Turbulence and Mixing Estimates Using a Towed Horizontal microstructure Profiler

Paul Macoun: Turbulence and Mixing Estimates Using a Towed Horizontal microstructure Profiler

Turbulence and mixing estimates using a towed horizontal microstructure profiler.
Paul Macoun

The Ocean Turbulence Laboratory

University of Victoria

The Purpose

Mixing is the key element in the redistribution of salt, heat and energy in the ocean. Understanding the mechanisms and magnitude of turbulence and other mixing processes is crucial to the improvement of models that predict oceanic and atmospheric change. Our elusive goal is the parameterization of the vertical fluxes of salt and heat based upon the physics of oceanic mixing processes.

The horizontal profiler TOMI (Towed Ocean Microstructure Instrument) is used to make simultaneous measurements of temperature, conductivity, vertical velocity, and their fluctuations. The measurement of vertical velocity provides a means of estimating the rate of dissipation of turbulent kinetic energy. The respective products of instantaneous velocity and temperature, and that of velocity and conductivity, provide a direct measure of the vertical fluxes of heat and salt.

Simultaneous vertical profiles of current and its shear from a ship mounted ADCP (Acoustic Doppler Current Profiler) provide a means to relate the measured fluxes to the Froude Number and the Buoyancy Reynolds Number over a wide range of these parameters. The efficiency of mixing, the ratio of buoyancy-to-kinetic energy production, reaches 0.5 in near coastal regions and is generally much larger than the value of 0.2 assumed to apply to the open ocean.

This analysis is to be the first task to undertake with respect to the data set collected at Race Rocks on August 17th, 2000. At present, the processing is at a preliminary stage.

The Instrument

TOMI is a towed oceanographic vehicle designed to measure turbulence in both shallow and deep water. TOMI can support a multitude of instruments, from sonar to underwater cameras. Its primary oceanographic and electronic sensors are as follows:

1) Four airfoil shear probes and two fast-response thermistors on the nose.

2) A seabird temperature and conductivity sensor adjacent to the nose probes.

3) A seabird temperature and conductivity sensor, and a flowmeter, on the upper mast.

4) A seabird temperature and conductivity sensor, and a flowmeter, on the lower mast.

5) A pressure sensor mounted mid-body, internally.

6) An inertial motion sensor package, internal.

The sample rates for these instruments vary from 64 samples per second up to 512 samples per second. The airfoil shear probe is a unique instrument that measures the cross-stream component of velocity. The force generated by cross-stream flow bends a tiny ceramic bi-morph beam, which generates a voltage that is amplified and recorded. The motion sensor contains accelerometers and gyros. Its presence is required because of low frequency body motion contamination that finds its way into the shear probe signals. By having a record of the vehicle’s behaviour, the probe signals can be decontaminated through processing.

(Photos to be added)

Return to P. Macoun- Oceanographic Research

The Johan Ashuvud Project, 2000

crews-1

Victor David and Satoshi: For two weeks in May and June of 2000, Lester Pearson College graduating students, Victor Rakou, David Mesiha and Satoshi Kimura, and in the last week, Juan Manuel Alva and Martin Kryl, joined the sea gulls and stayed at Race Rocks running daily programs on a live camera, and broadcasting directly to the web. Faculty member Garry Fletcher worked with them for the daily webcasts from the shore and from underwater. Sponsorship for this week came from the Johan Ashuvud memorial fund.

The first big event was the Swiftsure Race Weekend. A camera was set up along with a supporting G4 computer in the top of the light tower. Two streams were broadcast, one to camera 4 on the website and a special experimental dedicated stream to Shaw Cable. This stream was of TV quality at 1Mbps and 21 FPS.

Our thanks to Kevin Sytsma of LGS for coming out to help setup for this 2 day broadcast and to Ken Dunham ( PC year 9) for reconfiguring the server from Ottawa in order to handle this experiment.

Each day at Low tide we set up in different locations around the island, always being careful to not disturb the nesting seabirds futher up on land. A Sony camera linked by Firewire to a G3 500 Mghz computer was located in the intertidal zone. From here, Audio and Video Signal went by the wireless Macintosh AirPort Link to the Science Centre. From here the signal traveled by Cat.5 cable to the top of the light tower where it was sent by radio to the Telus antenna at Lester Pearson College. From there it was webcast in live streaming video to the internet by a Macintosh G4 500.

Content through the week ranged from adaptations of organisms to the special ecological niches of tidepools and intertidal slopes, to First Nations use of resources and the role of community/ stakeholder participation in the Marine Protected Areas Pilot process.

The airport wireless base station was tried in a number of locations. We relied on David to find the best locations for connectivity. Best wireless transmission was achieved when we hoisted it up to the roof of the science house. The radio waves go through buildings but not through rocks!

Further editing for the video archives took place in the science centre in the evenings.

Video created this week by the team:

june92000s jochensealions newgulls wwfgulls
Underwater Invertebrates and Fish On the last day of live webcasting, sea lions visited Glaucous-winged gull behaviour Gull territorial aggression

Chris Blondeau from Lester Pearson College joined us for a session on the care and maintenance of the underwater camera and housing. Chris is in charge of the shore-front at the college and is in charge of the SCUBA Diving program there.

