CRUISE PLAN FOR CGCS SIR WILFRID LAURIER CRUISE, JULY 2003
(Dutch Harbor to Barrow, AK)
Jackie M. Grebmeier and Lee W. Cooper
(Co-PIs), NSF-funded “An Arctic Environmental
Observatory in Bering Strait, The
University of Tennessee, Department of Ecology and Evolutionary Biology, Marine
Biogeochemistry and Ecology Group, 10515 Research Dr., Bldg. A, Suite 100, The
University of Tennessee, Knoxville, TN 37932; ph. (865) 974-2592; fax (865)
974-7896; email:jgrebmei@utk.edu; grant NSF-OPP 9910319
I. PURPOSE
Annual hydrographic and benthic sampling
at select sites north and south of Bering Strait are part of our NSF-funded
Bering Strait Long-Term Observatory project. These studies extend our existing 19-year time-series of
sediment flux measurements of dissolved oxygen, benthic biomass, and other
chemical and biological parameters at productive benthic stations, both north
and south of Bering Strait (Fig. 1) using the CGCS Sir Wilfred Laurier transiting through Bering Strait. A major premise for our sediment-based
work in the Bering and Chukchi seas is that appropriate chemical and isotopic
indicators in the benthos and bottom waters in this shallow, productive
continental shelf ecosystem can provide accurate indications of the locations
of particulate deposition and overlying water column processes. We have taken
advantage in our past work of the longer-term integration of oceanographic
change that is reflected in many benthic indices, which might vary as a result
of changes in particle sedimentation, the strength of pelagic-benthic coupling,
changes in apex predator populations, or other physical and biological
events. The tools we have been
using to evaluate possible changes in the Bering and Chukchi benthic ecosystem
have included sediment oxygen demand, deposition patterns of the
particle-reactive natural radionuclide 7Be, the stable carbon
isotope composition of sediment organic matter, elemental carbon/nitrogen
ratios, sediment grain size, as well as more direct benthic metrics such as
macrofaunal biomass and community ecological structure. Annual July sampling
since 1998 has been supported in collaboration with Dr. Eddy Carmack (IOS) and
the Canadian Coast Guard ship Sir Wilfrid Laurier enroute to resupply communities in the
Canadian Arctic.
In addition to the core LTO sampling, Dr.
Jack DiTullio (University of Charleston) has been collaborating on the project
since 2001 to investigate DMSP and sulfur cycling in the Bering and Chukchi
seas. Several trace
biogenic gases have been implicated in significantly affecting global climate
change processes. Water collections during the cruise allow measurement of the
production of dimethylsulfide (DMS), dimethylsulfoxide (DMSO) and their
precursor dimethyl-sulfoniopropionate (DMSP by bloom-forming algal species during
bloom periods during the cruise.
In 2003 we will place a mooring in the
SLIP region southwest of St. Lawrence Island as part of a NOAA collaborative
project with Drs. Jim Overland (Pacific Marine Environmental Laboratory, PMEL)
and Terry Whitledge (University of Alaska Fairbanks, UAF).
II.
CRUISE PLAN
Sampling is planned at 27 stations in the
Bering and Chukchi seas, including 6 water column stations in transit from
Dutch Harbor to the A-SLIP region (Figure 1) as part of the annual IOS sampling
plan. The core LTO sites include 16 water column and benthic stations in areas
A, B,
and D and 5 hydrographic stations in the US-portion of Bering Strait (Area C). In 2002 a mooring will be emplaced in the A-SLIP region near stations SLIP-1 and SLIP-2. The following information lists the planned participants and site of embarkation and disembarkation for the science party.
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Figure 1. Station cruise track for
July 2003 cruise on the CCGS Sir Wilfrid Laurier |
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4. Arianne Balsom (F)-U Tennessee
5.
Rebecca Pirtle-Levy
(F)-U Tennessee
6. Betty Carvellas (F)-TEA teacher, Essex
High School, Vermont
7. David Brown (M)-TEA teacher, St. Peter
School, Quincy, IL
9. Nathan Garcia (M)- U of Charleston, SC
10. Sarah Thornton (F)-U Alaska Fairbanks
11.
