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U.S-Arm 
Coast Ens. an Ctr. 


MR 78-3 
(AD -A062. OLS) 


Ecological Effects of an Artifical Island, 
Rincon Island, Punta Gorda, California 


by 
G.F. Johnson and L.A. deWit 


MISCELLANEOUS REPORT NO. 78-3 
SEPTEMBER 1978 


WHOT™ 


DOCUMENT 
COLLECTION 


Approved for public release; 
distribution unlimited. 


Prepared for 
U.S. ARMY, CORPS OF ENGINEERS 
COASTAL ENGINEERING 
RESEARCH CENTER 


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as, Fort Belvoir, Va. 22060 


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Contents of this report are not to be used for advertising, 


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commercial products. 


The findings in this report are not to be construed as an official 
Department of the Army position unless so designated by other 


authorized documents. 


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REPORT DOCUMENTATION PAGE sea Se nates 


T. REPORT NUMBER 2. GOVT ACCESSION NO.| 3. RECIPIENT'S CATALOG NUMBER 
MR 78-3 


4. TITLE (and Subtitle) a re = 5. TYPE OF REPORT & PERIOD COVERED 
ECOLOGICAL EFFECTS OF AN ARTIFICIAL ISLAND, 
RINCON ISLAND, PUNTA GORDA, CALIFORNIA Miscellaneous Report 


6. PERFORMING ORG. REPORT NUMBER 


7. AUTHOR(a) B. CONTRACT OR GRANT NUMBER(4) 


G.F. Johnson 
L.A. deWit DACW 72-76-C-0011 


9. PERFORMING-ORGANIZATION NAME AND ADDRESS 10. PROGRAM ELEMENT, PROJECT, TASK 


Dame = & Moore Vas AREA & WORK UNIT NUMBERS 
—Dame 
C _1100.Greendon Avenue G31532 

Los Angeles, California 90024 


11. CONTROLLING OFFICE NAME AND ADDRESS 12. REPORT DATE 

Coastal Engineering Research Center 13. NUMBER OF PAGES 

Kingman Building, Fort Belvoir, Virginia 22060 
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UNCLASSIFIED 


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SCHEDULE 


16. DISTRIBUTION STATEMENT (of thia Report) 


Approved for public release; distribution unlimited. 


17. DISTRIBUTION STATEMENT (of the abstract entered in Block 20, if different from Report) 


18. SUPPLEMENTARY NOTES 


19. KEY WORDS (Continue on reverse side if necessary and identify by block number) 


Artificial island Microecosystem 
Bottom sediment Punta Gorda, California 
Ecological effects Rincon Island 


20. ABSTRACT (Continue om reverse sida if neceasary and identity by block number) ‘ 
This study documents marine ecological conditions at Rincon Island, 


located approximately 0.8 kilometer offshore between Ventura and Santa 
Barbara, California, in a depth of 14 meters. The island, which was con- 
structed between 1957 and 1958 to serve as a permanent platform for oil and 
gas production, is particularly suitable for ecological study. Habitat fea- 
tures associated with the armor rock and concrete tetrapods surrounding the 
island support a "microecosystem' which differs. in biotic composition from 
surrounding natural bottom areas. (continued) 


FORM 
DD . jan 73 1473 —- EDrTIon OF 1 Nov 65 1S OBSOLETE UNCLASSIFIED 


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SECURITY CLASSIFICATION OF THIS PAGE(When Data Entered) 


Major associations of macrobiota (organisms >1 millimeter in size) were 
distinguished on the basis of cooccurrences of conspicuously dominant organ- 
isms. Thirteen major associations, covering various parts of the island 
between the upper intertidal zone and shell debris or natural bottom at the 
foot of the rock revetments, were defined. The boundaries of each of the 
major associations and certain questionable or transition zones were mapped 
over the entire island. These associations were further characterized by 
extensive measurements of biomass and abundance of macrobiota occurring in 
quadrats placed according to a stratified random sampling scheme. Using 
these data, statistically based comparisons of biotic character were made 
between certain transition areas and definite associations. In some cases, 
questionable associations were lumped together. 


A major part of the study was devoted to analysis of seasonal dynamics 
in biotic composition. Permanent transects extending from the high inter- 
tidal to natural bottom were established normal to each of the four cardinal 
sides of the island. All macrobiota were censused in duplicate 1-square 
meter quadrats along each transect during each of the four seasons. Data 
analysis indicated that many species exhibit significant variability in 
abundance from one season to the next. 


Other studies included a gill net survey of fish fauna, mapping of 
mussel "talus" beds at the base of the island, and a survey of biota along 
a natural bottom transect between the island and shore. 


In general, the findings indicate a rich and varied fauna and flora 
associated with the high-relief solid substrate of Rincon Island which 
differs substantially from the more depauperate natural bottom habitats 


in the area. 


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SECURITY CLASSIFICATION OF THIS PAGE(When Data Entered) 


PREFACE 


The U.S. Army Coastal Engineering Research Center (CERC) conducts 
and sponsors research to provide definitive information on the ecological 
impacts of constructing coastal structures such as groins, jetties, 
breakwaters, and islands. Rincon Island, Punta Gorda, California, was 
the first major artificial island to be constructed with full ocean © 
exposure. This report describes an 18-month study sponsored by CERC to 
examine ecological effects of construction of Rincon Island (CERC Con- 
tract No. DACW 72-76-C-0011). 


The report was prepared by G.F. Johnson, Project Marine Ecologist, 
and L.A. deWit, Staff Marine Ecologist, with supervision provided by Dr. 
B.A. Wales, Principal-in-Charge; all of Dames §& Moore, Consultants in 
the Environmental and Applied Earth Sciences, Los Angeles, California. 
Professor W.L. Brisby of Moorpark College, Moorpark, California, partici- 
pated in the fieldwork and provided valuable consultation and review. 


Special recognition is due to the following students of Professor 
Brisby, who were responsible for a major part of the field data acquisi- 
tion: G. Wilson, D. Ospenson, D. Rasmussen, and R. Dawson. The authors 
gratefully acknowledge the interest in the project and valuable assist- 
ance provided by Dr. J. Siva, J. Hundley, C. Miller, and R. Carlson, all 
of Atlantic Richfield Corporation. 


Marine Ecological Consultants, Inc. of Solana Beach, California, 
were subcontractors for taxonomic work. Dr. K.R. Critchlow of Dames §& 
Moore assisted during two of the seasonal surveys of permanent transects. 
Dr. R.A. Park III, Professor of Geology and Ecosystem Analysis, Renssalaer 
Polytechnic Institute, directed an analysis of data using an R-mode 
cluster analysis computer program. 


A.K. Hurme of the CERC Coastal Ecology Branch was the technical 
monitor for this contract under the general supervision of E.J. Pullen, 
Chief, Coastal Ecology Branch. 


Comments on this publication are invited. 


Approved for publication in accordance with Public Law 166, 79th 
Congress, approved 31 July 1945, as supplemented by Public Law 172, 
88th Congress, approved 7 November 1963. 


OHN H. COUSINS 
Colonel, Corps of Engineers 
Commander and Director 


IV 


V 


VI 


APPENDIX 


A 


CONTENTS 


CONVERSION FACTORS, U.S. CUSTOMARY TO METRIC (SI). 
INTRODUCTION . 
POW ACIE ASIFIMUUING Ss 5 o G-6 6 


PREVIOUS SREEATED SHUDEESMcecene aes 
1. General Studies of Artificial Heibatexe. 
2. Previous Studies at Rincon Island. 


SHON WIENUCOISS so Glo 5 6 6 oo 6 656 Go 

Ho, Geiveraits 6 oo 6 6 

2. Reconnaissance Dies 

3. Talus Bed Measurements 

4, Seasonal Survey of Permanent TRANSCCES 
5. Mapping of Major Species Associations. 
6 
7 
8 


- Quantitative Characterization of Species Acsockasions. 


. Natural Bottom Survey. 
- Gill Net Surveys 


RESULTS AND DISCUSSION . 

1. General. 3/0 

2. Volume and Dinensdons of Talus Bedel 

3. Analysis of Seasonal Data from Permanent Tansee 
4. Distribution of Major Species Associations 

5. Quantitative Characteristics of Major Species 

Associations. 
6. Gill Net Survey RoswiEs. 
7. Natural Bottom Survey Results. 


SUMMARY AND CONCLUSIONS. 


LITERATURE CITED . 


DETAILED METHODOLOGY . 
SUMMARY DATA, SURVEY OF PERMANENT SEASONAL TRANSECTS . 


R-MODE DENDROGRAMS AND BOUNDARIES OF PRELIMINARY SPECIES 


ASSOCIATIONS . dep By wy Lolooswosntal Yo 

SUMMARY DATA, QUANTITATIVE CHARACTERIZATION OF MAJOR 
SPECIES ASSOCIATIONS . OB uor we seb tes Jom Jo 
OBSERVATIONS ALONG NATURAL BOTTOM TRANSECT . 

SIEVE ANALYSIS OF NATURAL BOTTOM SEDIMENT SAMPLES. 
GLOSSARY . 


Page 


101 
103 
107 


Ss e & 


14 


15 


16 


LY 
18 
19 
20 
21 


CONTENTS--Continued 
TABLES 


Master species list for Rincon Island. 


Seasonal transect data summary 
Gill net catch per hour at Rincon Island . 


Biota of natural bottom sediment samples 


FIGURES 
Aerial photograph of Rincon Island, spring 1977. 


Local bathymetry of Rincon Island. 


Locations of permanent seasonal transects, gill nets, natural 
bottom transect, and sediment grab sampling stations. 


Structrue of permanent seasonal transects. 
North-side talus bed and armor rock measurements 
West-side talus bed and armor rock measurements. 
South-side talus bed and armor rock measurements 
East-side talus bed and armor rock measurements. 
Major species associations, northwest quadrant 
Major species associations, southwest quadrant 
Major species associations, southeast quadrant 
Major species associations, northeast quadrant 


Seasonal overview of distribution of major species associations 
and substrate character, north-side permanent transect. 


Seasonal overview of distribution of major species associations 
and substrate character, west-side permanent transect 


Seasonal overview of distribution of major species associations 
and substrate character, south-side permanent transect. 


Seasonal overview of distribution of major species associations 
and substrate character, east-side permanent transect 


Vertical distribution for dominant biota, north side 
Vertical distribution for dominant biota, west side. 


Vertical distribution for dominant biota, south side 


Vertical distribution for dominant biota, east side. 


Dominant biota and substrate type along natural bottom transect. 


Page 


40 


41 


42 


43 
44 
45 
46 


47 
59 


CONVERSION FACTORS, U.S. CUSTOMARY TO METRIC (SI) 
UNITS OF MEASUREMENT 


U.S. customary units of measurement used in this report can be converted 
to metric (SI) units as follows: 


Multiply by To obtain 
inches 25.4 millimeters 
2.54 centimeters 
square inches 6.452 square centimeters 
cubic inches 16.39 cubic centimeters 
feet 30.48 centimeters 
0.3048 meters 
square feet 0.0929 square meters 
cubic feet 0.0283 cubic meters 
yards 0.9144 meters 
square yards 0.836 square meters 
cubic yards 0.7646 cubic meters 
miles 1.6093 kilometers 
square miles 259.0 hectares 
knots 1.852 kilometers per hour 
acres 0.4047 hectares 
foot-pounds 1.3558 newton meters 
millibars NOI 83 IOe kilograms per square centimeter 
ounces 28.35 grams 
pounds 453.6 grams 
0.4536 kilograms 
ton, long 1.0160 metric tons 
ton, short 0.9072 metric tons 
degrees (angle) 0.01745 radians 
Fahrenheit degrees 5/9 Celsius degrees or Kelvins! 


1To obtain at aie (C) temperature readings from Fahrenheit (F) seaginesy 


use formula: 


To obtain Kelvin (kK) readings, 


= (6/9) @ -82))o 


use formula: 


= (6/9) | - 32) + 273.15. 


ECOLOGICAL EFFECTS OF AN ARTIFICIAL ISLAND 


Rincon Island, Punta Gorda, California 


by 
G.F. Johnson and L.A. dewit 


I. INTRODUCTION 


Several studies on the ecological effects of the addition of 
artificial substrate in a nearshore coastal marine environment have 
been conducted in the past. The California Department of Fish and 
Game, for example, has made detailed studies at oil platforms and in 
areas where artificial reefs composed of streetcars, old car bodies, 
concrete cubicles, and riprap have been established (Carlisle, Turner, 
and Ebert; 1964; Turner, Ebert, and Given, 1969). 


In general, these studies conclude that the habitat features 
created by the addition of solid substrate are beneficial to the 
local ecosystem, especially in areas where such substrate is limited. 
In time, communities of organisms develop which usually support more 
species. than the sedimentary habitat that existed before the addition 
of hard, high-relief substrate. The biomass of the encrusting flora 
and fauna is an important food source for species of recreational, 
commercial, or aesthetic value which would otherwise not populate the 
area. In addition, physical characteristics of the solid substratum, 
such as crevices and vertical relief in an otherwise featureless 
bottom, attract a variety of fishes. 


The armor rock revetments of Rincon Island represent a signifi- 
cant addition of solid substratum to the local nearshore marine envi- 
ronment which has contributed to an enhancement in the richness of 
local marine communities (Carlisle, Turner, and Ebert, 1964; Brisby's 
Biota Appendix in Keith and Skjei, 1974). Although observations on 
Rincon Island's marine life have been made since these studies, no 
comprehensive delineation of major habitats nor detailed character- 
ization of communities extant at any one time or on a seasonal basis 
has been done. This study was undertaken with the recognition that 
this information would be valuable in understanding the ecological 
consequences of artificial island construction. The objectives of 
the study were to: 


(a) Delineate, map, and quantitatively characterize major 
species associations around Rincon Island, and compare 
these with the biota of the natural bottom between the 
island and shore; 


(b) document the morphology and volume of the beds of shell 
debris lying along the flanks of each of the four cardinal 
sides of the island; 


(c) establish permanent transects on each side of the island 
and survey major benthic organisms along these transects 
on a seasonal basis, documenting changes in biotic compo- 
sition and habitat character; and 


(d) conduct a gill net survey of the fish on each side of the 
island; and 


(e) expand the existing species list of the area. 
II. PROJECT SETTING 


Rincon Island is located in the Santa Barbara Channel approxi- 
mately midway between the cities of Santa Barbara and Ventura, 
California. The island is about 0.8 kilometer off Punta Gorda in 
about 14 meters of water, and is connected to the mainland by a 
causeway (Fig. 1). The extreme tidal range at the island is 3.05 
meters. Mean sea level (MSL) lies 0.79 meter above mean lower low 
water (MLLW). The island covers about 0.026 square kilometer of 
ocean floor and the area above MLLW is approximately 0.013 square 
kilometer. 


The island is constructed of rock revetments containing sandfill. 
It was constructed in stages between February 1957 and September 
1958, using many types and gradations of quarry rock. The most 
exposed face (west side) is protected with 1,130 concrete tetrapods, 
each weighing about 31,000 kilograms. The general shape of the is- 
land and the local bathymetry are shown in Figure 2 (Dames § Moore, 
1974). Bottom conditions vary uniformly throughout the area (Blume 
and Keith, 1959). The sediment consists of siity sand ranging into 
sandy silt with a thickness ranging from 4.3 to 7.6 meters. It 
overlies a geologically recent shale or "siltstone" formation. 
Average bottom slope is 3 percent. 


Details of the construction and engineering considerations in 
the design of Rincon Island are summarized in Keith and Skjei (1974) 
and Blume and Keith (1959). 


III. PREVIOUS RELATED STUDIES 


i General Studies of Artificial Reef Habitat. 


The value of artificial structures for attracting marine fishes 
was the subject of many papers presented at an International Arti- 
ficial Reef Conference, cosponsored by Texas A&M University, the 
Texas Coastal and Marine Council, and the National Marine Fisheries 
Service (Colunga and Stone, 1974). The fish-attracting properties of 
nearshore artificial reefs composed of tires, car bodies, and riprap 
on the gulf and Atlantic coasts have been documented by Buchanan 
(1972), Stone (1972, 1973); Stone, Buchanan, and Parker (1973); 
and Stone, Buchanan, and Steimle (1974). The latter investigators 
reported an increase in the fish-carrying capacity of an area 300 to 
1,800 times that of the open bottom before reef construction. 


Figure 1. Aerial photograph of Rincon Island, spring 1977. 


100 METERS 


KEY: 


=== APPROXIMATE LOCATION OF RUBBLE=HOUND TOE 


= BATHYMETRIC CONTOURS IN FEET BELOW MLLW 


Figure 2. Local bathymetry of Rincon Island 
(from Dames § Moore, 1974). 


Studies of artificial substrate properties affecting fish attrac- 
tion and ecological succession in southern California were reported 
by Carlisle, Turner, and Ebert (1964), Turner, Ebert, and Given 
(1969), and Fager (1971). Carlisle, Turner, and Ebert (1964) con- 
ducted visual surveys of biota in bottom areas before and after 
artificial reef establishment, noting that fishes were attracted 
within hours of reef construction. Carlisle, Turner, and Ebert 
(1964) also made ecological observations at a number of offshore oil 
installations, including Rincon Island. They concluded that these 
sites exhibited similar attractions for fish and, more generally, 
that "habitat changes brought about by establishing offshore oil- 
drilling installations were generally beneficial to the flora and 
fauna." 


Results of a 4-year study of various aspects of manmade reef 
ecosystems and optimal materials for reef construction, conducted by 
the California Department of Fish and Game, were published by Turner, 
Ebert, and Given (1969). Of four types of reef construction mate- 
rials evaluated, quarry rock was judged optimal on the basis of 
practicalities of cost and handling, fish attraction (although con- 
crete shelters were better in this regard), and minimal sediment 
disturbance. More than 200 invertebrate taxa were recorded during 
the study. Succession on the newly established reefs proceeded from 
an initial barnacle-hydroid phase, into a mollusk-polychaete assem- 
blage, to an ascidian-sponge stage, and finally a stage characterized 
by the presence of abundant encrusting ectoprocts (moss animals). 
Aggregate anemones, gorgonians, and stony corals appeared in later 
stages. Approximately 5 years was required for successional change 
to cease on these artificial reefs. 


Drs Previous Studies of Rincon Island. 


The California Department of Fish and Game biologists made an 
initial survey of Rincon Island in July 1958, 18 months after con- 
struction of the island began (Carlisle, Turner, and Ebert, 1964). 
They conducted 26 observational dives over the period, August 1958 to 
December 1960. Despite many fluctuations, possibly due to water 
clarity or incoming year classes of fishes, an overall upward trend 
in fish populations was observed. Toward the end of the survey 
period the biota of the island had the appearance of ''a well-balanced 
animal community.'' Fifty-three species of fish belonging to 44 
genera in 22 families were observed during this study. About 97 
percent of the fish fauna belonged to the following groups: silver- 
Side, (Atherinidae), surfperch (Embiotocidae), sea bass (Serranidae), 
damselfish (Pomocentridae), rockfish (Scorpaenidae), and halfmoon 
(Scorpidae). The biologists noted populations of large, active 
fishes in turbulent waters along the west (seaward) side of the 
island, sedentary forms such as sculpin (Cottidae), and rockfish 
occupying Spaces among the rocks, and the young of many species 
(especially keip bass (Paralabrax clathratus), blacksmith (Chromis 


punctipinnis), and species of surfperch and rockfish) apparently 
using the kelp beds in the lee of the island as nursery grounds. 


Approximately 54 months after island construction, the inverte- 
brate fauna and algae were surveyed along a transect on the east 
(lee) side of the island by sampling a 0.09-square meter area at each 
3.05-meter depth interval, This sampling was augmented with 
numerous diving observations. The results of the survey are sum- 
marized in Appendix H of Carlisle, Turner, and Ebert (1964). Rela- 
tively high densities and a pronounced vertical zonation in major 
taxonomic groups were apparent. 


The work of the California Department of Fish and Game biolo- 
gists provided an idea of the pattern of early colonization for 
Rincon Island. Brisby's Biota Appendix in Keith and Skjei (1974) 
provided valuable insight into the contrast between ecological con- 
ditions associated with the island and those of the natural bottom at 
the site of the island before its construction. Brisby knew the area 
before construction, and has had an arrangement with the Atlantic 
Richfield Company to use the island since its construction as a field 
station for educational purposes. His study methods involved use of 
scuba techniques, surface craft, mechanical collecting gear (includ- 
ing Peterson grabs, dredges, trawls, traps, and other fishing gear), 
and underwater photography. Brisby's conclusions provide a basic 
introduction to the island's ecology. 


In summary, Brisby found that with construction of the island, 
the area developed from a biologically depauperate condition into a 
mature and balanced reef. Before construction, only 14 species of 
benthic fish were observed. After establishment of a "climax" com- 
munity on the island, 298 species, representing all major marine 
phyla, were recorded. Ecological characteristics were somewhat 
different on each of the four sides of the island, owing to differ- 
ences in degree of exposure to waves and currents. High water tur- 
bidity typified conditions on the landward side of the island. The 
seaward side was reported to be particularly rich in life. The other 
two sides were observed to provide an intermediate environment and 
each, because of differences in exposure, had a somewhat different 
ecology. "Talus slopes" of mollusk shells were observed along the 
bases of the three seaward sides. 


IV. STUDY METHODS 
ihe General. 


This study was divided into five major subtasks. Detailed 
information on specific methodologies is provided in Appendix A. 


2 Reconnaissance Dives. 


The first subtask involved reconnaissance dives by two diver 
biologists to make a preliminary survey of major species associations 
around the island. A limited amount of randomly placed quadrat 
sampling was done to determine variability in densities of biota. . 


So Talus Bed Measurements. 


The second subtask was to calculate the volume of the mounds of 
mollusk shells and shell fragments at the base of the rock revetments 
around the island (shell "talus''). The dimensions of the talus beds 
were determined and volumes of shell debris in the beds along each of 
the four cardinal sides were estimated. 


Dimensions of the shell talus beds were determined by the follow- 
ing method. Divers swam along each of the cardinal sides of the is- 
land, noting significant changes in the morphology of the talus bed 
(i.e., changes in slope or upper and lower margin). Where such 
changes occurred, the distance between the upper and lower margins 
was measured using a steel tape. Depths of the upper and lower 
margins were also recorded to +0.2 meter. Cross-sectional geometry 
of the talus bed at each measurement point was determined from the 
distance from the waterline, water depth, and slope of the rock revet- 
ment. These cross sections were plotted on base charts for each of 
the four cardinal sides. The volume of the accumulated shell mate- 
rial along each side of the island was then estimated. Boundaries of 
the talus beds were charted. 