We were also fortunate to have some visitors take part in the intertidal discussions we had on the islands. Dr. Jochen Kuum ( PC year 10) is seen here with Garry and diving with Satoshi and Victor Stephen Haggarty (PC year19) also participated above and below water. This video was made on the last dive

 

Carol Slater, who along with her husband Mike are the guardians of the MPA joined us to talk about the Black Oyster Catcher. We examined the trays of shells from last years midden of one nest. This parent bird was foraging off to the East of the dock where they hatched two chicks this year

Race Rocks viewed from the South at Rosedale Rocks Buoy.

One of the best parts in staying at Race Rocks overnight while doing these webcasts was the great sunsets. Sometimes you can view these on the remote control camera 1 and camera 5.

 

Live Transmission to the Internet from Underwater-2000

n June 2000, Lester B. Pearson College divers stayed at Race Rocks for two weeks, for the Johan Ashuvud Week doing live underwater transmissions to the internet. This video is a sample of scenes from the live webcast. It shows some of the colourful invertebrate life at 8 meters depth, on the north side of Great Race.

See https://www.racerocks.ca/the-johan-ashuvud-project-2000/

Webcasting from Race Rocks for the Johan Ashuvud Project week in 2000.

For two weeks in May and June of 2000, Lester Pearson College graduating students, Victor Rakou, David Mesiha and Satoshi Kimura, and in the last week, Juan Manuel Alva and Martin Kryl, joined the sea gulls and stayed at Race Rocks running daily programs on a live camera, and broadcasting directly to the web. Faculty member Garry Fletcher worked with them for the daily webcasts from the shore and from underwater. Sponsorship for this week came from the Johan Ashuvud memorial fund.

Pictures toFiollow

Tidepool # 8 at Race Rocks

Pool # 8 is the small pool just visible at the bottom of this picture.

This pool is one of the most highly elevated pools in the peg six area of Race Rocks. It has a south-westerly aspect, is relatively shallow (its maximum depth being nine cms). It is also fairly small, having an area of just 0.36 square metres, and a perimeter of 0.39 metres.

At certain times of the year, pool # eight is literally packed with life! Within its confines we were able to locate filamentous diatoms (a brown-gold, highly productive microscopic organism), small barnacles, and red harpacticoids..

On the day of our observations (in late April 2000) we found that the surface temperature was 13.5 degrees Celsius and a temperature at the deepest point 11.0 degrees Celsius. At 5cm, we recorded a temperature of 12.0cm. This is what we would have expected, because the temperature is affected by the heating effect of the sun, and the water forms stratified layers of temperature. These temperatures will vary with the season and time of day. In this relatively small pool, one would expect a large temperature range which will create a large variation in the life-cycles within the pool, changing as the seasons change. For organisms with a longer life-cycle, it will be necessary to have the ability to adapt to a high temperature range.

As temperature decreased as the pool became deeper, we observed the opposite effect with regard to salininty. At the surface, for example, a salinity of 13.5 parts per thousand was recorded, and at the depths, a salinity of 16.5 parts per thousand was found. This is fairly typical of a small, brackish pool in the inter-tidal zone. This is another example of stratification and this variation creates differences in productivity and affect. So we could day that this small pool on this particular day had both a halocline and a thermocline.

(Adapted from a student’s lab write up, 2000)

Some ideas to consider:

Tidepools 7and 8 are very close together, varying only a few cm in elevation. The salinity and temperatures of the pools may vary however. It might be worthwhile to document these variations and propose some explanations for the variation.

The Ecological Niche of Anthopleura elegantissima at Race Rocks”

“The Ecological Niche of
Anthopleura elegantissima at Race Rocks”
by: Santiago Salinas
Candidate number:
0034 – 119
Subject:
Biology   Best Language Spanish

Student , Lester B. Pearson College of the Pacific
Submitted as partial fulfillment for the International Baccalaureate diploma program, January 2000

 

Abstract
 

As with any other species at Race Rocks, Anthopleura elegantissima is an important member of the ecosystem to which it belongs. By knowing its ecological niche, trends can be analyzed, niche overlapping or other predictions may be made, particularly, for example, if new species are introduced.

The field work consisted of taking three variables (elevation, rock temperature and time underwater) and testing them against number of organisms. Three different populations were selected and a transect containing subsequent quadrats for each was used (a Mann-Whitney test was performed to determine whether or not there is a general trend between the three populations). The variables were selected because they are known to be influential in the determination of the distribution of species. Since the field work took place during only one day due to the limiting factor of low tide level, a good and thorough design was created. The priorities were the elevation of the terrain and the number of organisms per quadrat in view of the fact that the tidal level was constantly altering, making the measurements inaccurate otherwise. The rock temperature was taken once these two sets of values had been gathered from the three locations.

?Since the statistical device suggested that the three populations are organized in the same way, a general description of the ecological niche was given. The species prefer a temperature range of 11-13ƒ C, the ideal elevation span goes from 1.5 to 2.8 meters, thus, it is an inter tidal species, and finally, the preferable time underwater was found to be 5 to 15 hours.

____________________________________________________________

Table of Contents
Introduction

?The Problem ………..?………….9 ?

