Chlorophyll Methods

Chlorophyll Determination

 


SUMMARY: Chlorophyll a is extracted in an acetone solution. Chlorophyll and phaeopigments are then measured fluorometrically using an acidification technique.


 

1. Principle

Seawater samples of a known volume are filtered (< 10 psi) onto GF/F filters. These filters are then placed into 10ml screw-top culture tubes containing 8.0ml of 90% acetone. After a period of 24 to 48 hours, the fluorescence of the samples is read on a fluorometer. Then samples are acidified to degrade the chlorophyll to phaeopigments (i.e. phaeophytin) and a second reading is taken. The readings prior to and after acidification are then used to calculate concentrations of both chlorophyll a and ‘phaeopigment’. The method used today is based on those developed by Yentsch and Menzel (1963), Holm-Hansen et al. (1965) and Lorenzen (1967).  Note that concentrations of ‘phaeopigments’ are not a good measure of Chl a degradation products present in the sample since Chl b present in the sample will be measured as ‘phaeopigments’.

2. Sample Drawing

2.1.

Chlorophyll bottles should be rinsed three times with sample prior to filling. The bottles are calibrated for volume, so the sample drawer must insure that air bubbles are not clinging to the sides of the bottle and it is filled completely.  The sensitivity of the fluorometric method allows for sample bottles of ~50 to 250 ml.

3. Sample Filtration

3.1.

Check that the filtration funnels are well seated on the base, and be sure that the filters (Whatman GF/F) are in place. Improperly placed filters or loose funnels will result in loss of sample. The chlorophyll samples are volumetric and should sample loss occur, replace the filter with a new one and redraw the sample.

3.2.

Turn on the vacuum pump, pour the sample into the filter funnel, and open the valve. Check the vacuum pressure to see that it does not exceed 10 psi or ~500mm Hg. Generally samples are filtered in such a way as to insure that the deepest samples (i.e. those typically containing less chlorophyll) are filtered at the same manifold positions in each time. When a shallow cast is performed and a reduced number of samples is taken, it is advisable to filter them on positions typically used for those approximate depths. This reduces the potential for contaminating filter funnels used for filtering deep samples that in general contain low levels of chlorophyll.

3.3.

When a sample has finished filtering, turn off the valve; once all the samples have filtered, turn off the pump; use designated sample forceps to pick off the filter and place it in the appropriate numbered tube containing 8 mL 90% acetone. Make sure that the filter is completely submerged in the acetone.

3.4.

Cap TIGHTLY but be aware that tube tops can break off, then place the sample tubes in a rack. The sample rack is then placed in a refrigerator and the filtration time is recorded.

4. Standardization of Fluorometer

4.1.

A commercially available chlorophyll standard (e.g. Anacystis nidulans, Sigma Aldrich) should be used to calibrate the fluorometer, preferably before and after each cruise. The Chl a standard is dissolved in 100% acetone to yield approximately 0.1mg-Chl per ml solution. 1ml of this solution can then be diluted in 100ml 100% acetone and read in a spectrophotometer at 664nm. A second reading at 750nm is also recorded as a blank value to correct for sample turbidity. The remainder can be aliquotted into cryo tubes and stored in liquid N2 for future use. Chl a standards such stored are stable for years. The initial dilution is made with 100% acetone because it stores better in liquid N2 than those made with 90%. However, since 90% acetone is used for the extraction, it is also used for dilutions when generating a standard curve.

4.2

The concentration (mg l-1) of the standard is determined by the following equation:

Chl a =           Equation1

A664 = absorption at 664nm

A750 = absorption at 750nm

E = Extinction coefficient (100% acetone = 88.15, 90% acetone = 87.67) from Jefferies and Humphrey (1975)

l = cuvette path length (cm)

4.3.

A series of dilutions using 90% acetone (N> 5) are then made and read, recording both Rb and Ra values. Blank values should be subtracted from the Rb and Ra prior to performing calculations. If using a fluorometer with multiple sensitivity and range settings such as a Turner model 10, then the proper blank value must be subtracted for readings taken at a given setting.