4. Seasonal Survey of Permanent Transects. 


The third subtask was to survey permanent transects on the island 
to determine seasonal variability in densities of macrobiota. Transects, 
extending from the upper limit of the wave splash zone to the limit of 
the island's influence on the bottom, were established on the four car- 
dinal sides of the island (Fig. 3). These transects were surveyed dur- 
ing each season for 1 year (see App. B for a summary of the data). 


Heavy stakes of steel angle iron marked the upper and lower 
limits of each transect. A single stake was anchored in the armor 
rock above the splash zone on each side of the island, marking the 
upper limit of the transect. Three identical stakes were driven into 
the natural bottom sediment near the seaward margin of the talus bed, 
and were alined parallel to each side. The three stakes were con- 
nected with 0.6-centimeter-diameter polyethylene line and floats were 
attached to each stake to facilitate locating them during conditions 
of restricted visibility (Fig. 4). 


A nylon line marked off in 1-meter increments, was used as the 
transect line. During each survey, one end of the transect line was 


13 


Yo- 

Se 
WEST SIDE TRANSECT 
‘ 
‘ APPROXIMATE TOE OF REVETMENT 

%O e : PPROXIM ae 
1 
! APPROXIMATE MLLW LINE 

‘ 1 
94° 21 00 


S10E 
TRANSECT 


“ok. =) 


\ ae) oe 


TRANSECT 
9 

NOE a Aaa) 
© PERMANENT SEASONAL SURVEY TRANSECT 
bs) GILL NET LOCATIONS 
9 —— NATURAL BOTTOM TRANSECT 
= @ SEDIMENT GRAB SAMPLE STATION 

{o) 50 , 100 M 
Figure 3. 


Locations of permanent seasonal transects, gill nets, natural 
bottom transect, and sediment grab sampling stations. 
(Depth contours in feet below MLLW.) 


STEEL STAKE LODGED 
IN ROCKS ABOVE WATER 


WATERLINE 


TRANSECT LINE 
(REMOVED BETWEEN SURVEYS) 


POLYPROPYLENE LINE 
MARKER FLOATS 


X-SECTION THROUGH 
ISLAND REVETMENT 


1.5-M STEEL STAKES DRIVEN INTO BOTTOM 


Figure 4. Structure of permanent seasonal survey transects. 


attached to the upper (splash zone) marker stake and the other end 
was attached to the center stake on the bottom. This ensured exami- 
nation of the same area on each side during the four seasonal sur- 
veys. Divers carrying 1-square meter quadrats, underwater clip- 
boards, and plastic collecting bags swam the transect lines, re- 
cording data on densities of all species of macrobiota (in duplicate. 
samples) at l-meter increments. 


Seasonal density values were recorded as percent of unit area 
covered for algae and encrusting colonial animals or as number per 
unit area for species for which individuals could be counted. Cer- 
tain species (e.g., Serpulorbis squamigerus, the scaled worm shell) 
were recorded for both numbers of individuals and percent coverage. 
Species of uncertain identity were collected, making notation of 
the quadrat number from which they were collected, and later identi- 
fied. Each transect was photographed using an underwater camera. 


The marker stakes remained intact during the entire year of sur- 
vey. They were located on each sampling trip except one on the north 
side of the island. Extreme water turbidity precluded attachment of 
the transect line to the bottom marker. In this case, the transect 
was repeated by placing the line on structures (including a submerged 
pipeline) recognized from previous surveys. 


The same two diver biologists recorded the data on each seasonal 
survey with the exception of the north side during the summer (August 
1976) and the west side during the winter (February 1977) surveys, 
when another diver was used. Heavy surf prevented collection of 
complete data on the west-side transect during the fall (November 
1976) and winter (February-March 1977). Data were not collected in 
the upper zone during either of these two seasons. 


All data were transcribed from the field sheets to data tables 
which listed densities of both plants and animals in each quadrat. 
Fifty-four of the more common species were analyzed for seasonal 
abundance. Details of the methods used in the analyses of the perma- 
nent transect data for significant seasonal differences in species 
densities are provided in Subsection 2 of Appendix A. 


S. Mapping of Major Species Associations. 


The fourth subtask was to chart the distribution of major species 
associations over all submerged parts of the island. A series of 
charts was prepared depicting the boundaries of major species associ- 
ations and the spatial disposition of these associations, accurate to 
+0.2 meter in depth and +0.3 meter in horizontal distance from perma- 
nent reference points on the island. This phase of the work required 
identification of faunal and floral associations on the basis of sub- 
strate character and recurrent groups of species that were conspicu- 
ous by virtue of size, abundance, or biomass. 


16 


Initial identification of major species associations was based 
on subjective judgment developed during reconnaissance and permanent 
transect diving. These preliminary identifications were corroborated 
by computer analysis of the field data. An R-mode cluster analysis 
program (unweighted pair-group arithmetic average clustering method 
(UPGMA) as described by Sneath and Sokal, 1973) was used. Input data 
consisted of presence-absence designations for all species encoun- 
tered in each 1-square meter quadrat from the east and north sides 
for the summer (August) and fall (November) seasonal surveys. 


The program generates a matrix of similarity for all species. 
A CALCOMP plotter program was used to generate dendrograms showing 
the aggregate hierarchical classification among species (see App. C). 
On the basis of this information, 13 tentative species associations 
were identified. 


Measurements were made to the boundaries of the various species 
associations from fixed reference points around the island. Depths 
(referenced to MLLW) and distances were recorded at transition zones 
or boundaries. between associations. These measurements were taken 
along transects located at 10-meter intervals around the island (5- 
meter intervals were used around the four corners of the island to 
assure adequate radial coverage). The starting point for each tran- 
sect was the upper boundary of the barnacle-limpet zone. In plotting 
the data, boundaries of associations were extrapolated between transect 
lines to depict the distributions of the associations. Actual dis- 
tances were plotted on a base chart of the island. Boundaries of the 
talus beds, measured during the fourth subtask, were also plotted on 
this chart. The actual distances were then trigonometrically recti- 
fied for plan view plotting according to the methodology in Appendix 
AVS): 


Areas covered by each species association were determined by 
cutting out the associations on the base chart (before trigonometric 
rectification), weighing the pieces from each association on a 
Mettler analytical balance to a precision of +0.001 gram, and calcu- 
lating the percent each association represents of the total area of 
the island bounded by the upper limit of the barnacle-limpet zone and 
the lower limit of rock on the bottom. 


6. Quantitative Characterization of Species Associations. 


The fifth subtask involved quantitative characterization of the 
species associations. Biomass and densities of macrobiota around the 
island were measured. Analysis of these data provided the rationale 
for separating or combining associations lying adjacent to one 
another or on different sides of the island. 


Densities and biomass of macrobiota within the associations were 
determined using randomly placed sample quadrats. Quadrats used in 
all associations except those in the upper intertidal were of 0.25- 
square meter size. Duplicate 0.01-square meter quadrats were used in 
the upper zones. Numbers drawn from a random numbers table, equating 
to vertical and horizontal distances from permanent points on the ‘is- 
land, were used in locating the sampling quadrats. 


Divers measured the distances with an underwater steel tape and 
then, looking away from the bottom, released the quadrat about 1 
meter above the bottom. This minimized sampling bias. If the 
quadrat came to lie in or over a crevice between rocks, it was re- 
leased a second time. ; 


The depth of the quadrat and time of sampling were recorded and 
the area within the quadrat was photographed. A record was made of 
the densities of each species within the quadrat (numbers or percent 
coverage). Large organisms less than 50 percent enclosed within the 
quadrat boundaries were not recorded. All detachable macrobiota were 
removed and placed in labeled plastic bags for subsequent biomass 
measurement. The contents of each collecting bag were wet-blotted 
and weighed on a triple-beam balance (precision approximately +0.2 
gram). Wet weights were recorded for each species. ¥ 


To develop biomass data on organisms that are permanently at- 
tached to the substrate, measured areas were scraped by a diver using 
a steel chisel and hammer. The removed fragments were collected, 
using a specially designed slurp gun, fitted with a collecting cham- 
ber lined with Nitex plankton netting of 333-micrometer mesh size. 
Contents of the collecting chamber were subsequently weighed as 
described above. 


All raw data (numbers, percent coverage, and wet weight for each 
species) were tabulated for each quadrat. Tables were arranged in 
columnar form with species categories across the top and quadrat 
numbers along the left-hand margin. Quadrats were grouped according 
to the association and the sampling locations. Quadrats within tran- 
sition zones and from apparently similar associations on different 
sides of the island were separated to facilitate testing against 
"typel association quadrats (those lying well within the boundaries 
of distinct associations). These quadrats were then either combined 
with or separated from type associations. 


This method of tabulation permitted calculation of summary sta- 
tistics for all species in each association which in turn facilitated 
intercomparison of the characteristics of these associations. The 
following summary statistics were calculated: Frequency (ratio of 
number of quadrats of occurrence to number of quadrats sampled in 
each group); mean abundance and 95-percent confidence limits for the 
mean abundance; and average weight per individual (or per 100-square 


18 


centimeter coverage for species whose densities were estimated as 
percent coverage). 


Comparison of summary statistics on biomass and densities per- 
mitted separation of associations in a subjective manner for the 
intertidal associations (down to and including the macrophytic algae 
zone). However, this approach was too arbitrary when it came to 
identifying possible differences between similar associations on 
different sides of the island or between associations grading into 
one another on the same side. For these instances, a more rigorous 
statistical test was necessary. Application of parametric statistical 
tests requires that the data be normally distributed. This was not 
the case for most of the data collected during quantitative sampling. 
Also, it is unlikely that data transformation could be effectively 
used to normalize the data. The nonparametric Wilcoxon "'t"' test 
(Tate and Clelland, 1957) was applied to test differences between 
densities of selected dominant species within potentially similar 
associations and between dissimilar associations. An association on 
the north side, which is dominated by the encrusting coralline alga, 
Lithothamnium-Lithophyllum complex, was selected as the type associ- 
ation against which most other associations were tested. 


Uke Natural Bottom Survey. 


In addition to the above subtasks, ecological conditions in 
nearby natural bottom habitats were investigated. This information 
was to aid in interpreting the ecological changes induced by the 
presence of the island. 


The composition of the epibenthic macrobiota (plants and animals) 
on or just above the surface of the sediment or rock on the natural 
bottom between the island and shore was surveyed along a transect lo- 
cated away from the influence of the island and causeway (Fig. 3). 

The transect survey was completed in two segments. The first segment, 
over a depth of 13.7 meters MLLW near the island to a depth 6.1 
meters MLLW toward shore, was surveyed by divers using Farallon 
underwater propulsion units. The second segment, extending from 
shore to the 6.1-meter MLLW depth, was surveyed by divers entering 
through the surf and swimming offshore. Triplicate sediment samples 
for infauna (animals inhabiting the sediments) were taken at the 
outer terminus of the.transect at a 13.7-meter depth and at a point 
midway in the transect at a depth of 10.7 meters MLLW (Fig.3). The 
samples were collected by pushing 3.13-liter lidless coffee cans into 
the sediment and carefully sealing both ends of the cylinder with 
plastic caps. Samples for grain-size analysis were collected by 
pushing 0.2-liter jars 10 centimeters into the sediment. Infaunal 
samples were sieved through 1-millimeter sieve screens and preserved 
for later taxonomic analysis. 


8. Gill Net Survey. 


A gill net survey was conducted on 15 and 16 June 1977. A 
single multimesh nylon monofilament net, 30.5 meters long and 2.4 
meters deep, was deployed obliquely along each cardinal side of the 
island (Fig. 3). The nets consisted of ten 3.05-meter-long panels 
with two panels each of 1.27-, 2.54-, 3.81-, 5.08-, and 6.35-centi- 
meter bar mesh. Position of these panels in the net was random. 
When deployed, the nets extended from the intertidal zone of the 
island to the toe of the island revetment. The nets were fished for 
two periods: a daytime period of about 4 hours, and a day-night 
period ranging from a minimum of 17 hours (west side) to a maximum of 
23.5 hours (east side). 


Fishes caught in each net were removed and identified, and a 
record was made of the standard length (snout to distal end of caudal 
peduncle) for bony fishes and total length (snout to end of caudal 
fin) for sharks. Lengths were recorded to the nearest 0.5 centi- 
meter. Numbers of individuals occurring in each mesh size were also 
recorded. Summary data tables were prepared listing numbers of indi- 
viduals, mean length, and length range for each species captured on 
each side of the island. 


V. RESULTS AND DISCUSSION 
IL General. 


A total of 330 species of macrobiota was identified during this 
study; 160 of these taxa had not been reported as occurring at Rincon 
Island. This addition to the number of species reported in Keith and 
Skjei (1974) brings the total species list to 458. Many additional 
species undoubtedly exist among the island's varied habitats. An up- 
dated master list of taxa of Rincon Island is given in Table 1. 


DD Volume and Dimensions of Talus Beds. 


Dimensions of the shell talus beds along each of the four cardi- 
nal sides are shown in perspective view in Figures 5 to 8 and in plan 
view in Figures 9 to 12. (The upper boundaries of the talus beds do 
not match precisely with the lower boundaries of the deepest associ- 
ations in these figures for two reasons: First, talus bed measurements 
were taken at positions of change of the talus bed geometry, while 
associations were measured along fixed transects; second, the deepest 
association frequently extended into the talus bed on isolated rocks.) 
Approximate volumes of shell calculated from the measurement of 
talus bed dimensions are as follows: 


West side: 1,450 cubic meters 
South side: 98 cubic meters 


20 


Table 1. Master species list for Rincon Island. 


Occurrence during present study 


c aa 1 
Scientific name Common name North West South East 
ALGAE 

DIVISION CHLOROPHYTA 2 GREEN ALGAE 


Bryopsis corticulans 
Chaetomorpha aerea? 
Cladophora sp. x 
Codium fragile Deadman's fingers X 
Derbesia marina xX 
cf. Enteromorpha sp. x x 
Ulva sp. Sea lettuce x xX xX 
Unid. green algae #1 x 
DIVISION CYANOPHYTA BLUE-GREEN ALGAE 
cf. Phormidium sp. xX xX X xX 
DIVISION PHAEOPHYTA BROWN ALGAE 
Cystoseira osmundacea xX x 
Desmarestia herbaceae? 
Dictyota binghamiae xX 
D. flabellata , x xX xX 
Ectocarpus sp- 
Egregia menziesii (=laevigata) Feather-boa kelp xX x 
Giffordia granulJosa X 
Halidrys dioica 
Macrocystis sp. 2 Giant kelp x 
Petrospongium rugosum 
Pterygophora californica 
Ralfsia pacifica 
Taonia lennebackeriae 
Unid. brown alga #1 
Unid. brown alga #2 
Unid. brown alga #3 
Unid. juv. laminariales 
DIVISION RHODOPHYTA RED ALGAE 
Antithamnion sp. x 
Bossiella orbigniana x x x 
Bossiella sp. 
Callithamnion sp. 
Callophyllis flabellulata x 
Ceramium codicola 
cf. Ceramium sp. X x xX x 
Corallina officinalis x x x 
Cryptopleura cf. crispa 
Delesseria sp. x 
Gelidium coulteri 
G. cf. robustum 
G. purpurascens 
G. cartilagineum 
G. sp. #1 
G. sp. #2 x 
Gigartina canaliculata x 
G. cf. exasperata ; Re 
G. sp. 
G. spinosa armata x 
G. sp. (juv.) 
Grateloupia doryphora (=abreviata) x 
Hildenbrandia prototypus2 
Laurencia pacifica x 
Lithothamnium/Lithophyllum complex x x x x 
Lithothrix aspergillum 
Lomentaria hakodatensis x 
Microcladia cf, coulteri 
Neoagardhiella (=Agardhiella) sp. x x 
Peyssonellia sp, Kooi x x 


PS OO OS 


CN te) 
x 
DP SD OS 


SS OS OOS OOS 


See footnotes at end of table. 


2 | 


Table 1. Master species list for Rincon Island.--Continued. 


Occurrence during present study 


1 
Scientific name Common name North West South ‘East 
Scientific name 


DIVISION RHODOPHYTA (Continued) 


Platythamnion villosum 
P. sp. x X x 
Polysiphonia simplex x 
P. cf. pacifica x u 
P. spp. 
Porphyra perforata? 
Prionitis lanceolata x xX xX x 
Pterosiphonia dendroidea 
Pterosiphonia sp. x xX 
Rhodoglossum affine x x x 
Rhodymenia sp. F xX xX x 
R. californica X fs 
cf. R- sp. 
Schizymenia pacifica : 
Stenogramme interrupta x x xX xX 
Tiffaniella snyderiae xX 
Veleroa subulata/Murrayellopsis 

dawsonii complex 4 xX 
Unid. red alga #1 x 
Unid. red alga #2 
Unid. filamentous red alga #1 
Unid. juvenile red alga 
Unid. filamentous red alga #2 
Unid. "leafy" red alga 
Unid. "tall" red alga 
Unid. red alga #3 
Unid. red alga #4 
Unid. red alga #5 
Unid. "flat" red alga ig 
Unid. red alga #6 
Unid. red alga #7 
Unid. coralline #1 x 
Unid. coralline #2 % x 
Unid. coralline #3 


De DS OS OOS 


bd DS OO OK 


PHYLUM PORIFERA SPONGES 
Cliona celata californiana Boring sponge x x x x 
Geodia mesotriaenia2 
Halichoclona gellindra 
Haliclona ecbasis? 


Geode sponge 

Lavender sponge 

Lavender-blue encrust- 
ing sponge 

Hymenamphiastra (=Hymeniacidon) 
cyanocrypta Blue leaf sponge x x x 

Hymeniacidon ungodon2 Little leaf sponge 


H. sinapium Yellow leaf sponge 

Leucetta losangelensis x x 
Leucilla (=Rhabdodermella) nuttingi Urn sponge 
Leuconia heathi? 
Leucosolenia sp. Finger sponge 

Lissodendoryx noxiosa? Noxious sponge 

Spheciospongia confoederata Liver sponge x 
Tedania toxicalis 
Tethya aurantia2 
Verongia thiona 

Unid. "sulfur" sponge 
Unid. red sponge #1 
Unid. purple sponge #2 
Unid. orange sponge #3 
Unid. yellow sponge #4 


Thistle sponge 


Sponge 
Orange. puff-ball sponge 
Sulfur sponge x x 


See footnotes at end of table. 


22 


Table 1. Master species list for Rincon Island.--Continued. 


Scientific name 


PHYLUM PORIFERA (Continued) 


Unid. grey sponge #5 
Unid. sponge #6 
Unid. sponge #7 
Unid. "white" sponge 


PHYLUM CNIDARIA 


CLASS HYDROZOA 
Aglaophenia struthionides 
Antennella avalgnia 
Campanularia sp. 
cf. Eudendrium sp. 
Obelia sp. 

Sertularia cf. furcata 
cf. Plumularia sp. 

cf. P. lagenifera 

cf. Sertularia sp 
Unid. green hydroid 
Unid. hydroid sp. #1 
Unid. hydroids 


CLASS ANTHOZOA 


Anthopleura xanthogrammica/ 


A. elegantissima3 
Antropora tincta 
Astrangia lajollaensis 
Balanophyllia elegans 
Cerianthiopsis sp. 
Corynactis californica 
Eugorgia rubens2 
cf. Epiactis prolifera 
Lophogorgia chilensis 
Metridium sp. 2 
Muricea californica/ 

M. fruticosa3 
cf. Pachycerianthus sp. 
Paracyathus stearnsii 
Renilla kollikeri? 
Stylatula elongata? 
Tealia sp. 

Unid. anemone #1 

Unid. white anemone #2 
Unid. burrowing anemone 
Unid. red cerianthid 


PHYLUM ANNELIDA 2 
Chaetopterus variopedatus 


cf. Chaetopterus sp. 
Dexiospira spirillum 
Diopatra ornata 
Dodecaceria fewkesi 
Eudistylia polymorpha 
Eudistylia sp- 

Eunereis longipes 
Eupomatus gracilis 
Halosydna tuberculifera 
H. brevisetosa? 


See footnotes at end of table. 


Common name 


ANEMONES, HYDROIDS, 
CORALS, GORGONIANS 

HYDROIDS 

Ostrich plume hydroid 


Campanulate hydrozoan 


ANEMONES /CORALS 
Green anemone 


Colonial coral 
Solitary orange coral 
Burrowing anemone 
Colonial red anemone 
Purple sea fan 
Prolific anemone 
Pink gorgonian 
Solitary anemone 
California/rust 
gorgonians 
Tube anemone 
Solitary coral 
Sea pansy 
Elongate sea pen 
Anemone 


WORMS 
Parchment tube worm 
Parchment tube worm 


Feather-duster worm 
Feather-duster worm 
Nereid worm 


Scale worm 
Scale worm 


23 


Occurrence during present study 


North 


SO OOM 


West 


MOS OO 


mS OS 


be 


South 


mM OS OS 


x 


Ete 


East 


DS PS Od OS 


Table 1. 


Scientific name 


PHYLUM ANNELIDA (gontinued) 
Nereis eakini 
N. mediator? 
Paleonotus bellis? 


Salmacina tribranchiata 


Serpula vermicularis? 
Spirorbis eximius 
Polyopthalmus pictus 
Unid. serpulids 

Unid. Syllidae 


PHYLUM ARTHROPODA 
CLASS CRUSTACEA 

Alpheus clamator 
Ampithoe sp. 
Balanus cariosus? 
B. crenatus2 
B. galeata 
B. glandula 
B. nubilus 
B. pacificus 
B. tintinnabulum 
B. sp. 
Cancer antennarius2 
(a5 anthonyi2 ; 
Cancer cf. productus 
Chthamalus fissus 
Crangon dentipes2 


Erichthonius brasiliensis 


Heptacarpus palpator 


Hippolysmata californica? 


Hyale frequens 
Jaeropsis dubia 
Loxorhynchus crispatus 
L. grandis? 


