Z @@@ @@@@ `e#@RDQ & EN DB      & .7/ >v^XP F n_Z`kendall-frost pubs 99-00ENDBENDN` NRS libraryENDBENDN` scripps publications 99-00ENDBENDN` student reportsancelj0X ,jPPk@L7 4L<Ejectk`0 ,kP(kЫ@8 7<PL<Desktopl 0,l`P l Scanland1971qO Schlising1982 Siegal1984 Siegal1984& Stewart1980F Stewart1982? Tutschulte@ Van Blaricom1978H Vaske1979' Warme1969( Warner1984A Wolfson1973BYoshioka1973xcz! w  cz} xz`}  xz@}&%x$%$%%&&&"{P! wz0|{~xHH{0}L${%&$%$%%&&D"!D"x|}&%{$%$%%&&|~{HHp|0~z!` w mzHH3}@! w7z<} p z}Ы@P????????|><<81#18<????????????????}p}\\\\\\\\\\\~@p  /}Pp /}p`p  (}@p&%}$%$%%&&&0 }}}dATVk}/9!0 wB=B=B==B=B=B=BB=B=B=B==B=B=B=B0pL$%&$%$%%&&f^&_V綹ۻp&%$%$%%&&og~ws?v?ߝ~}PHH}!` w}@!0 w O/}pPMMNNONOMNMMNMyzy PNs607!  wOO}Q}pp! wLOpMNNONOMNMy! wOO}Q}pi}iii}zyzy p! w0p ! w !pp0HH`!P w,GG`IP! w `! wmOp 0! wHD,;9!` wHH@00@ @ fvv2b5ZP@! w@!p wld@xUUUU w0!@ w'HH(`0P`@"(aA6Ⱥ"fdFd*۹fodBd"&81ґBfFD"$Ri@Yj#cfoB[ bDhfDY &R$g&BN! BlBl[Ș&J@"FBAF@`BHD  0D H @ R ($@ "&BI Hρ!sG DƠ@fbME ((@tdt 4ʊ^ĂrBA\C&BDF94ѨdLpFfD щ9&ff`hW8q1 d b&ɑyhf/d!]*Dz&eDIBf(&nxf>ɑofvfj&Jfbj#J8jff'bVgB Qfdffd *f&$"f&t9[j&Db٘PvFsvb&Fbu$9v4@cdb H"$`FpA TFbF) L@ `ʑPcB" F  ` A " @@  @HA@d0"@D@ )@C!,IyP; $.Tc)Hq@ ʼnhJ*R BdBJDFcF"Vx&"&$`d&m1顙.ffhBXb@$r&&$-jdgEB.b BgbF&9=&g&nfb]cLGeF-]^fdFFbbev$fPzfwBfo$t  ]drNn `flwP.AlFbb"hdd#`ffg fV@D@pAgedfd ddD"I8 B&$$ BBP@$d   D@P  "l@DZ`)H%@ %@@ ! WVhrr%_w,\c۾W[}Hpc1YNv$'>wwc@6|ߵ8anchor species, epiphytes, intertidal, algae, algal turf.This study characterizes a turflike vegetation composed of benthic marine algae, in the low intertidal in southern California, by means of quantitative relative abundance data collected over a 2-year period. The algae comprise a relatively homogeneous assemblage that is fastened to the substrate by one to six "anchor" taxa with thalli that persist throughout the year and become reestablished on exposed surfaces within several months. Two species of Corallina together occupy more than 60 percent of the total substrate sampled. Epiphytes attached to these anchor species include 42 species that are con-sistently found and another 25 that are infrequently or incidentally recorded. Abundances of several of the epiphytes fluctuated during the sampling period, but the number of species present showed no distinct seasonal change. In the northern Gulf of California a similar-appearing turf includes several of the same species in different proportions, but anchor species are different. Many unrelated taxa in both turfs exhibit the same morphological characters. A census of macroinvertebrates associated with the southern California vegetation suggests that grazing is not important in maintaining the relatively uniform height of these plants.@   Tutschulte, T.:3The Comparative Ecology of Three Sympatric Abalone."ecology, sympatric, abaloneVan Blaricom, G.R. 1978Disturbance, Predation, and Resource Allocation in a High Energy Sublittoral Sand Bottom Ecosystem: Experimantal Analyses of Critical Structuring Processes.d]disturbance, predation, resource allocation, sublittoral, sandy bottom, structuring processese Vaske, F. and O. Clarke8 1979JDA proposed addition to the Scripps' Shoreline Reserve, La Jolla, CA. Warme, N.F.` 1969JCMarine borers in calcareous terrigenous rocks of the Pacific coast. Am. Zoologist9765-7740F?marine borers, calcareous rock, terrigenous rock, Pacific coast{Warner, J.A., C. Arneson, R.W. Austin, D. Bailey, G. Huszar, P. James, R.R. McConnaughey, K. Nealson, and E.A. Stephan, Jr. 1984d^Scripps Canyon sea structure: A designated deployment for the study of oceanic bioluminesence.Marine Tech. Society J.174 40-47<6Scripps, Scripps Canyon, sea structure, bioluminesence Wolfson, A.A. 1973jdSome Effects of High Temperature on the Settlement and Development of a Marine Community in the Lab.JChigh temperature, settlement, development, temperature, marine, labjYoshioka, P.M. 1973ZThe Population Dynamics and Ecology of the Encrusting Ectoproct Membranipora serrilamells. @ Y ~Npopulation dynamics, ecology, encrusting, ectoproct, Membranipora serrilamells 5  ^S 76"Hartwick, R.F. 1975[Orientation Behavior in Beach Hoppers of the Genus Orchestoidea: Capacities and Strategies. 3 ? b2orientation, behavior, beach hoppers, Orchestoidea &  Hayes, W.B.