Neutral lipid concentrations from sediment cores collected during R/V Thomas G. Thompson cruise TT013 in the Equatorial Pacific in 1992 during the U.S. JGOFS Equatorial Pacific (EqPac) project

Website: https://www.bco-dmo.org/dataset/2707
Version: December 18, 1995
Version Date: 1995-12-18

Project
» U.S. JGOFS Equatorial Pacific (EqPac)

Program
» U.S. Joint Global Ocean Flux Study (U.S. JGOFS)
ContributorsAffiliationRole
Wakeham, StuartSkidaway Institute of Oceanography (SkIO)Principal Investigator
Chandler, Cynthia L.Woods Hole Oceanographic Institution (WHOI BCO-DMO)BCO-DMO Data Manager


Dataset Description

Neutral lipid concentrations, Sediment cores


Methods & Sampling

   PI:              Stuart Wakeham
   of:              Skidaway Insitute of Oceanography
   dataset:         Neutral lipid concentrations, Sediment cores
   dates:           October 30, 1992 to December 13, 1992
   location:        N: 9  S: -12  W: -140  E: -140
   project/cruise:  EQPAC/TT013 - Benthic cruise
   ship:            Thomas Thompson
 
   Samples collected with a mulicore device, see event log for precise
   locations of multicore sampling.
 
 

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Data Files

File
lipid_core.csv
(Comma Separated Values (.csv), 2.04 KB)
MD5:8efa2bc1f4655d00b7243f42b3796044
Primary data file for dataset ID 2707

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Parameters

ParameterDescriptionUnits
neutral_lipids

concentration of neutral lipids (see list of lipid names below)

ng/g dry wt.
n9_0_0d5

Nominal latitude (9N) of the core location along 140W, (0-0.5)cm is the interval in the core sampled.

n9_10_12

Nominal latitude (9N) of the core location along 140W, (10_12)cm is the interval in the core sampled.

n5_0_0d5

Nominal latitude (5N) of the core location along 140W, (0-0.5)cm is the interval in the core sampled.

n5_10_12

Nominal latitude (5N) of the core location along 140W, (10_12)cm is the interval in the core sampled.

n2_0_0d5

Nominal latitude (2N) of the core location along 140W, (0-0.5)cm is the interval in the core sampled.

eq_0_0d5

Nominal latitude (0N) of the core location along 140W, (0-0.5)cm is the interval in the core sampled.

eq_10_12

Nominal latitude (0N) of the core location along 140W, (10_12)cm is the interval in the core sampled.

s2_0_0d5

Nominal latitude (2S) of the core location along 140W, (0-0.5)cm is the interval in the core sampled.

s5_0_0d5

Nominal latitude (5S) of the core location along 140W, (0-0.5)cm is the interval in the core sampled.

s12_0_0d5

Nominal latitude (12S) of the core location along 140W, (0-0.5)cm is the interval in the core sampled.

Neutral Lipid names have been prefixed with nl_, which must be

ignored when deciphering the lipid name.

14ROH

C14-alcohol

2,6,10-TMP-one

2,6,10-trimethylpentadecanone

15ROH

C15-alcohol

16ROH

C16-alcohol

17ROH

C17-alcohol

18ROH

C18-alcohol

phytol

phytol

19ROH

C19-alcohol

20ROH

C20-alcohol

21ROH

C21-alcohol

22ROH

C22-alcohol

23ROH

C23-alcohol

27HC

C27-alkane

24ROH

C24-alcohol

28HC

C28-alkane

squalene

squalene

25ROH

C25-alcohol

29HC

C29-alkane

26ROH

C26-alcohol

30HC

C30-alkane

27ROH

C27-alcohol

31HC

C31-alkane

27(5,22)

cholesta-5,22-dien-3B-ol

27(22)

cholest-22-en-3B-ol

28ROH

C28-alcohol

27(5)

choles-5-en-3B-ol

27(0)

cholestan-3B-ol

bisnorhopane

bisnorhopane

28(5,22)

24-methylcholesta-5,22-dien-3B-ol

28(22)

24-methylcholest-22-en-3B-ol

27(4-en-3-one)

cholest-4-en-3-one

28(5,24(28))

24-methylcholesta-5,24(28)-dien-3B

28(5)

24-methylcholest-5-en-3B-ol

28-diol

C28-alkane-diol

29(5,22)

24-ethylcholesta-5,22-dien-3B-ol

DM-29(5,22)

23,24-dimethylcholesta-5,22-dien-3

29(5)

24-ethylcholest-5-en-3B-ol

29(0)

24-etylcholestan-3B-ol

29(5,24(28))