Membranobalanus orcutti 


Munna chromatocephala 
Pachycheles pubescens 
Pachygrapsus crassipes 
Paguristes turgidus2 
P. ulreyi 

Pagurus californiensis 
Pandalus gurneyi? 
Panulirus interruptus 


Petrolisthes cinctipes2 


5 Bs 

Pollicipes polymerus 
cf. Isocheles pilosus 
Pugettia producta 

P. sp. 


Scyra acutifrons* 


Spirontocaris brevirostris? 
Tetraclita squamosa rubescens 


Unid. pagurids 
Unid. shrimp ; 
Unid. barnacles 


PHYLUM MOLLUSCA 


CLASS GASTROPODA 
Acanthina spirata 
Acanthodoris lutea 
Acmaea mitra 


See footnotes at end of table- 


Occurrence during present study 


Common name North 


Nereid worm 

Nereid worm 
Chrysopetalid worm 
Colonial tube worm 
Serpulid worm 


JOINT-LEGGED ANIMALS 
CRUSTACEANS 

Shrimp 

Amphipod 

Acorn barnacle 

Acorn barnacle 


Acorn barnacle 
Acorn barnacle 
Acorn barnacle 
Acorn barnacle 
Tcorn barnacle 
Rock crab 
Yellow crab 
Rock crab 
Acorn barnacle 
Pistol shrimp 
Amphipod 
Shrimp 

Red rock shrimp 
Amphipod 
Isopod 

Sheep crab 
Sheep crab 
Barnacle 
Amphipod 
Hermit crab 
Striped shore crab 
Hermit crab 
Hermit crab 
Hermit crab 
Shrimp 


Porcelain crab 
Porcelain crab 
Gooseneck barnacle 
Hermit crab 

Kelp crab 

Kelp crab 

Masking crab 
Bent-back shrimp 
Thatched barnacle 
Hermit crabs 


SNAILS, NUDIBRANCHES, 
CLAMS, OCTOPUSES 


SNAILS AND NUDIBRANCHES 


Oyster drill 
Nudibranch 
White-cap limpet 


24 


Master species list for Rincon Island.--Continued. 


West South 


mM 


x OM OS 


East 


x 


CLASS GASTROPODA 


Table l. 


Scientific name 


A. persona? 

Amphissa sp.2 
Anisodoris nobilis 
Antiopella barbarensis 
Aplysia californica 

A. vaccarla 

Archidoris montereyensis 
Armina californica? 
Astraea undosa? 
Cadlina luteomarginata 


Callistochiton crassicostatus 


Calliostoma annulatum 

Cc. canaliculatum 

Cc. gloriosum 

Ce supragranosum? 

Ceratostoma nuttalli 

Collisella cf. conus 

C. digitalis 

c. cf. limatula 

(G5 pelta? 

C. scabra 

Go Bao fink 

C. sp. #2 (ridges) 

Cc. sp. #3 

C. cf. strigatella 

Conus californicus 

Coryphella trilineata 

Crepidula Cf- aculeata 

Crepipatella lingulata 

Cypraea spadicea 

Diaulula sandiegensis 

Diodora aspera 

Doriopsilla albopunctata 
(=Dendrodoris fulva) 

Fissurella volcano 

Flabellinopsis iodinea 

Haliotis corrugata2 

H. cracherodii2 

He fulgens? 

H. rufescens 

Hermissenda crassicornis 


Hypselodoris californiensis? 


Jaton festivus 
Kelletia kelletii 
Laila cockerelli? 
Littorina planaxis2 
L. scutulata? 

L. sp. 

Lottia gigantea 
Maxwellia gemma 
Megathura crenulata 
Mitrella carinata 
Mitra idae 
Nassarius mendicus 
Navanax inermjs 
Neosimnia sp. 
Norrisia norrisii? 
Ocenebra foveolata 


See footnotes at end of table. 


(Continued) 


Common name 


Mask limpet 
Amphissa 

Nudibranch 
Nudibranch 

Sea hare 

Sea hare 

Light yellow sea slug 
Pansy sea slug 

Wavy turban snail 
Nudibranch 

Chiton 
Purple-ringed top shell 
Channeled top shell 
Glorious top-shell 
Granulose top-shell 
Nuttall's hornmouth 
Limpet 

Fingered limpet 
File limpet 

Shield limpet 

Rough limpet 

Limpet 

Limpet 

Limpet 

Limpet 

California cone 
Nudibranch 

Spiny slipper shell 


Half-slipper shell 
Chestnut cowry 
Circle-spotted sea slug 
Rough keyhole limpet 
Yellow sea slug 


Volcano limpet 
Purple sea slug 
Pink abalone 

Black abalone 

Green abalone 

Red abalone 
Yellow-green sea slug 
Blue-orange sea slug 
Festive murex 
Kellet's whelk 
Orange-white sea slug 
Eroded periwinkle 
Checkered periwinkle 
Periwinkle 

Owl limpet 

Gem murex 

Giant keyhole limpet 
Carinate dove shell 
Ida's mitre 

Lean nassa 
Nudibranch 

Pink louse shell 
Smooth turban 


25 


Master species list for Rincon Island.--Continued. 


Occurrence during present study 


North 


DS OS PS PS OP 


be 


West 


South 


MOS OO OM 


East 


Table 1. Master species list for Rincon Island.--Continued. 


Occurrence during present study 


Scientific name 1 Common name North West South East 


CLASS GASTROPODA (Continued) 


oO. poulsoni? 
O. cf. barbarensis 


Poulson's dwarf triton 


O. sp. x 
Polycera tricolor Nudibranch x 
Pteropurpura festiva Festive murex x xX x 
P. macroptera Murex xX 
Pterynotus trialatus? Three-winged murex 
Serpulorbis squamigerus Scaled worm shell x xX xX x 
Simnia (Neosimnia) vidleri Vidler's simnia x x 
Tegula aureotincta? Gilded tegula 
T. brunnea? Brown tegula 
T. funebralis Black turban snail 
Triopha maculata Nudibranch 
Tritonia festiya Nudibranch x 
Unid. limpet #1 x 
Unid. limpet #2 2 
Unid. blue/white eolid a 
Unid. navanax-like eolid x 
Unid. gastropod #1 as 
Unid. dorid #1 2s 
Unid. chiton #1 23 
Unid. limpet #3 28 
Unid. eolid #1 2 
Unid. eolid #2 % 
CLASS PELECYPODA CLAMS AND SCALLOPS 
Anomia peruviana/ Pearly jingle/ 
Pododesmus cepio3 Abalone jingle x x x x 
Bankia setacea Ship worm 
Chaceia ovoidea? Wart-necked piddock 
Chama pellucida Agate chama ? x 
Chlamys latiaurata? Kelp scallop 
Gari californica? Sunset clam 
Hiatella arctica Nestling clam x x 
Hinnites multirugosus Rock scallop 
Kellia laperousii xX 
Lima hemphilli? File shell 
Lithophaga plumula Date mussel 
Mytilus californianus California mussel xX xX 
M. edulis Bay mussel x x x 
Nettastonnella rostrata? Beaked piddock 
Parapholas sp. Boring clam x x x 
Pecten diegensis San Diego scallop 
Penitella penita? Flap-tipped piddock 
Pseudochama exogyra Reversed chama 
Semele rupicola? Rock dwelling semele 
Teredo diegensis? Ship worm 
Unid. pholads x x 
Unid. boring clam x 
CLASS CEPHALOPODA OCTOPUSES AND SQUIDS 
Octopus bimaculoides Two-spot octopus 
Octopus. sp. : x x 


CLASS POLYPLACOPHORA 


Mopalia muscosa2 
Callistochiton crassicostatus 


See footnotes at end of table. 


26 


Table 1. Master species list for Rincon Island.--Continued. 


Occurrence during present study 


1 Common name North West South East 


Scientific name 


PHYLUM ECTOPROCTA 


MOSS ANIMALS 


Antropora tincta x xX x 
Bugula neritina xX X x x 
Crisia occidentalis xX 
Diaperoecia californica x xX xX 
Filicrisia franciscana X 
Lagenipora punctulata x X xX x 
Hippothoa hyalina 
Membranipo.a membranacea 
M. savarti? 
M. tuberculata X 
Phidolopora pacifica xX xX x X 
Rhyncozoon rostratum x ».4 x xX 
Scrupocellaria diegensis xX X x x 
Smittina sp.2 
Thalamorporella californica? 
Unid. encrusting ectoprocts x x x xX 
Unid. ectoproct #1 x x 
Unid. yellow ectoproct X xX 
PHYLUM ECHINODERMATA SEASTARS, URCHINS, 
BRITTLE STARS, 
CUCUMBERS 
CLASS ASTEROIDEA SEASTARS 
Astropecten armatus Sand starfish 
Patiria miniata Bat star x xX x x 
Pisaster brevispinus Pink seastar <a ».4 x 
P. giganteus Giant seastar Xx x x D4 
P. ochraceus Ochre seastar xX X x X 
P. sp. -(juv.) x 
Solaster dawsoni? Sunburst starfish 
CLASS ECHINOIDEA URCHINS 
Lytechinus pictus Pale urchin x 
Strongylocentrotus franciscanus Red urchin x xX X xX 
S. purpuratus Purple urchin x X x x 
CLASS OPHIUROIDEA BRITTLE STARS 
Ophiopsilla californica xX 
Ophiopteris papillosa2 Brittle star 
Ophiothrix spiculata x x 
Unid. ophiuroid x x 
CLASS HOLOTHUROIDEA SEA CUCUMBERS 
Cucumaria sp.2 Sea cucumber 
Dermasterias imbricata2 Leather star 
Eupentacta quinquesemita? Yellow sea cucumber 
Parastichopus californicus/ 
P. parvimensis3 x x x x 
Unid. holothuroid x x 
Unid. burrowing holothuroid x x 
PHYLUM CHORDATA CHORDATES 
CLASS ASCIDIACEA TUNICATES (Sea squirts) 
cf. Amaroucium californicum x 
Aplidium californicum 
Boltenia villosa X xX x 
Chelyosoma productum? Simple sea squirt 
Cystodytes lobatus2 Compound sea squirt 
Didemnum carnulentum x 


Pyura haustor 


See footnotes at end of table. 


Tunicate 


27 


Table 1. Master species list for Rincon Island.--Continued. 


» Scientific ae 


CLASS ASCIDIACEA (Continued) 
Styela gibbsii 
S. montereyensis 
S. sp. 
Unid. white tunicate 
Unid. orange tunicate 
Unid. encrusting pink tunicate 


CLASS CHONDRICHTHYES 
Cephaloscyllium ventriosum 
Cetorhinus maximus 
Heterodontus francisci? 
Prionace glauca? 
Rhinobatos productus2 
Sphyrna zygaena? 

Squalus acanthias 
Triakis semifasciata? 
Urolophus halleri? 


CLASS OSTEICHTHYES 
Alloclinus holderi? 
Amphistichus argenteus 
A. koelzi? 
Anisotremus davidsoni 
Artedius lateralis? 
Atherinops affinis 
Atherinopsis californiensis 
Brachyistius frenatus 
Cheilotrema saturnum 
Chromis punctipinnis 
Citharichthys sordidus? 
Clinocottus globiceps 
Clupea harengus pallasi 
Coryphopterus nicholsi 
Cymatogaster aggregata? 
Cynoscion nobilis 
Embiotoca jacksoni 
E. lateralis 
Genyonemus lineatus 
Gibbonsia metzi~ 
G. montereyensis? 
Girella nigricans 
Gymnothorax mordax? 
Halichoeres semicinctus? 
Heterostichus rostratus 
Hyperprosopon argenteum 
H. ellipticum? 
Hypsoblennius gilberti? 
Hypsurus caryi2 
Hypsypops rubicunda 
Leuresthes tenuis? 
Lynthrypnus dalli? 
Medialuna californiensis 
Mola mola? 

Myliobatus californica’ 
Oncorhynchus kisutch? 
Ophiodon elongatus 
Oxyjulis californicus 
Oxylebius pictus 
Paralabrax clathratus 
P. maculato-fasciatus2 


2 


See footnotes at end of table. 


Occurrence during present study 


Common name North West South East 
x 
x X x x 
x 
x 
xX 
x 


CARTILAGINOUS FISHES 
Swell shark 
Basking shark 
Horn shark 
Blue shark 
Shovelnose guitarfish 
Smooth hammerhead shark 
Spiny dogfish 
Leopard shark 
Round stingray 


BONY FISHES 
Island kelpfish 
Barred surfperch 
Calico surfperch 
Sargo 

Smoothead sculpin 
Topsmelt 
Jacksmelt 

Kelp perch 

Black croaker 
Blacksmith 
Pacific sanddab 
Mosshead sculpin 
Pacific herring 
Blue-spot goby 
Shiner surfperch 
White seabass 
Black perch 
Striped seaperch 
White croaker 
Striped kelpfish 
Crevice kelpfish 
Opaleye 
California moray 
Rock wrasse 
Giant kelpfish 
Walleye surfperch 
Silver surfperch 
Rockpool blenny 
Rainbow surfperch 
Garibaldi 
California grunion 
Bluebanded goby 
Halfmoon 

Ocean sunfish 
Bat ray 

Coho salmon 
Lingcod 

Senorita 

Convict fish 
Kelp bass 

Spotted sand bass 


28 


Table 1. Master species list for Rincon Island.--Continued. 


Occurrence during present study 


Scientific name 1 Common name North West South East 


CLASS OSTEICHTHYES (Continued) 


P. nebulifer 
Paralichthys californicus 
Pimelometopon pulchrum 
Platichthys stellatus? 
Phanerodon furcatus 
Porichthys spp. 


Barred sand bass 
California halibut 
California sheephead 
Starry flounder 
White seaperch 
Midshipman 


Rathbunella hypoplecta Smooth ronquil x x 
Rhacochilus toxotes Rubberlip seaperch 
Rhacochilus vacca Pile perch 
Sardinops sagax? Pacific sardine 
Scomber japonicus? Pacific mackerel 
Scomberomorus concolor? Monterey Spanish 
mackerel 
Scorpaena guttata California scorpionfish 
Scorpaenichthys marmoratus Cabezon xX 
Sebastes atrovirens Kelp rockfish 
S. auriculatus Brown rockfish x 
S. cf. caurinus Copper rockfish 
S. chlorostictus? Greenspotted rockfish 
Ss elongatus? Greenstriped rockfish 
S. miniatus2 Vermilion rockfish 
S. mystinus Blue rockfish 
S. paucispinis? Bocaccio 
Sig rastrelliger? Grass rockfish 
S. rubrivinctus? Flag rockfish 
S. serranoides Olive rockfish 
S. serriceps2 Treefish 
Se Sp. Hl 
95 Sjas ii 
Seriphus politus Queenfish 
Sphyraena argentea2 Pacific barracuda 
Symphurus atricauda? California tonguefish 
Syngnathus californiensis2 Kelp pipefish 
Thunnus alalunga2 Albacore 
Trachurus symmetricus? Mack mackerel 
Unid. blenny x 


al ; c A 
Taxa without superscript were observed during this study. 


2 : ; 
Taxa reported by Carlisle, Turner, and Ebert (1969) or Brisby 
in Keith and Skjei (1974), but not observed during this study. 


3 i : 
The two species were not differentiated during this study. 


29 


SCALE 


1= TALUS PRESENT BUT © 2= IRREGULAR POINT WHERE te) 10 20 
ONLY A THIN OVER— TALUS PRESENT, BUT Ce 
BURDEN ON ROCK CALCULATED AS BELOW 

EXTENDED SLOPE (=OFT) METERS 
DEPTHS SCALED TO MLLW 


Figure 5. North-side talus bed and armor rock measurements, 15 October 1976. 


30 


KEE 


(0) 60 120 


3| 


LLZZ 


L-AAA-ZTZZZZZZZZZZZ 
Z77---Z-ZZZZEZEE — 


METERS 
DEPTHS SCALED TO MLLW 


_ 7I7™”z =_— 


LBA 


Ta 


\ 


West-side talus bed and armor rock measurements, 15 October 1976. 


Figure 6. 


“961 LOGUOAON 61 ‘S}USWOINSesM YOOX LOWLe pue peq SNTe} eptTs-yyNos ‘7 san3TY 


(140=) 3d01S G30N31LX3 
MO138 Sv d31vqNndqVv2 4904 NO N3GuNB 
MTIW OL G31V9S SH1d3d ing ‘1N3S3Y¥d SNtVvL —-Y3AO NIHL Vv ATINO 
SualaW 3Y3HM LNIOd YvINDaNY! =z ing LN3S3ud SNIvl =1 


lnm) 
OL : 0) 


a1Wwds 


e111 / 


sualaw 


LY 
Lip 
Q> 


saw 


32 


x 
S 
Bs) 


SCALE 
0 10 20 
ee 
METERS 1= TALUS PRESENT BUT 
ONLY A THIN OVER— 
DEPTHS SCALED TO MLLW BURDEN ON ROCK 


Figure 8. East-side talus bed and armor rock measurements, 15 October 1976. 


33 


+ -@-© OUTLINE OF TALUS BED 


—-— TRANSECT LINES(DEPTH IN METERS BELOW MLLW) 


FIMAL ASSOCIATIONS BASED OM STATISTICAL COMPARISONS: 


- BARNACLE/LIMPET 

- MYTILUS/POLLICIPES 

. ANTHOPLEURA SPP 

» MACROPHYTIC ALGAE 

~ LITHOTHAMNIUM/VELEROA 

« VELEROA/LAGENIPORA/LOPHOGORGIA/MURICEA 
. RIODYMENTA/VELEROA. 

LITHOTHAMN] UM/TETRACLITA 
DIOPATRA/CERIANTHID ANEMONES 


H=ammonw> 


O10 20-30 40 __SOFEET 


C) 5 10 15 20 METERS 
— 


(FOR ACTUAL DISTANCES DOWN NORTH AND WEST SIDES, 
DIVIDE BY 0.893 AND 0.925, RESPECTIVELY) 


Figure 9. Major species associations, northwest quadrant. 


34 


(SCR ACTUAL DISTANCES DOWN WEST AND SOUTH SIDES, 


DIVIDE BY 0,925 AND 0.892, RESPECTIVELY) 


<3 


x E 
Sn 
~ 9-), 
~> 
TT . 
% ® 
: 
‘ 
My 


go 
bd AS 
id i 
x ~ s 
‘ get 
g Nowe 
PSP SS SSSS 
t 
+ 
¢ 
t 
+ 
— ¢ “ 
a + 
ce fe : = 
Se 
einer O-s N17 at 
11.9 EGE Ppa 
— 10.4 pa = ae 
Ze : = 5 
. a 81S mr i 
F 
C = E 
4p 
6.8 ~ 


\ e+e OuTLINe oF TALUS AcD 
| \\ HE vocari0y oF prrsnwent gaanscers 
sete —-—— TRANSECT LINFSIOEPTH IN METERS BELOW MLLW) 


/ FIMAL ASSOCIATIONS BASED OM STATISTICAL COMPABIGOMS: 


BARNACLE/LIMPET 

MYTILUS/POLLICIPES 

ANTIIOPLEURA SPP. 

MACROPHYTIC ALGAE 

~ LITHOTHAMNIUM/VELEROA 
VELEROA/LAGENIPORA/LOPHOGORGIA/MURICEA 
- RIODYM! VELEROA 

LITHOTHAMNJ UM/TETRACLITA 

+ DIOPATRA/CERIANTHID ANEMONES 


Hzanmong» 


© SAMPLE SIZE INADEQUATE FOR STATISTICAL COMPARISON 


E \ 
. —— 0 19 20 30 _40__SOFEET 
: ——= = S — 
Nh a 
\ \ 0 5 lo 15 20 METERS 


Figure 10. Major species associations, southwest quadrant. 


55 


TRANSECTS 


——-—- TRANSECT LINES(DEPTH IN METERS BELOW MLLW) 


FINAL ASSOCIATIONS BASED ON STATISTICAL COMPARISONS; 


A. BARNACLE/LIMPET 
B. MYTILUS/POLLICIPES 


- LITHOTHAMNIUM/TETRACLITA 
+ DIOPATRA/CERIANTHID ANEMON 


O10 2030 -40__SOFEET 


10 15 20 METERS 


(FOR ACTUAL DISTANCES DOWN SOUTH AND EAST SIDES, 
DIVIDE BY 0.892 AND 0.877, RESPECTIVELY) 


Figure 11. Major species associations, southeast quadrant. 


36 


P TALUS BEC 


TON OF PERMANENT TRANSECTS 


— TRANSECT LINES(DEPTH IN METERS BELOW MLLW) 


FIMAL ASSOCIATIONS BASED OM STATISTICAL COMPARISONS: 


A. BARNACLE/LIMPET 
B, MYTILUS/POLLICIPES 

ANTHOPLEURA SPP. 

IC ALGAE 

NIUM/VELEROA 
ENIPORA/LOPHOGORGIA/MURICEA 


D 
E 
= 
c 
4 
I 


* SAMPLE SIZE INADEQUATE FOR STATISTICAL COMPARISON 


50 FEET 


I 


Figure 12. Major species associations, northeast quadrant. 


Sil 


North side: 49 cubic meters 
East side: No significant accumulation. 


Moreuls 1,597 cubic meters 


These figures apply only to the talus beds shown in Figures 9 to 
12. The talus beds extended around the southwest and northwest wings 
of the island and contained a large volume of shell debris. At the 
west edge of each of these wings, talus beds were of dimensions 
similar to those lying along the west side. The beds diminished 
markedly on the flanks of the southwest and northwest wings where 
they adjoin the south and north sides, respectively, of the island. 
No significant shell talus accumulations were observed around the 
base of either the northeast or the southeast wing. 


The west-side talus beds, averaging 16.5 cubic meters per meter 
of lineal distance along the west revetment, were considerably more 
voluminous and extensive than the beds on the other sides. This is 
because the tetrapods on the west side supported a very heavy growth 
of mussels (Mytilus californianus) in the intertidal zone. Parts of 
this are sometimes removed by heavy surf, which is most pronounced on 
the west (seaward) side. Some of the detached mussels gravitate into 
quarry rock and tetrapod interstices, but many accumulate at the foot 
of the revetments. 


West-side talus beds were composed almost entirely of mussel 
shells, many of which were of unusually large size for this species. 
Paine (1976) reported a specimen of M. californianus exceeding 26.6 
centimeters in length from a subtidal mussel bed on Duncan Rock off 
Washington. The previous record was 25.1 centimeters, as reported by 
Chan (1973). A mussel measuring 25 centimeters has been reported at 
an offshore oil platform in southern California (Southern California 
Coastal Water Research Project, 1976). Although no measurements were 
taken on shells in the Rincon Island talus bed, many specimens appar- 
ently approaching this size were observed. Some shells of Pododesmus 
cepio were also present in the west-side talus area. The seaward 
boundary of the west-side talus bed (where it graded into natural 
sedimentary bottom) was very distinct and lacking in irregularities. 
The inner margin was somewhat irregular and interspersed with iso- 
lated rocks. Isolated pockets of talus existed above the upper 
margin of the main talus bed. 


In contrast, the east side was nearly devoid of shell talus. 
Only one pocket'of talus was observed, approximately 4 meters from 
the south boundary of the side. Small mounds of mussel shells were 
observed at the bases of causeway pilings. The east side is the most 
sheltered side, and appears to act as a deposition site for sediment 
carried to the rear of the island in turbulent eddies (Keith and 
Skjei, 1974). The middepth and deeper parts of the east-side re- 
vetments were always overlain by a veneer of fine sediment: the 


38 


transition from rock revetment to sedimentary bottom is distinct, 
primarily because of a contrast in slope of the two substrate types. 