` 1969KEcological Studies on the High Beach Isopod Tylos punctatus Holmes and Gay. , ; T#high beach, isopod, Tylos punctatush  @:Holland, K.T., B. Raubenheimer, R.T. Guza, and R.A. Holman 1995,%Run-up kinematics on a natural beach.:&Journal of Geophysical Research 100C3 4985-4993`03/15/95 kinematics, natural beachRunup kinematics on a gently sloping natural beach are examined with detailed measurements from video images, resistance wires deployed at five elevations (between 5 and 25 cm) above and parallel to the beach face, and pressure sensors located in the inner surf zone. As suggested in a previous study comparing a single-level resistance wire and manually digitized films, runup measurements are sensitive to the sensor elevation above the bed, owing to the elongated shape of the runup tongue. The measured mean runup elevation (setup) and vertical excursion increase as the sensor elevation decreases, with the video-based runup estimates having the maximum means and variances. For the six data runs the average ratios of the video-based setup and significant runup excursion to estimates based on wires elevated 15 cm above the bed are 2.7 and 1.5, respectively. These trends, combined with the high coherence and small phase difference between the video and the lowest wire, demonstrate that the video-based estimates correspond to a very near-bed (less than a few centimeters elevation) wire measurement. The measured increase in runup excursion with decreasing sensor elevation and the cross-shore variation in the amplitudes of pressure fluctuations at infragravity frequencies, are consistent with the theory for linear, inviscid, normally incident standing waves. For example, valleys in the pressure spectra occur at apporximately the predicted standing wave nodal frequencies. Also in accord with smal-amplitude wave theory, observed swash excursions are nearly identical to pressure fluctuations at the location of the measured runup mean (for pressure sensors located seaward of the most offshore bed-level rundown). However, at very low frequencies, where reflection is typically assumed complete and dissipation negligible, the observed, near-bed swash magnitudes are overamplified relative to a best fit of the linear standing wave model based on the amplitude and phase of the seaward observations.4-From research done at Scripps Coastal Reserved Hurley, A.C. 1973OFecundity of the acorn barnacle Balanus pacificus Pilsbury: A fugitive species.   1  Limnology and Oceanography183386-393n=fecunidty, acorn barnacle, fugitive species Balanus pacificus ,  Hurley, A.C. 1973nLarval settling behavior of the acorn barnacle (Balanus pacificus, Pilsbury) and its relation to distribution. 0 B  Journal of Animal Ecology42599-609@larval settling, acorn barnacle, Balanus pacificus, distribution ! 2 2,Inman, D.L., C.E. Nordstrom, and D.G. Aubrey"Longshore transport of sand. chapter 18:3longshore, sand transport, sediment transport, sand<Z;R:D #d"9!*8HN @0*Inman, D.L., R.J. Tait, and C.E. Nordstrom 1971 Mixing in the surf zone.P&Journal of Geophysical Researchi7615 3493mixing, surf zone2,Inman, D.L., C.E. Nordstrom, and D.G. Aubrey 19772+Beach profile analysis underway at Scripps.D82Southern California Sediment Management Newsletter24beach profile, Scripps2,Inman, D.L., C.E. Nordstrom, and D.G. Aubrey 19786/The impact of coastal structures on shorelines.,{Proceedings of the Symposium on Technical, Environmental, Socioeconomic, and Regulatory Aspects of Coastal Zone Management. 2265-2272:3coastal structures, shoreline, environmental impact.(Jenny, H., R.J. Arkley, and A.M. Schultz 1969XQThe Pygmy Forest-podsol ecosystem and its dune associates of the Mendocino coast. Madrono202@p. 60-74LFPygmy Forest-podsol podsol Pygmy Forest dune Mendocino Mendocino coast Jones, L.L. 1978dThe Life History Patterns and Host Selection Behavior of a Sponge Symbiont, Membranobalanus orcutti. L c Qlife history, host selection, behavior, sponge, symbiont, Membranobalanus orcuttit :  Klapow, L.A. 1970;Ovoviviparity in the genus Excirolana (Crustacea: Isopoda).  % J. Zool., London 162-359-369^-ovoviviparity, Crustacea, Isopoda, Excirolana #  Klapow, L.A. 1971The Ecology and Behavior of a Sand Beach Isopod, Excirolana chiltoni: Distribution, Abundance, and Temporal Patterns in Molting, Reproduction, and Swimming Activity.b 1 D ecology, behavior, sandy beach, isopod, distribution, abundance, temporal patten, molting, reproduction, swimming, Excirolana chiltoni s  Klapow, L.A. 197282Natural and artificial rephasing of a tidal rythm.J. Comp. Physiol.-79233-258rephasing, tidal rythm Klapow, L.A. 1972YFortnightly molting and reproductive cycles in the sand-beach Isopod Excirolana chiltoni.p E X Biological Bulletinn 143568-591.vEmolting, reproductive cycle, sandy beach, Isopod, Excirolana chiltoni 2   Kobayashi{ 1979~California Marine Waters: Areas of Special Biological Significance Reconnaissance Survey Report: San Diego Marine Life Refuge. *#State Water Resources Control Boardo68"Reconnaisance Survey Report `YCalifornia, marine, San Diego marine life refuge, Area of special Biological significanceDraft Report, discusses location and size; nearshore waters and submarine topography; geophysical characteristics; climate; biota of both subtidal and intertidal habitats; landside flora.a' UCSD Lewbel, G.S. 1976P Sex ratios in Caprella gorgonia.  Lsex ratio, Caprella gorgonia    Mynderse, J.[Halogenated Monoterpenes from Plocamium cartilagineum Dixon and Plocamium violaceum Farlow.  