http://lod.bco-dmo.org/id/dataset/686982
eng; USA
utf8
dataset
Highest level of data collection, from a common set of sensors or instrumentation, usually within the same research project
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
2017-04-06
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Core-top (0-1cm) sediment data collected by monocore from R/V Thomas G. Thompson TN303 (GP16; EPZT) GEOTRACES cruise from November to December 2013 (GEOTRACES EPZT project)
2017-04-06
publication
2017-04-06
revision
BCO-DMO Linked Data URI
2017-04-06
creation
http://lod.bco-dmo.org/id/dataset/686982
Christopher R. German
Woods Hole Oceanographic Institution
principalInvestigator
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
publisher
Cite this dataset as: German, C. R. (2017) Core-top (0-1cm) sediment data collected by monocore from R/V Thomas G. Thompson TN303 (GP16; EPZT) GEOTRACES cruise from November to December 2013 (GEOTRACES EPZT project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 06 April 2017) Version Date 2017-04-06 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/686982 [access date]
Core-top (0-1cm) sediment data from GEOTRACES EPZT (GP16) cruise Dataset Description: <p>Core-top (0-1cm) sediment data from monocores collected on the GEOTRACES EPZT (GP16; TN303) cruise.</p> Methods and Sampling: <p>On the TN303 cruise, attempts to collect mono-cores were made during the final deep cast of the ODF CTD rosette at each station except Station 18 at the EPR ridge-axis.&nbsp;Cores were stored upright and refrigerated before return to LDEO where each mono-core was split and analyzed non-destructively.&nbsp;One half core was then archived at LDEO and the other half made available for sampling.&nbsp;In Summer 2015, the sampling halves of each core were transported to WHOI for subsampling of core top material then returned to LDEO.</p>
<p>Approximately 5 g (wet-weight) of core top (0-1cm wet) material was extracted from each EPZT half-core with a stainless steel spatula, placed in a glass vial, dried at 60 degrees C overnight and then lightly homogenized with an agate pestle and mortar before being re-weighed.</p>
<p>Major elements were determined by fusing 10-20mg of dried sediment with Spectroflux and analyzed followed by ICP-ES analysis following the method of Ingamells (1970).</p>
<p>Total carbon and inorganic carbon concentrations was determined using a Perkin Elmer 2400 Elemental Analyzer and a UIC Coulometric Analyzer with Carbonate Module (Honjo et al., 1995). Organic carbon concentrations were calculated by difference between the total carbon and inorganic carbon concentrations.</p>
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1235248 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1235248
completed
Christopher R. German
Woods Hole Oceanographic Institution
508-289-2853
266 Woods Hole Rd Clark South 276 (MS #24)
Woods Hole
MA
02543
USA
cgerman@whoi.edu
pointOfContact
asNeeded
Dataset Version: 06 April 2017
Unknown
cruise_id
GEOTRC_INSTR
GEOTRC_SAMPNO
GEOTRC_EVENTNO
core_number
STNNBR
CASTNO
SAMPNO
Al_DRY_MONOCORE
Ba_DRY_MONOCORE
Ca_DRY_MONOCORE
Fe_DRY_MONOCORE
Mg_DRY_MONOCORE
Mn_DRY_MONOCORE
Si_DRY_MONOCORE
Sr_DRY_MONOCORE
Ti_DRY_MONOCORE
C_TOT_DRY_MONOCORE
C_INORG_DRY_MONOCORE
CaCo3_DRY_MONOCORE
C_ORG_MONOCORE
DATE_START
TIME_START
ISO_DATETIME_START
DATE_END
TIME_END
ISO_DATETIME_END
LATITUDE
LONGITUDE
depth
COMMENT
BTMDEPTH
CTDDEPTH
monocorer
theme
None, User defined
Cruise identfier
instrument
sample identification
event
station
cast
bottle
No BCO-DMO term
date_start
time_start
date end
time_end
latitude
longitude
depth
comments
depth_bottom
featureType
BCO-DMO Standard Parameters
Gravity Corer
instrument
BCO-DMO Standard Instruments
TN303
service
Deployment Activity
Eastern Tropical Pacific - Transect from Peru to Tahiti
place
Locations
otherRestrictions
otherRestrictions
Access Constraints: none. Use Constraints: Please follow guidelines at: http://www.bco-dmo.org/terms-use Distribution liability: Under no circumstances shall BCO-DMO be liable for any direct, incidental, special, consequential, indirect, or punitive damages that result from the use of, or the inability to use, the materials in this data submission. If you are dissatisfied with any materials in this data submission your sole and exclusive remedy is to discontinue use.