4.4.

A calibration factor (F) must be calculated for each fluorometer. It is the slope of the line resulting from plotting the fluorometer reading (x-axis) vs. chlorophyll concentration (y-axis). This line is forced through zero. An acidification coefficient (τ) is the average acid ratio (Rb/Ra) for the pure chlorophyll standards used in the calibration.

4.5.

Calculating chlorophyll and phaeopigment concentration in a sample is accomplished by using the following equations (Knap et al., 1996):

Chl (µg/l) =  Equation2

Phaeo (µg/l) =   Equation3

F = Linear calibration factor (see 4.4)

τ = Average acid ratio (Rb/Ra) – Note that these are actually corrected values, with the blank readings already subtracted.

Ve = Volume of extract (ml)

Vf = Volume of sample filtered (l)

S = Sensitivity setting of fluorometer (Applicable to Turner model 10. If using a model 10AU or another fluorometer, use a value of “1”)

Rng = Range setting of fluorometer (Applicable to Turner model 10. If using a model 10AU or another fluorometer, use a value of “1”)

There are variations of this equation that can be used and other factors that can affect chlorophyll measurements. More detailed descriptions can be obtained in Strickland and Parsons (1968) and Holm-Hansen and Riemann (1978).

Note: After a cruise, the fluorometer is calibrated again and the calibration factors and average acid ratios obtained from pre and post-cruise calibrations are averaged for final data processing.

5. Reading Samples on the Fluorometer

5.1.

The fluorometer should be allowed to warm up for approximately 1/2 hour before using it. Samples must extract in acetone for at least 24 hours prior to reading on the fluorometer and should be read before 48 hours.

5.2.

Samples must be at room temperature prior to reading. One hour before samples are to be read, they should be removed from the refrigerator and allowed to warm up in a dark place.

5.3.

A blank tube containing the same acetone batch used for the extractions should be prepared and read prior to reading samples. This blank should be read before and after every sample run and after door setting have been changed (Turner model 10 fluorometer)

5.4.

A coproporphyrin standard should be read prior to reading samples (D’Sa et al., 1997). While not used in any calculation, it is useful to monitor the performance of the fluorometer over time between calibrations. Significant changes in coproporphyrin readings may indicate a problem with the fluorometer.

5.5.

Remove the filter, shake the sample to insure that it is well mixed, and use a Kimwipe to remove fingerprints from the exterior of the tube prior to running samples.

5.6.

Read the sample and record the number (Rb). Add 100µl of 10% HCl and wait approximately 30 seconds for the number to stabilize and record the value (Ra).

6. Equipment/Supplies

· Whatman 25mm GF/F filters (Fisher Scientific)

· Volumetric sample bottles (~130-150ml)

· Vacuum filtration apparatus with vacuum pump capable of maintaining 10 p.s.i

· Fluorometer and proper filter kit for measuring chlorophyll a/phaeophytin with acidification method (Turner model 10AU uses a 10-037R optical kit).

· Pipet (or re-pipet) capable of delivering 100µl.

· Personal protection equipment (PPE) consisting of gloves and safety glasses.

· Kimwipes or equivalent laboratory wipes.

· 10ml screw-top sample tubes (Fisher Scientific)

· Two sets of forceps (one for sample manipulation and one for replacing clean filters)

· Assorted laboratory glassware, including volumetric flasks for diluting calibration standards

7. Reagents

· Milli-Q or equivalent polished water source.

· HPLC-grade or equivalent low-fluorescing acetone. Note that volume is not conserved when preparing solution of water and acetone. The addition of 413ml Milli-Q water to 3800ml of acetone results in 4130ml of 90% acetone.

· 10% HCl solution

· Chlorophyll a (Sigma Aldrich catalog number C6144)

· Coproporphyrin III tetramethyl ester (Sigma Aldrich catalog number C7157)

8. References

· D’Sa, E.J., Lohrenz, S.E, Asper, V.L., and Walters, R.A. (1997). Time Series Measurements of Chlorophyll Fluorescence in the Oceanic Bottom Boundary Layer with a Multisensor Fiber-Optic Fluorometer. , 167: 889–896. DOI: 10.1175/1520-0426(1997)0142.0.CO;2

· Holm_Hansen, O., Lorenzen, C.J., Holms, R.W., Strickland, J.D.H. (1965). Fluorometric Determination of Chlorophyll. J. Cons.perm.int Explor. Mer. 30: 3-15.