5 @ S vFhalogenated, monoterpene, Plocamium cartilagineum, Plocamium violaceum   Navarro, Jennie M. 2001LFDensity of Juvenile Mussels in San Diego County: A Study on Two Scales La Jolla UCSD/SIO 1-14 SeptemberzsMytilus mussles, marine invertebretes, rocky intertidal, San Dieog County, Pre-settlement, post settlement, densityMystilus mussels are a group of marine invertebrets that occur throughout the rocky intertidal of San Diego county. Declining populations of adult mussel beds in a marine protected area, Cabrillo National Monument, has become a topic of concern. The purpose of the study was to determine if this problem is related to pre-settlement or post settlement processes by determining density of juvenile mussels in certain zones of Cabrillo as well as at a larger, regional scale. Results showed that there are few settlers in Cabrillo, most notably in the southern section. This indicates that pre-settlement processes are, at least in part contributing to a decline in adult mussels in Cabrillo National Monument..(research done at Scripps Coastal Reserve Nishimori, R.zThe Petrology and Geochemistry of Gabbros from the Penninsular Ranges Batholith, California, and a Model for Their Origin.RKpetrology, geochemistry, gabbros, Penninsular Ranges, Batholity, Californiag  BTQlife history, host selection, behavior, sponge, symbiont, Membranobalanus orcuttidalife history, littoral, gastropod, Prosobranchia, Muricidae, Shaskyus festivus, Ocenebra poulsoni83longshore, sand transport, sediment transport, sand Los Angelesa @=lunar orientation, Amphipoda, stout, Orchestoidea corniculataD?marine borers, calcareous rock, terrigenous rock, Pacific coastA| MendocinoMendocino coastds,(microspicules, fan coral, Eugorgia ampla,&migration, homing, marine invertebrate; Mima Moundsmixing, surf zoneHEmolting, reproductive cycle, sandy beach, Isopod, Excirolana chiltoni MontereyxsMytilus mussles, marine invertebretes, rocky intertidal, San Dieog County, Pre-settlement, post settlement, densityb82orientation, behavior, beach hoppers, Orchestoidea origin!;0-ovoviviparity, Crustacea, Isopoda, ExcirolanaPacific Northwest$!patch, rocky intertidal, dynamicsPKpetrology, geochemistry, gabbros, Penninsular Ranges, Batholity, Californiaplant podsolForPMpopulation dynamics, ecology, California spiny lobster, Panulirus interruptusTNpopulation dynamics, ecology, encrusting, ectoproct, Membranipora serrilamells4.Porifera, bacteria, primitive, marine organism(%predation, epifauna, submarine canyon Pygmy Forest-Pygmy Forest-podsol<8rephasing, tidal rythm;@=reproduction, abnormal reproduction, sand crab, nuclear powerRichvale Vernal Pools(#run-up, earth science, oceanography40San Diego, La Jolla, reserve, ecological reserveSanta Monica Mountains!< Scrippsni<6Scripps, Scripps Canyon, sea structure, bioluminesenceA|@:sea urchin, settlement patterns, S. francis, S. purperatus840sediment, marine sediment, Polychaete, tube worm<9selection, coevolution, kelp, canopy, southern California sex ratio, Caprella gorgonia$solar wind, IPS?,)sonar altimeter, nearshore, earth sciencesouthern Californiain<8southern California, nearshore, sandy beach, sand bottomLFstorm, catastrophe, catastrophic storm, El Nino, patch stabiligy, kelp swash, beach, gentle slope"HDtemperature compensation, stout-duration, time, intertidal, Amphipod`]territorial, behavior, population dynamics, Pomacentrid, fish, garibaldi, Hypsypops rubicundad_territorial, behavior, population dynamics, Pomacentridae, fish, garibaldi, Hypsypops rubicunda@Ttidal rythm, entrainment$ tidal rythm, Isopod, sandy beach,$tide, extreme tide, CaliforniaP@=triglyceride, wax ester, digestion, fish, triglyceride lipaseturbulence, surf zone,'upwelling, plankton, larvae, tidal borevascular plant)d vegetation Venturael vernal poolrn WashingtonsWashington State@$wave height, pressure, sand bedP4/wave transformation, inner surf zone, surf zone$wave, ripples, nearshore, sand*?lzonation, mysidsQJ=$54hM\3vr210lfOlson, M.S., T.D. Finnigan, A. Milgram, R.A. Arkin, V.J. Paul, S. Glass, G.B. Rankin, and R.S. Kaufman 1979kObservations on the population dynamics and ecology of the California spiny lobster, Panulirus interruptus. U j ~Mpopulation dynamics, ecology, California spiny lobster, Panulirus interruptus  8  Patton, J.Comparative Studies of Triglyceride and Wax Ester Digestion in Fish and the Characterization of a Novel Nonspecific Triglyceride Lipase.D=triglyceride, wax ester, digestion, fish, triglyceride lipase Pawlik, J.R. 1988b\Chemical induction of the larval settlement of honeycomb worms (Polychaeta: Saberllariidae).