Organic Geochemical Flux Studies in the Equatorial Pacific Using
Swimmer-Excluding Rotator Traps
Stuart G. Wakeham, Cindy Lee and John I. Hedges
Goal: To quantitatively evaluate the dynamics of particles
through the water column and into surface sediments in the equatorial North
Pacific as reflected by their organic composition, and to determine
relative reactivities for different molecular organic substances. The
approach includes measurements of lipids, amino acids, and carbohydrates
obtained in floating and moored sediment traps and in surface sediments
obtained along the latitudinal transect across the equator.
Measurements, Protocols etc:
- Sample Types:
A variety of particle samples will be collected in the water column,
including: 1) large volume in-situ filtration samples in surface
waters near the chlorophyll maximum at each survey station (coordinated
with J. K. B. Bishop), 2) particulate matter sinking out of the euphotic zone
(100 m depth) collected by floating sediment traps (coordinated with
J. W. Murray and J. Newton), and 3) particles collected in moored sediment
traps at about 1,000 m below the sea surface and 1,000 m off the bottom
(coordinated with S. Honjo and J. Dymond). The large-volume filtration
samples and floating sediment trap samples will be collected on both
survey cruises, while the moored trap samples will be collected at
stations located at 9° and 5°N and at the equator
(coordinated with M. Leinen). Bottom sediments will be collected
from box cores at all sites of the benthic cruise. Depending on time
available, we also hope to obtain vertical profiles of size-fractionated
large-volume filtration samples at the three moored-trap sites (with
J. K. B. Bishop).
- Cruise Personnel:
Moored trap deployment and recovery - Peter Hernes (UW)
Survey No. 1 John Hedges (U.W.) and Michael Peterson (UW)
Survey No. 2 Stuart Wakeham (Skidaway) and Michael Peterson (UW)
Benthic Cruise - Brian Bergamaschi (UW)
- Analyses:
Particle and sediment samples will be analyzed for a wide range of
major biochemical properties: 1) lipids by extraction, fractionation, and gas
chromatography and gas chromatography/mass spectrometry (Wakeham); 2) amino
acids by hydrolysis and HPLC analysis of OPA fluorescent derivatives
(Lee); 3) aldoses and cyclitols by acid hydrolysis and GC and GC/MS
analysis of peracetate or TMS derivatives (Hedges); 4) elemental
composition by CHN analysis (Hedges). We plan to provide aliquots of
particle and trap samples to J. K. B. Bishop (elemental composition),
J. R. Murray/J. Newton (pigments, elemental composition, radionuclides),
and R. Bidigare (isotopic composition of pigments) if sample sizes are
adequate.
- QA/QC:
An intercomparison of elemental compositions of samples will be made with
other EqPac investigators. We also intend to archive large amounts of
sediment for eventual use as organic geochemical ``reference materials.''
However, because the molecular organic measurements to be carried out by
our groups are practiced in a limited number of laboratories worldwide and
because standard reference materials are not available, the corresponding
QC strategies must be individualistic at this point pending the
development of protocols and reference materials as suggested by the
recent FRECLES Workshop.