· Holm-Hansen, O., and B. Riemann. (1978). Chlorophyll a determination: improvements in methodology. Oikos, 30: 438-447.

· Jeffery, S.W. and Humphrey, G.F. (1975). New spectrophotometric equations for determining chlorophylls a, b, c1, and c2 in higher plants, algae and natural phytoplankton. Biochem. Physiol. Pflanz. 167: 191-194.

· Knap, A., A. Michaels, A. Close, H. Ducklow and A. Dickson (eds.). (1996). Protocols for the Joint Global Ocean Flux Study (JGOFS) Core Measurements.
JGOFS Report Nr. 19, vi+170 pp. Reprint of the IOC Manuals and Guides No. 29, UNESCO 1994.

· Lorenzen, C. J. (1967) Determination of chlorophylls and phaeopigments: spectrophotometric equations. Limnol. Oceanogr. 12: 343–346.

· Strickland J. D. H., Parsons T. R., (1968). A practical handbook of seawater analysis. Pigment analysis, Bull. Fish. Res. Bd. Canada, 167.

· Yentsch, C.S., Menzel, D.W. (1963). A method for the determination of phytoplankton chlorophyll and phaeophytin by fluorescence. Deep-Sea Res. 10: 221-231

Methods Timeline

CalCOFI Time Series data are over 67 years old. New adopted practices, methods, software and hardware are thoroughly tested to maintain dataset continuity as the program & science evolves. Core measurements are maintained and many new measurements added. CTD temperature sensors, for example, provide data at a much higher resolution than a 20 bottle hydrocast equipped with reversing thermometers pre-9308 (Aug 1993).

Although the CTDs casts on CalCOFI started in 1990, CTD-rosette casts did not replace bottles-on-wire hydro casts completely until Aug 1993 (9308). In 2004, LTER joined the CalCOFI cruises, expanding the seawater analyses, adding new measurements.

Changes of standard practices, methods, software, & equipment will be tabulated here, particularly those affecting the hydrographic data or other data products.

 Cruise/Date

 Measurement, 
 Equipment,  Method

 Changes    

Comments

CalCOFI Methods Timeline
  Methods Timeline Started  

This page is ‘dynamic’ so new items will be added whenever new methods, measurements, equipment are implemented. Older changes will be added as time-permits and they are remembered.

1708SR CCE-LTER ISUS upgraded to fw v3 ISUS upgraded to firmware v3 Seabird acquired Satlantic and took several month to get ISUS service online. Once done, they upgraded the CCE-LTER MBARI-ISUS v2 to firmware v3. Allows easy in-house or at-sea calibration.
1708SR Oxygen Stable Isotope Seawater samples collected for OSI 5ml of seawater collected from two depths (10m & 50m) on 18 stations
1701RL
1704SH
LARS rosette 24-btl LARS rosette used Even though RV Reuben Lasker & FSV Bell M Shimada do not have a LARS CTD deployment system, the height clearance allows the use of the LARS rosette. SIO-CalCOFI will use this rosette as primary unless the height clearance becomes a problem, such as on RV Ocean Starr.
1611SR First RV Sally Ride SIO RV Sally Ride used for CalCOFI RV Sally Ride used for the first time to do CalCOFI station work; acoustics operational but not calibrated
1611SR RINKO III Optode RINKO III Oxygen sensor deployed Optode used on non-basin stations deeper than 500m, where altimeter was not needed
1611SR Seawater samples Domoic Acid & Th-234 Collected ancillary seawater & deploy insitu pumping system
pre-1611SR ISUS (Frank’s) Repaired Peter Frank’s ISUS repaired & upgraded to firmware v3 ISUS was not working so it was sent to Satlantic who repaired it and upgraded the firmware to v3
1609SR New research vessel SIO RV Sally Ride test for CalCOFI Shakedown cruise for RV Sally Ride to do CalCOFI – new LARS, epoxy-coated rosette deployed
1609SR LARS epoxy-coated rosette First use of new 24-bottle rosette 24-btl white epoxy coated aluminum rosette deployed with stainless steel LARS support
1607OS Seawater Samples Domoic Acid samples collected Ancillary seawater sample collection
1604SH Nutrient Analysis New (returning) in-house nutrient chemist Nutrients run by SIO-CalCOFI analyst DGS
1507OC Underway Measurements RV Oceanus MET system logs data into individual data files; combined data are unavailable unless merged manually Unlike other UNOLS vessels, particularly SIO RV New Horizon, the underway TSG & meterological data are logged at 1Hz into individual files. A combinded data file will have to be generated post-cruise by merging individual sensor data files using the common UTC timestamp. Software pending…
1504NH Underway Measurements PCO2 and pH measurements added to CCE-LTER suite

