Allan Phipps: Fish heads, fish heads, rolly polly fish heads…. July 31, 2012

NOAA Teacher at Sea
Allan Phipps
Aboard NOAA Ship Oscar Dyson
July 23 – August 11, 2012

Mission: Alaskan Pollock Mid-water Acoustic Survey
Geographical Area: Bering Sea
Date: July 31, 2012

Location Data
Latitude: N 61°39’29″
Longitude: W 117°55’90″
Ship speed: 11.7 knots (13.5mph)

Weather Data from the Bridge
Wind Speed: 26 knots (30mph)
Wind Direction: 044°
Wave Height: 4 meters (12 ft)
Surface Water Temperature: 8.2°C ( 46.8°F)
Air Temperature: 7.4°C (45°F)
Barometric Pressure: 994 millibar (0.98 atm)

Science and Technology Log:

Last blog, we learned about the different trawl nets and how the NOAA scientists are comparing those nets while conducting the mid-water acoustic pollock survey.  We left off with the fish being released from the codend onto the lift table and entering the fish lab.  Here is where the biological data is collected.

Walleye pollock on the sorting table. Various age groups are seen here, including one that is 70cm long and may be over 12 years old! Most are 2 to 4 year olds.

The fish lab is where the catch is sorted, weighed, counted, measured, sexed, and biological samples such as the otoliths, or earbones,  are taken (more about otoliths later in this post).  First, the fish come down a conveyor belt where they are sorted by species (see video above).  Typically, the most numerous species (in our case pollock) stay on the conveyor and any other species (jellyfish and/or herring, but sometimes a salmon or two, or maybe even something unique like a lumpsucker!), are put into separate baskets to weigh and include in the inventory count.  In the commercial fishing industry, these species would be considered bycatch, but since we are doing an inventory survey, we document all species caught.  Here are some pictures of others species caught and included in the midwater survey.

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The goal of each trawl is to randomly select a sample of 300 pollock to measure as a good representation of the population (remember your statistics!  Larger sample sizes will give you a better approximation of the real population).  If more than 300 pollock are caught, the remainder are weighed in baskets and quickly sent back to sea.  All of the catch is weighed so the scientists can use the length and gender data taken from the sample to extrapolate for the entire catch.  This data is combined with the acoustics data to estimate the size of the entire fishery (more on acoustic data in a future post). Weights are entered via touch screen into a program (Catch Logger for Acoustic Midwater Surveys – CLAMS) developed by the NOAA scientists onboard.

The CLAMS display showing that I am “today’s scientist.”

The 300 pollock are sexed to determine the male/female ratio of this randomly selected portion of the population.  Gender is determined by making an incision along the ventral side from posterior to anterior beginning near the vent.  This exposes the internal organs so that either ovaries or testes can be seen.  Sometimes determining gender is tricky since the gonads look very different as fish pass through pre-spawning, spawning, or post-spawning stages.  When we determine gender, the fish are put into two separate hoppers, the one for females is labeled “Sheilas” and the hopper for males is labeled “Blokes.”

Making incision to determine gender on pollock sample.

Hopper for female pollock ready to be measured with the Ichthystick and entered into CLAMS.

We use an Ichthystick to then measure the males and females separately to collect length data for this randomly selected sample.  Designed by NOAA Scientists Rick and Kresimir, the Ichthystick very quickly measures lengths by using a magnet placed at the fork of the fish’s tail (when measuring fork-length).  This sends a signal to the computer to record the individual fish’s length data immediately into a spreadsheet and the software creates a population length distribution histogram in real-time as you enter data.

The Ichthystick with fingertip magnet used to quickly measure and enter length data into CLAMS.

A randomly selected subset of 40 pollock get individually weighed, length measured, sexed, evaluated for gonadal maturity and have the otoliths removed.  Otoliths (oto = ear, lithos = bone) are calciferous bony structures in the fish’s inner ear.  These are used to determine age when examined via cross-section under a dissecting scope.  The number of rings corresponds to the age of the pollock, similar to rings seen in trees. The otoliths are taken by holding the fish at the operculum and making an incision across the top of the head to expose the brain and utricle of the inner ear.  The otolith is found inside the utricle.  Forceps are used to extract the otoliths, which are then washed and put in individual bar-coded vials with glycerol-thymol solution to preserve them for analysis back at the Alaska Fisheries Science Center.

Incision across the skull revealing the otoliths on either side of the brain stem.

One otolith from a Walleye pollock.

Watch this short video to see what the entire process of data collection looks like.

So… why collect all of this data?  How is this data analyzed and used?  Stay tuned to my next blog!

Personal Log:

Well, I can officially say… the honeymoon is over.  The Bering Sea had been so extremely kind to us with several days of great weather while we had a high pressure system over us.  We enjoyed spectacular sunrises and sunsets, cloudless days and calm seas.