Sigrid Salo
(F)-PMEL (Dr. Jim Overland, PI)
B.
Science Station Planning
The following plan includes station locations for planned sampling (see Fig. 1):
1. five long-term sites south of St. Lawrence in a “hot spot” region (A) where we have been observing bivalve and upper trophic level declines over the past decade [1 day sampling];
2. deployment of NBS mooring near stations SLIP1 and SLIP 2 [<1 day, likely part of #1]
3. four stations in the NE Bering Sea (B); [1 day sampling]
4.
five
station CTD transect across Bering Strait (C) (U.S. waters only), with a 12 hr
stop at Little Diomede Island in Bering Strait for site survey [1 day total time]; and
5. seven stations in the SE Chukchi Sea (D)
as completed previously during 1998, 1999, 2000 and 2001 [2 days on-site
sampling time total];
C. Standard Station Sampling Within
The SLIPP01 Station Grid
1. Water
column CTD with rosette deployment
for S/T/D and water column collections at 5 m depth intervals to bottom of
deployment (one deployment). Note that the CTD should be collected continuously
for physical oceanographic collections during the descent, then stopped at
designated intervals on the ascent for water collections. Two bottom-water
bottles will be collected for experimental purposes. Once returned to the deck,
seawater will be collected from each rosette bottle on the CTD for the
following measurements:
a. nutrients-subsamples collected in acid-washed plastic vials
and frozen shipboard
b. chlorophyll-subsamples collected
and processed shipboard on a Turner fluorometer
c. oxygen-18-subsample collected in
glass vials and sealed for land-based analyses
d. DMS-seawater subsamples filtered
to measure DMS back on land using cryogenic purge and trap gas chromatography
later in the land-based laboratory (DiTullio)
e. algal species-subsamples collected
for HPLC pigment analyses.
Table 1. LTO station locations to be occupied
in 2003 (note BS stations are part of
IOS hydrographic sampling where DMSP samples are also collected.
|
Station (2003) |
Historical Station |
Latitude (°N) |
Longitude (°W) |
Depth (m) |
Sampling |
|
BS-1 |
same |
56.312 |
-172.824 |
|
water |
|
BS-2 |
same |
56.418 |
-172.793 |
|
water |
|
BS-3 |
same |
56.476 |
-172.779 |
|
water |
|
BS-4 |
same |
56.546 |
-172.756 |
|
water |
|
BS-5 |
same |
56.645 |
-172.732 |
water |
|
|
BS-6 |
same |
59.320 |
-173.500 |
|
water |
|
SLIP1 |
VNG1 |
62.013 |
-175.056 |
80 |
water,
sediment |
|
SLIP2 |
NWC5 |
62.051 |
-175.207 |
82 |
water,
sediment |
|
NBS |
no |
-175.400 |
78 |
Draft mooring
site |
|
|
SLIP3 |
NWC4 |
62.394 |
-174.570 |
73 |
water,
sediment |
|
SLIP5 |
VNG3.5 |
62.563 |
-173.556 |
65 |
water,
sediment |
|
SLIP4 |
NWC2.5 |
63.029 |
-173.457 |
72 |
water,
sediment |
|
UT-BS5 |
OK93-038 |
64.683 |
-169.099 |
47 |
water,
sediment |
|
UT-BS2 |
HX73-075 |
64.667 |
-169.922 |
45 |
water,
sediment |
|
Laurier1999 |
64.959 |
-169.883 |
50 |
water,
sediment |
|
|
UT-BS1 |
HX59-120 |
64.992 |
-169.135 |
50 |
water,
sediment |
|
BRS5 |
HX171-69 |
65.652 |
-168.217 |
40 |
water |
|
BRS4 |
HX171-70 |
65.668 |
-168.400 |
46 |
water |
|
BRS3 |
HX171-71 |
65.682 |
-168.567 |
51 |
water |
|
BRS2 |
HX171-72 |
65.700 |
-168.717 |
50 |
water |
|
BRS1 |
HX171-73 |
65.717 |
-168.900 |
50 |
water |
|
10 hr stop |
Little Diomede
Is. |
|
|
|
site survey,
offload |
|
UTN-1 |
Stoker-172 |
66.709 |
-168.400 |
36 |
water,
sediment |
|
UTN-2 |
Laurier1998 |
67.051 |
-168.733 |
47 |
water,
sediment |
|
UTN-3 |
HX189-076 |
67.333 |
-168.998 |
52 |
water,
sediment |
|
UTN-4 |