The north- and south-side talus beds are intermediate in size 
between those of the west and east sides. The upper and lower mar- 
gins are highly irregular on both the north and south sides. Some 
"fingers' of talus extend more than 3 meters up the north-side re- 
vetment, and an isolated shallow pocket of talus exists in a flat 
area about half way down the side near the location of the permanent 
transect. The sediment lying near the base of the island on both the 
north and south sides is inclined, possibly because it overlies a 
buried part of the talus bed. Many isolated rocks punctuate the 
natural bottom sediment, particularly along the north side. Shells 
of the bivalves, Pododesmus cepio (jingles), Hinnites multirugosus 
(rock scallop), and unidentified species form the bulk of the talus 
beds on the north and south sides. Some Mytilus talus exists near 
the west end of the north side which may have been carried around 
from the west side by currents. Biota frequently encountered in 
association with the talus beds include the tube worm, Diopatra 
ornata; the tube anemone, Pachycerianthus sp; the nudibranch, 
Dendrodoris fulva; the whelk, Kelletia kelletii; the bat star, 
Patiria miniata; and hermit crabs including Paguristes ulreyi and 
Isocheles pilosus. 


Sr Analysis of Seasonal Data from Permanent Transects. 


An overview of the vertical distribution of tentatively discrimi- 
nated major species associations, synthesized from data of the first 
two seasonal permanent transect surveys (summer and fall, 1976) is 
graphically represented for each side of the island in Figures 13 to 
16. Figures 17 to 20 augment information provided in Figures 13 to 
16 by illustrating the vertical distributions of selected dominant 
macrobiota over the permanent transects. A broad vertical pattern 
for Patiria miniata is apparent on all sides. Also noteworthy is the 
dominance of the Lithothamnium-Lithophyllum complex over the upper 
reaches of all but the east side. The east side also appears unique 
in that distributions of several species are much less restricted 
vertically than is the case on the other sides (e.g., the red algae, 
Veleroa subulata-Murrayellopsis dawsonii complex and the abundant 
ectoproct, Lagenipora punctulata). 


A total of 250 taxa of macrobiota was identified during the four 
seasons of the permanent transect sampling program. These taxa are 
listed in Table 1 together with information on which side of the is- 
land each occurred. The species occurring in transects on all four 
sides of the island may be regarded as ubiquitous and generally the 
dominant macrobiota over the entire island. Many of the species listed 
in Table 1 undoubtedly occur on more sides of the island than indi- 
cated. An example is the giant kelp, Macrocystis sp. Kelp is most 


39 


Waterline 
(MLLW) 


Depth MLLW 
(m) 


LITHOTHAMNION 


with Muricea 
MACROPHYTIC 
ALGAE ZONE 
BARNACLE/LIMPET ZONE 


Transition 
present 


10 | 


| 
Distance (meters) 


@ 


©) i) 


SUBSTATE: SCATTERED ROCKS WITH TALUS ROCKS WITH SOME POCKETS ROCK ROCK 
OF COBBLES 


DOMINANT BIOTA: Cerianthid anemones Muricea spp. Gelidium robustum Collisella spp. 


Astrangia lajollaensis Dodecaceria fewkesi Corallina officinalis Lottia gigantea 


Lophogorgia chilensis Serpulorbis squamigerus Prionitis lanceolata Pachygrapsus crassipes 


Phidolopora pacifica Lithothamnion complex Egregia laevigata Balanus glandula 


Diopatra ornata Veleroa/Murrayellopsis complex Chthamalus fissus 
Tetraclita squamosa 


Figure 13. Seasonal overview of distribution of major species 
associations and substrate character, north-side 
permanent transect. 


40 


41.5 


Waterline 
(MLLW) 


TRANSITION LITHOTHAMNION 


ZONE 


TALUS SLOPE 


ZONE 


MUSSEL/GOOSENECK BARNACLE ZONE 


MACROPHYTIC ALGAE ZONE 
BARNACLE/LIMPET ZONE 


SUBSTRATE 


DOMINANT BIOTA 


SUBSTRATE: 


DOMINANT BIOTA: 


TALUS WITH 


ISOLATED ROCKS 
Cerianthid anemones 


Doriopsilla albopunctata 


Muricea spp. (R)* 


Diopatra ornata 


Corynactis californica (R) 


@ 


TETRAPODS 


Egregia laevigata 


Coralline algae 


Stenogramme interrupta 


(R) = Associated only with isolated rocks in 
this zone 


Figure 14. 


Seasonal overview of distribution of major species 


Distance (meters) 


@ 


ROCK 


Corynactis californica 
Veleroa/Murrayellopsis complex 
Lagenipora punctulata 
Scrupocellaria diegensis 


Phidclopora pacifica 


© 


TETRAPODS 


Mytilus californianus 


Pollicipes polymerus 


TETRAPODS 
Lithothamnion complex 
Serpulorbis squamigerus 


Dodecaceria fewkesi 


Strongylocentrotus purpuratus 


© 


TETRAPODS 


Balanus glandula 
Chthamalus fissus 
Collisella spp. 


Lottia gigantea 


associations and substrate character, west-side 
permanent transect. 


4 


SUBSTRATE ; 


DOMINANT BIOTA: 


SUBSTRATE: 


DOMINANT BIOTA 


TRANSITION ZONE 


LITHOTHAMNION 
|ZONE 


MACROPHYTIC ALGAE ZONE 


BARNACLE/LIMPET ZONE 


Waterline (MLLW) 


Depth MLLW 


TALUS WITH ISOLATED ROCKS 


Cerianthid anemones 
Diopatra ornata 

Astrangia lajollaensis (R)* 
Lophogorgia chilensis (R) 


@ 


ROCK 
Lithothamnion complex 
Dodecaceria fewkesi 


Strongylocentrotus purpuratus 


(Note: Veleroa very sparse 
in this zone) 


(R) = Associated only with isolated rocks 
in this zone 


20 
Distancq (meters) 


@ 


ROCKS WITH TALUS POCKETS 


Corynactis californica 
Lagenipora punctata 
Scrupocellaria diegensis 
Phidolopora pacifica 


© 


ROCK 


Gelidium coulteri 
Corallina officinalis 
Lithothamnion complex 
Codium fragile 


Tetraclita squamosa 


ROCK 


Lithothamnion complex 


Veleroa/Murrayellopsis complex 
Serpulorbis squamigerus 


© 


ROCK 

Lottia gigantea 
Collisella spp. 
Chthamalus fissus 
Balanus glandula 
Pachygrapsus crassipes 


(}) Not a separate zone but shows less Veleroa and greater 
Lithothamnion coverage than the lower zone 3. 


Figure 15. Seasonal overview of distribution of major species 
associations and substrate character, south-side 


permanent transect. 


TETRACLITA 
ZONE 


| } ZONE 
| +09 


PILING 


LOPHOGORGIA| TRANSITION 
ZONE ZONE 


PILING 


Depth MLLW 
(a) 


® 


SUBSTRATE : ROCK WITH SILT 


DOMINANT 


BIOTA ; Lophogorgia chilensis 


Corynactis californica 
Veleroa/Murrayellopsis complex 
Scrupocellaria diegensis 


Serpulorbis squamigerus 


10 pDistance| (meters 


@ 


ROCK 


Veleroa/Murrayellopsis complex 


Dodecaceria fewkesi 


Lagenipora punctulata 
Scrupocellaria diegensis 


(20 | 


®@ | ® | @ 


r at 


@ 


ROCK 


Lithothamnion complex 


Lagenipora punctulata 
Veleroa/Murrayellopsis complex 


(Ny, BARNACLES/LIMPET 


Waterline 


(MLLW) 


@ 


ROCK 
Tetraclita squamosa 
Collisella spp. 
Lottia gigantea 


Balanus glandula 


Chthamalus fissus 


Figure 16. Seasonal overview of distribution of major species 


associations and substrate character, east-side 
permanent transect. 


43 


tal 
o 4 
a EY % 
* Q tl un 2) is) 
o 5 vu 4 Gal za 
= 4 Dd a Q S % 
12] Qy ro) 1) 1 . S C q\ vv 
3 E 0 E a oO 0 (<) % 
2 ° % “< o a, 4 oq 4 rt) 
% £0) 13) v = 3 0) vu “4 ion 4 ie) 
4 q v oO o v << Oo i) & 
os wv Ss 4 Y Q n % (3) ~ % 3 
al gu is) 5 3 s 0 vu is) Q 
fs MB Q % ) Q 4 oO % |] a) 
al Og g 3 al al Q fe) Qy tal a) % U 
n E Ow [= a) Ny Q C a dD a) | 4 bea 
o 40 cy oO re (3) % q 4 v Q s 
Yn Lal % Dw c vu 16) fo) "4 KK vu fe) d ie) v 
7s) is} aa BH oO % bal v v o d S % ta] Ss 
v o is iis) Q is iS) 3 1) % aS) Q A Ss g % 
Q, Ss Tr) OSs eS ie) oO Q % Q q << 4 =) a) atl 
Bo te) eS ge 0S) t yal oe ee Slee men Ch 
al % al 7 
4 a Q HAY HN 5 Q Lop) Ay Q = g x 1s) ny 1S) 


Coan 150/ (%) 8/1 9/1 (%) (%) (%) 73/ 3/1 100/ 7/1 4/1 (%) (%) (%) 60/ 
(m2) 10 100/ 100/ 90/ 26/ 1 1 10/ 10/ 20/ 1 
: 20 i eas yp eben 

(1) 


Values below each column indicate maximum (upper value) 

and minimum (lower value) densities encountered in 1-square 
meter quadrats over those depths where each species occurred. 
Values below the (%) signs represent percent coverage for 
encrusting forms. The remaining values represent numerical 
densities. 


Figure 17. Vertical distribution for dominant biota, north side. 


44 


(il 


% % 
* | 4 73) ~ a 
ery ‘a 3 0 v 3 A s 
Oy as] y # S ~ % ~ % ‘4 
7) s mi i} 3 7) “41 ar) is uy 
ci Se pea 8 ‘A S (ty ise % Yu q % 
0 4 Os] a £ 3 Cl tl “4 a5 c “OO SM 4 re) ~ 
4 D fal a oO E Quy fag Mm waa HY ee) 
4 ce gi g sits} Cy Oy ye) OS Qs 9 % 4 U4 
o 4 YW Tw SK aX ADT ON © OM VWH DW GH An BV H 970 04 
a 3 30 On HO OO WH DH AH AH DH HE BOND O b nO c 
gl Sai AGS OA re) ied) ORG Ky eis Maly Wat SCS) fet) O-n R60 
4 G ed PA SO oO a WX cd Rus RS VG HH GO US & ao 3b 
ol 4 tn 4 2 Is ae AN O> @ Gs TMH HN DE SH 0 NHS HY 
fo) Gg De Sax A ao OW ge Ss OS SH AN OG R38 O03 vA 54 Ov 
.S) gm =u PA HO SO OO H & HH PH Ah VO 2&2 AG QA FH HV 
60 se) ze) 
Q H 


50 


+ 
eit 
a 

| 


40 


d---- 


30 


20 


— <q] 

e— —ee— 
tof - - 
pet: - 


10 


1 
Max/Min 120/ (%) (%) 39/1 (%) (%) (%) (%) 15/ 28/ 9/1 3/1 (%) (%) 4/1 98/7 10/ (4) 
(m2) 1 35/ 100/ MOO/ Bo)? HO/ 257 “1 Tl 60/ 20/ 2 OY; 
1 3 1 sty Sie Si i oR iL 
(1) 


Values below each column indicate maximum (upper value) 

and minimum (lower value) densities encountered in 1-square 
meter quadrats over those depths where each species occurred. 
Values below the (%) signs represent percent coverage for 
encrusting forms. The remaining values represent numerical 
densities. 


Figure 18. Vertical distribution for dominant biota, west side. 


45 


y 
es %  & u 
4 vo “4 vO 4 
ii a 1 g Dd a] 7) 
S jon n q Ta v i= 
GAS Q ® Wo 
| fo} xX oo a % v o 
1) ie) is) 4 % Ry ty) al 3 is} to 
o wv “4 3 v v Oy] oS & fo} ° v % 
Ls Lan wy S n S % w 4 0 a 3 7> q A 
al 3 w ie) 5 8 4 3 is) Q % q 
oS ee Sah re MG MSO oe See, eb Mu gchas 
oO hy © 5 5 Ga) E wy 7) > Q q 6 in) 
v “ 5 ag 3 8) 0 sf q g 3s On 
q tr) "i fs a, S % O wx OO fey a H OO 
is) v 5 4 xy rm) 4 % 4 % OO ra ste S Seas 
6 us} tal 9 By q is} is} a is} 3 S % x O 
S a ba) 4 % S Q Ww ia oO oa Q a) q BD 
4 E is] 4 yy rt) ee) UO 5 re 4 co v ie) Yo 
© Q is) fy) e) “A . . % 2 o 3° i) 8 Lo) Ba) Gey 
a ee S & § SF & & & So § 4 = Qa aD 
40 
1 1 
a hh op 1 
30 
@ 


hes 

cod} gs 

| 

- 4 
--| 


st 


@id) , 
30/ 110/ (%) (%) (%) (%) 29/7 6/1 10/ (%) (%) (%) 48/7 (%) (8) 50/ (8) 
oe IM BY AS) BO? Gor Heap “a 1 30/2 90/457) al (50/1257, Il 140/, 
Loris eae ee te see eka 1 
(1) 


Values below each column indicate maximum (upper value) 

and minimum (lower value) densities encountered in 1-square 
meter quadrats over those depths where each species occurred. 
Values below the (%) signs represent percent coverage for 


encrusting forms. The remaining values represent numerical 
densities. 


Figure 19. Vertical distribution for dominant biota, south side. 


46 


Serpulorbis squamigerus 
Corynactis californica 


Lithothamnion complex 
Lagenipora punctata 
Patiria miniata 
Parastichopus sp. 
Dodecaceria fewkesi 
Strongylocentrotus 
purpuratus 
Phidalopora pacifica 
Velorea subulata 
Lophogorgia chilensis 


complex 
Scrupocellaria 


diegensis 


nw 
ov 
a 
12} 
oO 
i= 
My 
oO 
a 


Limpets 


40 


30 


10 


CER. - 
5s 2 
ee ae 
fee = 


1 
@Oiax/min (s) 35/ (8) (%) go/ 9/1 6/1 (%) 26/ (%) (%) (8) 5/1 (8) 
(m2) 100/ 6 25/ 85/ 1 50/ 1 10/ 30/ 95/ 80/ 
7 1 al 


(1) 


Values below each column indicate maximum (upper value) 

and minimum (lower value) densities encountered in 1-square 
meter quadrats over those depths where each species occurred. 
Values below the (%) signs represent percent coverage for 
encrusting forms. The remaining values represent numerical 
densities. 


Figure 20. Vertical distribution for dominant biota, east side. 


47 


abundant on the south end of the west side of the island, but sparse 
in the central part, which is where the transect was located. This 
small kelp bed on the southwest wing of the island varied considerably 
in size during the course of the study. Heavy wave action and grazing 
by sea urchins may have offset normal seasonal growth. Also, many 
species, in addition to those listed in Table 1, have distributions 
that did not coincide with the permanent transects. Some of these 
were collected during quantitative characterization of major species 
associations using randomly placed quadrats. Others were found dur- 
ing reconnaissance dives. 


The analysis of the permanent transect data for significant sea- 
sonal differences in species densities is summarized in Appendix B, 
Table B-1. Table 2 provides a summary of the permanent seasonal tran- 
sect data. The table shows that a total of 37 of the 52 taxa (71 
percent) examined exhibited significant variability in mean abundance 
in the transects, apparently due in most cases to seasonal changes in 
population densities. Twenty of these taxa were absent from the 
transects during one or more seasons. Seventeen taxa showed signifi- 
cant seasonal differences despite being present in the transects 
during all four seasons. Table 2 also indicates the side of the 
island and season of maximum abundance in the transects for each 
species. 


Among echinoderms, the urchins (Strongylocentrotus franciscanus 
and S. purpuratus) and cucumbers (Parastichopus spp.) showed apparent 
seasonal differences, while none of the four starfish species examined 
were Significantly variable. The results for motile species such as 
these must be interpreted with caution: seasonal differences may re- 
flect changes in distribution rather than actual variations in abun- 
dance. All three ectoproct (moss animal) species examined, which 
collectively account for the bulk of ectoproct biomass on the island, 
showed seasonal variability. Gorgonians of genus Muricea varied sea- 
sonally; Lophogorgia chilensis did not. Among other coelenterates, 
significant differences were shown by the anemone, Corynactis 
californica, and the coral, Paracyathus stearnsii, but not by 
Anthopleura sp. or Astrangia lajollaensis. The two sponges examined 
showed seasonal differences. Most of the red algae species (Codes 22 
to 45 in Table 2, and Table B-1) were seasonally variable, as was 
expected. The only exceptions were Laurencia pacifica, Prionitis 
lanceolata, and Rhodoglossum affine. Most red algae showed peak den- 
sities in spring and summer, as was the case with the green algae 
(Codes 1 to 6 in Table 2, and Table B-1) and generally with the 
browns (Codes 11 to 20). Conversely, the widely distributed blue- 
green alga, Phormidium sp., was most abundant during the winter. 


48 


Table 2. 


Species 


Common Name 


Enteromorpha sp. 
Ulva sp. 
Codium fragile 
Cystoseira osmundacea 
Egregia menziesii 
Unid. juv. laminariales 
Dictyota flabellata 
Bossiella orbigniana 
Corallina officinalis 
Gelidium coulteri 
G. robustum 
Gigartina canaliculata 
G. exasperata 
Laurencia pacifica 
Lithothamnion- ; 
Lithophyllum complex 
Peyssonellia sp. 
Prionitis lanceolata 
Rhodoglossum affine 
Rhodymenia sp. 
R. californica 
Stenogramme sp. 
S. interrupta 
cf. Phormidium sp. 
Cliona sp. 
Hymenamphiastra cyanocrypta 
Anthopleura sp. 
Astrangia lajollaensis 
Corynactis californica 
Lophogorgia chilensis 
Muricea spp. 
Paracyathus stearnsii 
Anomia peruviana 
Pododesmus cepio 
Doriopsilla albopunctata 
Kelletia kelletii 
Lottia gigantea 
Megathura crenulata 
Mytilus californianus 
M. edulis 
Serpulorbis squamigerus 
Diopatra ornata 
Dodecaceria fewkesi 
Eudistylia sp. 
Lagenipora punctulata 
Phidalopora pacifica 
Scrupocellaria diegensis 
Parastichopus spp. 
Patiria miniata 
Pisaster brevispinus 
P. giganteus 
P. ochraceus 


Strongylocentrotus franciscanus 


S. purpuratus : 


Sea lettuce 
Deadman's fingers 


Boring sponge 

Blue leaf sponge 
Anemone 

Colonial coral 
Colonial red anemone 
Pink gorgonian 
Gorgonians 

Solitary coral 
Jingles 


Yellow sea slug 
Kellet's whelk 

Owl limpet 

Giant keyhole limpet 
California mussel 
Bay mussel 

Scaled worm shell 
Worm 

Worm 
Feather-duster worm 
Moss animal 

Lace moss animal 
Moss animal 

Sea cucumber 

Bat star 

Pink seastar 

Giant seastar 

Ochre seastar 

Red urchin 

Purple urchin 


1 
Species code referenced in Appendix B, Table B-1. 


*(s) 
'S) 
NS 


Significant, based on absence during one or more seasons 
Significant, despite presence during all seasons 
Not significant at the 95 percent confidence level 


49 


Seasonal transect data summary. 


Seasonal 


Variability’ 


(S) 
NS 
(S) 
(S) 
NS 
(S) 
(S) 
(Ss) 
Ss 
(S) 
(S) 
(S) 
(S) 
NS 


High Densit 


Side 


East 
East 
South 
North 
West 
East 
West 
West 
South 
South 
North 
East 
West 
West 
South 


South 
North 
North 
East 
North 
North 
East 
East 
West 
East 
South 
East 
West 
East 
North 
East 
East 


West 
West 
South 
West 
North 
North 
North 
South 
North 
North 
East 
East 
East 
East 
North 
North 
West 
East 
North 
West 


Season 


Summer 
Summer 
Summer 
Spring 
Summer 
Fall 

Spring 
Spring 
Summer 
Fall 

Spring 
Winter 
Summer 
Winter 
Spring 


Winter 
Spring 
Summer 
Spring 
Winter 
Summer 
Summer 
Winter 
Winter 
Summer 
Spring 
Spring 
Spring 
Spring 
Winter 
Winter 
Spring 


Summer 
Spring 
Summer 
Summer 
Spring 
Winter 
Fall 

Fall 

Summer 
Winter 
Fall 

Summer 
Fall 

Spring 
Winter 
Summer 
Winter 
Winter 
Spring 
Fall 


4. Distribution of Major Species Associations. 


Dendograms resulting from the computer analysis are presented 
in Appendix C. The species groups identified by the computer generally 
agreed with the field observations. Clusters are particularly distinct 
for intertidal associations, as might be expected. On the basis of 
this exercise and first-hand field observations, the following 13 
species associations (not including the shell talus beds) were tenta- 
tively identified and designated with generic names of conspicuously 
dominant species: 


Diopatra/cerianthid anemones 
Astrangia/gorgonians 
Lagenipora/Scrupocellaria 

Lithothamnium complex/Serpulorbis/Veleroa 
Macrophytic algae 

Mytilus/Pollicipes 

Barnacles/limpets 

Corynactis/Astrangia 

Lithothamnium complex/Serpulorbis/Dodecaceria/Veleroa 
Astrangia/Corynactis/Lophogorgia 
Tetraclita/Lithothamnium complex 
Lithothamnium/Lagenipora/Veleroa 
Lophogorgia/Corynactis/Veleroa 


lo Oe 2 oe © a’) 


The results of the fieldwork which entailed charting of the bound- 
aries of these preliminary or tentatively identified associations rela- 
tive to permanent features on the island are shown in Appendix C (Figs. 
C-3 to C-6). The scale on each of these charts may be used to determine 
plan view distances and actual (i.e., measured down the slope of each 
side) distances of all association boundaries from permanent features 
on the island. Permanent features include: navigational warning 
devices, surveyor triangulation points, and corners of concrete 
planter boxes used for landscaping the island. 


Over most transects, boundaries between associations were distinct. 
Certain areas which appeared to have characteristics in common with 
adjacent associations are labeled "transition" zones in the charts. 

The intertidal associations 5, 6, 7, and 11 were particularly dis- 
tinct. They contained species not found in other associations, their 
boundaries were sharply defined, and they were generally much nar- 
rower than the remaining (subtidal) associations. Associations 4 and 
9, characterized by heavy coverages of Lithothamnium complex, accounted 
for the largest subtidal area of the island. 