U.S. GEOTRACES
http://www.geotraces.org/
U.S. GEOTRACES
GEOTRACES is a SCOR sponsored program; and funding for program infrastructure development is provided by the U.S. National Science Foundation.
GEOTRACES gained momentum following a special symposium, S02: Biogeochemical cycling of trace elements and isotopes in the ocean and applications to constrain contemporary marine processes (GEOSECS II), at a 2003 Goldschmidt meeting convened in Japan. The GEOSECS II acronym referred to the Geochemical Ocean Section Studies To determine full water column distributions of selected trace elements and isotopes, including their concentration, chemical speciation, and physical form, along a sufficient number of sections in each ocean basin to establish the principal relationships between these distributions and with more traditional hydrographic parameters;
* To evaluate the sources, sinks, and internal cycling of these species and thereby characterize more completely the physical, chemical and biological processes regulating their distributions, and the sensitivity of these processes to global change; and
* To understand the processes that control the concentrations of geochemical species used for proxies of the past environment, both in the water column and in the substrates that reflect the water column.
GEOTRACES will be global in scope, consisting of ocean sections complemented by regional process studies. Sections and process studies will combine fieldwork, laboratory experiments and modelling. Beyond realizing the scientific objectives identified above, a natural outcome of this work will be to build a community of marine scientists who understand the processes regulating trace element cycles sufficiently well to exploit this knowledge reliably in future interdisciplinary studies.
Expand "Projects" below for information about and data resulting from individual US GEOTRACES research projects.
U.S. GEOTRACES
largerWorkCitation
program
U.S. GEOTRACES East Pacific Zonal Transect (GP16)
http://www.geotraces.org/
U.S. GEOTRACES East Pacific Zonal Transect (GP16)
<p><strong>From the NSF Award Abstract</strong><br />
The mission of the International GEOTRACES Program (<a href="https://www.geotraces.org/" target="_blank">https://www.geotraces.org/</a>), of which the U.S. chemical oceanography research community is a founding member, is "to identify processes and quantify fluxes that control the distributions of key trace elements and isotopes in the ocean, and to establish the sensitivity of these distributions to changing environmental conditions" (GEOTRACES Science Plan, 2006). In the United States, ocean chemists are currently in the process of organizing a zonal transect in the eastern tropical South Pacific (ETSP) from Peru to Tahiti as the second cruise of the U.S.GEOTRACES Program. This Pacific section includes a large area characterized by high rates of primary production and particle export in the eastern boundary associated with the Peru Upwelling, a large oxygen minimum zone that is a major global sink for fixed nitrogen, and a large hydrothermal plume arising from the East Pacific Rise. This particular section was selected as a result of open planning workshops in 2007 and 2008, with a final recommendation made by the U.S.GEOTRACES Steering Committee in 2009. It is the first part of a two-stage plan that will include a meridional section of the Pacific from Tahiti to Alaska as a subsequent expedition.</p>