?Purpose and Background of the Study………9

?Hypothesis …………………………….…..9

?Assumptions …………………………..…..1

?Limitations …………………………….….10

?Definition of Terms ………………………11

Review of Literature and Related Research

?Introduction, Information about the Organism …..13

?The Theory ………………………………….15

?Research Results in Related Areas ……16

Research Design and Procedures

?The Setting and Population of the Stud…18

?Field Work …………………19?

Instruments…………………………21

?Statistical Techniques Used ………22

Analysis of Data

?

Introduction …………………………………….23

?Findings ………………………………………23

Conclusions and Recommendations for Further Study

?

Interpretation and Implications of the Findings……………40

?Recommendations …………………………….42

Appendix

Bibliography

Table of Figures and Tables
Figures

Figure 1. Topographic representation of Race Rocks…….12

Figure 2. Representation of Anthopleura elegantissima and Anthopleura xanthogrammica …………………..14

Figure 3. Location of Populations at Race Rocks…18

Figure 4. Tidal Height graph ………………………. …23

Figure 5. Terrain Gradient graph (Population 1) ……25

Figure 6. Abundance graph (Population 1) …………..26

Figure 7. Elevation against # of Organisms graph (Population 1.27

Figure 8. % of Organisms at different Temperatures graph (Population 1) ……..28

Figure 9. Terrain Gradient graph (Population 2) …30

Figure 10. Abundance graph (Population 2)………31

Figure 11. Elevation against # of Organisms graph (Population 2) 32

Figure 12. % of Organisms at different Temperatures graph (Population 2) ……33

Figure 13. Terrain Gradient graph (Population 3) …….35

Figure 14. Abundance graph (Population 3) ……………36

Figure 15. Elevation against # of Organisms graph (Population 3)…37

Figure 16. % of Organisms at different Temperatures graph (Population 3) ……………………38

Figure 17. Elevation, Temperature and # of Organisms graph (Population 1) …………………40

?Figure 18. Elevation, Temperature and # of Organisms graph (Population 2) …………………41

Figure 19. Elevation, Temperature and # of Organisms graph (Population 3) ………………….42

Tables

Table 1. Data Collection for Population 1 ………24

Table 2. Data Collection for Population 2 ………29

Table 3. Data Collection for Population 3…………34

Acknowledgments
?I would like to express my sincere gratitude to Guillermo Montero and Garry Fletcher for immersing me in the fascinating world of ecology, and also for the support and direction that they provided me. I am also grateful to Sylvia Roach for her invaluable contribution not only to this work but for her constant encouragement.

?Finally, I would like to thank all the organisms at Race Rocks, especially Anthopleura elegantissima, for their patience and understanding of my investigations and for not complaining from my sometimes careless techniques.

Introduction

The Problem: Anthopleura elegantissima (common name: aggregating anemone) plays, along with all other biotic and abiotic components, an important role in the ecosystem to which it belongs. It is a highly valuable member of many food webs and participates in symbiotic relationships with other species. Taking this information into account, it would be useful to know facts about A. elegantissima in order to be able to predict and analyze trends in the ecosystem so as to gain an insightful knowledge about the species and its relation to the ecosystem found at Race Rocks.

Purpose and Background of the Study: To achieve the goals presented, a wide range of proposals were identified, leading to the decision to investigate the ecological niche as a focused and clear plan. The final design involved testing three populations at different locations of the island with the purpose of determining the preferred range of abiotic conditions for A. elegantissima. Four very significant variables were examined, all of them intimately related with intertidal zonation. These four variables were: the slope of the gradient, the tidal height, the time covered by sea water and the rock temperature. Carrying out the field work in three different sites allowed room for generalized conclusions about the species to be made.

Hypothesis: A null hypothesis for the Mann-Whitney test was formulated: “the three different locations are not inter-related and the similarities that may occur are merely coincidental.” If rejected, some conjectures about the species had to be formed. Given that Anthopleura elegantissima is a low inter tidal species, its range of positioning would not be between 1 to 3 meters. A hypothesis was made based on the fact that sea water is generally at about 10ƒ C, thus the rock temperature was not expected to be similar to this.

Assumptions: One of the major assumptions made was that the tide tables for Victoria, British Columbia, Canada are the same as these for Race Rocks. In theory this may not be true since Race Rocks is located approximately 10 km. away from Victoria. Therefore, there might exist a slight difference in tidal heights between the two zones.

Limitations: The entire experiment and data collection was done on the 27th of October, 1999, due to the limiting factor of relative low tides occurring in day-light hours. Hence the experiment could not be repeated on another day. Therefore, the research reveals the ecological niche of Anthopleura elegantissima at a fixed point in time and not the variations or changes in its distribution over a period of time. Furthermore, based on these results, the general ecological niche of the species cannot be concluded since all the data was gathered in a specific place, Race Rocks, which is a distinct site due to its location.

Another major limitation is that the “ecological niche” is an abstract term and therefore, the ecological niche of a species can never be fully represented. What was done in this case was to narrow the aspects to be considered and try to work with them by relating each factor to the others to acquire an approximation of the ecological niche. In this essay, four abiotic components were measured in order to obtain an insight to the ecological niche of Anthopleura elegantissima.

