Accessing BCO-DMO data
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BCO-DMO ERDDAP
Accessing BCO-DMO data |
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| Dataset Title: | [WS1005 cruise track] - Cruise track (1-min fixes; from R2R) from R/V F.G. Walton Smith cruise WS1005 from Miami to the Bahamas in 2010 (Were Protists the Beginning of the End for Stromatolites? ) 
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| Institution: | BCO-DMO (Dataset ID: bcodmo_dataset_3993) |
| Information: | Summary
| License
| FGDC
| ISO 19115
| Metadata
| Background
| Files
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Attributes {
s {
date_utc {
Int32 _FillValue 2147483647;
Int32 actual_range 20100318, 20100324;
String bcodmo_name "date_utc";
String description "Year, month, and day (UTC) in YYYYmmdd format.";
String long_name "Date Utc";
String units "unitless";
}
time_utc {
String bcodmo_name "time_utc";
String description "Time (UTC) in hours, minutes, and decimal minutes; 24-hour clock.";
String long_name "Time Utc";
String units "HHMM.mmmmm";
}
latitude {
String _CoordinateAxisType "Lat";
Float64 _FillValue NaN;
Float64 actual_range 24.6997025, 25.83778167;
String axis "Y";
String bcodmo_name "latitude";
Float64 colorBarMaximum 90.0;
Float64 colorBarMinimum -90.0;
String description "Latitude (-90 to 90 decimal degrees).";
String ioos_category "Location";
String long_name "Latitude";
String nerc_identifier "https://vocab.nerc.ac.uk/collection/P09/current/LATX/";
String standard_name "latitude";
String units "degrees_north";
}
longitude {
String _CoordinateAxisType "Lon";
Float64 _FillValue NaN;
Float64 actual_range -80.19414733, -76.8221655;
String axis "X";
String bcodmo_name "longitude";
Float64 colorBarMaximum 180.0;
Float64 colorBarMinimum -180.0;
String description "Longitude (-180 to 180 decimal degrees).";
String ioos_category "Location";
String long_name "Longitude";
String nerc_identifier "https://vocab.nerc.ac.uk/collection/P09/current/LONX/";
String standard_name "longitude";
String units "degrees_east";
}
sog {
Float32 _FillValue NaN;
Float32 actual_range 0.0, 6.05;
String bcodmo_name "sog";
String description
"Instantaneous speed-over-ground (in meters per second); computed from single-differences
of successive positions (from the current position to the next position).";
String long_name "Speed Over Ground";
String units "m/s";
}
cog {
Float32 _FillValue NaN;
Float32 actual_range 0.0, 359.566;
String bcodmo_name "cog";
String description "Instantaneous course-over-ground measured in degrees clockwise from north.";
String long_name "Course Over Ground";
String units "degrees clockwise from North";
}
time {
String _CoordinateAxisType "Time";
Float64 actual_range 1.268870400405e+9, 1.269462180388e+9;
String axis "T";
String bcodmo_name "ISO_DateTime_UTC";
String description "Date/Time (UTC) formatted to ISO8601 standard. T indicates start of time string; Z indicates UTC.";
String ioos_category "Time";
String long_name "ISO Date Time UTC";
String nerc_identifier "https://vocab.nerc.ac.uk/collection/P01/current/DTUT8601/";
String source_name "ISO_DateTime_UTC";
String standard_name "time";
String time_origin "01-JAN-1970 00:00:00";
String time_precision "1970-01-01T00:00:00.000Z";
String units "seconds since 1970-01-01T00:00:00Z";
}
}
NC_GLOBAL {
String access_formats ".htmlTable,.csv,.json,.mat,.nc,.tsv,.esriCsv,.geoJson,.odvTxt";
String acquisition_description
"Original navigation and other data are available from the NSF R2R data
catalog:
[https://www.rvdata.us/search/cruise/WS1005](\\\\\"https://www.rvdata.us/search/cruise/WS1005\\\\\")";
String awards_0_award_nid "54952";
String awards_0_award_number "OCE-0926421";
String awards_0_data_url "http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=0926421";
String awards_0_funder_name "NSF Division of Ocean Sciences";
String awards_0_funding_acronym "NSF OCE";
String awards_0_funding_source_nid "355";
String awards_0_program_manager "David L. Garrison";
String awards_0_program_manager_nid "50534";
String cdm_data_type "Other";
String comment
"WS1005 Cruise Track (1-min resolution)
from Rolling Deck to Repository (R2R)
R/V F.G. Walton Smith
Chief Sci: Joan Bernhard (WHOI)
Version: 09 July 2013";
String Conventions "COARDS, CF-1.6, ACDD-1.3";