 

1504NH Nutrient Analysis Standard matrix; sample vials

Standards now prepared in low nutrient seawater (collected from the end of lines 93.3 or 90.0 and processed with UV light, filtration and aged before use).  New 30 mL polypropylene tubes in use.

06 Aug 2014 calcofi.com calcofi.com 2014 online

Developmental site web.calcofi.com replaces Joomla 1.5 calcofi.com; Joomla 3+ fully implemented. calcofi.com old site moved to old.calcofi.com

1402SH Nutrient Analysis New in-house Nutrient Technician

Nutrients run by SIO-CalCOFI analyst LJE.

1402SH NCOG DNA/RNA NCOG sample collection started NCOG DNA/RNA samples collected at ~4 depths (10m, chl max, 170m, 515m)
1311NH DIC measurments Sampling expands

Dissovled inorganic carbon samples are now drawn at more locations along the cruise track with 14 profile and 8 additional surface water stations per cruise.

1211NH Rinko Oxygen Optode RINKO III Optode deployed RINKO III Oxygen Optode sensor replaced 2nd SBE43 oxygen sensors on stations where the altimeter was not needed – non-basin stations deeper that 500m.
01Mar2013 web.calcofi.com website update Upgrading calcofi.com to latest Joomla

web.calcofi.com started to migrate calcofi.com 1.5 to 3.0; to improve responsiveness with new dynamic templates – desktop, tablet, and smartphone auto-formatting. Security improvements, auto-updating, jQuery & other new features of version 3.+

1207OS Nutrient Analysis New in-house Nutrient Technician

Nutrients run by former ODF chemist, now a SIO-CalCOFI analyst MTM.

01May2012 dev.calcofi.com blog started SIO-CalCOFI Technical Group developmental blog started.

For metadata: documenting changes in software, data-processing methods, formats, products, & practices.

1203SH Nutrient Analysis Instrument and analyst change, new Seal QuAAtro Analyzer purchased.

Transitioned to in-house nutrient analysis on new Seal QuAAtro Nutrient Analyzer, nutrients run by SIO-CalCOFI analyst DNF.  Replacing sample analysis by ODF chemist on an AA3 analyzer.

Standards now prepared in artificial seawater.

NO3 data calculated using regression coefficients from ISUS voltage vs NO3 for 1202NH & 1203SH look nearly identical.

1203SH atsea.calcofi.com blog online Setup to keep notes during quarterly cruises, particularly those related to data, equipment, & generally noteworthy.

Connected-linked to CalCOFI’s Twitter feed

1202NH Nutrient Analysis  Last cruise where nutrients were run by ODF chemist on an AA3 analyzer.

 

1202NH+ Data Processing IEH retired as primary data processing file format. Sta.csvs and casts.csv adopted. After parallel-processing (IEH & csv file format) 1104, 1108, 1110 cruise data. Sta.csvs & casts.csv data processing is being used to process, merge, quality-control, publish all hydrographic data. IEH-format is a data product along with the hydrographic database.
1108 All measurements & data products Hydrographic data are processed using both old & new methods and compared.