Definition of Terms: A number of terms should be defined at this point in order to ensure a clear understanding of this essay. One of these terms is population, which is defined as: all members of a species living in a particular area and making up one breeding group (Kucera, 1978). This is of particular importance since a similar species, Anthopleura xanthogrammica, may be found on the island, a phenomenon which would cause some distortions in the results if they are counted as Anthopleura elegantissima. Tides – the gravitational effects of the sun and moon on the oceans of the earth – are also a fundamental pivot in intertidal life. Tides along the Pacific coast of North America are of the mixed semidiurnal type; that is, there is a pronounced difference between the levels to which two successive low tides fall, and a lesser, but still apparent, difference between the levels reached by two successive high tides (Carefoot, 1977). Lastly, the most important term to be defined is ecological niche. The niche of a population or species is its functional role in an ecosystem. Using a human analogy, the niche is the species’ profession or way of life whereas the habitat is where this way of life is carried on — its address. The way a population responds to the various characteristics of its habitat is part of this population’s way of life and, therefore, of its niche. Hutchinson was the first to formally quantify the niche concept in terms of geometric space. The level of activity describes the ability of the individual to exploit the resources in a given level of each environmental factor (Odum, 1963). Then the niche space occupied by the species is the 3-dimensional space actually occupied by all individuals (Rickleffs, 1996). An empirical model (Box and Draper, 1989) can be obtained by the empirical determination of niche occupancy (number of individuals, in this case) in terms of n environmental variables (slope, tidal height, time covered and rock temperature).

Review of Literature and Related Research

Introduction, Information about the Organism: The field work was conducted at Race Rocks, Southern Vancouver Island, British Columbia, Canada. This area was chosen for ecological reserve status because of its unique richness and diversity of marine life. Race Rocks is ideally located to receive a constant supply of plankton swept past by almost continuous strong currents (up to 7 knots) . This provides nourishment for a complex group of underwater organisms.

Figure 1. This image is a view from the South of Race Rocks looking Northward. Colors toward the blue scale are representing depths of almost 100 meters. (3d capture of entire area from south – 1x magnification – 3 x vertical exaggeration).

One of the many organisms found at Race Rocks are sea anemones. Sea anemones belong to the phylum known as the Cnidaria, from the cnida or stinging cells that are present in this major group of animals that also include corals, jellyfish, hydroids, medusae, and sea fans. Sea anemones, corals and their allies form the class know as the Anthozoa. Anthopleura elegantissima (Phylum Cnidaria, Class Anthozoa, Subclass Zoantharia, Order Actiniatia, Family Actiniidae) is abundant on rock faces or boulders, in tide pools or crevices, on wharf pilings, singly or in dense aggregations (Smith and Carlton, 1975). It is a species characteristic of middle intertidal zone of semi protected rocky shores of both bays and outer coast from Alaska to Baja California. Aggregating individuals do not exceed 6 centimeters in column diameter and 8 centimeters across the tentacular crown. The column is light green to white, and twice as long as wide when extended, with longitudinal rows of adhesive tubercles (verrucae) often bearing attached debris (Carefoot, 1977). The species presents numerous short tentacles, in five or more cycles, which are variously colored. Anthopleura elegantissima reproduces both sexually and asexually. In sexual reproduction, ova are present as early as February and grow steadily until their release in July; the ovarian is then resorbed and new eggs do not appear until the following February. Sperm are released through the summer. The asexual reproduction occurs by longitudinal fission. This process results in aggregations or clones of anemones pressed together in concentrations of several hundred per square meter. Anthopleura elegantissima feeds on copepods, isopods, amphipods, and other small animals that contact the tentacles. On the other hand, it is preyed upon by the nudibranch Aeolidia papillosa, which usually attacks the column, by the snail Epitonium tinctum, which attacks the tips of the tentacles, and by sea stars such as Dermasterias imbricata that can engulf an entire small anemone. Moreover, in some anemones, small pink amphipods, Allogaussia recondita, make a home in the gastro vascular cavity (Carefoot, 1977).

Figure 2. Schematic representation of Anthopleura elegantissima and Anthopleura xanthogrammica, the two major sea anemones found at Race Rocks.

The theory: In 1957, G. E. Hutchinson defined the niche concept formally. One could describe the activity range along every dimension of the environment. Physical and chemical factors such as temperature, humidity, salinity, and oxygen concentration, as well as biological factors such as prey species and resting background against which an individual may escape of predators, could be determined. Each of these dimensions could be thought of as one of the n-dimensions in space. Visualizing a space with more than three dimensions is difficult, thus the concept of the n-dimensional niche is an abstraction. We may, however, deal with multi-dimensional concepts mathematically and statistically, depicting their essence by physical or graphical representations in three or fewer dimensions. Moreover, Ricklefs notes that “… for example, a graph relating biological activity to a single environmental gradient represents the distribution of a species’ activity along one niche dimension. The level of activity, whether oxygen metabolism as a function of temperature or consumption rate as function of prey size, conveys the ability of an individual to exploit resources in a particular part of the niche space and, conversely, the degree to which the environment can support the population of that species. In two dimensions the individuals niche may be depicted as a hill with contours representing the various levels of biological activity. In three dimensions, we must think of a cloud in space whose density conveys niche utilization. Beyond three the mind boggles.”