String creator_email "info@bco-dmo.org";
String creator_name "BCO-DMO";
String creator_type "institution";
String creator_url "https://www.bco-dmo.org/";
String data_source "extract_data_as_tsv version 2.3 19 Dec 2019";
String date_created "2013-07-09T20:03:09Z";
String date_modified "2019-11-12T20:32:53Z";
String defaultDataQuery "&time<now";
String doi "10.1575/1912/bco-dmo.3993.1";
Float64 Easternmost_Easting -76.8221655;
Float64 geospatial_lat_max 25.83778167;
Float64 geospatial_lat_min 24.6997025;
String geospatial_lat_units "degrees_north";
Float64 geospatial_lon_max -76.8221655;
Float64 geospatial_lon_min -80.19414733;
String geospatial_lon_units "degrees_east";
String history
"2024-12-23T16:08:13Z (local files)
2024-12-23T16:08:13Z https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_3993.html";
String infoUrl "https://www.bco-dmo.org/dataset/3993";
String institution "BCO-DMO";
String keywords "bco, bco-dmo, biological, chemical, cog, course, data, dataset, date, date_utc, dmo, erddap, ground, iso, latitude, longitude, management, oceanography, office, over, preliminary, sog, speed, time, time_utc";
String license "https://www.bco-dmo.org/dataset/3993/license";
String metadata_source "https://www.bco-dmo.org/api/dataset/3993";
Float64 Northernmost_Northing 25.83778167;
String param_mapping "{'3993': {'lat': 'master - latitude', 'lon': 'master - longitude', 'ISO_DateTime_UTC': 'master - time'}}";
String parameter_source "https://www.bco-dmo.org/mapserver/dataset/3993/parameters";
String people_0_affiliation "Woods Hole Oceanographic Institution";
String people_0_affiliation_acronym "WHOI";
String people_0_person_name "Joan M. Bernhard";
String people_0_person_nid "51285";
String people_0_role "Chief Scientist";
String people_0_role_type "originator";
String people_1_affiliation "Woods Hole Oceanographic Institution";
String people_1_affiliation_acronym "WHOI BCO-DMO";
String people_1_person_name "Shannon Rauch";
String people_1_person_nid "51498";
String people_1_role "BCO-DMO Data Manager";
String people_1_role_type "related";
String project "Protists_Stromatolites";
String projects_0_acronym "Protists_Stromatolites";
String projects_0_description
"Collaborative Research: Were Protists the Beginning of the End for Stromatolites?
This award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5).
Microbial mats are conspicuous components of many benthic marine and aquatic settings. A subset of these microbial mats binds sediments to form potentially fossilizable structures, often called stromatolites or microbialites. While much is known about microbialite autotrophs, little is known about their heterotrophic eukaryotes. The lack of understanding is surprising given that stromatolites have an extensive geologic record spanning most of Earth's history. Stromatolites are layered sedimentary structures formed by a combination of microbial activities, abiotic carbonate precipitation, and sedimentary processes. Details of stromatolite formation and preservation are poorly understood, and a drastic decline in stromatolite occurrence and diversity in the late Precambrian has long been a conundrum. A popular hypothesis to explain this decline at ~1 billion years ago is that eukaryotic organisms evolved to become predators on stromatolites. To date, the most commonly proposed predatory culprit is an unidentified metazoan, although evidence of such an organism is lacking from the fossil record. Protists, most of which are not expected to leave an obvious fossil record, are additional possible stromatolitic predators, but they have been largely ignored in this context. The hypotheses of this project are: (1) Heterotrophic protist activity caused the textural change from stromatolites (layered sediment fabric) to thrombolites (clotted sediment fabric) and (2) Heterotrophic protists caused the decimation of Neoproterozoic stromatolites. Since it is impossible to recreate the Neoproterozoic, studies of modern analogs serve to indirectly test these hypotheses. The overall goal of this project is to describe the eukaryotic communities associated with modern stromatolites and thrombolites from the Bahamas and Australia, compare the communities from the two sites, and to relate the communities to stromatolitic / thrombolitic sediment fabric and biomarker signatures.