<p>This award provides funding for management of the U.S.GEOTRACES Pacific campaign to a team of scientists from the University of Southern California, Old Dominion University, and the Woods Hole Oceanographic Institution. The three co-leaders will provide mission leadership, essential support services, and management structure for acquiring the trace elements and isotopes samples listed as core parameters in the International GEOTRACES Science Plan, plus hydrographic and nutrient data needed by participating investigators. With this support from NSF, the management team will (1) plan and coordinate the 52-day Pacific research cruise described above; (2) obtain representative samples for a wide variety of trace metals of interest using conventional CTD/rosette and GEOTRACES Sampling Systems; (3) acquire conventional JGOFS/WOCE-quality hydrographic data (CTD, transmissometer, fluorometer, oxygen sensor, etc) along with discrete samples for salinity, dissolved oxygen (to 1 uM detection limits), plant pigments, redox tracers such as ammonium and nitrite, and dissolved nutrients at micro- and nanomolar levels; (4) ensure that proper QA/QC protocols are followed and reported, as well as fulfilling all GEOTRACES Intercalibration protocols; (5) prepare and deliver all hydrographic-type data to the GEOTRACES Data Center (and US data centers); and (6) coordinate cruise communications between all participating investigators, including preparation of a hydrographic report/publication.</p>
<p>Broader Impacts: The project is part of an international collaborative program that has forged strong partnerships in the intercalibration and implementation phases that are unprecedented in chemical oceanography. The science product of these collective missions will enhance our ability to understand how to interpret the chemical composition of the ocean, and interpret how climate change will affect ocean chemistry. Partnerships include contributions to the infrastructure of developing nations with overlapping interests in the study area, in this case Peru. There is a strong educational component to the program, with many Ph.D. students carrying out thesis research within the program.</p>
<p><em>Figure 1. The 2013 GEOTRACES EPZT Cruise Track. [click on the image to view a larger version]</em><br />
<a href="http://dmoserv3.whoi.edu/data_docs/GEOTRACES/EPZT/GEOTRACES_EPZT_TN303_CruiseTrack.png" target="_blank"><img alt="" src="https://datadocs.bco-dmo.org/d3/data_docs/GEOTRACES/EPZT/GEOTRACES_EPZT_TN303_CruiseTrack.png" /></a></p>
U.S. GEOTRACES EPZT
largerWorkCitation
project
GEOTRACES: Suspended particle geochemistry along the US GEOTRACES Eastern Pacific Zonal Transect, from high productivity ocean margin to deep sea hydrothermal plume
https://osprey.bco-dmo.org/project/640083
GEOTRACES: Suspended particle geochemistry along the US GEOTRACES Eastern Pacific Zonal Transect, from high productivity ocean margin to deep sea hydrothermal plume
<p>During the 2013 GEOTRACES Eastern Pacific cruise a diverse range of oceanic environments will be encountered from the high productivity/high particle flux waters off Peru to the Peru-Chile oxygen minimum zone, the hydrothermal plume of the East Pacific Rise, and finally to some of the most oligotrophic waters around Tahiti. Scientists from Rutgers University and Woods Hole Oceanographic Institution will sample suspended particulates from the same GO-Flo bottles that will be used to sample dissolved trace metals and their isotopes (TEIs) across this entire transect. The suspended matter samples will be analyzed for 42 elements, including the particle-reactive rare earth elements. In addition, core-top sediments will be collected at every water-column sampling station and analyzed for both bulk composition (i.e., relative % content of organic carbon, opal, biogenic carbonate and lithogenic components) and the same 42 elements to be analyzed in the suspended particulates. Results from this study will be used to assess the role of suspended particulates in the biogeochemical cycling of TEIs across the Eastern Pacific by addressing three key sets of questions: (1) How does uptake of TEIs into phytoplankton and non-living particles in the upper ocean drive the suspended particulate composition through the deeper water column, along the substantial gradient from the high productivity Peru margin to the oligotrophic ocean interior?; (2) How faithfully is the along-transect variability in the upper ocean transmitted to the sediment (paleo) record?; (3) What are the relative influences of vertical recycling versus lateral advection in generating the distributions of dissolved and particulate TEIs observed in the Peru-Chile OMZ?; (4) Is there a characteristic signature of OMZ activity that is preserved in core-top sediments?; (5) What dominates TEI uptake onto/into authigenic particles in hydrothermal plumes and to what extent are these processes augmented by continuing uptake in core-top sediments?; and (6) What is the net effect from submarine venting on global TEI budgets?</p>
