|Thamatrakoln, Kimberlee||Rutgers University (Rutgers IMCS)||Principal Investigator|
|Brzezinski, Mark A.||University of California-Santa Barbara (UCSB-LifeSci)||Co-Principal Investigator|
|Copley, Nancy||Woods Hole Oceanographic Institution (WHOI BCO-DMO)||BCO-DMO Data Manager|
Particulate organic carbon and nitrogen measurements from CTD casts in the Monterey Bay area on RV/Point Sur cruise PS1312, June-July 2013
Whole seawater was collected using Niskin bottles mounted on a CTD rosette. Water was filtered onto 25 mm pre-combusted GF/F filters, flash frozen in liquid nitrogen, and stored at -80C until analysis. Prior to analysis, samples were thawed and dried overnight at 60C. Filters were acidified in a glass desiccator with concentrated HCl overnight, then dried again for at least 24 h. Samples were then run on a CHN Elemental Analyzer.
Milligrams of particulate organic carbon and nitrogen were determined according to standard measurements. The carbon and nitrogen content (mg) was then converted to a molar content (micromol) and divided by the volume of seawater filtered.
BCO-DMO Processing Notes:
- added conventional header with dataset name, PI name, version date
- modified parameter names to conform with BCO-DMO naming conventions
- re-formatted date from m/d/yyyy to yyyy-mm-dd
- added ISO_DateTime_Local column
- calculated decimal degrees for lat and lon
|ISO_DateTime_Local||Local date and time of sampling formatted as yyyy-mm-ddTHH:MM:SS||unitless|
|date_local||Local date formatted as yyyy-mm-dd||unitless|
|time_local||Local time (Pacific Standard Time)||unitless|
|cast_CTD||CTD cast number||unitless|
|lat||latitude; north is positive||decimal degrees|
|lon||longitude; east is positive||decimal degrees|
|PON||Particulate Organic Nitrogen concentration||micromol/liter (umol/L)|
|POC||Particulate Organic Carbon concentration||micromol/liter (umol/L)|
|Dataset-specific Instrument Name|| |
CHN Elemental Analyzer, Na 1500 series 2, Carlo Erba Instruments
|Generic Instrument Name|| |
CHN Elemental Analyzer
|Generic Instrument Description|| |
A CHN Elemental Analyzer is used for the determination of carbon, hydrogen, and nitrogen content in organic and other types of materials, including solids, liquids, volatile, and viscous samples.
R/V Point Sur
|Start Date|| |
|End Date|| |
Cruise DOI: 10.7284/903425
Description from NSF award abstract:
Diatoms, unicellular, eukaryotic photoautotrophs, are among the most ecologically successful and functionally diverse organisms in the ocean. In addition to contributing one-fifth of total global primary productivity, diatoms are also the largest group of silicifying organisms in the ocean. Thus, diatoms form a critical link between the carbon and silicon (Si) cycles. The goal of this project is to understand the molecular regulation of silicification processes in natural diatom populations to better understand the processes controlling diatom productivity in the sea. Through culture studies and two research cruises, this research will couple classical measurements of silicon uptake and silica production with molecular and biochemical analyses of Silicification-Related Gene (SiRG) and protein expression. The proposed cruise track off the West Coast of the US will target gradients in Si and iron (Fe) concentrations with the following goals: 1) Characterize the expression pattern of SiRGs, 2) Correlate SiRG expression patterns to Si concentrations, silicon uptake kinetics, and silica production rates, 3) Develop a method to normalize uptake kinetics and silica production to SiRG expression levels as a more accurate measure of diatom activity and growth, 4) Characterize the diel periodicity of silica production and SiRG expression.
It is estimated that diatoms process 240 Teramoles of biogenic silica each year and that each molecule of silicon is cycled through a diatom 39 times before being exported to the deep ocean. Decades of oceanographic and field research have provided detailed insight into the dynamics of silicon uptake and silica production in natural populations, but a molecular understanding of the factors that influence silicification processes is required for further understanding the regulation of silicon and carbon fluxes in the ocean. Characterizing the genetic potential for silicification will provide new information on the factors that regulate the distribution of diatoms and influence in situ rates of silicon uptake and silica production. This research is expected to provide significant information about the molecular regulation of silicification in natural populations and the physiological basis of Si limitation in the sea.