The overall goal will be achieved by addressing the following specific aims: (1) Identify, via morphologic and molecular approaches, the eukaryotic community of modern stromatolites and thrombolites; (2) Analyze modern and fossil stromatolites and thrombolites for their eukaryotic lipid biomarkers using solvent extraction, chromatographic and mass spectrometric methods; (3) Using the Fluorescently Labeled Embedded Core (FLEC) method, document the sub-millimeter distributions of the heterotrophic eukaryotic community inhabiting modern stromatolites and thrombolites in conjunction with fine-scale sediment fabric; (4) Using solvent extraction, chromatographic and mass spectrometric methods, analyze cultures of allogromiid foraminifers to survey for lipid biomarkers unique to them; (5) After incubation of modern stromatolites with heterotrophic protists, use FLEC methodology to determine how their activity affects sediment fabric and conduct preliminary comparisons of these modern fabrics to those of stromatolite fossils.
Intellectual Merit: The oldest fossil stromatolites are >3.4 billion years old and are the most visible manifestations of pervasive microbial life on the early Earth. The changes in stromatolite abundance and morphology document complex interplays between biological and geological processes. This project addresses multiple aspects of stromatolite genesis and pre-fossilization alteration but at its core, focuses on one of the greatest geological enigmas: the possible connection between stromatolite decline and the rise of complex life.";
String projects_0_end_date "2013-08";
String projects_0_geolocation "Highborne Cay, Bahamas and Carbla Station (Shark Bay), Western Australia";
String projects_0_name "Were Protists the Beginning of the End for Stromatolites?";
String projects_0_project_nid "2203";
String projects_0_start_date "2009-09";
String publisher_name "Biological and Chemical Oceanographic Data Management Office (BCO-DMO)";
String publisher_type "institution";
String sourceUrl "(local files)";
Float64 Southernmost_Northing 24.6997025;
String standard_name_vocabulary "CF Standard Name Table v55";
String summary "1-minute resolution navigation from the WS1005 cruise aboard the R/V F.G. Walton Smith from 18 March to 24 March 2010.";
String time_coverage_end "2010-03-24T20:23:00.388Z";
String time_coverage_start "2010-03-18T00:00:00.405Z";
String title "[WS1005 cruise track] - Cruise track (1-min fixes; from R2R) from R/V F.G. Walton Smith cruise WS1005 from Miami to the Bahamas in 2010 (Were Protists the Beginning of the End for Stromatolites? )";
String version "1";
Float64 Westernmost_Easting -80.19414733;
String xml_source "osprey2erddap.update_xml() v1.3";
}
}
Data Access Protocol (DAP) and its
selection constraints.
The URL specifies what you want: the dataset, a description of the graph or the subset of the data, and the file type for the response.
Tabledap request URLs must be in the form
https://coastwatch.pfeg.noaa.gov/erddap/tabledap/datasetID.fileType{?query}
For example,
https://coastwatch.pfeg.noaa.gov/erddap/tabledap/pmelTaoDySst.htmlTable?longitude,latitude,time,station,wmo_platform_code,T_25&time>=2015-05-23T12:00:00Z&time<=2015-05-31T12:00:00Z
Thus, the query is often a comma-separated list of desired variable names,
followed by a collection of
constraints (e.g., variable<value),
each preceded by '&' (which is interpreted as "AND").
For details, see the tabledap Documentation.