<p>As regards broader impacts, the scientist from Rutgers University is collaborating with the Education Director of the Centers for Ocean Science Education Excellence Networked Ocean World (COSEE-NOW) to contribute to the MARE (Marine Activities, Resources, and Education) program by inviting teachers and high school students to workshops and presentations on climate and ocean sciences. With the help of COSEE-NOW, he also plans to create educational video clips during the Pacific cruise and the subsequent laboratory based analytical work to educate them on the use of geochemistry to understand how the ocean works. Both scientists also plan to develop a teaching module entitled "Particles, Metals, and Carbon" for an Introduction to Oceanography class taught by the Rutgers scientist. One postdoc from Rutgers University would be supported and trained as part of this project.</p>
GEOTRACES EPZT Suspended Particles
largerWorkCitation
project
eng; USA
oceans
Eastern Tropical Pacific - Transect from Peru to Tahiti
-152.0005
-77.8182
-15.0002
-10.5003
2013-11-02
2013-12-18
From projects that focused on the following 2 locations: 1. Eastern Tropical Pacific - Transect from Peru to Tahiti (GP16) 2. Subtropical Southeastern Pacific Ocean
0
BCO-DMO catalogue of parameters from Core-top (0-1cm) sediment data collected by monocore from R/V Thomas G. Thompson TN303 (GP16; EPZT) GEOTRACES cruise from November to December 2013 (GEOTRACES EPZT project)
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
http://lod.bco-dmo.org/id/dataset-parameter/687022.rdf
Name: cruise_id
Units: unitless
Description: <p>Cruise identification</p>
http://lod.bco-dmo.org/id/dataset-parameter/687023.rdf
Name: GEOTRC_INSTR
Units: unitless
Description: <p>Sampling instrument</p>
http://lod.bco-dmo.org/id/dataset-parameter/687024.rdf
Name: GEOTRC_SAMPNO
Units: unitless
Description: <p>GEOTRACES Sample Number</p>
http://lod.bco-dmo.org/id/dataset-parameter/687025.rdf
Name: GEOTRC_EVENTNO
Units: unitless
Description: <p>GEOTRACES Event Number</p>
http://lod.bco-dmo.org/id/dataset-parameter/687026.rdf
Name: core_number
Units: unitless
Description: <p>Core identification number and depth range</p>
http://lod.bco-dmo.org/id/dataset-parameter/687027.rdf
Name: STNNBR
Units: unitless
Description: <p>Station number; joined from BCO-DMO EPZT master event file.</p>
http://lod.bco-dmo.org/id/dataset-parameter/687028.rdf
Name: CASTNO
Units: unitless
Description: <p>Cast number; joined from BCO-DMO EPZT master event file.</p>
http://lod.bco-dmo.org/id/dataset-parameter/687029.rdf
Name: SAMPNO
Units: unitless
Description: <p>Sequential sample number within the cast (usually corresponds to bottle number).</p>
http://lod.bco-dmo.org/id/dataset-parameter/687030.rdf
Name: Al_DRY_MONOCORE
Units: weight %
Description: <p>Aluminum concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687031.rdf
Name: Ba_DRY_MONOCORE
Units: weight %
Description: <p>Barium concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687032.rdf
Name: Ca_DRY_MONOCORE
Units: weight %
Description: <p>Calcium concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687033.rdf
Name: Fe_DRY_MONOCORE
Units: weight %
Description: <p>Iron concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687034.rdf
Name: Mg_DRY_MONOCORE
Units: weight %
Description: <p>Magnesium concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687035.rdf
Name: Mn_DRY_MONOCORE
Units: weight %