The cruise is once again processed twice, in parallel, using the IEH old-school method and the new csv-format method. GTool development & refinement continues as sta.csvs & casts.csv formats are improved. Final data products are compared for agreement. This is the first cruise to generate data products using new csv-database data processing methods not based on IEHs.

1104 GTool Matlab program developed SIO-CalCOFI Technical Team implement a new graphical matlab tool to point-check CalCOFI hydrographic data

MGS, in cooperation with the CCTG, develops GTool to replace Andyplots, our legacy method to visually inspect all bottle data on one figure. CTD continuous data are plotted with bottle parameters to cross-check and eliminate fliers.

1104 All measurements; data products Hydrographic data are processed using both old & new methods and compared.

The cruise is processed twice, in parallel, using the IEH old-school method and the new csv-format method. GTool, a matlab plotting & data-quality control program script, is developed to ingest CTD & sta.csvs to graphically assess CTD & bottle data-quality. Final data products are compared for agreement. This should be the last cruise processed using 00/20/22 & IEHs.

1101 Reported standard level O2 CTD primary or secondary oxygen sensor bottle–corrected measurements are reported instead of interpolated standard level (ISL) oxygen values Pretains to final, standard-level bottle data reported in all data products – with the reliability of the SBE 43 oxygen sensors and consistently high data quality when calibrated bi-yearly (twice/year) and bottle-corrected. Bottle-corrected CTD primary or secondary oxygen values (whichever sensor is performing better that cast) are reported instead of interpolated (calculated) standard level bottle oxygen values.
1101  Data storage format, ieh phase out begins; all measurements affected Sta.csv & casts.csv implementation begins, replacing 00/20/22 & IEH data process methodology. IEH-method is used as CSV-method is developed.

Bottle data & CTD data processing up til now have been relatively separate although data-quality cross-check are common. Other than CTD temperatures, all hydrographic data reported in IEHs or hydrographic database are bottle sample measurements. In 2011, our new data processing strategy merges the bottle & CTD starting at seawater sample collection. CESL generates individual sta.csvs combining CTD & bottle data immediately after seawater sample collection. Casts.csv is also generated and contains station specific information, replacing the Station Cast Description & Weather files (stacst & weather).

1101  DECODR DECODR migration to the new sta.csv and casts.csv data-processing scheme in full development

DECODR (Data Entry & Compile Oceanographic Data Reports) program modules are adapted to process either old or new hydrographic data formats. Sta.csvs & casts.csv adaptations are implemented and different data products are generated directly or by generating an IEH first then data products.

0901  DIC measurements resume DIC (dissolve inorganic carbon) sampling resume after a hiatus.

DIC, aka Keeling, samples were commonly taken on two CalCOFI stations but the new sampling scheme covers several additional stations and depths.

2008  Nutrient Analysis Began ammonium analysis

Nutrient analysis expanded to include ammonium.

0701  Salinity measurement SalReCap – Salinity Record & Capture program introduced, replacing the PSal (DOS shell executable).

SalReCap, Windows program developed by SIO-CalCOFI, replaces ODF-developed PSal, a DOS executable. Immediate comparisons to CTD salinities during analysis becomes available.

Apr-05  Primary Productivity New specific activity procedure The procedure for calculating cruise 14C specific activity for the productivity assay was changed to reflect daily 14C additions averaged over the course of a cruise.  The six dark bottles have one milliliter removed, added to ethanolamine spiked scintillation cocktail for counting.  Previously specific activity was calculated for a batch of stock and used for the entire cruise.  The new method served to check pipeting, inoculation amounts and any changes in volatile 14C stocks.
0411  Ancillary measurements such as HPLC, DOM, Size fractionations, Epifluorescence LTER affiliation on CalCOFI cruises begins

CCE-LTER (California Current Ecosystem Long Term Ecological Research Site) is established and LTER participation on all CalCOFIs begins. A large suite of additional measurements, particularly seawater samples from the rosette, and PRPOOS vertical plankton tow are added to CalCOFI hydrography.