HX74-010 |
67.501 |
-168.913 |
51 |
water,
sediment |
|
UTN-5 |
HX171-076 |
67.671 |
-168.958 |
54 |
water,
sediment |
|
UTN-6 |
AK47-055 |
67.736 |
-168.439 |
50 |
water,
sediment |
|
UTN-7 |
HX85-090 |
67.999 |
-168.933 |
60 |
water,
sediment |
2. Quantitative benthic samples will be
undertaken using the following equipment and sampling protocol:
a. Five 0.1 m2 van Veen grabs at each station, with:
i. The
first grab will be used for surface sediment subsampling for:
· chlorophyll-two surface sediment
sample collected by syringe, and processed for fluorometric analyses shipboard
· TOC/TON, C-13, grain size-subsamples
collected, bagged, and frozen
· HPLC pigment analyses-subsample
collected, placed in vials, and frozen (DiTullio)
· 7-Beryllium-subsample collected
and frozen for land-based analyses on gamma counter
ii. The
remaining 4 van Veen sediment collections will be sieved for faunal collections.
Each van Veen sediment sample is placed in a 1 mm stainless steel screen box
and sieved using regular seawater, the remaining animals subsequently preserved
in 10% sea water formalin, buffered with hexamethylenetetramine, stored in
plastic Whirl-pak bags, and saved for laboratory analyses back at the
University of Tennessee.
b. Three deployments of a single hole HAPS sediment corer (number of deployments depends on
sediment conditions). The following methods are used for analyses:
i. Two
cores are used for sediment respiration experiments The two cores collected
for shipboard incubation will be maintained in the dark at in situ bottom
temperatures in the low temperature stand-up incubators for 10-12 hours. Subsamples from the overlying water in
these cores will be analyzed in the shipboard chambers for dissolved oxygen, ,
nutrients, denitrification, alkalinity, pH and total CO2. Subsequent to the end of the experiment, cores are sieved and
fauna packaged and preserved with formalin for land-based identification.
ii. One
core for subsampling for vertical sediment parameters at the following
intervals:
·
remaining
sediments placed in 90 cc aluminum cans and frozen. Subsequent land-based
analyses include TOC/TON, C-13, and grain size determinations.
NOTE: Both the van Veen grab and single Haps
corer weigh about 150 lbs each and are easily deployed on a side-winch cable
with a 50-60 m/min descent/assent rate.
D. Mooring Deployment Near Slip 1 And Slip2
In
summer 2003, we will deploy a subsurface mooring in 75-78 m of water near
SLIP-1 and SLIP-2 in the northern Bering biological hot spot (Region A). This mooring will consist of two
seacats and ten microcats to measure profiles of temperature and salinity, two
fluorometers to assess chlorophyll (phytoplankton biomass), two current meters
and a nutrient meter (Table ). In the second year, we will recover the first-year
mooring and procure and deploy a second system to provide a multi-year
continuous capability. Table 1
provides the mooring deployment array.
E. Site Survey At Little Diomede Island
(10 Hrs)
During a 10 hr stop at Little Diomede Island,
we will need assistance and use of a small boat from the Sir Wilfrid Laurier to
transport equipment and personnel to the island and to undertake a site survey
around the proposed outlet of the submerged seawater pipeline for the
observatory. We have "key" measurements to make as part of our Bering
Strait Observatory study that need to be measured at approximately 0800, 12
noon, and 1600 at Diomede Island for the pipeline site.
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