Description: <p>Manganese concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687036.rdf
Name: Si_DRY_MONOCORE
Units: weight %
Description: <p>Silicon concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687037.rdf
Name: Sr_DRY_MONOCORE
Units: weight %
Description: <p>Strontium concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687038.rdf
Name: Ti_DRY_MONOCORE
Units: weight %
Description: <p>Titanium concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687039.rdf
Name: C_TOT_DRY_MONOCORE
Units: weight %
Description: <p>Total Carbon concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687040.rdf
Name: C_INORG_DRY_MONOCORE
Units: weight %
Description: <p>Inorganic Carbon concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687041.rdf
Name: CaCo3_DRY_MONOCORE
Units: weight %
Description: <p>Calcium Carbonate concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687042.rdf
Name: C_ORG_MONOCORE
Units: weight %
Description: <p>Organic Carbon concentration (dry)</p>
http://lod.bco-dmo.org/id/dataset-parameter/687043.rdf
Name: DATE_START
Units: unitless
Description: <p>Date at start of sampling in yyyymmdd format</p>
http://lod.bco-dmo.org/id/dataset-parameter/687044.rdf
Name: TIME_START
Units: unitless
Description: <p>Time at start of sampling in HHMM format</p>
http://lod.bco-dmo.org/id/dataset-parameter/687045.rdf
Name: ISO_DATETIME_START
Units: unitless
Description: <p>Date and time at start of sampling formatted to ISO 8601 standard</p>
http://lod.bco-dmo.org/id/dataset-parameter/687046.rdf
Name: DATE_END
Units: unitless
Description: <p>Date at end of sampling in yyyymmdd format</p>
http://lod.bco-dmo.org/id/dataset-parameter/687047.rdf
Name: TIME_END
Units: unitless
Description: <p>Time at end of sampling in HHMM format</p>
http://lod.bco-dmo.org/id/dataset-parameter/687048.rdf
Name: ISO_DATETIME_END
Units: unitless
Description: <p>Date and time at end of sampling formatted to ISO 8601 standard</p>
http://lod.bco-dmo.org/id/dataset-parameter/687049.rdf
Name: LATITUDE
Units: decimal degrees
Description: <p>Latitude</p>
http://lod.bco-dmo.org/id/dataset-parameter/687050.rdf
Name: LONGITUDE
Units: decimal degrees
Description: <p>Longitude</p>
http://lod.bco-dmo.org/id/dataset-parameter/687051.rdf
Name: depth
Units: meters
Description: <p>PI-provided depth</p>
http://lod.bco-dmo.org/id/dataset-parameter/687052.rdf
Name: COMMENT
Units: unitless
Description: <p>Comment/notes about the sampling</p>
http://lod.bco-dmo.org/id/dataset-parameter/687053.rdf
Name: BTMDEPTH
Units: meters
Description: <p>Bottom depth; joined from BCO-DMO EPZT master event file.</p>
http://lod.bco-dmo.org/id/dataset-parameter/687054.rdf
Name: CTDDEPTH
Units: meters
Description: <p>CTD bottle firing depth; joined from BCO-DMO EPZT master event file.</p>
GB/NERC/BODC > British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
3974
https://datadocs.bco-dmo.org/file/P66Gk1RC4jqyLy/monocore_joined.csv
monocore_joined.csv
Primary data file for dataset ID 686982
download
https://osprey.bco-dmo.org/dataset/686982/data/download
download
onLine
dataset
<p>On the TN303 cruise, attempts to collect mono-cores were made during the final deep cast of the ODF CTD rosette at each station except Station 18 at the EPR ridge-axis.&nbsp;Cores were stored upright and refrigerated before return to LDEO where each mono-core was split and analyzed non-destructively.&nbsp;One half core was then archived at LDEO and the other half made available for sampling.&nbsp;In Summer 2015, the sampling halves of each core were transported to WHOI for subsampling of core top material then returned to LDEO.</p>
<p>Approximately 5 g (wet-weight) of core top (0-1cm wet) material was extracted from each EPZT half-core with a stainless steel spatula, placed in a glass vial, dried at 60 degrees C overnight and then lightly homogenized with an agate pestle and mortar before being re-weighed.</p>
<p>Major elements were determined by fusing 10-20mg of dried sediment with Spectroflux and analyzed followed by ICP-ES analysis following the method of Ingamells (1970).</p>