(Ed note: See exercise on Ecological niche)

To be more precise, it should be recognized that there are three different definitions for the term niche. The first one (also known as “niche as community function”) comes from Elton (1927) defining it as the animal’s place in the biotic environment, its relation to food and enemies. The second definition is called “niche in the species” and reveals that a specific set of capabilities for extracting resources, for surviving hazard, and for competing, coupled with a corresponding set of needs (Colinvaux, 1982). The most used and known is the one defined by Hutchinson, which was explained previously. 

Research Results in Related Areas: Even though only one research paper was found containing information about Anthopleura elegantissima at Race Rocks, many investigations have been carried out with Anthopleura elegantissima and its physiology. The paper obtained on Anthopleura elegantissima at Race Rocks (Zahid, 1987) tries to detail the distribution of the species in one crack by two statistical methods (Plotless and Poisson techniques). It is concluded that A. elegantissima is an intertidal organism showing a clumped distribution. The clonal form, being lower mid-intertidal is exposed to sunlight and air much more than the solitary form in the sub-tidal zone. Hence, the clumped distribution is very useful and is also an important factor in reducing desiccation and water loss, as clumping reduces the surface area exposed to light.

Research Design and Procedures

The Setting and Population of the Study: The field work was designed to take place in three different locations of Race Rocks (see Figure 4), in order to gain a more detailed examination of the ecological niche of Anthopleura elegantissima in this island. Another reason for doing so was well explained by Odum: “It is also true that the same species may function differently —that is, occupy different niches- in different habitats or geographical regions.” The three places exhibit different environmental conditions and, therefore, the species may experience changes in its distribution. These changes could be current flow (which is in and of itself a major contributor to tidal life), light exposure, and even different rock composition.

A hazardous inconvenience that had to be overcome before doing the field work was to be able to distinguish among the two major types of sea anemones at Race Rocks, Anthopleura elegantissima and Anthopleura xanthogrammica. In order to achieve this, a key book was consulted. In the book, the distinctive characteristics between the two are described (see Appendix.)

 
Figure 3. Hand-made representation of Race Rocks showing the location of the three populations, the lighthouse and the docks.

Field Work: The complete field work took place on the 27th of October, 1999 due to the limiting factor of low tide level. The priorities were the elevation of the terrain and the number of organisms per quadrat in view of the fact that the tidal level was constantly altering, making the measurements inaccurate otherwise. The rock temperature was taken once these two sets of values had been gathered from the three locations. For the sake of help, a line transect was set in each crack to make the data collection uncomplicated and feasible.

Elevation: With the aim of measuring the elevation of the terrain for each population, a rudimentary, home-made apparatus was created. Due to the fact that the topography of the shore is extremely irregular at Race Rocks, it is not possible to assume that the elevation is a straight line. Thus, to have a detailed insight of Anthopleura elegantissima —or any other intertidal organism- at Race Rocks, an imperative factor to be considered is elevation. To approach this, the first action taken was to delimit the transect (generally a straight line along which observations are made in a systematic fashion) and the quadrats (starting from where the tidal level equals 0 meter). Since there was not a zero meter tide predicted, it was decided to start at 0945 approximately —tidal height equal to 2- and calculate the zero tide level. To accomplish the task, a two meter stick was used perpendicular to the sea water since tidal height is a vertical measure of water. Following this, a 4 meter stick was put where the tidal level equals 0 meter -quadrat number 15- (perpendicular to the sea water) and, with the help of a rope, a triangle was formed between the stick, the rope and the last quadrat —number 1. Once the triangle was finished, the elevation existing between quadrat number 1 and number 15 is known by the distance in the stick from the land to the conjuncture of it and the rope (for example, 3.9 in the first population). The subsequent measurements were much easier to carry since only a meter stick and a measuring tape were needed. Starting from quadrat number 1, a meter was measured with the measuring tape along the land. Then, the meter stick was put in such a manner that it formed a 90ƒ angle with the top of the quadrat, giving a number (0.3 in the first population). Therefore, 3.1 minus 0.3 equals 2.6, the elevation for quadrat number 2). So on and so forth the procedure was repeated until quadrat number 15 was reached.

Number of organisms: A very important feature involving the number of organisms per quadrat is the quadrat’s size. It was proven by Grey-Smith (1952) that the size of a quadrat could actually determine some erroneous conclusions in a population by using a series of progressively larger quadrats to measure the distribution in an artificial situation in which individuals were represented by colored disks. A reasonably good size for the quadrats was estimated to be 0.5 by 0.5 meters, given personal observation. Once the quadrats were sorted out, the counting took place. Only if more than 75 % of the organism was inside the quadrat was it counted. A difficult aspect of the counting was to differentiate individuals from the same group clone or aggregation. This difficulty was expected since the clones are held together very tightly and because at this time of the year young anemones are developing their bodies (as fertilization occurs during summer).

Rock temperature: This process was relatively simple compared to the previous two. It consisted of using the thermometer in small crevices in rocks —for each quadrat- in order to get the rock temperature.

?Time underwater: Aided by the tide table for the day (starting at 0500 and finishing at 2300), it is possible to calculate how much time a certain elevation is exposed to sea water. Assume that it is desirable to know the underwater time of a quadrat at 2.5. Then, we trace a line at 2.5 and the area under the curve will indicate the time that quadrat was covered by water.