0310  Oxygen measurement Autotitrator replaces manual modified Winkler titrations

After substantial assay-comparative testing, an ODF-developed oxygen auto-titrator is used to titrate discrete, rosette-bottle, seawater oxygen samples at-sea. New oxygen data format & data processing module is introduced in DECODR.

0204  CalCOFI Data Report Last bound hardcopy of the bi-annual CalCOFI Hydrographic Data Report is published, CC Reference 03-01 31 July 2003

CalCOFI Hydrographic Data Reports will continue being published electronically as pdfs for global distribution. Bound hardcopies, sent my mail, to different libraries & institutions will stop.

0104  Chlorophyll measurement FLog, chlorophyll data logging fluorometer program introduced

Prior to FLog, our 24+hr acetone cold-extracted chlorophyll samples were manually logged by hand to a sample form then key-entered into CODES. FLog records fluorometer values automatically in a data-processing friendly format so no transcription is required.

Jun 2001 Seasave for Windows Seabird releases Windows versions Seasoft/Seasave & SBE Data Processing software for Windows 98/NT  released by Seabird
2000  CTD Fluorometer Seapoint Fluorometer

Seapoint Chlorophyll Fluorometer in use.

9807 (Jul 1998) CTD Seasave Con file readable by Seasave v5 con files prior to 9807 will not open it Windows SBE Data Processing software v5 or v7
9308  Temperature measurement 4sec ave (prior to bottle closure) CTD temperatures replace reversing thermometer measurements

CTD temperatures are the only measurement entering the hydrographic timeseries (until 2011 when CTD standard level temperature, salinity, & oxygen replace interpolated values).

9308  Seabird CTD-Rosette w/ 24-10L Niskin-type PVC Bottles Replace 20 bottle hydro cast & 6 bottle prodo cast

10L Niskin-like bottle constructed by Research support have plastic-coated springs, nylon lanyards, Viton or nitrile o-rings. No metal, rubber, or latex come incontact with seawater samples. Bottles are disassembeld &  ‘productivity-cleaned’ between cruises.

1993  CTD Fluorometer SeaTech Fluorometer

1993-2000

1973  Chlorophyll measurement Began

Discrete chlorophyll analysis was added to the hydrographic dataset.

1961  Nutrient Analysis Expands beyond phosphate

Nutrient analysis expanded to include silicate, nitrate and nitrite.

     

 

 

Primary Productivity Methods

PRIMARY PRODUCTIVITY

 


OVERVIEW: Primary production is estimated from 14C uptake using a simulated in situ technique in which the assimilation of dissolved inorganic carbon by phytoplankton yields a measure of the rate of photosynthetic primary production in the euphotic zone.


 

1. Principle

Seawater samples are incubated with a radioactive substrate to determine the incorporation of inorganic carbon into particulate organic carbon due to photosynthesis at selected light levels.  The data have units of mg-carbon per m3 per half day.

2. Productivity Cleaning Procedures

2.1.

Micro-90 Cleaning solution is diluted to 2% solution using de-ionized water (DW).  Hydrochloric acid (HCl) Trace Metal Grade, Fisher Scientific, solution (1.2M) diluted with DW. Acid-washing of Teflon should be done with great care as Teflon is porous to HCl which can compromise dilute basic stock solutions of 14C -bicarbonate.

2.2.

250 ml polycarbonate incubation bottles are filled to capacity with 2% MICRO for 3 days with the cap on in an inverted position. Next, rinse all Micro away and then rinse down the walls with 20 -30mls 10%HCl and recap and shake  to acid rinse inside bottle.  This should be left overnight 12-16 hours. The acid is removed by rinsing the bottles three times with milliQ clean water before air drying.

2.3.

10 liter rosette sample bottles are cleaned with a 2% MICRO soak for 3 days, rinsed with de-ionized water and then dipped in 10% metals free HCl.  Caps, special coated springs and valve assemblies are also cleaned with a 2% MICRO soak for 3 days and then rinsed with de-ionized water and dried. 

2.4.