<p>Total carbon and inorganic carbon concentrations was determined using a Perkin Elmer 2400 Elemental Analyzer and a UIC Coulometric Analyzer with Carbonate Module (Honjo et al., 1995). Organic carbon concentrations were calculated by difference between the total carbon and inorganic carbon concentrations.</p>
Specified by the Principal Investigator(s)
<p><strong>Intercalibration:</strong>&nbsp;International Standard Used for Intercalibration: MAG 1. See the&nbsp;<a href="http://dmoserv3.whoi.edu/data_docs/GEOTRACES/EPZT/german/MAG_1_Ref_Std.pdf">detailed analyses for accuracy and precision document</a> (PDF).</p>
<p><strong>BCO-DMO Processing:</strong><br />
- modified parameter names to conform with BCO-DMO and GEOTRACES naming conventions;<br />
- copied columns from metadata sheet (lat/lon, dates, times, etc.) to data sheet.</p>
<p><strong>Additional GEOTRACES Processing:</strong><br />
As was done for the GEOTRACES-NAT data, BCO-DMO added standard US GEOTRACES information, such as the US GEOTRACES event number, to each submitted dataset lacking this information. To accomplish this, BCO-DMO compiled a 'master' dataset composed of the following parameters:</p>
<p>cruise_id, EXPOCODE,SECT_ID, STNNBR, CASTNO, GEOTRC_EVENTNO, GEOTRC_SAMPNO, GEOTRC_INSTR, SAMPNO, GF_NO, BTLNBR, BTLNBR_FLAG_W, DATE_START_EVENT, TIME_START_EVENT, ISO_DATETIME_UTC_START_EVENT, EVENT_LAT, EVENT_LON, DEPTH_MIN, DEPTH_MAX, &nbsp;BTL_DATE, BTL_TIME, BTL_ISO_DATETIME_UTC, BTL_LAT, BTL_LON, ODF_CTDPRS, SMDEPTH, FMDEPTH, BTMDEPTH, CTDPRS, CTDDEPTH.</p>
<p>This added information will facilitate subsequent analysis and inter comparison of the datasets.</p>
<p>Bottle parameters in the master file were taken from the GT-C_Bottle and ODF_Bottle datasets. Non-bottle parameters, including those from GeoFish tows, Aerosol sampling, and McLane Pumps, were taken from the TN303 Event Log (version 30 Oct 2014). Where applicable, pump information was taken from the PUMP_Nuts_Sals dataset.</p>
<p>A standardized BCO-DMO method (called "join") was then used to merge the missing parameters to each US GEOTRACES dataset, most often by matching on sample_GEOTRC or on some unique combination of other parameters.</p>
<p>If the master parameters were included in the original data file and the values did not differ from the master file, the original data columns were retained and the names of the parameters were changed from the PI-submitted names to the standardized master names. If there were differences between the PI-supplied parameter values and those in the master file, both columns were retained. If the original data submission included all of the master parameters, no additional columns were added, but parameter names were modified to match the naming conventions of the master file.</p>
<p>See the dataset parameters documentation for a description of which parameters were supplied by the PI and which were added via the join method.</p>
Specified by the Principal Investigator(s)
asNeeded
7.x-1.1
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
monocorer
monocorer
PI Supplied Instrument Name: monocorer Instrument Name: Gravity Corer Instrument Short Name:Gravity Corer Instrument Description: The gravity corer allows researchers to sample sediment layers at the bottom of lakes or oceans. The coring device is deployed from the ship and gravity carries it to the seafloor. (http://www.whoi.edu/instruments/viewInstrument.do?id=1079). Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/51/
Cruise: TN303
TN303
R/V Thomas G. Thompson
Community Standard Description
International Council for the Exploration of the Sea
R/V Thomas G. Thompson
vessel
TN303
James W. Moffett
University of Southern California
http://dmoserv3.whoi.edu/data_docs/GEOTRACES/EPZT/GT13_EPZT_ODFReport_All.pdf
Report describing TN303
R/V Thomas G. Thompson
Community Standard Description
International Council for the Exploration of the Sea
R/V Thomas G. Thompson
vessel