*#Scripps Institution of Oceanographya  San Diego, CA *#University of California, San Diego Ph.D.VPinduction, larval settlement, honeycomb worms, worms, Polychaeta, Saberllariidae Pineda, J. 1991f_Predictable Upwelling and the Shoreward Transport of Planktonic Larvae by Internal Tidal Bores.lScience` 253548-551.'upwelling, plankton, larvae, tidal bore>7Raubenheimer, B., R.T. Guza, S. Elgar, and N. Kobayashi 1995&Swash on a gently sloping beach`&Journal of Geophysical Research  100lC5 8751-8760 swash, beach, gentle slopeWaves observed in the inner surf and swash zones of a fine grained, gently sloping beach are modeled accurately with the nonlinear shallow water equations. The model is initialized with observations from pressure and current sensors collocated about 50 m from the mean shoreline in about 1 m depth, and model predictions are compared to pressure fluctuations measured at five shoreward locations and to run-up. Run-up was measured with a vertical stack of five wires supported paralles to and above the beach face at elevations of 5, 10, 15, 20, and 25 cm. Each 60-m-long run-up wire yields time series of the most shoreward location where the water depth exceeds the wire elevation. As noted previously, run-up measurements are sensitive to the wire elevation owing to thin run-up tounges not measured by the more elevated wires. As the wire elevation increases, the measured mean run-up location moves seaward, low-frequency (infragravity) energy decreases, and higher-frequency sea swell energy increases. These trends, as well as the variation of wave spectra and shapes (eg., wave skewness) across the inner surf zone, are well predicted by the numerical model.4-From research done at Scripps Coastal Reserve#0> LXR/rL .G -x T,8+*DK)ECJZIVTMPreliminary report: Engineering geology of the city of San Diego, California.XRReconnaissance study: Black's Beach and Sunset Clifs areas; San Diego, California.  1978rlReconnaissance Survey of the San Diego La Jolla Ecological Reserve: Area of Special Biological Significance.60San Diego, La Jolla, reserve, ecological reserve  1984:4The Coast of California Storm and Tidal Waves Study. "U.S. Army Corps of Engineers<6coast, California, storm, wave, tidal wave, storm wave Anderson, R.LFChemical Studies of Primitive Marine Organisms: Porifera and Bacteria.4.Porifera, bacteria, primitive, marine organism Axelrod, D.I. 19822,Age and origin of the Monterey Endemic Area.Madrono293 p. 127-1474.age origin Monterey endemic California Scripps Barry, C.K. 1973nExperimental Analysis of Habitat Selection in Epiphytic Shrimps of the Genus Hippolyte in Southern California. M V tChabitat selection, epiphyte, shrimp, southern California, Hippolytee :  Barry, J.P.p 1988b[Pattern and process: patch dynamics in a rocky intertidal community in Southern California.t*#Scripps Institution of Oceanographya  San Diego, CA *#University of California, San Diegoo Ph.D.(!patch, rocky intertidal, dynamicsBernstein, B.B. 1977\VSelective Pressures and Coevolution in a Kelp Canopy Community in Southern California.@9selection, coevolution, kelp, canopy, southern Californiat"Bishop, M.J. and S.J. BishopJCA census of marine prosobranch gastropods at San Diego, California.pVeliger162143-152$census, prosobranch, gastropod Clarke, T.A.mTerritorial boundaries, courtship, and social behavior in the Garibaldi, Hypsypops rubicunda (Pomacentridae).  I \  295 Clarke, T.A. 1968oTerritorial Behavior and Population Dynamics of Garibaldi, Hypsypops rubicunda (Girard), Pisces: Pomacentridae.. ; N f_territorial, behavior, population dynamics, Pomacentridae, fish, garibaldi, Hypsypops rubicunda Clarke, T.A. 1970hTerritorial behavior and population dynamics of a Pomacentrid fish, the garabaldi, Hypsypops rubicunda. T Ecological Monographs402!189-212@d]territorial, behavior, population dynamics, Pomacentrid, fish, garibaldi, Hypsypops rubicundar Clutter, R.I. 1963|Distribution Pattern, Aggregation Behavior, and Dynamics of a Population of a Hypoplanktonic Mysid, Metamysidopsis elongata. d { hdistribution, aggregation, behavior, population dynamics, hypoplanktonic, mysid, Metamysidopsis elongata Q  Clutter, R.I. 1967$Zonation of near shore mysids.Ecology"482" 201zonation, mysids"Davies, B.M and A.R. French 1992xrPocket gopher abundance, soil depth, and vegetation relationships in coastal sage scrub and grassland communities. Davis, N.JCStudies of the Southern California Nearshore Sand Bottom Community.>8southern California, nearshore, sandy beach, sand bottom"Dayton, P.K. and M.J. Tegner 1984`ZCatastrophic storms, El Nino, and patch stability in a southern California kelp community.Science 224283-285LFstorm, catastrophe, catastrophic storm, El Nino, patch stabiligy, kelpDe Coursey, P.J. 19762,Biological Rhythms in the Marine Environment  Columbia, SC South Carolina Press60biological rythms, biorythms, marine environment(!Del Moral, R. and D.C. Deardorff 197660Vegetation of the Mima Mounds, Washington State.Ecology57 p. 520-530PJvegetation flora Mima Mounds Washington Washington State Pacific Northwest Dingler, J.R. 1970.'Wave-formed ripples in nearshore sands.*#Scripps Institution of Oceanography  San Diego, CA *#University of California, San Diegoo$wave, ripples, nearshore, sand Dingler, J.R. 1974.'Wave-Formed Ripples in Nearshore Sands.