All lab ware to be used is cleaned in this manner.

 

3. Preparation  of Isotope Stock

3.1.

To prevent contamination of self or solutions, work with the isotope stock is performed wearing vinyl gloves.

3.2.

A solution of 0.3 g of Na2CO3 anhydrous (ALDRICH 20,442-0, 99.995%) per liter Milli-Q filtered DW in a Micro cleaned 1 liter Teflon bottle to yield a concentration of 2.8 mM Na2CO3.   This solution is filtered through 0.2µM Nucleapore filter to remove particulate carbonate.

3.3.

Concentrated stock, 50ml of NaH-14CO3 (~50-57 mCi mmole; MP Biomedicals LLC.) was diluted with 350 ml the 2.8mM Na2CO3 solution in productivity-cleaned 1 liter polycarbonate graduated cylinder.  It has become necessary to pH this up with an ultra clean 1N NaOH solution to raise the pH to ~10.

3.4.

Specific activity can be checked by diluting the above made solution to working concentrations, ie 50-200µl added to 250ml polycarbonate centrifuge bottle and measuring out triplicate 1ml portions into beta ethanolamine spiked (1.5%v/v) Ecolume scintillation cocktail.

3.5.

 To check for  14C-organic carbon contamination another working aliquot of 200µl can be placed into a scintillation vial and acidified with 0.5ml 10% HCl and placed on a shaker overnight. This is done in the hood as it liberates 14C-CO2. The acidified dpm should be <0.0001% of the total dpm of the 14C preparation.

 

4. Incubation Systems: situ incubation techniques

4.1.

 Incubation apparatus consists of seawater-cooled, temperature monitored incubator tubes wrapped with neutral-density screens which simulate in situ light levels.    

 

 

4.2.

Six incubation depths are selected, they represent 56, 30, 10, 3, 1  and ~0.3 % light level.  These values are estimated using a wand type PAR meter after cleaning tubes and screens covering them.  The near surface light level is reduced to 56% using common plastic screening to prevent a lense effect and subsequent cooking of the surface samples. 

 

5. Sampling

5.1.

Primary productivity samples are taken each day shortly before local apparent noon (LAN).  Light penetration was estimated from the Secchi depth (Using the definition that the 1% light level is three times the Secchi depth).  The depths with ambient light intensities corresponding to light levels simulated by near surface and the on-deck incubators were identified and sampled on the rosette up-cast.  Extra bottles were tripped in addition to the usual 20 levels sampled in the combined rosette-productivity cast in order to maintain the normal sampling depth resolution.

5.2.

 


5.3.

Using a dark sleeve to subdue the light, water samples are transferred to the incubation bottles (250 ml polycarbonate bottles) and stored in a dark box until inoculation. 

 

Triplicate samples (two light and one dark control) were drawn from each productivity sample depth.

 

6. Isotope Addition and Sample Incubation

6.1.

Samples are inoculated with 50-200 µl of 14C as NaHCO3 stock solution of sodium carbonate (Fitzwater et al., 1982).

6.2.

Samples are incubated from LAN to civil twilight in a surface seawater-cooled incubators with neutral-density screens which simulate in situ light levels, corresponding to those from which samples were taken (see 4.2).

6.3.

At civil twilight the incubation is terminated and the time noted.  Sea state and safety is the only exception accepted to delay the end time.

 

7. Filtration

7.1.

At the end of the incubation, all bottles have subsamples of 10mls removed for DO14C analysis. The LTER DOC filtrate apparatus consists of a plexi-glass filtration manifold to hold up to 18 scintillation vials over which syringe needles with 0.45um equivalent micro-syringe filters can be passed through stoppers with 25 ml syringe bodies serving as filter funnels.  The exception to this is dark bottles are only sampled for DO14C on two each high and low chlorophyll stations.

7.2.

Additionally, from dark bottles a 1ml sample is placed into beta mercapto-ethanol spiked (1.5%v/v) Ecolume scintillation cocktail  to determine the specific radioactivity in the samples.   These values are used to calculate an average cruise value after removing outliers.

7.3.