The east (protected) side differs in the general pattern of as- 
sociations from the other three (more exposed) sides. Over most of the 
east side, sea cucumbers (Parastichopus), gorgonians (Muricea, 
Lophogorgia), stony corals (Astrangia, Paracyathus), and ectoprocts 
(Lagenipora, Scrupocellaria) occurred in abundance. These groups were 


50 


generally restricted to the deeper waters on the other three sides. On 
the east side, a layer of silt varying in thickness from a few milli- 
meters to over a centimeter covered most rock surfaces up to the lower 
intertidal. This silt precludes growth of some encrusting organisms 
(especially Lithothamnium complex), while others (e.g., Veleroa com- 
plex) seem tolerant of it. 


Se Quantitative Characteristics of Major Species Associations. 


The following average biomass values were developed for common 
attached biota not amenable to routine quantitative removal from the 
substrate: 


Dodecaceria fewkesi (animals only, no tubes): 465 grams per 
0.25 square meter 

Lithothamnium complex: 783 grams per 0.25 square meter 

Serpulorbis squamigerus (animals only, no shells): 1.9 grams 
per individual 

Veleroa complex: 242 grams per 0.25 square meter 

Corynactis californica: 190 grams per 0.25 square meter 


When the 250 quantitative quadrats were grouped according to the 
preliminary association in which the quadrat was placed and the side 
of the island sampled, 26 groups or "subareas'' resulted (see App. D, 
Table D-1). The designation of each of the 26 subareas in Table D-1 
corresponds to the numerical association designations in Figures C-3 
to C-6. For example, the data in Table D-1 for south-side association 
5, refer to the macrophytic algae association on the south side only. 
Data for this association in other areas of the island are found under 
correspondingly different designations. 


For all species encountered in each of the 26 subareas, the fol- 
lowing summary statistics are tabulated in Tables Dl and D-2: fre- 
quency of occurrence (ratio of occupied quadrats to total number of 
quadrats examined in the subarea; mean abundance per quadrat (numer- 
ical or percent coverage); 95-percent confidence limits for mean 
abundance; and average weight per individual (or per 100-square 
centimeter coverage for species with densities estimated as percent 
coverage). Multiplication of the value for mean density by the aver- 
age weight value yields an estimate of biomass for any species in any 
of the 26 groupings. Reliability of this estimate will be best for 
common species whose densities are relatively uniform from one 
quadrat to the next, as indicated by relatively narrow confidence 
limits for the mean. Table D-3 contains information on areas covered 
by each of the 26 subareas which were subjected to statistical 
analysis. 


The resulting biomass data are useful in characterizing and com- 
paring the major species associations of Rincon Island. However, the 


S| 


data are of limited use beyond this for species whose weight is 
largely composed of nonliving material (e.g., clams, stony ectoprocts). 


Species associations as determined by statistical differences 
within and between the 13 preliminary associations on each side of 
the island are shown in Figures 9 to 12. These associations may be 
compared with the preliminary species associations of Figures C-3 to 
C-6. Based upon statistical analysis, 4 of the 13 preliminary associ- 
ations were combined with other associations, resulting in a total 
of 9 distinctly different major species associations. Areas covered 
by each of these final associations are given in Table D-3. 


The quantitative characteristics of these major species associ- 
ations are discussed below. 


a. Barnacle-Limpet Association. This uppermost association 


(association A in Figs. 9 to 12) was relatively uniform in composi- 
tion on all sides of the island. Dominant biota include acorn barna- 
cles (Chthamalus fissus, Balanus glandula, and Tetraclita squamosa, 
in descending order of abundance) and limpets (Collisella digitalis, 
C. scabra, and Lottia gigantea). 


The thatched barnacle, Tetraclita squamosa, was the species with 
the highest biomass in the aggregate samples. The only algae occur- 
ring in the samples from this zone were small amounts of Enteromorpha 
sp. and patches of Ralfsia sp. 


b. Mytilus/Pollicipes Association. This association (associ- 
ation B in Figs. 9 to 12) is largely confined to a narrow band (about 
2 meters wide) on the west side of the island. A small area of this 
association also exists on the southwest wing, but it was not sam- 
pled. The association is dominated in biomass by the California 
mussel (Mytilus californianus), which has an average biomass of 16.9 
kilograms per square meter, and gooseneck barnacles (Pollicipes 
polymerus) which average 1.0 kilograms per square meter. A few 
limpets, striped shore crabs (Pachygrapsus crassipes), and acorn 
barnacles (Balanus spp.) are also found here. Small bay mussels 
(Mytilus edulis) were common below the surface layer of larger 
California mussels. Both species also occur in small numbers on the 
north and south sides, but only M. edulis was found on the east (most 
sheltered) side. Algae occurring in this association include 
Bossiella orbigniana and Lithothamnium complex. The Mytilus- 
Pollicipes association is higher in biomass per unit area than any 
other association on the island. — 


c. Anthopleura spp. Association. This association (associ- 
ation C in Figs. 9 to 12) is composed almost entirely of green 
anemones of the genus Anthopleura. Although Anthopleura spp. occur 
in large numbers in the macrophytic algae zone, their occurrence in 


52 


large patches which could reasonably be labeled as a distinct associ- 
ation was limited to a few areas on the southeast and northeast 
"wings'' of the island. 


, 


d. Macrophytic Algae Association. The macrophytic algae 


association (association D in Figs. 9 to 12), extends around the 
island in a continuous band except on the east side under the wharf, 
where light is presumably the limiting factor. Its composition is 
variable from side to side. Statistical comparisons between associ- 
ation D in various parts of the island and association E on the north 
side (the type Lithothamnium association) generally showed no signifi- 
cant differences for the three taxa selected as characteristic domi- 
nants for association E (Lithothamnium complex, Veleroa complex, and 
Dodecaceria fewkesi). The only exceptions were the south side, 
which had significantly less Veleroa and Dodecaceria than association 
E, and the southeast wing, which had significantly less Veleroa. 
Thus, it appears reasonable to consider association D as an extension 
of association E, overgrown by macrophytes to depths where physical 
conditions (including illumination) are favorable. 


Lithothamnium dominates algal biomass on all sides of the island. 
The macrophytic algae zone on the south side is unusual in that 
Lithothamnium complex there is composed of much thicker and irregular 
patches than elsewhere on the island. The south side also supports 
the densest growths of a coralline alga (Corallina officinalis) and a 
green alga (Codium fragile). Other common species on the south side 
include feather boa kelp (Egregia menziesii), Gelidium robustum, and 
Gigartina canaliculata. The north side also supports substantial 
beds of Egregia. Other north-side macrophytic dominants include 
Prionitis lanceolata and Gelidium robustum. Cystoseira osmundacea 
and coralline algae are abundant in some areas of the north side. 
Quantitative data for the west side are of limited value in character- 
izing the macrophytic algae because none occurred in any of the ran- 
dom west-side quadrats. Qualitative observations and results of the 
seasonal surveys suggest that this zone is dominated by Egregia, 
Cystoseira, coralline algae, and Gigartina canaliculata. A bed of 
giant kelp (Macrocystis sp.) is located at the south end of the west 
Side of the island. Judging from earlier air photos, however, the 
present kelp bed is small compared to the extensive beds that have 
existed in the past. Large numbers of sea urchins now exist on the 
island and may account for this phenomenon. It is possible that kelp 
and urchins alternate in cycles of abundance on the island. The in- 
verse relationship between urchin and algae abundance has been dis- 
cussed, for example, by North (1962). 


e. Lithothamnium-Veleroa Association. 


The Lithothamnium association (association E in Figs. 9 to 
12) is characterized by high concentrations of Lithothamnium complex, 


53 


Veleroa complex, and Dodecaceria fewkesi. Macrophytic algae and 
deeper dominants such as Corynactis, Astrangia, gorgonians, and 
ectoprocts are scarce. An exception to this generalization is found 
on the north side, where a dense band of gorgonians (Muricea 
fruticosa and M. californica) exists (see Figs. 9 to 12). Dense 
growths of ectoprocts (mostly Lagenipora punctulata, Scrupocellaria 
diegensis, and Phidolopora pacifica) and Serpulorbis squamigerus are 
found at the bases of the gorgonians, apparently taking advantage of 
sheltered habitat conditions. A quadrat from the northeast wing 
Lithothamnium-Veleroa association (outside the dense Muricea band) 
produced the highest number of species (37) of all 250 quadrats 
analyzed. Bat stars (Patiria miniata) and urchins are abundant over 
the Lithothamnium-Veleroa association on all sides. The giant key- 
hole limpet (Megathura crenulata) is frequently encountered here, as 
are sea cucumbers (Parastichopus californicus and P. parvimensis). 
This association accounts for more subtidal areal coverage than all 
other associations combined and it is highly uniform in species 
composition around the island. Despite relatively intensive sampling, 
no statistically significant differences in biomass of the character- 
istic dominants (Lithothamnium, Veleroa, and Dodecaceria) were found 
between this association on the ncrth side and similar associations 
elsewhere on the island (associations 4, 9, and 12 in Figs. C-3 to C-6 
were found not significantly different from the north-side 
Lithothamnium-Veleroa association). 


Bo Veleroa-Lagenipora-Lophogorgia-Muricea Association. 


In deeper areas of the Lithothamnium zone around the island, 
the upper parts of the rocks support species representative of that 
association, while ectoprocts abound on the side and undersurfaces. 
Deeper yet, the dominant taxa are distinctly different from those 
characteristic of the Lithothamnium association. Taxa commonly oc- 
curring in this area include Veleroa complex, solitary and colonial 
corals Paracyathus stearnsii, Balanophyllia elegans, and Astrangia 
lajollaensis), gorgonians Muricea spp. Lophogorgia chilensis), 
colonial anemones (Corynactis californica), ectoprocts 
(Scrupocellaria diegensis, Lagenipora punctulata, and Phidolovora 
pacifica) and the scaled worm shell gastropod, Serpulorbis 
Ssquamigerus. During the phase of work involving charting of the major 
species associations, five associations were provisionally discrimi- 
nated (2, 3, 8, 10, and 13 in Figs. C-3 to C-6) in this deeper area. 
Although this group of associations is distinctly different from the 
Lithothamnium association, there was no statistical reason on the 
basis of the data and observations to separate any of the five pre- 
liminary associations from one another. Accordingly, these deep as- 
sociations are combined under the letter designation F in Figs. 9 to 
12. A large "transition zone'' on the west side was not significantly 
different from the Lithothamnium association; however, two smaller 
transition areas, one on the northwest wing and one on the southeast 
wing, were significantly different. 


54 


g. Rhodymenia-Veleroa Association. 


On the east side, an association exists which is signifi- 
cantly depauperate in Lithothamnium complex and significantly en- 
riched (relative to adjacent Lithothamnium associations) in the red 
alga, Rhodymenia sp. This is the Rhodymenia-Veleroa association, 
labeled G in Figs. 9 to 12. High densities of Veleroa complex, 
ectoprocts, colonial anemones, corals, Serpulorbis squamigerus, and 
the densest growths of Dodecaceria fewkesi on the island are found 
here. Nudibranches, especially Flabellinopsis iodinea, are also 
common in this zone. The more fragile branching ectoprocts which 
occur in deeper water on all four sides of the island exist at shallow 
depths only on the east side, apparently because wave forces are much 
reduced relative to the other three more exposed sides. 


le Lithothamnium-Tetraclita Association. 


Above the Rhodymenia-Veleroa association (association G) on 
the east side, an association composed almost entirely of Lithotham- 
nium complex and the large thatched barnacle, Tetraclita squamosa 
occurs over extensive shallow subtidal and intertidal areas (associ- 
ation H in Figs. 9 to 12). Although the two species are found in 
association in other parts of the island's intertidal and shallow sub- 
tidal areas, these occurrences are very limited in extent. 


Th. Diopatra-Cerianthid Anemones Association. 


Small pockets of shell talus, usually partially covered 
with silt, are commonly found in the deeper areas of association F. 
These areas are designated as association I in Figures 9 to 12, and 
they extend over the talus beds to the natural bottom. The tube 
worm, Diopatra ornata; tube anemones, Pachycerianthus spp.; bat 
stars, Patiria miniata, and nudibranches (Dendrodoris fulva) are 
very common in these associations. 


6. Gill Net Survey Results. 


Results of the gill net survey are summarized in Table 3. The 
nets yielded a total of 270 fishes of 23 species. Five taxa ac- 
counted for 61 percent of individuals captured. In decreasing order, 
they were: olive rockfish, Sebastes serranoides; midshipman, 
Porichthys spp.; walleye surfperch, Hyperprosopon argenteum; swell 
shark, Cephaloscyllium ventriosum; and white seaperch, Phanerodon 
furcatus. Four of these species (all except C. ventriosum) were 
captured on all four sides of the island. The highest number of 
individuals and species was captured on the east (most protected) 
side of the island. Average catch rates were highest during the day 
on the west side, lowest on the east side. However, for the gill net 
sets overlapping day and night periods, this pattern was reversed. 
The south and east sides had the greatest number (15) of species in 
common; the north and west sides were least similar in this respect. 


35 


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57 


White croakers (Genyonemus lineatus) were captured only on the east 
side and an unidentified species of rockfish was captured only on the 
south side. 


We Natural Bottom Survey Results. 


Figure 3 shows the location of the natural bottom transect and 
sampling stations for sediment infauna. Dominant epibiota (organisms 
on the surface of rocks or sediments) and substrate type encountered 
along this transect are shown in Figure 21. In general, the deeper 
areas of the transect, which are representative of the natural bottom 
existing before the island was constructed, are predominantly sedi- 
mentary (sandy silt grading into silty sand in the shoreward direc- 
tion). On the basis of diver observations, it may be stated that the 
biomass, numbers, and variety of epibiota encountered visually over 
natural bottom areas are much lower than that of epibiota oberved on 
the rock revetments of the island. Although rocky areas exist in the 
shallower parts of the transect, the biota they support was observed 
to be of lower abundance and variety than the biota occurring at 
corresponding depths on the island. The macrophytic algae band is 
broader over the transect than on the island; however, zonation in 
general is much less distinct over the natural bottom transect than 
over the island's revetments. A more detailed account of biota and 
habitat types observed along this transect is provided in Appendix E. 


The results of analysis of the sedimentary infauna samples are 
summarized in Table 4 (data on grain-size distributions for the two 
sediments sampled are given in App. F). A total of 62 species was 
encountered in the six samples. Disregarding sample 4 (a part of 
which was lost), polychaetes accounted for 35 percent of the wet 
weight biomass and 50 percent of the taxa present in the samples 
taken collectively. 


Diversity, as represented by Simpson's Index, was relatively 
uniform and high, averaging about 0.93 for the five complete samples. 
These high numbers reflect the relatively even distribution of 
individuals among the species present and the fact that the propor- 
tion of total individuals accounted for by any single species is 
small in these samples. 


The biomass values, which averaged approximately 0.7 gram per 
sample, convert to approximately 14 grams per 0.25 square meter of 
sedimentary bottom. Even considering the added contribution of 
epifaunal biomass, the quantitative samples indicate that the biomass 
of natural bottom habitats is much lower overall than that of the 
rock revetments of the island (see Tables D-1 and D-2). Also, the 
number of species encountered during limited sampling of natural 
bottom areas is much less than recorded on the rock habitats of the 
island. 


58 


94° 2/00" 


° 
5 
© 
o 
ic} 
d 
SS 
~ 


B0 100 M @ SEDIMENT GRAB SAMPLE STATIONS 
——-TRANSECT SWIM 


Figure 21. Dominant biota and substrate type along natural 


bottom transect. (Depth contours in feet below MLLW. ) 


59 


Table 4. Biota of natural bottom sediment samples. 


Station No. 1 Il 1 2 

Grab sample replicate No. 1 2 3 jl 
Taxon Depth (m): WS J 1eo7 1.7) 10.7 

PLATYHELMINTHES 

Unid. flatworm aL 
NEMERTINA 

Nemertean sp. #1 2 He TL 

Nemertean sp. #2 : i dl 

Nemertean sp. #3 dL 

Nemertean sp. #4 i 
MOLLUSCA 

Pelecypoda 

Axinopsida sericata 2 2 

Thracia curta iL 

Naculana sp. (juv.) He 


Macoma sp. (juv.) 


SIPUNCULIDA 
Unid. sipunculid aL 1 1 


ANNELIDA 

Polychaeta 
Driloneris falcata 
Lumbrineris sp. 
Sigambra tentaculata 
Haploscoloplos mexicanus 
Spiophanes missionensis 
Tauberia gracilis 
Axiothella sp. 
Cossura candida 
Unid. Polynoidae 
Tharyx sp. 
Ampharete labrops 
Notomastus sp. 
Glycera sp. 
Loimia medusa 
Scoloplos armiger 
S. acmeceps profundus 
Mediomastus californiensis TL 
Protodorvillea gracilis 
Sthenelanella uniformis 2 3 
Pista fasciata 
Glycera capitata 1 
Ancistrosyllis hamata 4L 
Nephthys caecoides ih 
Polydora sp. alt 
Amaena occidentalis 
Polycirrus perplexus 
Prionospio nr. malmgreni 
Praxiella affinis pacifica 
Diopatra ornata 
Spiochaetopterus costarum 
Typosyllis hyalina 


PUN N 
NO 


PRERPPOFPWNOAKPNNEFE 
i 
PwWHEN 


= 
= 
= 


Sie i 
See footnotes at end of table. 


60 


i) 
I) OS) l=! [f 


PNPRPRPEPRH 


Table 4. Biota of natural bottom sediment samples.--Continued. 

1 2 2 2 

3 11 2 3 
55 7/ 10.7! 10.7 10.7 


Station No. 1 
Grab sample replicate No.: 1 
Taxon Depth (m): W959 133; 


We 


ARTHROPODA CRUSTACEA 

AMPHIPODA 
Ampelisca cristata 1 
Paraphoxus obtusidiens 
Synchelidium sp. 
Monoculodes cf. hartmanae 
Aorides columbiae 
Metaphoxus frequens 1 
Paraphoxus heterocuspidatus 1 


PrN ND 


DECAPODA 
Cancer sp. (juv.) 1 
Pinnotheridae (juv.) iL it al 


CUMACEA 

Diastylopsis tenuis 6 3 
Cyclaspis sp.> al 
Hemilamprops californica al iL 2 3 
Lamprops cf. carinata 2 1 


OSTRACODA 
Asteropella sp. 1 


ISOPODA 
Serolis carinata iL 


ECHINODERMATA 

OPHIUROIDEA 
Amphiodia digitata 1 1 
A. sp. (juv.) 2 
Amphipholis squamata 
Amphiodia occidentalis 4 


HOLOTHUROIDEA 
Unid. holothurian Jk 


CHORDATA 
CEPHALOCHORDATA 
Branchiostoma californiense 1 5 


Total species 20 17 25 7 23 14 
Total individuals 38 30 35 16 35 20 


Simpson's index of 
diversity4 0.94 0.92 0.95 0.79 0.94 0.91 


Wet weight (gm) 
Polychaetes 0.42 0.19 0.19 0.01 0.22 0.18 


Total 0.44 0.72 1.20 0.02 0.86 0.22 


A part of this sample was lost 
A hard bottom-type species. 


Undescribed species 


De= lee 
2D (p,)? 


1 
2 
3 
4 


6| 


VI. SUMMARY AND CONCLUSIONS 


Rincon Island's rock revetments offer a diversity of habitat 
features for a great variety of marine species which do not occur in 
adjacent natural bottom areas. This study added 160 taxa of macro- 
biota to the master species list for the island, bringing the total 
to 458. 


Extensive beds of mollusk shells lie at the bases of the three 
sides of the island most exposed to wave action. The bed on the west 
(seaward-facing) side is the most extensive; it is composed primarily 
of shells of the California mussel, Mytilus californianus. The 
volume of shell on the north and south sides combined are an order of 
magnitude less than on the west-side bed. Species other than mussels 
characterize these beds. Shell accumulations are lacking along the 
flanks of the east (landward) side. 


Densities of 53 common taxa occurring in permanent transects on 
each of the four sides of the island were analyzed for seasonal 
variability. About three-fourths of these showed statistically 
Significant variation. This was the case for most of the algae 
tested and generally for ectoprocts, sea urchins, and certain worms, 
coelenterates, and sponges. 


Thirteen major species associations were provisionally iden- 
tified on the basis of dominant biotic components. Detailed charts 
of the boundaries of these associations, referenced to permanent 
features on the island, were prepared from field measurements of 
depths and distances. Sharpness of the boundaries generally de- 
creases with depth. In general, the associations are continuous 
horizontally around the island and grade into one another vertically. 


Statistical analysis of species abundance and biomass data from 
each of the 13 preliminary major species associations provided a 
basis for final characterization of associations. Five of the pre- 
liminary 13 associations could not be differentiated statistically. 
Combination of these and addition of one association resulted in a 
total of nine distinctly different major species associations. An 
association dominated by acorn barnacle and limpet biomass encircles 
the island in the uppermost part of the intertidal. Below this on 
the west side lies a mussel-gooseneck barnacle association, which ex- 
ceeds all other associations in biomass per unit area. Small pockets 
of an intertidal anemone association are found on the southeast wing. 
Starting at about the MLLW line and extending a few meters down the 
revetments, a macrophytic algae association is found on all but the 
east sides. Below this is a broad zone characterized by encrusting 
and filamentous algae and a species of polychaete worm. The deeper 
parts of the revetments are characterized by an association dominated 
by ectoprocts, colonial anemones, corals, and gorgonians. Talus beds 


62 


with high densities of tube worms and tube anemones separate the deep 
associations from natural bottom on all sides except the east side. 
Two associations are unique to the east side. The shallower of the 
two is composed almost entirely of large barnacles and encrusting 
algae. The deeper association has high densities of certain species 
of red algae. 


Twenty-three species of fishes were captured in gill nets placed 
on all four sides of the island. Rockfish, surfperch, toadfish, and 
swell sharks dominated the catch. Nets on the west (most exposed) 
side yielded the highest catch (numbers and species) during day- 
time sets. The east-side nets had the highest catches in the com- 
bined day-night sets. 


The biota along a transect over natural bottom from near the 
island to shore were considerably lower in abundance or density and 
in number of species relative to biota at corresponding depths on the 
island's revetments. This was especially the case for sedimentary 
bottom in deeper water where the island is situated. Samples of 
natural sediments were dominated by polychaete worms (35 percent of 
biomass and 50 percent of species), small crustaceans, clams, ribbon 
worms, and brittle stars. 


The construction of Rincon Island has had a major beneficial 
effect on local ecological conditions. The quarry rock and tetrapod 
construction materials offer habitat features which are not found in 
a natural sedimentary bottom area. The solid substratum is colonized 
by a high diversity of encrusting and attached biota. Many of these 
are habitat-forming species in the sense that they provide shelter 
and food for additional species. High vertical relief and vast 
amounts of interstitial space attract many species of fishes which 
are seldom or never encountered over sedimentary bottom areas. 


