt;a href=&quot;http://usjgofs.whoi.edu/PI-NOTES/arabian/Prell/8.5_DAY_FAUNA_FLUXES.xls&quot;&gt;fauna flux data&lt;/a&gt;
  -- &lt;a href=&quot;http://usjgofs.whoi.edu/PI-NOTES/arabian/Prell/JGOFS_c14data.xls&quot;&gt;C14 data for G.menardii and G.sacculifer&lt;/a&gt;

&lt;/pre&gt;

from Cruise: TT047 &lt;pre&gt;  &lt;b&gt;PI:&lt;/b&gt;              Warren Prell
  &lt;b&gt;of:&lt;/b&gt;              Brown University
  &lt;b&gt;dataset:&lt;/b&gt;         Sediment Composition
  &lt;b&gt;dates:&lt;/b&gt;           November 1994 and May 1995
  &lt;b&gt;location:&lt;/b&gt;        N: 17.812  S: 10.0345  W: 57.5058  E: 65.0852
  &lt;b&gt;project/cruise:&lt;/b&gt;  Arabian Sea
  &lt;b&gt;ship:&lt;/b&gt;            R/V Thomas Thompson

  &lt;a href=&quot;http://usjgofs.whoi.edu/PI-NOTES/arabian/Prell_sed_comp.html&quot;&gt;&lt;b&gt;PI Notes and Methodology&lt;/b&gt;&lt;/a&gt;

  
  Some additional undocumented information was submitted 
  with this data and is available for download as Excel files:
  -- &lt;a href=&quot;http://usjgofs.whoi.edu/PI-NOTES/arabian/Prell/TN041_047_cores.xls&quot;&gt;core meta data&lt;/a&gt;
  -- &lt;a href=&quot;http://usjgofs.whoi.edu/PI-NOTES/arabian/Prell/8.5_DAY_FAUNA_FLUXES.xls&quot;&gt;fauna flux data&lt;/a&gt;
  -- &lt;a href=&quot;http://usjgofs.whoi.edu/PI-NOTES/arabian/Prell/JGOFS_c14data.xls&quot;&gt;C14 data for G.menardii and G.sacculifer&lt;/a&gt;

&lt;/pre&gt;</gco:CharacterString>
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                <gco:CharacterString>&amp;lt;font face=Times New Roman, Times, serif&amp;gt;
&amp;lt;h2&amp;gt;U.S. JGOFS Arabian Sea Process Study&amp;lt;br&amp;gt;
Sediment Composition&amp;lt;/h2&amp;gt;
&amp;lt;/font&amp;gt;
&amp;lt;font face=Times New Roman, Times, serif size=3&amp;gt;


&amp;lt;img height=1 width=&amp;quot;100%&amp;quot; http://us

jgofs.whoi.edu/images/greendot.gif&amp;quot; alt=&amp;quot;-- line--&amp;quot;&amp;gt;
&amp;lt;p&amp;gt;

&amp;lt;b&amp;gt; Processing notes:&amp;lt;/b&amp;gt; &amp;lt;br&amp;gt;
&amp;lt;i&amp;gt; December 2002, Warren Prell &amp;lt;/i&amp;gt;
&amp;lt;p&amp;gt;
1. Data for -1 to O interval are measure on unconsolidated phytodetritus layer&amp;lt;br&amp;gt;
    sitting on top of sediment water interface&amp;lt;br&amp;gt;
2. Letter for each core refers to a multicore section&amp;lt;br&amp;gt;
3. Opal determined using Mortlock and Froelich (1989, DSR, vol 36, 1415-1426)&amp;lt;br&amp;gt;

4. CaCO3 detemined on automated Carbonate rig similar to Ostermann et al. (1990)&amp;lt;br&amp;gt;
5. CaCO3-ICP = 2.5* Ca determined from ICP.&amp;lt;br&amp;gt;
6. Corg and N% determined using technique of Verardo et al. (1990, DSR, 37, 157-165)&amp;lt;br&amp;gt;
7. Ca, Mn, Fe, Al, Ti, and P determined on ICP-AES using technique of&amp;lt;br&amp;gt;
    Murray and Leinen (1996, GCA, 3869-3878)&amp;lt;br&amp;gt;
8. Density calculated from dried weight of known volume of sample extruded from subcore&amp;lt;br&amp;gt;
9. Sedimentation rates estimated from C-14 dating of monospecific foraminifer shells&amp;lt;br&amp;gt;
    from sampled depths.  For all but JGOFS-1, both menardii and sacculifer (when available)&amp;lt;br&amp;gt;

    ages were used to calculate sedimentation rate. In practice JGOFS-5 had one sacculifer&amp;lt;br&amp;gt;
    and 5 menardii and Owen Ridge 2 had 8 menardii and 6 sacculifer, the rest have only&amp;lt;br&amp;gt;
    menardii. For JGOFS-1, the data on the 2 species measured were significantly different&amp;lt;br&amp;gt;
    so two separate rates were calculated- one for each species (C14_sed_rate calculated &amp;lt;br&amp;gt;
    from G. menardii, and C14_sed_rate_2 from G. sacculifer). &amp;lt;br&amp;gt;