$wave, ripples, nearshore, sand60Ebert, T.A., S.C. Schroeder, J.D. Dixon, Kalvass 1994USettlement patterns of red urchins (S. francis and S. purperatus) in California, USA. $ / 3 @ &Marine Ecology Progress Societyt 111 41-52:sea urchin, settlement patterns, S. francis, S. purperatus ! + - 4-From research done at Scripps Coastal Reserve0)Elgar, S., B. Raubenheimer, and R.T. Guza2000 (submitted)2+Current meter performance in the surf zone..'Journal of Atmospheric Ocean Technologycurrent meter, surf zone4-From research done at Scripps Coastal Reserve Enright, J.T. 1961@Lunar orientation of Orchestoidea corniculata Stout (Amphipoda).  - Biological Bulletin# 1202148-156#n=lunar orientation, Amphipoda, stout, Orchestoidea corniculata %  Enright, J.T. 1961\Distribution, Population Dynamics, and Behavior of a Sand Beach Crustacean, Synchelidium sp. L adistribution, population dynamics, behavior, sandy beach, crustacea, crustacean, Synchelidium sp.y Q  Enright, J.T. 19624-Responses of an Amphipod to pressure changes.PComp. Biochem. Physiol.7n131-145 Amphipod, pressure changed Enright, J.T. 1963:3The tidal rythm of activity of a sand-beach Isopod.hComp. Biochem. Physiol. 46276-313$& tidal rythm, Isopod, sandy beach Enright, J.T. 1965$Entrainment of a tidal rythm.aScience$ 147 3660864-867@tidal rythm, entrainment Enright, J.T. 1967b[Temperature compensation in stout-duration and time measurements by an intertidal Amphipod.nScience 156 3781 1510-1512 JDtemperature compensation, stout-duration, time, intertidal, Amphipod Enright, J.T. 1971,&The internal clock of drunken Isopods.Z. Vergl Physiologie75332-346internal clock, Isopod Enright, J.T. 1972F?A virtuoso Isopod: Circa-lunar rythms and their fine structure.J. Comp. Physiol.%77141-162Isopod, lunar rythm% Enright, J.T. 1976NHPlasticity in an Isopod's clockworks: Shaking shapes form and frequency.J. Comp. Physiol. 107  13-37Isopod, shakingI Enright, J.T. 1978NHMigration and homing of marine invertebrates: a potpourri of strategies..(Animal Migration, Navigation, and Homing,&migration, homing, marine invertebrate Fager, E.W. 1964>8Marine sediments: Effects of a tube-building Polychaete.Science 143 3604356-35960sediment, marine sediment, Polychaete, tube worm <;R:D #d"9!*8HN @0*Inman, D.L., R.J. Tait, and C.E. Nordstrom 1971 Mixing in the surf zone.P&Journal of Geophysical Researchi7615 3493mixing, surf zone2,Inman, D.L., C.E. Nordstrom, and D.G. Aubrey 19772+Beach profile analysis underway at Scripps.D82Southern California Sediment Management Newsletter24beach profile, Scripps2,Inman, D.L., C.E. Nordstrom, and D.G. Aubrey 19786/The impact of coastal structures on shorelines.,{Proceedings of the Symposium on Technical, Environmental, Socioeconomic, and Regulatory Aspects of Coastal Zone Management. 2265-2272:3coastal structures, shoreline, environmental impact.(Jenny, H., R.J. Arkley, and A.M. Schultz 1969XQThe Pygmy Forest-podsol ecosystem and its dune associates of the Mendocino coast. Madrono202@p. 60-74LFPygmy Forest-podsol podsol Pygmy Forest dune Mendocino Mendocino coast Jones, L.L. 1978dThe Life History Patterns and Host Selection Behavior of a Sponge Symbiont, Membranobalanus orcutti. L c Qlife history, host selection, behavior, sponge, symbiont, Membranobalanus orcuttit :  Klapow, L.A. 1970;Ovoviviparity in the genus Excirolana (Crustacea: Isopoda).  % J. Zool., London 162-359-369^-ovoviviparity, Crustacea, Isopoda, Excirolana #  Klapow, L.A. 1971The Ecology and Behavior of a Sand Beach Isopod, Excirolana chiltoni: Distribution, Abundance, and Temporal Patterns in Molting, Reproduction, and Swimming Activity.b 1 D ecology, behavior, sandy beach, isopod, distribution, abundance, temporal patten, molting, reproduction, swimming, Excirolana chiltoni s  Klapow, L.A. 197282Natural and artificial rephasing of a tidal rythm.J. Comp. Physiol.-79233-258rephasing, tidal rythm Klapow, L.A. 1972YFortnightly molting and reproductive cycles in the sand-beach Isopod Excirolana chiltoni.p E X Biological Bulletinn 143568-591.vEmolting, reproductive cycle, sandy beach, Isopod, Excirolana chiltoni 2   Kobayashi{ 1979~California Marine Waters: Areas of Special Biological Significance Reconnaissance Survey Report: San Diego Marine Life Refuge. *#State Water Resources Control Boardo68"Reconnaisance Survey Report `YCalifornia, marine, San Diego marine life refuge, Area of special Biological significanceDraft Report, discusses location and size; nearshore waters and submarine topography; geophysical characteristics; climate; biota of both subtidal and intertidal habitats; landside flora.a' UCSD Lewbel, G.S. 1976P Sex ratios in Caprella gorgonia.  Lsex ratio, Caprella gorgonia    Mynderse, J.[Halogenated Monoterpenes from Plocamium cartilagineum Dixon and Plocamium violaceum Farlow.  