|Saito, Mak A.||Woods Hole Oceanographic Institution (WHOI)||Principal Investigator, Contact|
|Santoro, Alyson E.||University of California-Santa Barbara (UCSB-LifeSci)||Co-Principal Investigator|
|Ake, Hannah||Woods Hole Oceanographic Institution (WHOI BCO-DMO)||BCO-DMO Data Manager|
R/V Falkor 160115 TMR log from the ProteOMZ expedition in the Central Pacific during 2016.
R/V Falkor 160115 TMR log data.
Sampling was conducted using a Trace Metal Clean Rosette (TMR).
BCO-DMO Data Processing Notes:
- reformatted column names to comply with BCO-DMO standards.
- replaced spaces in column names with underscores.
- removed special characters from column names.
- removed units from column names
- added ISO_DateTime_UTC
|date||Date of sampling; YYYY/MM/DD||unitless|
|time||Local time of sampling; HH:MM||unitless|
|lon||Longitude; E is positive||decimal degrees|
|lat||Latitude; N is positive||decimal degrees|
|cast||Cast ID number||unitless|
|TMR_pin||Trace Metal Clean Rosette pin number||unitless|
|niskin_num||Niskin bottle number||unitless|
|real_depth||Actual depth where sample was measured||meters|
|notes||Notes on sampling||unitless|
|ISO_DateTime_UTC||Date ISO formatted; UTC||unitless|
|Dataset-specific Instrument Name|| |
|Generic Instrument Name|| |
Trace Metal Bottle
|Dataset-specific Description|| |
Trace Metal Clean Rosette
|Generic Instrument Description|| |
Trace metal (TM) clean rosette bottle used for collecting trace metal clean seawater samples.
|Start Date|| |
|End Date|| |
Project: Using Proteomics to Understand Oxygen Minimum Zones (ProteOMZ) More information is available from the ship operator at https://schmidtocean.org/cruise/investigating-life-without-oxygen-in-the... Additional cruis information is available from the Rolling Deck to Repository (R2R): https://www.rvdata.us/search/cruise/FK160115
From Schmidt Ocean Institute's ProteOMZ Project page:
Rising temperatures, ocean acidification, and overfishing have now gained widespread notoriety as human-caused phenomena that are changing our seas. In recent years, scientists have increasingly recognized that there is yet another ingredient in that deleterious mix: a process called deoxygenation that results in less oxygen available in our seas.
Large-scale ocean circulation naturally results in low-oxygen areas of the ocean called oxygen deficient zones (ODZs). The cycling of carbon and nutrients – the foundation of marine life, called biogeochemistry – is fundamentally different in ODZs than in oxygen-rich areas. Because researchers think deoxygenation will greatly expand the total area of ODZs over the next 100 years, studying how these areas function now is important in predicting and understanding the oceans of the future. This first expedition of 2016 led by Dr. Mak Saito from the Woods Hole Oceanographic Institution (WHOI) along with scientists from University of Maryland Center for Environmental Science, University of California Santa Cruz, and University of Washington aimed to do just that, investigate ODZs.
During the 28 day voyage named “ProteOMZ,” researchers aboard R/V Falkor traveled from Honolulu, Hawaii to Tahiti to describe the biogeochemical processes that occur within this particular swath of the ocean’s ODZs. By doing so, they contributed to our greater understanding of ODZs, gathered a database of baseline measurements to which future measurements can be compared, and established a new methodology that could be used in future research on these expanding ODZs.
|Gordon and Betty Moore Foundation: Marine Microbiology Initiative (MMI)|
|Alfred P. Sloan Foundation (Sloan)|
|Schmidt Ocean Institute (SOI)|
This document is created by info v 4.1f 5 Oct 2018 from the content of the BCO-DMO metadata database. 2022-12-06 12:01:30