&amp;lt;br&amp;gt;

&amp;lt;/font&amp;gt;
&amp;lt;p&amp;gt;
&amp;lt;img height=1 width=&amp;quot;100%&amp;quot; http://us

jgofs.whoi.edu/images/greendot.gif&amp;quot; alt=&amp;quot;-- line--&amp;quot;&amp;gt;
&amp;lt;pre&amp;gt;
&amp;lt;b&amp;gt;References:&amp;lt;/b&amp;gt;
Mortlock, R.A., and Froelich, P.N., 1989.  A simple method for the rapid
determination of biogenic opal in pelagic marine sediments.  Deep-Sea Res.,
36:1415-1426.

Ostermann, D.R., Karbott, D., and Curry, W.B., 1990. Automated system to
measure carbonate concentration of sediments. Woods Hole Oceanog. Inst.
Tech. Rept., WHOI-90-03.

Verardo, D., Froelich, P.N., and McIntyre, A., 1990. Determination of
organic carbon and nitrogen in marine sediments using the Carlo Erba NA-1500
analyzer. Deep-Sea Research, 37: 157-165.

Murray, R. W. and Leinen, M. 1996.  Scavenged excess aluminum and its
relationship to bulk titanium in biogenic sediment from the central
equatorial Pacific Ocean.  Geochimica et Cosmochimica Acta, 60 (20):
3869-3878.

&amp;lt;/pre&amp;gt;

from Cruise: TT041 &lt;font face=Times New Roman, Times, serif&gt;
&lt;h2&gt;U.S. JGOFS Arabian Sea Process Study&lt;br&gt;
Sediment Composition&lt;/h2&gt;
&lt;/font&gt;
&lt;font face=Times New Roman, Times, serif size=3&gt;


&lt;img height=1 width=&quot;100%&quot; http://us

jgofs.whoi.edu/images/greendot.gif&quot; alt=&quot;-- line--&quot;&gt;
&lt;p&gt;

&lt;b&gt; Processing notes:&lt;/b&gt; &lt;br&gt;
&lt;i&gt; December 2002, Warren Prell &lt;/i&gt;
&lt;p&gt;
1. Data for -1 to O interval are measure on unconsolidated phytodetritus layer&lt;br&gt;
    sitting on top of sediment water interface&lt;br&gt;
2. Letter for each core refers to a multicore section&lt;br&gt;
3. Opal determined using Mortlock and Froelich (1989, DSR, vol 36, 1415-1426)&lt;br&gt;

4. CaCO3 detemined on automated Carbonate rig similar to Ostermann et al. (1990)&lt;br&gt;
5. CaCO3-ICP = 2.5* Ca determined from ICP.&lt;br&gt;
6. Corg and N% determined using technique of Verardo et al. (1990, DSR, 37, 157-165)&lt;br&gt;
7. Ca, Mn, Fe, Al, Ti, and P determined on ICP-AES using technique of&lt;br&gt;
    Murray and Leinen (1996, GCA, 3869-3878)&lt;br&gt;
8. Density calculated from dried weight of known volume of sample extruded from subcore&lt;br&gt;
9. Sedimentation rates estimated from C-14 dating of monospecific foraminifer shells&lt;br&gt;
    from sampled depths.  For all but JGOFS-1, both menardii and sacculifer (when available)&lt;br&gt;

    ages were used to calculate sedimentation rate. In practice JGOFS-5 had one sacculifer&lt;br&gt;
    and 5 menardii and Owen Ridge 2 had 8 menardii and 6 sacculifer, the rest have only&lt;br&gt;
    menardii. For JGOFS-1, the data on the 2 species measured were significantly different&lt;br&gt;
    so two separate rates were calculated- one for each species (C14_sed_rate calculated &lt;br&gt;
    from G. menardii, and C14_sed_rate_2 from G. sacculifer). &lt;br&gt;

&lt;br&gt;

&lt;/font&gt;
&lt;p&gt;
&lt;img height=1 width=&quot;100%&quot; http://us

jgofs.whoi.edu/images/greendot.gif&quot; alt=&quot;-- line--&quot;&gt;
&lt;pre&gt;
&lt;b&gt;References:&lt;/b&gt;
Mortlock, R.A., and Froelich, P.N., 1989.  A simple method for the rapid
determination of biogenic opal in pelagic marine sediments.  Deep-Sea Res.,
36:1415-1426.