Instruments Used: A simple technological apparatus was used for the field work. A measuring tape, a meter stick, a four meter stick, the tide tables for Victoria, BC, a thermometer, and a rope were all the required instruments.

Statistical Techniques Used: The technique used to verify that the distribution of the species was not random or by chance was the Mann-Whitney test. This non-parametric tool (meaning there are no specific distributional assumptions required) is sometimes called Wilcoxon test or rank sum test. This test relies on a special kind of transformation that replaces each observation by its rank in the combined sample. The purpose of this is to transform the data to a scale that eliminates the importance of the population distribution altogether (Ramsey and Schafer, 1997). In order to make it easier and more accurate, a web-page (VassarStats) was utilized to perform the calculations and the statistics values.

 

Analysis of Data

Introduction: The data will be presented by population and not by factor. This is aimed to help the understanding of the ecological niche of Anthopleura elegantissima at Race Rocks in a detailed and comprehensible fashion. Three separate populations were examined on different parts of the island The populations are numbered (1, 2 and 3) referring to a certain strip (see Figure 4.)

Findings: The Mann-Whitney test was used to determine whether or not there is a general trend between the three populations. Two populations were tested at a time, therefore, three runs of the test were conducted using the number of organisms as the variable to be ranked. Using VassarStats, an U value was calculated: 140.5 for populations 1 and 2, 96.5 for populations 1 and 3, and 44 for populations 2 and 3. These U values were then checked in the significance levels table:

n
5 per cent
1 per cent
15
185
170

 

By this, it is possible to conclude that, although it is impossible to be absolutely certain that the different is not due to chance, the probability is sufficiently small for it to be considered negligible. Thus, the null hypothesis can be rejected and assume that there are similarities among the three populations. Bearing that in mind, the variables should now be tested to determine the ecological niche of Anthopleura elegantissima at Race Rocks.

?Tidal Height:

Figure 4.

The variations of the tidal height of the day are normal and reflect the constant water movement that take place in the ocean affecting inter tidal life. Based on this chart, the underwater time will be calculated. Note that the chart begins at 0500 and ends at 2300 (therefore, total time underwater = 18:00).

Population # 1:

Quadrat #
Elevation (m.)
Rock Temperature (ƒ C)
# of Organisms
Time Underwater
1
3.9
12
0
00:00
2
3.6
12
0
00:00
3
3.7
12
0
00:00
4
3.4
13
5
00:00
5
3.2
12
10
00:00
6
3.0
12
21
00:00
7
2.9
11
32
00:00
8
2.5
12
56
04:30
9
2.4
12
68
05:15
10
2.1
13
55
07:55
11
1.7
13
76
14:10
12
1.2
12
45
15:30
13
0.9
12
25
16:15
14
0.6
12
18
17:05
15
0.0
12
21
18:00
Mean Temp. 12.133

Table 1.
 
Figure 5.

The terrain gradient for population number 1 is the typical slope and is also the most regular among the three. It has a steep drop at the end (quadrat # 15) where it meets the sea water at 0 m. (tidal level). This gradient features some small tide pools and is sometimes covered by kelp beds. By personal observations, I could say that it is the strip with the highest level of species diversity on it.

Figure 6.

Even though this is not the most abundant population (432 individuals), it features the largest number of individuals per quadrat (76) and has an extremely large number of Anthopleura elegantissima at a certain level of the gradient. It should also be noted that no individuals were found in the first three quadrats and there were not many before quadrat 6. The number of organisms was measured in quadrats of 0.25 square meters.

Figure 7.
 

This graph clearly shows the relationship between elevation and number of organisms. It is easy to recognize that the preferred place for Anthopleura elegantissima is around 1.2 to 2.5 meters, a fact that will be very useful when making conjectures about its niche. The drop of abundance at 2.1 is only a local anomaly. At high heights (3.9, 3.6, etc.) there were no organisms present while at low heights there were some (however not very many).

Figure 8. (Note that 1 symbolizes 11ƒ C, 2 symbolizes 12ƒ C, and 3, 13ƒ C)
 

Despite the fact that a correlation could not be found between rock temperature and elevation or tidal height, an important feature was discovered, this being the relationship involving surface rock temperature and abundance. It was discovered that Anthopleura elegantissima prefers a rock temperature of 11, 12 or 13 because of the fact that these were the only temperatures found on the rocks (higher elevations were found to be warmer and A. elegantissima apparently does not favor such conditions).

Population # 2:

Quadrat #
Elevation (m.)
Rock Temperature
(ƒ C)
# of Organisms
Time Underwater
1
3.8
12
0
00:00
2
3.7
13
2
00:00
3
3.4
12
24
00:00
4
3.3
12
33
00:00
5
3.1
12
50
00:00
6
2.8
11
47
00:00
7
2.5
11
58
04:30
8
2.4
11
61
05:15
9
2.1
12
62
07:55
10
1.6
12
46
14:20
11
1.2
12
40
15:30
12
1.3
13
34
15:15
13
0.8
11
26
16:30
14
0.3
12
29
18:00
15
0.0
12
23
18:00
Mean Temp. 11.866

Table 2.
Figure 9.