5 @ S vFhalogenated, monoterpene, Plocamium cartilagineum, Plocamium violaceum   Nishimori, R.zThe Petrology and Geochemistry of Gabbros from the Penninsular Ranges Batholith, California, and a Model for Their Origin.RKpetrology, geochemistry, gabbros, Penninsular Ranges, Batholity, Californiag &0O>%WV P 0)Raubenheimer, B., R.T. Guza, and S. Elgar 19966/Wave transformation across the inner surf zone.m&Journal of Geophysical Researchd 101 C1025, 589-525, 5976/wave transformation, inner surf zone, surf zoneSea and swell wave heights observed on transects crossing the mid and inner surf zone on three beaches (a steep concave-up beach, a gently sloped approximately planar beach, and a beach with an approximately flat terract adjacent to a steep foreshore) were depth limited (i.e., approximately independent of the offshore wave height), consistent with previous observations. The wave evolution is well predicted by a numerical model based on the one-dimensional non-linear shallow water equations with bore dissipation. The model is initialized with the time series of sea surface elevation and cross-shore current observed at the most offshore sensors (located about 50 to 120 m from the mean shoreline in mean water dpeths 0.80 to 2.10 m). The model accurately predicts the cross-shore variation of energy at both infragarvity (nominally 0.004 < f 0.05 Hz) and sea swell (here 0.05 < f 0.18 Hz) frequencies. In models of surf zone hydrodynamics, wave energy dissipation is frequently parameterized in terms of gs , the ratio of the sea swell significant wave height to the local mean water depth. The observed and predicted values of gs increase with increasing beach slope b and decreasing normalized (by a characteristic wavenumber k) water depth kh and are well correlated with b/kh, a measure of the fractional change in water depth over a wavelength. Errors in the predicted individual values of gs are typically less than 20%. It has been suggested that infragravity motions affect waves in the sea swell band and hence gs, but this speculation is difficult to test with firld observations. Numerical simulations suggest that for the range of conditions considered here, gs is insensitive to infragravity energy levels.   @ w x @{                @   @   @ 4-From research done at Scripps Coastal Reserve$Raubenheimer, B. and R.T. Guza 1996.'Observations and predictions of run-up.&Journal of Geophysical Research 101 C1025, 575-525, 588*#run-up, earth science, oceanography For a significant range of offshore wave conditions and foreshore slopes, run-up observations are compared to semiempirical formulations and predictions of an existing numerical model based on the depth-averaged one-dimensional nonlinear shallow water equations with bore-like breaking wave dissipation and quadratic bottom friction. The numerical model is initialized with time series of sea surface elevation and cross-shore velocity observed in 80 cm mean water depth (approximately 50 m offshore of the mean shoreline) on a gently sloping beach and in 175 cm water depth (100 m offshore of the shoreline) on a steep concave beach. Run-up was measured with a stack of resistance wires at elevations of 5, 10, 15, 20, and 25 cm above and parallel to the beach face. At sea swell frequencies (nominally 0.05 < f 01.8 Hz), run-up energy is limited by surf zone dissipation of shoreward propagating waves so that increasing the offshore wave height above a threshold value does not substantially increase the predicted or observed sea swell run-up excursions (e.g., run-up is "saturated"). Existing semiempirical saturation formulations are most consistent with the observations and numerical model predictions of run-up excursions nearest the bed. In contrast, at infragravity frequencies (0.004 < f 0.05 Hz) where surf zone dissipation is relatively weak and reflection from the beach face is strong (e.g., saturation formulas are not applicable), the run-up excursions increase approximately linearly with increasing offshore wave height. The numerical model also accurately predicts that the tongue-like shape of the run-up results in sensitivity of run-up measurements to wire elevation. For instance, run-up excursions and mean vertical superelevation (above the offshore still water level) increase with decreasing wire elevation, and continuous thinning of the run-up tongue during the wave uprush can result in large phase differences between run-up excursions measured at different wire elevations. Numerical model simulations suggest that run-up measured more than a few centimeters above the bed cannot be used to infer even the sign of the fluid velocities in the run-up tongue. . /   4-From research done at Scripps Coastal Reserven0)Raubenheimer, B., S. Elgar, and R.T. Guzae 1998D=Estimating wave heights from pressure measured in a sand bed.g<5Journal of Waterway, Port, Coastal, Ocean Engineering  124151-154&wave height, pressure, sand bednyComparison of predicted with observed attenuation of pressure fluctuations shows that wave heights can be estimated with observations from a pressure sensor that is buried a known depth in fine sand. The attenuation of pressure fluctuations within the sand bed under unbroken shoaling waves, bores in the surf zone, and swash near the shoreline was measured with vertical stacks of buried pressure sensors. The attenuation increased with increasing frequency and depth below the bed surface, consistent with previous observations of an infinitely deep soil skeleton that is much more compressible than the pore fluid, the predicted pressure fluctuations decrease exponentially with increasing burial depth, and the attenuation is independent of the sediment properties. For the fine-grained sand beds considered here, this exponential limit accurately predicts the observed attenuation.d4-From research done at Scripps Coastal Reserveh Rickett, B.J. 1972<5Disturbances in the solar wind from IPS measurements.