63 


LITERATURE CITED 


BLUME, J.A., and KEITH, J.M., "Rincon Offshore Island and Open 
Causeway,'' Journal of the Waterways and Harbors Division, 
American Society of Civil Engineers, Vol. 85, No. WW3, Sept. 1959, 
pp. 61-93. 


BUCHANAN, C.C., "A Comparison of Sport Fishing Statistics from 
Man-Made and Natural Habitats in the New York Bight," 
Coastal Plains Center for Marine Development Services, Seminar 
Series, No. 1, 1972, pp. 27-37. 


CARLISLE, J.G., Jr., TURNER, C.H., and EBERT, E.E., "Artificial 
Habitat in the Marine Environment,'' Fish Bulletin 124, The 
Resources Agency of California, Department of Fish and Game, 
Long Beach, California, 1964. 


CHAN, G.L., ''Subtidal Mussel Beds in Baja California With a New 
Record Size for Mytilus californianus, The Veliger,", Vol. 16, 
1973, pp. 239-240. 


COLUNGA, L., and STONE, R. eds., Proceedings of an International 
Conference on Artificial Reefs, Center for Marine Resources, 
Texas A & M University; National Marine Fisheries Service; and 
Texas Coastal and Marine Council, Houston, Tex., 1974. 


DAMES & MOORE, ''A Study of the Performance of Certain Artificial 
Islands on the Pacific Coast of the United States," Report No. 
2443-079-10, Los Angeles, Calif., 1974. 


FAGER, E.W., ''Patterns in Development of a Marine Community," 
Limnology and Oceanography, Vol. 16, No. 2, Mar. 1971, 
pp. 241-253. 


KEITH, J.M., and SKJEI, “Engineering and Ecological Evaluation 
of Artificial-Island Design, Rincon Island, Punta Gorda, 
California," TM-43, U.S. Army, Corps of Engineers, Coastal 
Engineering Research Center, Fort Belvoir, Va., Mar. 1974. 


NORTH, W.J., "Ecology of the Rocky Nearshore Environment in 
Southern California and Possible Influences of Discharged 
Wastes,'' International Conference on Water Pollution Research, 
London, Sept. 1962, pp. 247-273. 


PAINE, R.T., "Biological Observations on a Subtidal Mytilus 
californianus Bed,"" The Veliger, Vol. 19, 1976, pp. 125-130. 


64 


SNEATH, P.H.A., and SOKAL, R.R., Numerical Taxonomy: the Principles 
and Practice of Numerical Classification, Freeman § Company, 
San Francisco, 1973. 


SOKAL, R.R., and ROHLF, F.J., Biometry, the Principles and Practice 
of Statistics in Biological Research, Freeman §& Company, 
San Francisco, 1969. 


SOOT-RYEN, T., ''A Report on the Family Mytilidae (Pelecypoda) ," 
Allen Hancock Pacific Expedition, Vol. 20, No. 1, University 
of Southern California Press, Los Angeles, Calif., 1955. 


SOUTHERN CALIFORNIA COASTAL WATER RESEARCH PROJECT, 1976 Annual 
Report, El Segundo, Calif., 1976, pp. 179-186. 


STONE, R.B., ''Artificial Reefs of Waste Material for Habitat 
Improvement," Marine Pollution Bulletin, Vol. 3, No. 2, Feb. 1972, 
pp. 27-28. 


STONE, R.B., “Artificial Reefs and Coastal Fishery Resources," Pro- 
ceedings of the 10th Space Congress, Canaveral Council of Tech- 
nical Societies, 1973, pp. 2-19. 


STONE, R.B., BUCHANAN, C.C., and PARKER, R.O., ''Expansion and 
Evaluation of an Artificial Reef of Murrells Inlet, S.C.," 
Final Report, Coastal Plains Regional Commission, Washington, D.C., 
1973, p. 55. 


STONE, R.B., BUCHANAN, €.€., and STEIMLE, F.W., Jr., "Scrap Tires as 
Artificial Reefs," Report SW-119, U.S. Environmental Protection 
Agency, Washington, D.C., 1974. 


TATE, M.W., and CLELLAND, R.C., Nonparametric and Shortcut Statistics 
in the Social, Biological, and Medical Sciences, Interstate, 
Danville, I1l., 1957. 


TURNER, C.H., EBERT, E.E., and GIVEN, R.R., ''Man-made Reef Ecology," 


Fish Bulletin 146, The Resources Agency of California, Depart- 
ment of Fish and Game, Long Beach, Calif., 1969. 


65 


APPENDIX A 


DETAILED METHODOLOGY 


il. Details of Talus Bed Measurement and Data Processing Methodology. 


An initial dive was made to calibrate depth gages of all divers and 
to verify criteria for use in determining the inshore and offshore bound- 
aries of the talus bed. The north side had an irregular fill base (where 
rock and talus meet), and a heavy sediment overburden downslope which 
made the talus boundary difficult to determine. 


Using a steel tape, a metered line, and an underwater slate, one 
diver made the first measurement of the rock revetment, holding the free 
end of the 30.5-meter steel tape on an azimuth perpendicular to the 
cardinal side. When the diver reached the end of the rock revetment 
(beginning of the talus bed), the depth, distance, and time were re- 
corded. Three divers then swam to the first diver's location. Measure- 
ments were taken on the cardinal sides between the points where the 
angle of the side changed direction (beginning of "wing'' of the island). 
The first team of two divers measured the talus bed width (inner to 
outer margin) by having one diver hold the free end of a 50-meter line 
(marked) in meter intervals) while the sedond diver swam along the per- 
pendicular azimuth to the outer edge of the talus bed. At this point 
the second diver recorded depth, time, and distance. The first diver 
was then signaled to join the second diver at the outer edge. The pair 
then measured the outer edge of the talus along the entire length of the 
side, using the method discussed below. A second team of two divers 
measured the talus along the inner edge. 


Swimming along an azimuth parallel to the side, one diver deployed 
the steel tape along the inner or outer edge of the talus bed (the 
second diver held the free end of the tape and remained at the start 
point) until a change in depth (+0.15 meter) or direction (+10°) was 
noted. At that point the first diver stopped, noted distance swum, 
depth, and time. The second diver was then signaled to swim to the 
first diver. From this point the first diver swam up the revetment to 
the waterline. At the waterline, the diver noted distance and time. 

He then returned to the bottom where the second diver was waiting. The 
width of the talus bed was measured from this point to the outer edge 
where again time, depth, and distance were recorded. The first diver 
returned to the second diver and repeated the process, moving along the 
cardinal side. The team on the outer edge used an identical method 
except that team measured the width of the talus bed from the outer to 
inner edge. Each time a talus width was measured, the corresponding 
distance up the revetment (waterline to inner edge of talus bed) was 
measured. This method allowed multiple points of measurement and 
allowed divers to observe changes at the outside and inside limits of 
the bed. 


67 


The following diagrams illustrate the methodology used for 
charting the talus beds. 


(1) Line of measured distance (waterline to talus bed-revetment bor 
der) (dl) and width of talus bed (d2) was drawn on quadrangle 
paper (1 cm = 2.4m) 

Sos ‘ waterline 

al 

| 

| 

| ac 

| 

\ 

! 

(2) 


The next line (distance between revetment measurement points) was 


then plotted in the form of circle with that distance (d3) as the 
radius. 


waterline 


(3) 


The length of the second revetment measurement (a4) was then 
plotted to where it intersected the circle. This gave the dis- 


tance between measurements at the waterline (d>) which could be 
converted for three-dimensional diagraming. 


68 


Sa ——— Wwacerikne 


(4) The second talus bed length ca) was then plotted as shown 


—— — waterline 


(5) This methodology was continued along the entire side until a 
planar view of that side was constructed. 


(6) To show these data in three-dimensional diagram, the planar 
diagram was converted to a series of triangles using dl as the 
hypotenus of the revetment and d? as the hypotenus of the talus. 
Depths (height) were converted to MLLW by adding or subtracting 
the number of meters difference according to time (e.g., at 
1330 hours, 15 October 1976 tide at Rincon Island (Ventura) was 
+0.76 meter; thus, 0.76 meter would be subtracted from the 
height of the "revetment triangle''). 


waterline 


69 


(7) The series of triangles was then placed in Decspe ceive by con- 
verting the USUENCO between measurements (d> ) to a distance 
0.71 times d° The 0.71 conversion allowed a three-dimensional 
depiction of these triangles scaled to the total side of the 
lisitande) | (0.71l = sinwot alr she trrangillen= M2) 


De Permanent Transects Seasonal Data Analysis Methods. 


The master species list for the seasonal surveys included 250 
taxonomic categories (70 were marine algae and 180 were marine in- 
vertebrate taxa). From this master list 24 taxa of marine algae and 
30 taxa of invertebrates were selected for special study of seasonal 
variability. Proportionately, more algal taxa were used than in- 
vertebrate taxa, because seasonal effects are often well pronounced 
among algae, especially reds (Rhodophyta). The only algal taxa 
omitted from the analysis were those of uncertain identity or which 
(a) occurred in low density, and (b) were found on only one side and 
during only one season. The number of invertebrate taxa selected for 
analysis was in part dictated by data-handling considerations. Even 
when unidentified taxa were eliminated, the amount of data remaining 
was formidable. Many of these taxa were observed at such low fre- 
quencies as to be of little value in any seasonal analysis. Either 
these species are uncommon on the island; the transects missed their 
centers of abundance; or, if they were seasonally abundant, their 
peaks in abundance did not overlap the sampling periods. Many taxa 
were observed only once (i.e., in only one quadrat). It is assumed 
that most if not all of the singular-occurrence taxa and most of the 
low-frequency taxa were generally uncommon on the island. Observa- 
tions elsewhere:on the island during other times of the year (i.e., 
during reconnaissance diving, measurement of boundaries of associa- 
tions, and biomass measurements) tend to corroborate this. For these 
reasons, these rarely encountered taxa were excluded from the sea- 
sonal analysis. 


70 


For the 54 taxa selected for the seasonal effects analysis, ad- 
ditional analysis was necessary to maximize data utility. A bias 
factor existed if a particular species occurred over a limited part 
of a permanent transect, and its density was calculated by dividing 
total abundance by n, the total number of quadrat samples taken in 
the permanent transect. This provided a value for mean density 
over the entire island; however, this would be justified only for 
species ubiquitously distributed (i4.e., over the entire length of the 
transect). The distribution of only one species, the starfish, 
Patiria miniata, approaches this (see Figs. 17 to 20). A better 
approach would be to divide total abundance by the number (n) of 
quadrats where the species may reasonably be expected to occur, and 
express mean density with reference to the parts of the island over 
which the species actually occurs (or those associations of which it 
is a member). Mean densities of each species may be more meaning- 
fully compared to resolve seasonal differences using this approach. 
Briefly, the mechanics of this data processing operation involved 
scanning the raw data tables to bracket the upper and lower occur- 
rence limits for each species and then logging onto computer keypunch 
forms the frequency of every density value observed (including zero 
density values for quadrats lacking a given species, but falling 
within its range of occurrence). 


Before the data were subjected to parametric statistical analy- 
sis, it was necessary to perform data transformations to normalize 
the data. For species whose densities were recorded as percentage 
coverage, the values were transformed to angles through the use of 
the arcsine transformation (6 = arcsin WOE where pg is a proportion). 
This transformation rendered a distribution of percentages or pro- 
portions more nearly normal by stretching out both tails of the dis- 
tribution and compressing the middle values (Sokal and Rohlf, 1969). 
Numerical densities were subjected to the square root transformation. 
Because zero values were frequent in the data, the computer was pro- 
gramed to add 0.5 to all values before data transformation. The 
transformation was then of the form \/Y + % (Sokal and Rohlf, 
1969). 


The actual calculations of the means used all the raw data for 
variances to be calculated for each of the 54 taxa examined. 
Seasonal means (data for all four sides lumped) were first tested for 
Significant differences by performing an F test (variance ratio test) 
to determine whether variances for two seasons under comparison were 
equal. If the F test was nonsignificant (variances probably equal), 
the following student's t test for differences between seasonal 
means was applied (Sokal and Rohlf, 1969): 


| 


with n, =n 2 df. When significant F ratios were found, indicat- 
ing disparaté variances, an approximate t test was used (Sokal and 
Rohlf, 1969): \ 


Me er ~ ¥)) oa * 5) 
S 


Summary data for all 54 species selected for seasonal analysis 
are presented in Table B-1. For each species, this table presents 
transformed and untransformed means, standard deviations, transformed 
variances, transformed range data, and an indication of whether the F 
and t tests are significant at the 95-percent confidence level. 


These values are tabulated for each of the four seasons with 
data combined for all four sides, and for each of the four sides with 
data combined for all four seasons. Side differences were not tested 
for significance. 


Note that the values in Table B-1 of Appendix B for mean densities 
for each species refer to their abundance only over the parts of the 
island wherein the species may reasonably be expected to occur--not 
over the entire extent of the island revetments. 


Because of the lack of data during two seasons for the west-side 
macrophytic algae, Mytilus-Pollicipes, and barnacle-limpet zones, 
special consideration was required for the species that occurred in 
these zones. These included most of the algae species and the follow- 
ing invertebrates: Anthopleura sp., Lottia gigantea, Mytilus 
californianus, and Pisaster ochraceus. For these species, means for 
seasons 1 and 4 were compared since data from seasons 2 and 3 were 
questionable. A rerun of the entire analysis for all these species 
resulted in changes from significant to nonsignificant (at the 95- 
percent confidence level) for only four species: Laurencia pacifica, 
Rhodoglossum affine, Lottia gigantea, and Pisaster ochraceus. No 
species changed from nonsignificant to significant with the 
reanalysis. 


UZ 


oe Methodology for Preparation of Figures 9 to 12 and Appendix C 
Figures C-3 to C-6 (Boundaries of Major Associations). 


ARCO Drawing No. CE~1-8, dated 3 March 1965, was used as a base 
chart for plotting field-acquired data on boundaries of species asso- 
ciations. Different tide levels were shown on the drawing for four 
different parts of the island; these levels corresponded to times 
when measurements were taken over the four parts of the island. Spot 
measurements taken between fixed reference points and the waterline 
(which was not at MLLW) at times of corresponding tidal heights 
agreed well with the distances represented on the drawing. 


The first step was to adjust the waterline to MLLW. This was 
done by dividing the tidal height (e.g., +1.2 meters MLLW) by the 
tangent of the side-slope angle. The slope angle for each side was 
determined by averaging data obtained during the talus bed measure- 
ment phase of this project (see Figs. 5 to 8). The resulting MLLW 
line is as it would appear if observed directly from some altitude 
above the island. True distances measured down the slope of each 
side may be determined using the scale provided on each island sector 
chart (Figs. 9 to 12 and Figs. C-3 to C-6). 


Next, distances measured from fixed reference points at the top 
edge of the island to the upper limit of the splash zone (barnacle- 
limpet association) were trigonometrically corrected for slope and 
plotted. The width of the zone bounded at the top by the barnacle- 
limpet line and at the bottom by the MLLW line (representing the main 
part of the intertidal zone) was uniform around the island, providing 
a positive check on accuracy of the waterline shown on the drawing. 
Only 2 of the 15 points showed discrepancies. One on the south side 
was off by about 1.2 meters, and the decision was made to redraw the 
MLLW line at this point to maintain width uniformity for the inter- 
tidal. The other, on the west side, was off by almost 6.1 meters 
(the measurement during this study indicated a shorter distance). 
This discrepancy may be due to movements of tetrapods in response to 
wave forces since the 1965 drawing (a semisubmerged tetrapod lies 
just seaward of the "first" waterline); or the difference may be a 
result of the manner in which the measuring tape was laid over the 
tetrapods (i.e., a greater distance would result if the tape were 
placed over the highest points on the tetrapods). 


The top margin of the barnacle-limpet zone served as the ref- 
erence point for all distance measurements taken during the associ- 
ation mapping phase of the project. Distances to association bounda- 
ries measured down the slope of each side of the island were multi- 
plied by the sine of the average slope for each side. These cor- 
rected distances were plotted in Figures 9 to 12 and Figures C-3 to 
C-6. 


73 


APPENDIX B 
SUMMARY DATA, SURVEY OF 


PERMANENT SEASONAL 
TRANSECTS 


74 


SIDE/ 2 


SPECIES con! SEASON 


eee 


eee 


NNNN NANNY 


BAe FARR 


ll 
ll 
ll 
ll 


11 
1 
ll 
1) 


12 
12 
12 
12 


12 
12 
12 
12 


16 
16 
16 
16 


16 
16 
16 
16 


20 
20 
20 
20 


20 
20 
20 
20 


eee 


eo 


eee 


eee 


eee 


NAN ARAN eee eee 


ee ee 


eee 


eee 


eee 


rune 


Baru 


COMBINED 


rune 


By 


COMBINED 


Pune 


Ce) 


COMBINED 


eune 


DNA 


COMBINED 


rune 


Bae 


COMBINED 


rune 


Ce a) 


COMBINED 


@BvYAanN PUN 


COMBINED 


Table B-1. 
min 4 
2524 0.000 
0.000 0.000 
0.000 0.000 
0.000 0.000 
0.000 v.000 
0.000 0.000 
2524 0.000 
0.000 0.000 
524 0.000 
«464 0.000 
-322 0.000 
2580 0.000 
2464 0.000 
«322 0.000 
2071 0.000 
2580 0.000 
0.000 0.000 
2580 v.000 
2685 0.000 
2464 0.000 
0.000 0.000 
2685 0.000 
0.000 0.000 
2685 0.000 
9.000 0.000 
0.000 0.000 
2685 0.000 
0.000 0.000 
e142 0.000 
0.000 0.000 
2247 «0.000 
2247 0.000 
0.000 0.000 
2142 0.000 
0.000 0.000 
2247 0.000 
2.739 0.000 
1.225 2707 
1.225.707 
1.225 «707 
1.225 
2707 
°707 
2.739 
2.739 
0.000 0.000 
2580 0.000 
0.000 0.000 
0.000 0.000 
0.000 0.000 
0.000 0.000 
©580 0.000 
0.000 0.000 
2580 0.000 
0.000 0.000 
2100 0.000 
0.000 0.000 
2464 0.000 
0.000 0.000 
0.000 0.000 
e100 0.000 
2464 0.000 
2464 0.000 


Summary data: 


seasonal surveys of permanent transects. 


TRANSFORMED 


See footnotes at end of table. 


2003 
0.00U 
0.000 
0.000 


210s 
2054 
0.000 
0.000 


0.000 

2066 
0.000 
0.000 


o 
o 


0.000 
0.000 


0.000 
0.000 

201) 
0.000 


0.000 
02000 


veouu 
0.000 

2104 
0.000 


US) 


UNTRANSF OK MEO 


22.500 
15.u00 
0.000 
0.000 


? 


= 


Species 


(8) ©£. Enteromorpha sp. 


(s) 


(s) 


(s) 


(s) 


Ulva sp. 


Codium fragile 


Cystoseira osmundacea 


Egregia menziesii 


Unid. juvenile 
Laminariales 


Dictyota flabellata 


SPECIES 


37 
37 
37 
37 


37 
37 
= 
37 


39 
39 
39 
39 


39 
39 
39 
39 


40 
40 
40 
40 


40 
40 
40 
40 


41 
41 
41 
41 


41 
41 
41 
41 


42 
42 
42 
42 


42 
42 
42 
42 


48 
46 
48 
48 


48 
48 
48 
48 


CON 


wee 


s1oes 2 
SEASON 


rune 


DAW 


COMBINED 


rune 


DIAN 


COMBINED 


rune 


DAW 


COMBINED 


PUNE 


DAN 


COMBINED 


rwNe 


Daan 


COMBINED 


rune 


PNW 


COMBINED 


Pune 


PYDrH 


COMBINED 


rwne 


DATUM 


COMHINED 


TRANSFORMED 


MAX 


see2D s.vev.6 


0.000 
2049 
2057 
ley 


min 4 
0.000 001 
0.000 +000 
0.000 001 
0.000 0.000 
0.000 000 
v.000 2001 
0.000 =000 
0.000 -000 
0.000 +000 
0.000 +006 
0.000 2002 
0.000 =007 
0.000 2015 
0.000 +010 
0.000 -0ue 
0.000 0.000 
0.000 -002 
0.000 -007 
0.000 2022 
0.000 2003 
0.000 0.000 
0.000 011 
0.000 +015 
0.000 +01 
0.000 0.000 
0.000 v.000 
0.000 2010 
0.000 0.000 
0.000 2002 
0.000 +003 
0.000 2017 
+006 
+001 
008 
0.00u 
0.000 2006 
U.000 0.000 
0.000 v.000 
0.000 20le 
0.000 0.000 
0.000 
0.000 
0.000 
0.000 
0.000 
0.000 2005 


See footnotes at end of table. 


76 


UNTRANSFO*4ED 


SeNEv. MEAN 
239? 2005 
«lee +05) 
2 5b6 2066 

v.00  Uevu0 


1.ATT 2403 
1.604 +231 
2904 2667 


4.1719 eld 

2 BMG 200 
v.000 0.0u0 
1.41) 242 


4eB44 1-529 
+?36 2086 
v.000 0.000 
0.000 0.000 
4,963 1.019 
0.000 0.600 
1.239 22465 
12825 2323 


6.543 1.668 


4.024 2959 
-Slo +070 
4.141 «820 


0.000 0.000 


3.506 


v.000 0.000 
7.477 07193 
v.00 0.000 
7.609 +821 
0.000 02000 
v.000 uv.000 


D.06K 1.621 
v.000 0.000 
0.000 9.u00 
u.000 2000 


400 096 
4.650) leouse 
4.204 wKse 
cotue 2465 


€.40H 3432 
1e1sl e171 
0373 2069 
1.035 «169 
2.697 2357 
elie -017 
1.390 e151 


NS 


(s) 


(s) 


(s) 


(s) 


(s) 


Species 


Peyssonellia sp. 


Prionitis lanceolata 


Rhodoglossum affine 


Rhodymenia sp. 


Rhodymenia californica 


Stenogramma sp. 


Stenogramma 


interrupta 


cf. Phormidium sp. 