This gradient features a large tide pool at 1.25 meters level. In it, a whole new ecosystem is found due to different climatic conditions, therefore, it may create some distortions with the number of Anthopleura elegantissima expected. A steep fall at the end should also be noted as a probable cause for the distribution of the species.

Figure 10.

In this population some irregularities are shown. Quadrats 6 and 13, for example, are not quite as expected. The virtual absence of organisms in quadrat 1 and 2 has to be considered as well. Overall, an inverted u-shaped curve could be distinguished.

Figure 11.

Again, the same trend as in population 1 is presented. A major distribution is seen at 2.1 to 2.8 meters and none or very few organisms were found at high elevations. On the other hand, a large number of the species was encountered at very low elevations

 

Figure 12.

These results reinforce the idea that Anthopleura elegantissima prefer a range of temperatures of 11-13ƒ C. No further analysis could be made since it is unlikely that a distinction could be drawn using greater detail such as degree by degree. On the other hand, at temperatures significantly different from the range above, the species will not be found.

?

Population # 3:

Quadrat #
Elevation (m.)
Rock Temperature (ƒ C)
# of Organisms
Time Underwater
1
3.6
13
4
00:00
2
3.3
13
11
00:00
3
3.2
13
20
00:00
4
2.9
12
31
00:00
5
2.7
12
33
00:00
6
2.2
12
25
09:45
7
2.2
11
28
09:45
8
1.9
12
22
13:30
9
1.8
12
16
13:50
10
1.4
11
19
15:00
11
1.0
12
23
16:00
12
0.9
12
15
16:15
13
0.6
12
12
17:05
14
0.4
12
10
17:30
15
0.0
12
10
18:00
Mean Temp. 12.066

Table 3.
Figure 13.
 

This gradient was the most irregular of the three, featuring ups and downs from the first to the last quadrat. A fact that seems rather curious is that on top of this strip sea lions lie down to rest quite frequently whereas this does not happen in the other two strips, probably because this gradient starts from a very plain, big rock. Kelp beds are observed floating on water and algae is seen at higher elevations.

Figure 14.

Although this graph does not show a perfect inverted u form, a general trend is seen. This population is the less abundant of the three and shows some irregularities in the middle quadrats.

Figure 15.

Apparently, more organisms prefer a range of 2.9 to 2.2 meters in this gradient. Some animals were found at 0.0 meters but not many were seen at higher heights. Two major drops, at 2.2 and 1.8 meters, can be explained due to overpopulation of other species in those two tide pools.

Figure 16.

Once again, no other temperature ranges were found, leading to the conclusion that Anthopleura elegantissima does prefer temperatures of 11deg C to 13deg  C.

Conclusions and Recommendations for Further Study

Interpretation and Implications of the Findings: After looking at the graphs, general descriptions of the ecological niche of A. elegantissima could be made:

ideal temperature for the species is a range of 11-13ƒ C because at higher or lower temperatures, the number of organisms decrease significantly. The null hypothesis is then rejected.

 Idyllic elevation goes from 1.5 to 2.8 meters. Once again, the null hypothesis is rejected.

Since time underwater is a function of elevation, it was not considered on graphs. However, the preferable time underwater for Anthopleura elegantissima was found to be 5 to 15 hours approximately (out of 18 hs.)

A clear description of the ecological niche dimensions is observed in the graphs below. The larger bubbles represent the portion of the space that the species prefers:

 

Figure 17

Figure 18
Figure 19.
 

Recommendations: If a thorough understanding of the ecological niche of Anthopleura elegantissima is desired, these and more variables should be tested to obtain a more profound and detailed approximation. Also, by determining ecological niches of other species such as Anthopleura xanthogrammica and comparing them, it is possible to predict niche overlapping, which is very likely to lead to a constant competition and aggressive behavior of the species. Moreover, it could be used to predict changes in the ecosystem if introduced species are brought. The documentation of data like this provides an invaluable record for establishing baseline distributions of organisms. Scientists are often required to monitor anthropogenic changes in sensitive marine environments. Similar niche patterns could be done on the other key invertebrates of the inter tidal and sub-tidal zone at Race Rocks, for example black leather chitons, limpets, abalone and various species of algae.

Appendix
This appendix presents the dichotomous key for Anthopleura elegantissima and Anthopleura xanthogrammica.

“Column green to white; tubercles usually in distinct longitudinal rows; tentacles with pink tips; height up to about 5 cm; often in aggregating masses, and frequently buried by sand covering rocks to which they are attached Anthopleura elegantissima. ~~ Column green or olive green; tubercles usually not in distinct longitudinal rows; tentacles uniform in color and not pink-tipped; height regularly exceeding 5 cm; solitary and not often buried in sand Anthopleura xanthogrammica.”

Boughey, A.S. 1968. “Ecology of populations.” The Macmillan Company, New York.
Buschsbaum, R., Buschsbaum, M., Pearse, J, and Pearse, V. 1987. “Animals without backbones.” University of Chicago Press, Chicago, Illinois.

Carefoot, T. 1977. “Pacific seashores.” J.J. Douglas, Vancouver, BC, Canada.?

Colinvaux, P. 1986. “Ecology.” John Wiley & Sons, United States of America.