24-ethylcholesta-5,24(28)E-dien-3B

30(22)

4,23,24-trimentylcholest-22-en-3B-

30(0)

4,23,24-trimethylcholestan-3B-ol

30-diol

C30-alkane-diol

30-keto-ol

C30-alkane keto-ol

homohopane

homohopane

37:2 alkenone

C37:2 alkenone

38:2 alkenone

C38:2 ethyl-alkenone



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Instruments

Dataset-specific Instrument Name
Multi Corer
Generic Instrument Name
Multi Corer
Generic Instrument Description
The Multi Corer is a benthic coring device used to collect multiple, simultaneous, undisturbed sediment/water samples from the seafloor. Multiple coring tubes with varying sampling capacity depending on tube dimensions are mounted in a frame designed to sample the deep ocean seafloor. For more information, see Barnett et al. (1984) in Oceanologica Acta, 7, pp. 399-408.


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Deployments

TT013

Website
Platform
R/V Thomas G. Thompson
Start Date
1992-10-30
End Date
1992-12-13
Description
Purpose: Benthic Survey, 12°N-12°S at 140°W TT013 was one of five cruises conducted in 1992 in support of the U.S. Equatorial Pacific (EqPac) Process Study. The five EqPac cruises aboard R/V Thomas G. Thompson included two repeat meridional sections (12°N - 12°S), 2 equatorial surveys, and a benthic survey (all at 140° W). The scientific objectives of this study were to observe the processes in the Equatorial Pacific controlling the fluxes of carbon and related elements between the atmosphere, euphotic zone, and deep ocean. As luck would have it, the survey window coincided with an El Nino event. A bonus for the research team.


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Project Information

U.S. JGOFS Equatorial Pacific (EqPac)


Coverage: Equatorial Pacific


The U.S. EqPac process study consisted of repeat meridional sections (12°N -12°S) across the equator in the central and eastern equatorial Pacific from 95°W to 170°W during 1992. The major scientific program was focused at 140° W consisting of two meridional surveys, two equatorial surveys, and a benthic survey aboard the R/V Thomas Thompson. Long-term deployments of current meter and sediment trap arrays augmented the survey cruises. NOAA conducted boreal spring and fall sections east and west of 140°W from the R/V Baldridge and R/V Discoverer. Meteorological and sea surface observations were obtained from NOAA's in place TOGA-TAO buoy network.

The scientific objectives of this study were to determine the fluxes of carbon and related elements, and the processes controlling these fluxes between the Equatorial Pacific euphotic zone and the atmosphere and deep ocean. A broad overview of the program at the 140°W site is given by Murray et al. (Oceanography, 5: 134-142, 1992). A full description of the Equatorial Pacific Process Study, including the international context and the scientific results, appears in a series of Deep-Sea Research Part II special volumes:

Topical Studies in Oceanography, A U.S. JGOFS Process Study in the Equatorial Pacific (1995), Deep-Sea Research Part II, Volume 42, No. 2/3.

Topical Studies in Oceanography, A U.S. JGOFS Process Study in the Equatorial Pacific. Part 2 (1996), Deep-Sea Research Part II, Volume 43, No. 4/6.

Topical Studies in Oceanography, A U.S. JGOFS Process Study in the Equatorial Pacific (1997), Deep-Sea Research Part II, Volume 44, No. 9/10.

Topical Studies in Oceanography, The Equatorial Pacific JGOFS Synthesis (2002), Deep-Sea Research Part II, Volume 49, Nos. 13/14.



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Program Information

U.S. Joint Global Ocean Flux Study (U.S. JGOFS)


Coverage: Global


The United States Joint Global Ocean Flux Study was a national component of international JGOFS and an integral part of global climate change research.

The U.S. launched the Joint Global Ocean Flux Study (JGOFS) in the late 1980s to study the ocean carbon cycle. An ambitious goal was set to understand the controls on the concentrations and fluxes of carbon and associated nutrients in the ocean. A new field of ocean biogeochemistry emerged with an emphasis on quality measurements of carbon system parameters and interdisciplinary field studies of the biological, chemical and physical process which control the ocean carbon cycle. As we studied ocean biogeochemistry, we learned that our simple views of carbon uptake and transport were severely limited, and a new "wave" of ocean science was born. U.S. JGOFS has been supported primarily by the U.S. National Science Foundation in collaboration with the National Oceanic and Atmospheric Administration, the National Aeronautics and Space Administration, the Department of Energy and the Office of Naval Research. U.S. JGOFS, ended in 2005 with the conclusion of the Synthesis and Modeling Project (SMP).



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