SPECIES CON 


68 
68 
68 
68 


68 
68 
68 
68 


89 
89 
89 
69 


a9 
89 
89 
89 


103 
103 
103 
103 


103 
103 
103 
103 


104 
104 
104 
104 


104 
104 
104 
104 


106 
106 
106 
106 


106 
106 
106 
106 


108 
108 
108 
108 


108 
108 
108 
108 


109 
109 
109 
109 


109 
109 
109 
109 


110 
110 
110 
110 


110 
110 
110 
110 


mann 


NUNN 


NUNN NAN 


nun 


nnn 


NNANN ANAND 


SIDE/ 
SEASON 


rune 


mya 


COMBINED 


rune 


DNA 


COMBINED 


rune 


RiIT) 


COMBINED 


rue 


DARN 


COMBINED 


rune 


PAOD 


COMBINED 


rune 


Dar 


COMBINED 


rune 


DAA 


COMBINED 


rune 


BAW 


COMBINED 


2 max 3 


o1T4 
«226 
2396 
«322 


#226 
174 
322 
2398 


2398 


+226 
0.000 
0.000 
+142 


071 
9.000 
«226 
2174 


+226 


3.937 
3.536 
4.526 
4.528 


1.225 
4.52 
1.581 
2.915 


4.528 


«886 
464 
1.107 
1.173 


322 
1.107 
+785 
1.173 


1.173 


2.345 
22345 
2.550 
2.345 


1.581 
2.345 
2.550 
0.000 


2.550 


2.121 
2.739 
4.528 
3.937 


4.528 
0.000 
0.000 
0.000 


4.528 


1.671 
2.12) 
2elel 
1.871 


2.121 
1.581 
2.121 
0.000 


TRANSFORMED 

MINS seez5 S.vev.6 Fay 
0.000 001 2U2Zb 2005 
6.000 +002 +042 efit 
0.000 +00> 2070 2032 
0.000 006 «0646 Ned 
0.000 2002 =039 -O11 
0.000 001 +040 2010 
0.000 «002 2udU O17 
0.000 2006 -08U -037 
0.000 0023 2055 uly 
0.000 +003 205¢ -01> 
0.000 0.000 u.uou 0.006 
0.000 0.000 v.00Uu U.00U 
0.000 200) 2032 2007 
0.000 -0uU 2013 20nd 
0.0uuU 0.0uu veuou 0.000 
0.000 001 20365 2008 
0.000 001 +037 2906 
0.000 2001 «03 2006 
«707 «206 #454 2HNS 
«707 e137 371 o TAT 
707 +2lo +467 +796 
«707 +265 2515 ehl> 
«707 2010 2090 «720 
«707 1-306 1el4s 1.269 
«707 016 +13> +734 
+707 +09" +307 “777 
707 2207 2455 «HOL 
0.000 2006 077 2026 
0.000 2003 25a 200% 
0.000 2005 +Ule 20aT7 
0.000 2004 -09uU 2034 
0.000 2003 2059 2019 
0.000 +006 «0BY 2937 
0.000 006 090 2060 
0.000 001 2025 2003 
0.000 2006 076 +03¢ 
0.000 2050 e172 ell? 
0.000 2013 ell4 2055 
0.000 -036 «1AY ele7 
0.000 2044 +210 114 
0.000 2005 +060 2025 
0.000 2029 2176 207K 
0.000 «014 +116 20RD 
062 2469 215 

2054 + lR6 ell¢ 

707 elao 366 otha 
2707 +136 2369 24d 
2707 147 Perry B52 
«707 163 =404 2 A968 
-707 2011 +106 2725 
707 2091 «302 2 7TRO 
2707 2216 #464 2960 
0.000 0.000 u.2000 0.00U 
«707 «144 «379 2864 
2707 2200 2 46T 2975 
2707 2348 +590 14105 
+707 1.Sue 1eees 2450 
-707 2722 -85U 1.140 
«707 706 1.168 
0.000 0.000 0.000 
0.000 0.000 v.000 
0.000 0.000 0.000 
2707 2708 Bal 1.148 
2707 2021 0730 
«707 2060 2793 
707 071 oAle 
0707 2063 2804 
2707 2 0R1 +793 
«707 2071 2737 
«707 2071 otlT 
0.000 0.000 0.000 
707 2056 2 7hG 


e121 


See footnotes at end of table. 


(OG 


UN TH ANSF On ar) 


S.DEV. 


ejoT 
eT49 
1.790 
1.504 


MEAN 


269 
2149 
2D6R 
254 


eud4 
veuon 
+154 
2136 


(s) 


Species 


Cliona sp. 


Rymenamphiastra 
cyanocrypta 


Anthopleura sp. 


Astrangia 
dajollaensis 


Corynactis 
californica 


Lophogorgia 
chilensis 


Muricea spp. 


Paracyathus 
stearnsii 


TRANSFORMED UNTRANSFUR™EU 


SIDE/ 
spectes con! season 2 wax 3 NA rocco iapecien 
8 2 1 2707 2707 2000 2000 e797 u.000 ueduU Ale (s) , " 
5 2 2 1.225 2707 2009 097 2722 «147 2036 Hae sepeeayeeruviane 
128 2 3 1.225 707 2010 +101 eTe7 e195 2039 1hee ododesmus cepio 
128 e 4 2.739 2707 2060 2249 2756 Ton e135) Awe 
128 2 5 1.225 707 +01) +104 2774 220) 5042 1146 
128 2 6 2707 = 707 2000 2000 .707 0.000 U.000 Se. 
128 2 7 2.739 2707 2036 olde 2735 257? 207K Abe 
128 2 Pp 0.000 0.000 0.000 0.000 v.00 0.0u0 0.000 ve 
COMBINED 2.739 «707 01 2144 2730 244 2053 397. 
148 2 1 2.121 =o 707 2064 ra 2318 259K 2237) 1446 ss Doriopeilla 
148 2 2 1.225 707 2008 2092 2724 2177 eus2 124, albopunctata 
148 2 3 1.871 707 2023 2182 2739 2346 2070 «1A. 
148 2 4 2.121 «707 +060 2244 2795 257? 219) 19h. 
148 2 5 1.871 «707 2040 2190 2743 lib. 
148 2 6 1.581 707 2015 2124 +736 248. 
148 2 7 1.581 707 2027 +163 2752 170. 
148 2 8 2.121 .707 .074 2273 eID 250. 
COMBINED 2.121 4707 2041 2204 2770 2466 2144 744. 
153 2 1 1.871 «707 +205 2775 2444 2143) 154. (Ss) Kelletia kelletii 
153 2 2 2707 = 707 2000 2707 0.000 e000 Ino. 
153 2 3 1.871 707 2116 2725 2270 2940 176. 
153 2 4 2.121 707 2227 e777 2546 2155 lab. 
144 
153 2 5 1.871 707 0173 2748 2397 2090 O 
153 2 6 1.581 707 2088 e714 2194 2023-132. 
153 2h Guat) 1.871 2707 2166 e751 2367 2042 1206 
153 2 8 2.121 .707 -186 275> 2437 2105) can. 
COMBINED 2.121 707 20eT 2164 2745 2377 20d? 634. 
155 2 1 4.528 .707 1.038 1.019 1.201 4.673 1.960 38650. S&S Tottia gigantea 
155 2 2 3.674 707 2519 -720 2937 22953 2875 24, 
155 2 3 32240 2707 2269 2519 2925 1.738 2619 42. 
155 2 4 3.240 2707 237b 2615 2935 2.119 2750 4b. 
155 2 5 3.082 2728 1615 22423 16421 3h. 
155 2 6 4.183 1.073 1.292 4.628 ce2y5 ah, 
155 2 7 1.225 2097 2725 2187 2036 56. 
155 2 a 4.528 2776 2919 3.939 2923 Ao. 
COMBINED 4.528 +760 «1.015 30191 16104 164. 
157 2 1 1.581 .707 2033 -160 2375 e118 149. s Ss Megathura crenulata 
157 2 2 1.561 707 2013 elle 223? 2043 lhe. 
157 2 3 1.225 707 2013 2115 o2e2 2051 136. 
157 2 4 1.581 707 2022 2150 e311 207A 1h6. 
157 2 5 1.225 6707 2016 2127 2246 2064 1716 
157 2 6 1.225 707 2005 2070 2135 2019 Low. 
157 2 7 1.225 2707 2000 2091 2175 2032 272. 
157 2 8 1.581 707 2056 2236 2506 +205 132. 
COMBINED 1.581 e707 20A1 2144 0744 2296 0974 FASS 
158 2 1 30240 2707 2313 2560 Aol 20105 2542 Pee s NS Mytilus 
158 2 2 2707 «707 0.000 0.000 2707 0.000 v.000 2. californianus 
158 2 3 3.808 .707 0437 2661 2BOs €0965 +636 2c. 
158 2 4 11.853 6707 = 44790 9 2o HY =e LKO 270439 50500 
158 2 5 11.853 6707) «= 20860 = 16691) 10057) = ue 283) 341TH 
158 2 6 1.871 707 e117 2343 2713 2803 2273, 2. 
158 2 7 0.000 0.000 0.000 0.000 0.000 0.000 6.000 0. 
158 2 8 2707 «707 0.000 0.000 2707 0.000 v.000 4. 
COMBINED 11.853 6707 16891 14375 2965 166354 2.247) TH 
159 2 1 3.240 2707 2267 2517 2813 2.04) 2417 9 24 (s) Mytilus edulis 
159 2 2 0.000 
159 2 3 14.509 
159 2 4 0.000 
159 2 5 14,509 
159 2 6 2707 
159 2 7 0.009 
159 2 8 0.000 


COMBINED 14.509 


See footnotes at end of table. 


78 


SPECIES 


170 
170 
170 
170 


170 
170 
170 
170 


185 
185 
185 
145 


185 
185 
185 
165 


186 
186 
186 
186 


186 
186 
186 
186 


187 
187 
187 
187 


187 
167 
187 
187 


200 
200 
200 
200 


200 
200 
200 
200 


201 
201 
201 
201 


201 
201 
201 
201 


202 
202 
202 
202 


202 
202 
202 
202 


228 
228 
228 
228 


228 
228 
228 
228 


See footnotes at end of table 


1 SIDE/ 
CON * SEASON 
2 1 
2 2 
2 3 
2 4 
2 5 
2 6 
2 7 
2 a 
COMBINED 
2 1 
2 2 
2 3 
2 4 
2 5 
2 6 
2 7 
2 A 
COMBINED 
1 1 
1 2 
1 3 
1 4 
1 5 
1 6 
1 7 
1 8 
COMBINEU 
2 1 
é 2 
e 3 
2 4 
2 Ss 
2 6 
2 7 
2 8 
COMBINED 
1 1 
1 2 
1 3 
1 4 
1 5 
1 6 
1 v 
1 aR 
COMBINED 
1 1 
1 2 
1 3 
1 4 
1 5 
1 6 
1 7 
1 8 
COMBINED 
1 1 
1 2 
1 3 
1 4 
1 5 
1 6 
1 7 
1 8 
COMBINED 
2 1 
2 2 
2 3 
2 4 
2 5 
2 6 
2 7 
2 8 
COMBINED 


2 


TRANSFORFEIY 


UNTHANSF OREN) 


10,025 


A.9T2 
8.860 
10.025 
6-205 


10.025 


7.106 
9.925 
7.106 
7.106 


7.106 
7.106 
0.000 
9.925 


9.925 


+785 
+535 
2398 
2685 


2685 
540 
785 
2524 


«785 


1.871 
1.871 
1.581 
2.121 


2.121 
1.871 
1.225 
1.581 


2-121 


«846 
1.173 
2866 
0735 


3464 
580 
1.173 
2404 


1.173 


2322 
2398 
2142 
+226 


2247 
2396 
322 
«142 


2398 


322 
1.107 
2466 
2464 


322 
3464 
1.107 
322 


1.107 


2.550 
2.121 
3.536 
3.536 


2.345 
1.871 
3.530 
2.550 


3.536 


1.550 
1.635 
leetio 
1.767 


e.loe 
1-195 
1.591 
1.096 


ols 


11.30% 
13.604 

o.97) 
14.605 


lo.35A 
yelo7 
1.038 
Gaur 


6.002 
12.62) 
4.499 
b.150 


7.773 
7.53n 
v.900 
10.441 


79 


Species 


Serpulorbis 
squamigerus 


Diopatra ornata 


Dodecaceria fewkesi 


Eudistylia sp. 


Lagen{pora 
punctulata 


Phidolopora 
Pacifica 


Scrupocellaria 
diegensis 


Parastichopus spp. 


SPECIES 


229 
229 
229 
229 


229 
229 
229 
229 


230 
230 
230 
230 


230 
230 
230 
230 


231 
231 
231 
231 


231 
231 
231 
231 


241 
241 
241 
241 


241 
241 
261 
241 


242 
242 
242 
242 


242 
242 
242 
242 


con! Season 2 


SIDE/ 


NnaNnNNw 


NANNY 


NnNNN 


NANNY 


Nann 


NNN 


NUNN NANNY 


NNN 


NAnNnw 


NNN NaNNwNn 


rune 


DAD 


COMBINED 


rune 


@Onouw 


COMBINED 


rune 


@Ooryoryn 


COMBINED 


rUWNne 


@noyw 


COMBINED 


ewne 


Rana 


COMBINED 


rwne 


DBraDN 


COMBINED 


TRANSFORMED 


max3 MIN4 See22 5.0EV.9 MEAN 


3.536 2707 2409 2639 1.315 
3.937 0707 2359 2599 1.354 
4.301 2707 2501 2708 1.368 
3.808 0707 2429 2655 1.336 
4.301 2707 2551 2742 1.515 
3.536 2707 2516 2718 1.454 
3.0862 2707 0297 2545 1.277 
3.937 0707 2283 2532 1.172 
4.301 0707 2425 2652 1.3463 


1.225 °707 e011 2106 e73U 
1.225 2707 2004 Vol e714 
1.225 0707 2000 2089 e723 
1.225 2707 2004 2063 e715 
1.225 2707 e011 2107 0730 
1.225 707 2004 2065 e719 
0.000 0.000 0.000 0.000 0.000 
1.225 707 2005 2073 eTlT 
1.225 e707 2007 2 0ARc e720 
1.871 0707 2056 0236 0 ANG 
2.121 2707 20049 e221 2° 79K 
220345 e707 2063 2252 0h14 
2.12) o707 2051 2226 e791 
1.871 0707 2046 e215 eBN6 
1.581 2707 2038 0196 o7Re 
2.121 2707 2058 2240 2f12 
22345 0707 2067 2259 eANT 
223485 0707 2055 0234 ele 
1.225 e707 2008 2091 0773 
1.225 2707 e012 e110 e731 
1.581 e707 2037 0192 e774 
1.225 0707 2013 e1l5 0 134 
1.581 e707 2022 e149 e743 
1.225 0707 2017 e131 0742 
1.581 0707 2026 ol62 e756 
1.225 0707 2007 20RO e722 
1.581 e707 2917 0130 0739 
3.082 2707 0224 0473 0976 
20915 0707 0194 0440 0943 
32536 0707 e301 0546 1.0160 
3.082 2707 0308 2555 1.072 
3.391 °707 1.147 
22550 0707 1.004 
20121 2707 2856 
3.536 2707 0924 
3.536 .707 9254 2504 2996 


2707 2576 0759 1.195 
0707 070¢ °B38 1.209 
0707 0157 0396 
0707 0984 2992 
0707 048 2694 


See footnotes at end of table 


80 


UNTRANSFORMED 


SeDEV. 


NS 


NS 


Species 


Patiria miniata 


Pisaster 
brevispinus 


Pisaster 
giganteus 


Pisaste. 
ochraceus 


Strongylocentrotus 


Strongylocentrotus 
purpuratus 


N 


ONDMHHWN re 


= Arcsin conversion used for data transformation 


Square root conversion used for data transformation 


summer (July 1976) 
fall (November 1976) 
winter (February 1977) 
spring (April 1977) 
north side 

south side 

east side 

west side 


Sieecimem value of density (transformed) 


“gen dance value of density (transformed) 


variance 

standard deviation 

7y number of quadrats examined over zone of occurrence 

BF "F ratio'' (ratio of variances) 

2s "Student's t,'’ the deviation of the estimated mean from that of 
the sample population 

S Significant (95 percent confidence level) 

NS = Not significant (95 percent confidence level) 

(S) Significant difference in means due to absence during at least 


one season 


8| 


APPENDIX C 


R-MODE DENDROGRAMS AND BOUNDARIES 


OF PRELIMINARY (TENTATIVELY IDENTIFIED) SPECIES 


Note: 


ASSOCIATIONS 


In Figures C-3 to C-6, each association is labeled 
with an alpha or numeric designation. The number 
refers to the preliminary identity applied to each 
association for purposes of field recognition and 
charting of the boundaries of each major species 
association (see Sec. I1V,4). The letter represents 
the designation of the identity of the association 
after the completion of statistical analysis of 
quantitative compositional data as described in 
Section V,5. 


82 


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83 


North-side R-mode dendrogram showing similarities in occurrence among species 


Figure C-1. 


surveyed in a permanent transect (species with high frequencies of co-occurrence 


cluster at high similarity values) 


See Table C-1 for key to species codes. 


pop 
sainads 


howl $6°0 98'0 cL'0 e9'0 65'0 0s'0 Vheo 2e'0 €2'0 ALO s0'0 hO*O° 


S3ILIYBIIHIS 


84 


North-side R-mode dendrogram. --Continued. 


Figure C-1l. 


epo> | 


sarnads yo) 


= 
S60 


S= 
6S° 


= <I 
0 os‘ \n'o 
SSTLIYYIIWI 


85 


larities in occurrence among species surveyed 


th high frequencies of co-occurrence cluster at 


See Table C-1 for key to species code. 


East-side R-mode dendrogram showing simi 


in a permanent transect (s 
high similarity values). 


Figure C-2. 


pecies wi 


apo) 
sainads 


os"9 \n'o 
S3PLIYHVIHIS 


86 


East side R-mode dendrogram. --Continued. 


Figure C-2. 


ONOuSBWnNr 


48. 
49. 


58. 


él. 


Veleroa subulata 
Codium fragile 
Gelidium cartilagineum 
Grateloupia abreviata 
cf. Fucus sp. 
Litho/Lithop. 
Peyssonellia sp. 
Stenogramme interupta 
Corallina officinalis 
Unid. fil green alga 
Unid. fil red alga 
Unid. juv. red alga 
Unid. bushy red alga 
(c£. G. coulteri) 

cf. Enteromorpha sp. 
Prionitis lanceolata 


Unid. "brown scum" 
Unid. red alga #1 (WwW) 
Unid. red alga #2 (WwW) 


Unid. lobate red alga 
Egregia laevigata 
Unid. brown alga 
Unid. red alga #1 (E) 


Unid. red alga #2 (E) 
cf. Callophyllis 
Unid. red alga #3 (E) 


Unid. flat red alga (E) 
cf. Agardhiella sp. 

cf. Ceramium sp. 

Unid. red alga (N) 

cf. Gelidium sp. 
Gigartina spinosa armata 
Unid. red alga (S) 

Unid. fil red alga (S) 
Unid."spindly gr-br alga" 
Macrocystis sp. 

Unid. green algal slime 
Unid. coraline alga (N) 
(cf. C. officinalis) 
Rhodoglossum affine 

cf. Microcladia sp. (E) 
cf. Gigartina exasperata 
Unid. fil red alga (E) 
Unid. leafy red (E) 

Unid. small brown alga (E) 
cf. Platythamnion sp. (WwW) 
cf. Bossiella orbigniana 
"Wiry" red alga (E) 
"Spiny" red alga (E) 
Unid. sponge (W) 

Cliona sp. 

Spheciospongia confoederata 
Hymeniacidon cyanocrypta 
Unid. purple sponge (N) 
Unid. grey sponge (S) 
"Sulfur sponge" (S) 

Unid. sponge (N) 
Rhabdodermella nuttingi 
Unid. sponge (E) 

cf. Verongia thiona 3 
Leucetta losangelensis 
Astrangia lajollaensis 
Paracyathus stearnsii 


Table C-1. 


62. 
63. 


64. 
65. 
66. 


67. 
68. 
69. 
70. 
71. 
72. 
73. 
74. 
Wo 
76. 
ile 
78. 
79. 
80. 
81. 
82. 
GIs}o 
84. 
85. 
86. 
87. 
88. 
89. 
90. 
91. 
92. 
Or 
94. 
95. 
96. 
97. 
98. 
99% 
100. 
101. 
102. 
103. 
104. 
105. 
106. 
107. 
108. 
109. 
110. 
lll. 
112. 
113. 
114. 
115. 
116. 
117. 
118. 
119. 
120. 
121. 
122. 


Anthopleura cf. vanthogrammica 


Key to R-mode dendrograms 


Corynactis californica 
Lophogorgia chilensis 
Unid. hydroid (S) 
Unid. anemone (S) #1 
Unid. anemone #2 (S) 
Muricea fruticosa 
Unid. yellow hydroid 
cf. Sertularia sp. 
Balanophyllia elegans 
Cerianthid anemones 
Hydractinia sp. 

Unid. "alternate" hydroid (E) 
cf. Tealia sp. 

Unid. hydroids (N) 
Aglaophenia struthionides 
cf. Eudendrium sp. 

cf. Plumularia lagenifera 
Pteropurpura festiva 

cf. Dendrodoris fulva 
Kelletia kelletii 
Calliostoma canaliculatun 
Mitra idae 

Lottia gigantea 

Collisella digitalis 

Cc. cf. strigatella 

C. scabra 

Conus californicus 

Acanthina spirata 
Serpulorbis squamigerus 
Megathura crenulata 

Mytilus californianus 

cf. Anisodoris nobilis 

cf. Collisella limatula 
Dialula sandiegensis 
Hermissenda crassicornis 


(Ww) 


Navanax inermis 

Hinnites multirugosus 

Chama pellucida 

Unid. gastropod sp. #1 (N) 
Pholads (cf. Parapholas calif.) 
Unid. dorid (N) 
Collisella cf. conus 
Cypraea sSpadicea 

Acmaea mitra 

Pododesmus cepio 
Ceratostoma nuttalli 
Mytilus edulis 

Diodora aspera 
Nassarius mendicus 
Unid. black/yellow dorid 
Unid. nudibranch (S) 
Unid. orange dorid (Ss) 
Flabellinopsis iodinea 
Crepipatella lingulata 
Maxwellia gemma 

Octopus sp. 

Aplysia californica 
Unid. limpet (E) 

cf. Anomia sp. 

Unid. white spot dorid (Ww) 
Unid. yellow doris (W) 


(S) 


87 


123. 
124. 
125. 
126. 
127. 
128. 
129. 
130. 
131. 
132. 
133. 
134. 
iS}S)5 
136. 
137. 
138. 
WI), 
140. 
141. 
142. 
143. 
144. 
145. 
146. 
147. 
148. 
149. 
150. 
Glo 
1525 
153. 
154. 
NS 
156. 
157. 
158. 
159. 
160. 
161. 
162. 
163. 
164. 
165. 
166. 
167. 


168. 