Francis, L. 1973. “Clone specific segregation in the sea anemone Anthopleura elegantissima.” Biological bulletin. 144, 64-72.

Francis, L. 1973. “Intraspecific and its effects on the distribution of Anthopleura elegantissima and some related sea anemones.” Biological bulletin. 144, 73-92.

Kozloff, E.N. 1974. “Keys to marine invertebrates of Puget Sound, the San Juan Archipelago, and adjacent regions.” University of Washington Press, Washington State.

Kozloff, E.N. 1993. “Seashore life of the Northern Pacific Coast.” University of Washington Press, Seattle, Washington State.

?Kucera, C. L. 1978. “The challenge of ecology.” The C. V. Mosby Company, Saint Louis.

Lewis, J.P. 1995. “La biosfera y sus ecosistemas: una introducción a la ecología.” Ecosur, Rosario, Argentina.

Odum, E. P. 1963. “Ecology.” Holt, Rinehart and Winston, United State of America.

Odum, E.P. 1989. “Ecology and our endangered life-support systems.” Sinauer, Sunderland, Massachusetts.

Pianka, E. R. 1986. “Ecology and natural history of desert lizards.” Princeton University Press, Princeton, NJ.

Smith, R.I., and Carlton, J.T. 1975. “Intertidal invertebrates of the Central California Coast.” University of California Press, Los Angeles, California.

Zahid, M. 1987. “Distribution of Anthopleura elegantissima.” Extended Essay for the International Baccalaureate.

GO to the Ecological Monitoring Site 

Predation by the Black Oystercatcher….1999

In September of 1999, the students of the Environmental Systems Class collected the shells in the midden surrounding the nest of a pair of Black OysterCatchers at Race Rocks, They analysed the size, species diversity, and species frequency of the shells. The following data and charts are presented in order to provide information about the role of this seabird in the intertidal ecology of Race Rocks.

Numbers of Shells Collected Near Black Oyster Catcher’s Nest
    Limpets: Mask, Shield, and Plate 350    
    Limpets: Whitecap 70    
    Limpets: Fenestrate 19    
    Limpets: Rough Keyhole 2    
    Chitons: Black Katy 73    
    Chitons: Mossy 13    
    Chitons: Lined Red 7    
    California Mussels 342    
    Ribbed Whelk 5    
    Amphisia Snail 1    
         

Average Size of the Oyster Catcher’s Food california mussels –5.2875 cm plate,mask,shield limpets–3 cm whitecap limpets 5.2875 cm 3 cm 2.985 cm Size of Oyster Catcher’s Food: Raw Data, in cm

california mussels plate, mask and shield limpets white cap limpets
3 2 1.7
4 2.2 2.1
4.2 2.5 2.3
4.5 2.8 2.4
4.6 2.8 2.5
4.6 2.8 2.6
4.7 3 2.7
5.2 3 2.8
5.25 3.1 2.9
5.3 3.2 3
5.5 3.4 3.2
5.5 3.4 3.2
5.5 3.5 3.2
5.8 3.5 3.2
6. 3.5 3.3
6.5 3.5 3.6
6.6 3.6 3.7
7.5 3.8 3.8
7.8 3.8 3.8
gfcarolshell

Garry Fletcher and Ecoguardian Carol Slater examining sorted shells of black oystercatcher prey from on midden.

Image1 Image3

ORCA skeleton assembled

This article appeared in the Jnuary 17 , 2002  number 8 issue of the Collge newspaper

It’s a grand jigsaw puzzle – hundreds of bones, huge and tiny, all to be reassembled into the skeleton of a whale. Graduates returning to the June reunion will know the first whale project, and everyone at Pearson since then will know the vast frame of a whale erected behind the swimming pool. The present Orca project is well underway, and, happily for those currently working on it, well past the smelly stage.

Biology teacher Catrin Brown, a team of students, and Han Bauer, the first Biology teacher at Pearson, took the project a stage further this week, examining the skeleton of a porpoise – rather easier to fit into lab space! – in order to understand better the structure of the killer whale. Catrin gives us following explanation.

Catrin’s Explanation

In September 1999, a 27-year-old female killer whale known as L-51 was found dead in the waters off Race Rocks. Her death was presumably the result of a prolapsed uterus from a difficult childbirth a few months before, and fate of her young calf was unknown.

A team of Pearson divers towed the whale ashore, where it was disembowelled and transported back to the college in gorey chunks. Sections of the carcass were then suspended from the college docks, where ocean life feasted on the decaying meat over a period of months. Eventually the clean bones emerged and after a summer of drying and bleaching in the sun, the smell receded and the promise of a skeleton took shape.

At this stage outside help was sought, and found in the person of Hans Bauer, Biology teacher at the founding of the college, who is now retired and living in Sydney, near Victoria. With his good humoured guidance, students tackled the task of removing some of the more tenacious marrow by boiling the large bones in large vats over a fire. Many students have been involved in various stages of this project including Katy Green (year 25), Joao Marquez (year 26), Francoise Guigne (year 27) and Jaffar Saldeh (year 27).

We are now close to the stage of reassembling the bones into a permanent mount for display on campus. As the population of killer whales inhabiting the Juan de Fuca Strait has recently been declared an endangered species, L-51 is likely to be a focal point of interest.

January 17, 2002. number 8.