Finally the samples are filtered onto Millipore HA filters and placed in scintillation vials.  One half ml of 10% HCl was added to each sample.  The samples are then allowed to sit, without a cap, at room temperature for at least 3 hours (after Lean and Burnison, 1979).

 

8. 14C Sample Processing

8.1.

After addition of 10mls of Ecolume cocktail, vials are tightly capped and mixed before vials are counted for up to 10 minutes each for 14C  on a Beckman 6100LC liquid scintillation counter set to 1.0% counting precision.

8.2.

Data is captured to a flat file using Beckman data capture software for Windows in ASCII format.  This format is then used to integrate productivity depths into the CalCOFI data processing flow.

 

9. Calculations

Data is presented as mean mg Carbon assimilated per meter cubed of seawater for one half light day. 

mgC/m3 per one half light day =  ((Sampledpm Blankdpm) x W)/R, where

 

   W = 25200 = 12,000 x A  x FT  x 1.05

   12,000= molecular weight of carbon in milligrams

   A = carbonate alkalinity (milliequivalents/liter)

   FT = Total carbon dioxide content/ carbonate alkalinity

   1.05 is the 14C isotope fractionation factor, reflecting preferential use of C12 over C14 by a factor of 5%

   R = dpm added to sample (µCi/200µl x 2.2 x 106)

 

To better understand this equation and variables see Strickland and Parsons (1968).

10. Equipment/Supplies

·         10 liter pri. prod. cleaned sampling bottles

·         Secchi disk

·         Re-pipet dispensers for delivering 20µl, 200µl, 0.5ml

·         Pipets able to measure 1ml and 10ml

·         250 ml polycarbonate centrifuge bottles

·         liquid scintillation counting (LSC) vials

·         Seawater plumbed incubation rack with neutral density screening.

·         Par meter, wand type (Biospherical Instruments)

·          14C sodium bicarbonate stock solution (MP Biomedicals, LLC)

·         Millipore Type HA filters (Fisher Scientific)

·         vacuum filtration system including separate device for DOC filtrate capture

·         Polycarbonate centrifuge bottles

·         Teflon laboratory wares

·         vortex mixer

·         liquid scintillation counter (LS 6000LC Beckman Instruments, Inc.)

11. Reagents

·         Milli-Q filtration/anion exchange water purifier

·         Micro-90 Cleaning solution, Cole Palmer Instrument Co.

·         HCl for trace metal analysis (Fisher Chemical)

·         Na2CO3 (99.995%) Aldrich Chemical

·         NaH-14CO3 solution (cat #17441H MP Biomedicals, LLC.)

·         2-amino ethanol (ethanolamine)  ACS grade

·         Aquasol-II (Dupont)

·         Ecolume (MP Biomedicals, LLC.)

 

12. Re-count check

14C scintillation counts were checked for accuracy by re-counting an entire cruise (n>200) of vials 9 months after original counting.  Depletion due to half life was ignored due to the long half life of 14C.  Results for samples greater than 1000dpms were averaged resulting in a return of counts equal to 101.3%.  Efficiencies had a similar recount statistic of 100.9%.  The exercise lead to evaluating cruise counts where the source of some replicate inconsistency was the result of chemiluminescence problems in which the counter displays a “lumex %”. It is important to monitor for higher lumex numbers which result in elevated counts due to a chemiluminescent reaction. Samples were dark adapted and recounted resulting in much better replicates.

13. References

 

·         Fitzwater, S. E., G. A. Knauer and J. H. Martin, 1982.  Metal contamination and its effect on primary production measurements.  Limnol. Oceanogr., 27: 544-551.

·         Lean, D. R. S. and B. K. Burnison, 1979.  An evaluation of errors in the 14C method of primary production measurement.  Limnol. Oceanogr., 24: 917-928.

·         Steeman-Nielsen, E. (1951). “Measurement of production of organic matter in sea by means of carbon-14”. Nature 267: 684–685.

·         Strickland, J. D. H. and Parsons, T. R. 1968.  A Practical Handbook of Seawater Analysis pp. 267-278.