Sunny skies and calm seas on the Oscar Dyson.

Now… we have a low pressure system on top of us.  Last night, we experienced 35 knot winds and 12 foot seas.  I have spent a lot of time in my room in the past 24  hours…  Late this morning, the sun came out and the winds calmed down, but the barometric pressure was still very low (around 990 mbars) which basically meant we were in the center of the low pressure system (similar to the eye of a hurricane, but not as strong… thank goodness!).  We had a few hours relief, but we are back to pounding through the waves as the wind picks back up.  It will be another long and sleepless night for this landlubber…

On a positive note, we did see two Laysan Albatrosses (Phoebastria immutabilis) from the Bridge as the winds began to kick up.  They seemed to really enjoy the high winds as they soared effortlessly around the ship.  The Officer on Deck (OOD) also said he saw a humpback breaching, but by the time I got up to the Bridge, it had moved on…

Next blog, I will share pictures of my room, the galley, “the cave,” the Bridge, etc.  Right now, I am just trying to hold on to my mattress and my stomach…

Jessie Soder: Steamin’ and Swimmin’, August 10, 2011

NOAA Teacher at Sea
Jessie Soder
Aboard NOAA Ship Delaware II
August 8 – 19, 2011 

Mission: Atlantic Surfclam and Ocean Quahog Survey
Geographical Area of Cruise:  Northern Atlantic
Date: Wednesday, August 10, 2011 

Weather Data
Time:  16:00
Location:  40°41.716N, 67°36.233W
Air temp: 20.6° C (69° F)
Water temp: 17° C (63° F)
Wind direction: West
Wind speed: 11 knots
Sea wave height: 3 feet
Sea swell:  5-6 feet 

Science and Technology Log

View from the flying bridge departing Woods Hole

Our departure from Woods Hole has been delayed a number of times due to several factors.  We were scheduled to leave the dock on Monday at 2pm, but due to rough seas (8ft on Georges Bank—which was where we were planning to go first) and a crane that needed to be fixed our departure was rescheduled for Tuesday at 10am.  On Tuesday, the crane was fixed, but then it was discovered that the ship’s engineering alarm system was not working properly, so our departure was delayed again for a few hours.  The crew worked hard to get the ship off the dock and we departed at 1:15 on Tuesday.  Yay!  We were on our way to Georges Bank, which was about a 15 hour “steam,” or, trip.

The purpose of the NOAA Fisheries Atlantic surfclam and ocean quahog survey is to determine and keep track of the population of both species.  This particular survey is done every three years.  NOAA Fisheries surveys other species too, such as ground fish (cod, haddock, pollock, fluke), sea scallops, and northern shrimp.  These species are surveyed more often—usually a couple of times each year.  Atlantic surfclams and ocean quahogs are surveyed less often than other fished species because they do not grow as fast as other species.  In fact, the ocean quahog can live for more than 150 years, but it only reaches about 6  inches across!  In comparison, the sea scallop lives for only 10 to 15 years and reaches a size of 8 inches.

There are 27 people on board this cruise.  Each person is assigned a watch, or shift, so that there are people working 24 hours a day. The work never stops!  Seventeen people on board are members of the crew that are responsible for the operation and navigation of the ship, machinery operation and upkeep (crane, dredge, etc.), food preparation, general maintenance, and electronics operations and repair.  There are a lot of things that need to happen to make things on a research ship run smoothly in order for the scientific work to happen!

NOAA Ship Delaware II docked in Woods Hole

Twelve people on board are part of the science team, including me, who collect the samples and record the data.  We are split into two watches, the noon-midnight watch and the midnight-noon watch.  We sort through the material in the dredge for the clams and the quahogs.  We measure and weigh them as well as document the location where they are collected.  Several members of the science team are volunteers.

Personal Log

A swimming beach near Nobska Lighthouse

Our delayed departure has given me a lot of time to talk to crew and to explore Woods Hole—which I have really enjoyed.  I have learned a lot about the responsibilities of the different members of the crew and about the maritime industry, which is something that has always interested me.  I was also able to visit the Woods Hole aquarium (twice!) and attend a talk given by crew from the R/V Knorr. The Woods Hole Oceanographic Institute operates the R/V Knorr and it was on this ship that the location of the wreck of the Titanic was located for the first time in 1985.  Additionally,  in 1977 scientists aboard this ship discovered  hydrothermal vents  on the ocean floor.  And, lastly, I had time to go swimming in the Atlantic Ocean!  The water was a bit warmer off the coast of Massachusetts than it is off the coast of Alaska…

Questions to Ponder

What is the difference between an ocean quahog and an Atlantic surfclam?