Ostermann, D.R., Karbott, D., and Curry, W.B., 1990. Automated system to
measure carbonate concentration of sediments. Woods Hole Oceanog. Inst.
Tech. Rept., WHOI-90-03.

Verardo, D., Froelich, P.N., and McIntyre, A., 1990. Determination of
organic carbon and nitrogen in marine sediments using the Carlo Erba NA-1500
analyzer. Deep-Sea Research, 37: 157-165.

Murray, R. W. and Leinen, M. 1996.  Scavenged excess aluminum and its
relationship to bulk titanium in biogenic sediment from the central
equatorial Pacific Ocean.  Geochimica et Cosmochimica Acta, 60 (20):
3869-3878.

&lt;/pre&gt;

from Cruise: TT047 &lt;font face=Times New Roman, Times, serif&gt;
&lt;h2&gt;U.S. JGOFS Arabian Sea Process Study&lt;br&gt;
Sediment Composition&lt;/h2&gt;
&lt;/font&gt;
&lt;font face=Times New Roman, Times, serif size=3&gt;


&lt;img height=1 width=&quot;100%&quot; http://us

jgofs.whoi.edu/images/greendot.gif&quot; alt=&quot;-- line--&quot;&gt;
&lt;p&gt;

&lt;b&gt; Processing notes:&lt;/b&gt; &lt;br&gt;
&lt;i&gt; December 2002, Warren Prell &lt;/i&gt;
&lt;p&gt;
1. Data for -1 to O interval are measure on unconsolidated phytodetritus layer&lt;br&gt;
    sitting on top of sediment water interface&lt;br&gt;
2. Letter for each core refers to a multicore section&lt;br&gt;
3. Opal determined using Mortlock and Froelich (1989, DSR, vol 36, 1415-1426)&lt;br&gt;

4. CaCO3 detemined on automated Carbonate rig similar to Ostermann et al. (1990)&lt;br&gt;
5. CaCO3-ICP = 2.5* Ca determined from ICP.&lt;br&gt;
6. Corg and N% determined using technique of Verardo et al. (1990, DSR, 37, 157-165)&lt;br&gt;
7. Ca, Mn, Fe, Al, Ti, and P determined on ICP-AES using technique of&lt;br&gt;
    Murray and Leinen (1996, GCA, 3869-3878)&lt;br&gt;
8. Density calculated from dried weight of known volume of sample extruded from subcore&lt;br&gt;
9. Sedimentation rates estimated from C-14 dating of monospecific foraminifer shells&lt;br&gt;
    from sampled depths.  For all but JGOFS-1, both menardii and sacculifer (when available)&lt;br&gt;

    ages were used to calculate sedimentation rate. In practice JGOFS-5 had one sacculifer&lt;br&gt;
    and 5 menardii and Owen Ridge 2 had 8 menardii and 6 sacculifer, the rest have only&lt;br&gt;
    menardii. For JGOFS-1, the data on the 2 species measured were significantly different&lt;br&gt;
    so two separate rates were calculated- one for each species (C14_sed_rate calculated &lt;br&gt;
    from G. menardii, and C14_sed_rate_2 from G. sacculifer). &lt;br&gt;

&lt;br&gt;

&lt;/font&gt;
&lt;p&gt;
&lt;img height=1 width=&quot;100%&quot; http://us

jgofs.whoi.edu/images/greendot.gif&quot; alt=&quot;-- line--&quot;&gt;
&lt;pre&gt;
&lt;b&gt;References:&lt;/b&gt;
Mortlock, R.A., and Froelich, P.N., 1989.  A simple method for the rapid
determination of biogenic opal in pelagic marine sediments.  Deep-Sea Res.,
36:1415-1426.

Ostermann, D.R., Karbott, D., and Curry, W.B., 1990. Automated system to
measure carbonate concentration of sediments. Woods Hole Oceanog. Inst.
Tech. Rept., WHOI-90-03.

Verardo, D., Froelich, P.N., and McIntyre, A., 1990. Determination of
organic carbon and nitrogen in marine sediments using the Carlo Erba NA-1500
analyzer. Deep-Sea Research, 37: 157-165.

Murray, R. W. and Leinen, M. 1996.  Scavenged excess aluminum and its
relationship to bulk titanium in biogenic sediment from the central
equatorial Pacific Ocean.  Geochimica et Cosmochimica Acta, 60 (20):
3869-3878.

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