@ Solar PhysicsP43237-247solar wind, IPSScanland, T.B. 1971qHBEffects of Predation on Epifaunal Assemblages in Submarine Canyon.,%predation, epifauna, submarine canyon& Schlising, R.A. and E.L. Sanders 1982TMQuantitative analysis of vegetation at the Richvale Vernal Pools, California.aAmerican Journal of Bot.695 p. 734-742XQdata analysis vegetation flora plant Richvale Vernal Pools California vernal pool  Siegal, P.R. 1984EStudies of growth and reproduction in the sand crab, Emerita analoga.e 5 D  Santa Barbara, CAp .'University of California, Santa Barbara Ph.D.60growth, reproduction, sand crab, Emerita analoga$Siegal, P.R. and A.M. Wenner 1984tnAbnormal reproduction of the sand crab in the vicinity of a nuclear generating station in Southern California.Marine Biology80341-345 D=reproduction, abnormal reproduction, sand crab, nuclear power  Stewart, J. 1980f_Assemblages of algae and invertebrates in southern California dominated intertidal communities.!Aquatic Botany9P 73-94<5algae, invertebrates, southern California, intertidal 54hM\3vUTr210Y Flick, R. E. 20000*Time-of-Day of Peak in a Mixed-Tide Regime Shore & Beach684 15-17October$tide, extreme tide, CaliforniaThe occurance along the California coast of highest-high tides in the morning during winter and in the afternoon during summer is explained as the interaction of the two largest tide constituents (M2 and K1). This seasonally oscillating, loose phase locking of the time of day of peak high tides is a consequence of the area's mixed-tide regime, and an example of how tide characteristics of mixed-tide regions differ from those in areas with predominantly semi-daily tides. The observed pattern of peak high tides has has notable consequences for coastal storm-preparedness, nearshore sedimentation cycles, and the distribution of inter-tidal organisms.        Ford, R.F. 1965]Distribution, Population Dynamics, and Behavior of a Bothid Flatfish, Citharichtys stigmaeus. F Udistribution, population dynamics, behavior, bothid, flatfish, Citharichtys stigmaeush ? Fotheringham, N.mField identification of crab predation in Shaskyus festivus and Ocenebra poulsoni (Prosobranchia: Muricidae).a * ; @ Q  The Veligerp142 204(efield identification, crab, predation, Prosobranchia, Muricidae, Shaskyus festivus, Ocenebra poulsoni A Fotheringham, N. 1970Growth, Mortality, and Feeding Patterns of the Littoral Gastropods Shaskyus festivus (Hinds) and Ocenebra poulsoni Carpenter (Prosobranchia: Muricidae). C U a r wgrowth, mortality, feeding pattern, littoral, gastropod, Prosobranchia, Muricidae, Shaskyus festivus, Ocenebra poulsoni: S Fotheringham, N. 1971Life history patterns of the littoral gastropods Shaskyus festivus (Hinds) and Ocenebra poulsoni Carpenter (Prosobranchia: Muricidae). 1 B O ` Ecology'525'742-757alife history, littoral, gastropod, Prosobranchia, Muricidae, Shaskyus festivus, Ocenebra poulsonic = N P :3Fox, D.L., V.E. Smith, R.W. Grigg, and W.D. MacLeod 1969ZSome structural and chemical studies of the microspicules in the fan coral Eugorgia ampla. K Y Comp. Biochem. Physiol.i28 1103-1114X(microspicules, fan coral, Eugorgia ampla  @:Gallagher, E.L., W. Boyd, S. Elgar, R.T. Guza, B. Woodward 199682Performance of a sonar altimeter in the nearshore.Marine Geology 133p241-248@0)sonar altimeter, nearshore, earth sciencehA 1 MHz sonar altimeter with automatic gain control is shown to provide accurate estimates of the distance between the instrument and the seafloor. Laboratory experiments indicate that distance estimates degrade slightly when the bottom is rough or sloped and when sediment is suspended in the water column. Results from field tests, both within and seaward of the surf zone, show some degradation owing to a combination of suspended sediment and bubbles, bed undulations, and perhaps the dynamic nature of the sand bottom under waves. Seaward of the surf zone the bottom can be located within + or - 3 cm. A 300 m long cross-shore transect of 16 altimeters was deployed from the shoreline to about 4 m depth for 3 months in summer-fall 1994 near Duck, NC. Results show that the altimeters are robust and can usually provide estimates of the seafloor position every few minutes even in the surf zone during large storms.4-From research done at Scripps Coastal Reservel(!George, R., R.E. Flick, R.T. Guza 19942,Observations of turbulence in the surf zone.