169. 
170. 
171. 
172. 
W736 
174. 
175. 
176. 
177. 
178. 
WTS)e 
180. 
181. 
182. 
183. 
184. 
185. 


(Figs. C-l and C-2). 


Unid. orange cerata eolid (W) 
Unid. boring clam (S) 
Calliostoma annulatum 

Unid snail (N) 

Diopatra ornata 

Unid. serpulids (W) 
Dodecaceria fewkesi 

cf. Eudistylia sp. 

cf. Chaetopterus sp. 


Unid. cf. sabellid (N) 
Unid. serpulid (E) 
Salmacina tribranchiata 


Lagenipora punctulata 
Scrupocellaria diegensis 
Phidolopora pacifica 
Unid yellow ectoproct (W) 
Encrusting ectoprocts 
Unid. "brain coral" ectoproct 
Antropora tincta 
Diaperoecia californica 
Bugula neritina 

Unid. ectoprocts (E) 
Membranipora tuberculata 
Balanus pacificus 

B. tintinnabulum 

B. nubilus 

Tetraclita squamosa rubescens 
Chthamalus fissus 
Pollicipes polymerus 
Balanus glandula 

cf. Paguristes ulreyi 
Unid. pagurids (W) | 
Loxorhynchus crispatus 
Pachygrapsus Crassipes 


Unid. pagurid (N) 

Unid. shrimp (N) 

Unid. barnacles 

Unid. small barnacle (E) 
Unid. pagurid (E) 

cf. Isocheles pilosus 


Patiria miniata 

Pisaster brevispinus 

P. giganteus 

P. ochraceus 

Parastichopus sp. #1 

(short knob-like projections) 
P. sp. #2 (long black-tipped 
projections) 
Strongylocentrotus franciscanus 
S. purpuratus 

cf. Ophiopsilla californica 
Unid. holothuroid (N) 

Unid ophiuroid (S) 
Ophiothrix spiculata 

Unid ophuroid (E) 

Lytechinus sp. 

Boltenia villosa 

Unid. tunicate (W) 


Styela montereyensis 
cf. Amaroucium sp. 


Unid. organisms 
Ocenebra foveolata 
Not sampled 

Unid. coraline (E) 
Collisella spp. (E) 


(E) 


PRELIMINARY ASSOCIATIONS BASED ON FIELD OBSERVATIONS: 


. DIOPATRA/CERIANTHIDS 
» ASTRANGIA/GORGONIANS 

- LAGENIPORA/SCRUPOCELLARIA 

= LITHOTHAMNION COMPLEX/SERPULORBIS/VELEROA 
- MACROPHYTIC ALGAE 

+ MYTILUS/POLLICIPES 

- BARNACLES/LIMPETS 


CORYNACTIS /ASTRANGIA 
LITHOTHAMNION COMPLEX/SERPULORBIS/DODECACERIA/VELEROA 


- ASTRANGIA/CORYNACTIS/LOPHOGORGIA 
<= TETRACLITA/LITHOTHAMNION COMPLEX 
= LITHOTHAMNION/LAGENIPORA/VELEROA 
» LOPHOGORGIA/CORYNACTIS/VELEROA 


OUTLINE OF TALUS BED 
LOCATION OF PERMANENT TRANSECTS 


TRANSECT LINES(DEPTHS IN METERS BELOW MLLM) 


FIMAL ASSOCIATIONS BASED OW STATISTICAL COMPARISONS: 


HEONmMOOD> 


BARNACLE /LIMPET 
MYTILUS/POLLICIPES 

ANTHOPLEURA SPP. 

MACROPHYTIC ALGAE 
LITHOTHAMNION/VELEROA 
VELEROA/LAGENIPORA/LOPHOGORGIA/MURICEA 
RHODYMENIA/VELEROA 


. LITHOTHAMNION/TETRACLITA 
« DIOPATRA/CERIANTHID ANEMONES 


1020 30 _40__SOFEET 


5 lo 15 20 METERS 


(POR ACTUAL DISTANCES DOWN NORTH AND WEST SIDES, 
DIVIDE BY 0.893 AND 0.925, RESPECTIVELY) 


Figure C-3. Preliminary and final species associations, 


5 


a 


1 fe 


northwest quadrant. 


88 


eee 


(ESR ACTUAL DISTANCES DOWN WEST AND SOUTH SIDES, 
DIVIDE BY 0.925 AND 0.892, RESPECTIVELY) 


PRELIMINARY ASSOCIATIONS BASED OW FIELD OBSERVATIONS: 


. DIOPATRA/CERIANTHIDS 

« ASTRANGIA/GORGONIANS 

- LAGENIPORA/SCRUPOCELLARIA 

- LITHOTHAMNION COMPLEX/SERPULORBIS/VELEROA 


1 
2 
3 
4 
s 
6. MYTILUS/POLLICIPES 
7 
8 
9 
10 


- 1 MACROPHYTIC ALGAE 
> BARNACLES/LIMPETS 
* CORYNACTIS/ASTRANGIA 
) LYTHOTHAMNION COMPLEX /SERPULORBIS/DODECACERIA/VELEROA 
| _ASTRANGIA/CORYNACTIS/LOPHOGORGIA 
11. TETRACLITA/LITHOTHAMNION COMPLEX 
12) LITHOTHAMNION/LAGENIPORA/VELEROA 
13. LOPHOGORGIA/CORYNACTIS /VELEROA 
+ OUTLINE OF TALUS BED 
(=: * LOCATION OF PERMANENT TRANSECTS 


—-—— TRANSECT LINES(DEPTHW IM METERS BELOW KLLM) 


PIMAL ASSOCIATIONS BASED OM STATISTICAL COMPARISONS : 


BARNACLE /LIMPET 

MYTILUS/POLLICIPES 

ANTHOPLEURA SPP. 

MACROPHYTIC ALGAE 
LITHOTHAMNION/VELEROA 
VELEROA/LAGENIPORA/LOPHOGORGIA/MURICEA 
RHODYMENIA/VELEROA 
LITHOTHAMNION/TETRACLITA 

. DIOPATRA/CERIANTHID ANEMONES 


rzoannoos> 


O10 20 30 _40__SOFEET 


Figure C-4. Preliminary and final special associations, 
southwest quadrant. 


89 


PRELIMINARY ASSOCIATIONS BASED ON FIELD OBSERVATIONS: 


1. DIOPATRA/CERIANTHIDS 
2. ASTRANGIA/GORGONIANS 

3. LAGENIPORA/SCRUPOCELLARIA 

4. LITHOTHAMNION COMPLEX/SERPULORBIS/VELEROA 
5. MACROPHYTIC ALGAE 

6. MYTILUS/POLLICIPES 

7. BARNACLES/LIMPETS 

8. CORYNACTIS/ASTRANGIA 

9. LITHOTHAMNION COMPLEX/SERPULORBIS/DODECACERIA/VELEROA 
10. ASTRANGIA/CORYNACTIS /LOPHOGORGIA 
11. TETRACLITA/LITHOTHAMNION COMPLEX 
12. LITHOTHAMNION/LAGENIPORA/VELEROA 
13. LOPHOGORGIA/CORYNACTIS/VELEROA. 


+= OUTLINE oF TALUS BED 
* LOCATION OF PERMANENT TRANSECTS 


——-—— TRANSECT LINES(DEPTHS IN METERS BELOW MLLW) 


FIMAL ASSOCIATIONS BASED ON STATISTICAL COMPARISONS: 


BARNACLE/LIMPET 
MYTILUS/POLLICIPES 

ANTHOPLEURA SPP. 

MACROPHYTIC ALGAE 
LITHOTHAMNION/VELEROA 
VELEROA/LAGENIPORA/LOPHOGORGIA/MURICEA 
RHODYMENIA/VELEROA 
LITHOTHAMNION/TETRACLITA, 

+ DIOPATRA/CERIANTHID ANEMONES: 


HrONMOOeD> 


° 
i 


15 20 METERS 


(POR ACTUAL DISTANCES DOWN SOUTH AND EAST SIDES, 
DIVIDE BY 0.892 AND 0.877, RESPECTIVELY) 


| 1e 12/136 
AP PAB 


Figure C-5. Preliminary and final special associations, 
southeast quadrant. 


90 


12/136 


PRELIMIMARY ASSOCIATIONS BASED OW FIELD OBSERVATIONS: 


1 
2. 
3. 
a 
5. 
6 

7 


- DIOPATRA/CERIANTHIDS 
ASTRANGIA/GORGONIANS 
LAGENIPORA/SCRUPOCELLARIA 

LITHOTHAMNION COMPLEX /SERPULORBIS/VELEROA 
MACROPHYTIC ALGAE 

- MYTILUS/POLLICIPES 

BARNACLES/LIMPETS 

CORYNACTIS /ASTRANGIA 

LITHOTHAMNION COMPLEX/SERPULORBIS/DODECACERIA/VELEROA 
ASTRANGIA/CORYNACTIS /LOPHOGORGIA 

- TETRACLITA/LITHOTHAMNION COMPLEX 

. LITHOTHAMNION/LAGENIPORA/VELEROA 

- LOPHOGORGIA/CORYNACTIS/VELEROA 


+++ OUTLINE OF TALUS BED 
* LOCATION OF PERMANENT TRANSECTS 
—-— TRANSECT LINES(DEPTHS IN METERS BELOW MLLW) 


FIMAL ASGSOCIATIOMS BASED OM STATISTICAL COMPARISONS : 


BARNACLE /LIMPET 

MYTILUS/POLLICIPES 

ANTHOPLEURA SPP. 

MACROPHYTIC ALGAE 
LITHOTHAMNION/VELEROA 
VELEROA/LAGENIPORA/LOPHOGORGIA / MURICEA 
RHODYMENIA/VELEROA 
LITHOTHAMNION/TETRACLITA 

- DIOPATRA/CERIANTHID ANEMONES 


nxanmooo> 


(POR ACTUAL DISTANCES DOWN NORTH AND EAST SIDES, 
DIVIDE BY 0.876 AND 0.877, RESPECTIVELY) 


Figure C-6. Preliminary and final special associations, 


northeast quadrant. 


w)I 


APPENDIX D 


SUMMARY DATA, QUANTITATIVE CHARACTERIZATION OF 


Note: 


MAJOR SPECIES ASSOCIATIONS 


In order to calculate biomass values per 
unit area (0.25 square meter or, in the 
case of associations 6 and 7, 0.01 square 
meter), multiply values for average weight 
(average weight per individual specimen) 
by values for x (mean abundance per unit 
area). See Section 5 for average weight 
values applicable to Dodecaceria fewkesi, 
Lithothamnium complex, Serpulorbis 
squamigerus, Veleroa complex, and 
Corynactis californica. 


92 


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Table D-3. Areal coverages of major species associations (areal 
coverages are expressed as percent of total island 
area between the upper limit of the barnacle-limpet 
zone and the lower limit of revetment rock on the bottom). 


Provisional Species Associations (numerical designations for associ- 
ations on various sides of the island correspond to those designations 
in Table D-1 and Figs. C-3 to C-6). 


Table D-1 Percent Table D-1 
Subarea Coverage Subarea Percent coverage 
Upper Intertidal 11 2S 
Association #7 12 Sool 
(Barnacle-Limpet) 6.70 13 3.80 
Association #6 14 4.80 
(Mytilus-Pollicipes) 1.28 15 3.62 
Lower Intertidal and Subtidal 16 1.22 
1 0.76 17 185 
D 0.95 18 1.78 
3 DIN 19 2.36 
4 0.91 20 2.66 
5 0.54 21 1.02 
6 0.23 22 1.40 
7 0.70 23 1.69 
8 ADs 24 0.66 
9 Seri 
10 12.40 
Remaining island area not quantitatively sampled: polo} 
Total 100.00 


(15,560 m2) 


Final Species Associations (see Figs. 9 to 12) 


Association Percent 
Designation Coverage 
A Barnacle- limpet 6.70 
B Mytilus-Pollicipes ZS 
C Anthopleura Spp. 0.10 
D Macrophytic algae 7.38 
E Lithothamnium complex 53.47 
8 Veleroa-Lagenipora-Lophogorgia-Muricea 29.1 
G Rhodymenia-Veleroa 1.02 
H Lithothamnium- Tetraclita 0.61 
I Diopatra-cerianthid anemones 0.34! 
Total 100.00 


(15,560 m2) 


lpresent as small isolated pockets on the lower parts of association F 
and, on the north side, association E. 4 


100 


APPENDIX E 
OBSERVATIONS ALONG NATURAL BOTTOM TRANSECT 


The following is a discussion of substrate and biotic composition 
of the first segment of the transect (13.7- to 6.1l-meter depth). 


Over the depth range 13.7 to 11.3 meters, the substrate is silt 
with some shell fragments. The sediment is very soft and similar to 
that existing at the base of the east side of the island. The domi- 
nant biota are sea pens (Stylatula elongata), bat stars (Patiria 
miniata), whelks (Kelletia kelletii), and cerianthid anemones. Ona 
few isolated rocks (maximum vertical relief 0.25 meter) stony corals 
(Astrangia lajollaensis) were present and the tectibranch, Navanax 
inermis, was observed. 


At about 10.7 meters the substrate is more sandy with many shell 
fragments. Isolated smooth boulders (1- to 2-meter diameter) are 
present with the evidence that they are intermittently covered with 
sand (no epiphytic algae present). Diopatra spp. are common to abun- 
dant in patches of up to about 100 individuals. Kelletia, Patiria, 
and Strongylocentrotus franciscanus are present. Vertical pipes 
(about 1 meter high) were observed with cf. Metridium sp. attached. 
Diaulula sandiegensis, Corynactis california, Cancer sp., cf. 
Stylatula, and cerianthid anemones were present. Also at this depth, 
gorgonians (Muricea spp. and Lophogorgia chilensis) appear on iso- 
lated rocks, with Muricea common to locally abundant. 


From 10.7 to 9.1 meters, smooth boulders, as described above, 
dominate the substrate. However, these boulders are more heavily 
encrusted with Astrangia, Veleroa, and Lithothamnium complex. Around 
the rock bases, where some sand is present, Diopatra ornata occur. 

The midshipman (Porichthys spp.), juvenile olive rockfish (Sebastes 
serranoides) and sanddabs (Citharichthys sp.) are also present. 
Lithothamnium coverage ranges up to 15 to 20 percent of exposed rock 
areas. Also present on vertical pipes and rocks are sponges (Leucetta 
losangelensis), Metridium, and Strongylocentrotus franciscanus. 
Strongylocentrotus purpuratus was also observed along these depths, 
but this species was not abundant. Cypraea spadicea, Tethya aurantia, 
Pisaster brevispinus, P. giganteus, and Dermasterias imbricata were 
also present to common on the solid substrate. 


From 7.6 to 6.1 meters the substrate changes from smooth boulders 
to solid shale bedrock with isolated boulders and sand patches. 
Pholad bivalves, starfish, and urchins dominate the macrobiota. Some 
red alga (Veleroa complex and Lithothamnium) are present; also juve- 
nile red algae was observed attached to the rock. 


101 


The next segment of the transect, extending from a depth of 
about 4.6 meters to shore, is predominantly sand and largely de- 
pauperate in macrobiota (visibility was yery poor during the two 
occasions this area was examined). From this point shoreward, scat- 
tered rocks (30- to 60-centimeter diameter) were commonly encountered. 
Acorn barnacles were abundant on these rocks, and coverages of 
Lithothamnium complex and the tunicate, Styela montereyensis average 
about 15 and 45 percent, respectively. Other organisms present to 
common in this nearshore zone include starfish (Patiria miniata and 
Pisaster ochraceus), feather boa kelp (Egregia menziesii), hydroids 
and tunicates. Tunicates are especially abundant (60 to 70 percent 
coverage) between depths of 4.3 to 3.7 meters. 


In general, the deeper parts of this transect are predominantly 
Silt. Where rocks occur, they are comparable to the deeper areas of 
the east-side permanent transect (i.e., very little epibiota, and 
much silt). Farther inshore along the natural bottom transect, less 
silt and more sand are present. The rocks, which are smoother than 
in deeper water, resemble deeper rocks on the north side of the 
island in that much Astrangia lajollaensis is present but differs in 
that ectoprocts are for the most part missing. 


102 


APPENDIX F 


SIEVE ANALYSIS OF NATURAL BOTTOM 
SEDIMENT SAMPLES 


103 


Han 


i GHG Hl 
A 


¥aSuVOD INZ9u3d 


UNITS 


PHI 


Seive analysis results from natural bottom sediments 


(station locations shown on Fig. 


Figure F-1. 


18). 


104 


Table F-l. Sieve analysis, natural bottom sediments, Sample 1 
(Sample location shown on Figure 18.). 


T5307 
SIEVS ANALYSIS Sax.ie Date anc no. SED SamPes at) 
Megh. As2l. Shzet No. 3 os A 
(Revised Nov. 1930) ESSREY tp Null VINO ise RI anne oR 


Pe4 Mig = 3.65 
Big 2-25 Avspa 4 
prea Z eS = a4 Analyzed by Dy Dat P0hhlg7? 
£e.+816 () = Mg = 
Mg-Nas =(S) «= : 
S/og 0 = ag = KiJCOn 


SAMPLE DESCRIPTION 
Color __ Size 


Sorting Roundness 
Composition 
Wt. Dish] Wt. of | Wt. of % of Cum % Notes 


Sample Dish Sample | Tot21 


Wits 


Bs 
SNS 
wW 
Ly 

we 

ES 

S 

i) 
Be |hes 
~N 
> 


q 
uy 
Ki 
S 


™ 
~ 
WY 


~s 
ion 


| bs 


105 


Table F-2. Sieve analysis, natural bottom sediments, Sample 2 
(Location shown on Figure 18.). 


oe’ 
SIEVE ANALYSIS Sr 23 Date ane no. SBD Sampee ee 
Meck. Anal. Sh=2t No. 3 ‘ Sa =) 
(Reyised Nev. 1930) ccaLity 38 


Analyzed by D. Avarey DateCIWET? 


a a eye 

fgathyg 3.62) = Ng = 1 7G 
Mg-d 5s =S = Le 
S/og Sag = a 


SAMPLE DESCRIPTION 
Color Size 


Sorting Roundness 


Composition 
Dish [Wt. Dish} Wt. of | Wt. of hb of Cun -% Notes 
No. Sample Dish Sample Total i 
We. | 
az | F_|48.93014 05, | roo 


BS 
ns 


Ua (au 


SS 
& |X | 


NI 


eae 


Ry RIE 
oX\ 


Le, bad] 
4,823. 
Vea, 713 
| 32027 03. AF 
3 to 34 139.043 : /o4, 5. asthe 
shyt 74¢a Vox | 
ese EO pss hes 


106 


APPENDIX G 


GLOSSARY 


armor rock - Heavy rock, usually 
weighing 500 pounds or more, 
used to protect a coastal 
structure or shore from heavy 
wave attack. 


associations - In ecology, a 
subunit of community organi- 
zation identified by its 
major organisms. 


azimuth - In this case, the arc 
of the horizon measured in 
degrees, clockwise from 
north to the point toward 
which the diver is swimming. 


bathymetry - The measurement 
of depths of water in oceans, 
seas, and lakes, also infor- 
mation derived from such 
measurements. 


benthic - Pertaining to the 
subaquatic bottom. 


biomass - The amount of living 
material in a unit area for 
a unit time. 


biota - The living part of a 
system; flora and fauna. 


caudal peduncle - The con- 
stricted part of a fish 
immediately ahead of the tail 
fin. 


climatic community - a community 
that is in equilibrium with the 
general climate. 


climax - The final stage in 
community succession. 


complex - An assemblage of inter- 
connected or interacting parts. 


dendogram - The type of diagram 
commonly referred to as a 
"family tree'' designed to show 
postulated relationships between 
taxa. 


depauperation - Falling short of 
usual development or size. 


ecosystem - The living organisms 
and the nonliving environment 
interacting in a given area. 


ectoprocts - A bryozoan (moss 
animal) of the group Ectoprocta. 


epibiota - Life forms attached to 
or living upon surfaces. 


F test - A method used to test 
the hypothesis that the means 
in several classes statistically 
are similar. 


genus - A unit of biological 
classification (taxa) which 
includes one or several species 
that share certain fundamental 
characteristics, supposedly by 
common evolutionary descent. 


gill net - A single-webbed net 
with meshes sized to catch in 
the gills of the fish being 
sought. 


infauna - The animals that live 
in the bottom sediment. 


intertidal zone - The zone 
bounded by the high and low 
water extremes of the tide. 


macrobiota - Large forms of life 
visible to the naked eye. 


macrophytic - Refers to large 
aquatic plants, e.g., kelps. 


nonparametric test - A statistical 
test that is not concerned with 
the specific parameters, but 
rather with the distribution of 
the variates. Also referred to 
as distribution free. See 
parameter. 


parameter - A parameter is a 
measurable characteristic of a 
population. The mean is an 
example of a parameter. 


quadrat - A plot usually square 
but occasionally rectangular or 
circular, in which the organisms 
are intensely examined and one or 
several of which form the basis 
for assessing the entire popu- 
lation of the area. 


revetment - A facing of stone, con- 
Erete,) tC y,  DuIlitReonprorectaa 
Scarp, embankment, or a shore 
structure against erosion by 
wave actions or currents. 


riprap - A layer, facing, or pro- 
tective mound of stones randomly 
placed to prevent erosion, scour, 
or sloughing of a structure or 
embankment. Also, the stone so 
used. 


Simpson's Index - An index of the 
proportions and numbers of 
species and individuals in a 
community used to measure the 
diversity. 


species - A group of individuals 
having common attributes and 
designated by a common name. 


splash zone - The zone immediately 
landward of the mean high water 
level affected by the wave 
spray. 


substrate - The base on which an 
organism lives. 


subtidal - Below mean low water 
(lower low on the Pacific coast 
of the United States). 


succession - In ecology, an order- 
ly process of community 
development and changes with 
time which result from inter- 
actions between species and 
environment. 


108 


taxa - A taxanomic group or entity 
such as genus or species in a 
formal system of scientific 
nomenclature. 


tetrapod - A massive concrete 
shape for wave protection con- 
sisting of a central body and 
four equal-length limbs radiat- 
ing out at equal angles from 
the central body. The tetrapods 
at Rincon Island weigh between 
19.5 and 38.0 tons each. 


transect - A line (or belt) 
through a community along which 
the important characteristics 
of the individuals of the 
species being studied are 
observed and noted; sampling 
along a transect may be plotless 
or refer to specific plots 
located along a line. 


turbidity - An optical condition of 
water resulting from suspended 
matter; water is turbid when its 
load of suspended materials is 
conspicuous. 


Wilcoxon ''t'' test - A nonpara- 
metric test used to statistically 
determine whether the ranked 
differences between measurements 
came from the same or different 
populations. 


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