&Journal of Geophysical Research99C1801-81001/15/94turbulence, surf zonePTurbulence generated by waves breaking on a natural beach is examined using hotfilm anemometer data. Turbulence intensity is estimated from dissipation rates determined from wavenumber spectra of short (1/8 s) hotfilm time series. The resulting Froude-scaled turbulence intensities are relatively uniform between the seabed and the wave trough level and are similar in vertical structure but lower in magnitude than in existing laboratory studies. The magnitudes of turbulence intensities observed in both the field and laboratory are consistent with intensities generated by monochromatic waves in small-scale laboratory experiments to those generated by random waves in the natural surf zone.l4-From research done at Scripps Coastal Reserve Gomez, E.D.P 1973The Biology of the Commensal Barnacle Balanus galeatus (L.) with Special Reference to the Complemental Male-Hermaphrodite Relationship.@ & 6 Gcommensal, barnacle, Balanus galeatus, complemental male, hermaphroditee  % $Grayum, M.H. and D.L. Koutnik 1982New records of vascular plants from the Santa Monica Mountains, California, and adjacent parts of Los Angeles and Ventura Counties.V ALISO102 p. 313-320voflora plant vascular plant vegetation Santa Monica Mountains Los Angeles Ventura California southern California Grigg, R.W.0 1970^Ecology and Population Dynamics of the Gorgonians, Muricea californica and Muricea fruticosa. 3 G L ] Oecology, population dynamics, gorgonian, Muricea californica, Muricea fruticosa )  Grigg, R.W. 1972.(Orientation and growth form of sea fans. Limnology and Oceanography172185-192(!growth form, orientation, sea fanHartline, A.C. 1972GThe Ecology of the Subtidal Acorn Barnacle, Balanus pacificus Pilsbury.  , = p?ecology, population dynamics, acorn barnacle, Balanus pacificusu . Marine Geology 133p241-248@0)sonar altimeter, nearshore, earth sciencehA 1 MHz sonar altimeter with automatic gain control is shown to provide accurate estimates of the distance between the instrument and the seafloor. Laboratory experiments indicate that distance estimates degrade slightly when the bottom is rough or sloped and when sediment is suspended in the water column. Results from field tests, both within and seaward of the surf zone, show some degradation owing to a combination of suspended sediment and bubbles, bed undulations, and perhaps the dynamic nature of the sand bottom under waves. Seaward of the surf zone the bottom can be located within + or - 3 cm. A 300 m long cross-shore transect of 16 altimeters was deployed from the shoreline to about 4 m depth for 3 months in summer-fall 1994 near Duck, NC. Results show that the altimeters are robust and can usually provide estimates of the seafloor position every few minutes even in the surf zone during large storms.4-From research done at Scripps Coastal Reservel(!George, R., R.E. Flick, R.T. Guza 19942,Observations of turbulence in the surf zone.&Journal of Geophysical Research99C1801-81001/15/94turbulence, surf zonePTurbulence generated by waves breaking on a natural beach is examined using hotfilm anemometer data. Turbulence intensity is estimated from dissipation rates determined from wavenumber spectra of short (1/8 s) hotfilm time series. The resulting Froude-scaled turbulence intensities are relatively uniform between the seabed and the wave trough level and are similar in vertical structure but lower in magnitude than in existing laboratory studies. The magnitudes of turbulence intensities observed in both the field and laboratory are consistent with intensities generated by monochromatic waves in small-scale laboratory experiments to those generated by random waves in the natural surf zone.l4-From research done at Scripps Coastal Reserve Gomez, E.D.P 1973The Biology of the Commensal Barnacle Balanus galeatus (L.) with Special Reference to the Complemental Male-Hermaphrodite Relationship.@ & 6 Gcommensal, barnacle, Balanus galeatus, complemental male, hermaphroditee  % $Grayum, M.H. and D.L. Koutnik 1982New records of vascular plants from the Santa Monica Mountains, California, and adjacent parts of Los Angeles and Ventura Counties.V ALISO102 p. 313-320voflora plant vascular plant vegetation Santa Monica Mountains Los Angeles Ventura California southern California Grigg, R.W.0 1970^Ecology and Population Dynamics of the Gorgonians, Muricea californica and Muricea fruticosa. 3 G L ] Oecology, population dynamics, gorgonian, Muricea californica, Muricea fruticosa )  Grigg, R.W. 1972.(Orientation and growth form of sea fans. Limnology and Oceanography172185-192(!growth form, orientation, sea fanHartline, A.C. 1972GThe Ecology of the Subtidal Acorn Barnacle, Balanus pacificus Pilsbury.  , = p?ecology, population dynamics, acorn barnacle, Balanus pacificusu .