1 BULLETIN OF MARINE SCIENCE. 42(1): DAYTIME SURFACE SWARMS OF THYSANOESSA SPINIFERA (EUPHAUSIACEA) IN THE GULF OF THE FARALLONES, CALIFORNIA Susan E. Smith and Peter B. Adams ABSTRACT Daytime surface swarms of the euphausiid Thysunoessa spinifera were observed and sampled in spring I985 in the Gulf of the Farallones off San Francisco, California. Samples were dipnetted at the surface from nine discrete swarm patches: and depth-stratified plankton tows were made before, during, and after swarm activity. Analyses of sex and maturity stage of surface.patch samples showed that 94% of all euphausiids were in breeding condition. Sex ratios differed significantly in six of the nine patches, with males dominating four and females dominating two patches. This sexual segregation is thought to be related to differences in size between sexually mature males and females. Biological and oceanographic observations at the swarm site, and examinations of food baskets of swarm individuals, gave little indication that the animals were passively transported to the surface, or that they were there to feed or avoid predators. T. spinferu eggs and Stage I nauplii were numerous in plankton collections taken the night following, and day after surface swarming was observed. It is concluded that swarming in this species is related to reproduction. Its adaptive value in regard to different breeding-related activities is still unclear, but probably involves a combination of factors that relate to the timing of sexual maturation, egg release, and larval dispersal in the changeable upwelling environment off central California. The neritic euphausiid Thysanoessa spinifera aggregates in conspicuous daytime swarms at the ocean surface along the California coast during spring and summer. Little is known about these surface swarms or what triggers their formation, probably because of the unpredictable nature of their onset and duration. The behavior occurs during daylight when most vertically migrating euphausiids, including T. spinifera (Alton and Blackburn, 1972), are usually found at greater depths. In general, upwelling centers have been associated with highest densities of T. spinifera (Brinton, 1962); and in the Gulf of the Farallones, daytime swarms occur sporadically from about April to July, when upwelling events are the most frequent and intense along the central California coast (Bakun, 1975). During this time, northwest winds intensify, triggering the offshore transport ofwarm surface waters, which are then replaced by cool, nutrient-rich water from the depths (Bolin and Abbot, 1962). Periodically during the upwelling season, northwesterly winds slacken, the process temporarily subsides, and surface temperatures may rise due to solar radiation or intrusion of warmer offshore water (Bolin and Abbot, 1962; Hatfield, 1983). When the rust-colored patches appear, many of the commercial sport fishing boats, guided by flocks of feeding seabirds, seek them out in search of salmon, which we have found to feed heavily on euphausiids at this time of year. Although this daytime swarming is often highly visible and appears to be a relatively common event off central California, very little information is available on swarm population structure. The only published reports consist of brief accounts of swarms that washed ashore at La Jolla, California (Boden et al., 1955), and Bandon, Oregon (Pearcy and Hosie, 1985), which were composed entirely of spent females, and those observed in Monterey Bay by Barham (1956) for which sex and maturity composition are not known. 76
2 SMITH AND ADAMS: EUPHAUSIID DAYTIME SURFACE SWARMS 77 Over a dozen species of euphausiids from various parts of the world are known to appear in similar aggregations at the sea surface during the day (Komaki, 1967; Mauchline, 1980), but the frequency of swarming vanes from species to species. Euphausia superba of the Antarctic may swarm at the surface during the day throughout most of its life cycle (Marr, 1962) and is the best studied euphausiid; other species, such as T. spinifera, appear to swarm only seasonally or intermittently (Mauchline, 1980). The mechanism that brings about the formation of these swarms is not clear and may differ according to species. Theories proposed to account for daytime surface swarming of various euphausiid species generally fall into the following categories: (1) the animals actively congregate at the surface for some biological purpose-to feed (Paulsen, 1909; Brown et al., 1979), reproduce (Ponomareva, 1966; Mauchline, 1980; Nicol, 1984a; Endo, 1984; Endo et al., 1985) or escape predators (Komaki, 1967); (2) they are passively transported to the surface by water currents or turbulence (Aitken, 1960; Forsyth and Jones, 1966; Brown et al., 1979; Terazaki, 1980); or (3) a breakdown ofan environmental bamer, such as the thermocline, enables them to expand their vertical distribution to the surface (Komaki, 1967; Endo, 1984). These theories have proven difficult to substantiate since many aspects of the swarming phenomenon are not open to experimental investigation. Also, existing published accounts lack direct hydrographic evidence and comparative information on the vertical distribution of various components of the population before, during and after swarm activity. It is not known which of the above factors are implicated in T. spinifera swarming activity, but the dominance of spent females in swarms that washed ashore in southern California (Boden et al., 1955) and Oregon (Pearcy and Hosie, 1985) suggests that swarming may be related to reproduction. In the more northern part of its range in subarctic waters, this species is reported to have a 2-year life cycle, reaching sexual maturity in its second year, with a one-time breeding season (Nemoto, 1957). Males must transfer a pair of spherical spermatophore packets to females for fertilization to take place, and in members of this genus, females shed their fertilized eggs freely in the water (Boden et al., 1955). The length of time between spermatophore transfer and release of eggs is not known. The goal of the present study was to identify factors associated with swarming of T. spinifera off central California. We made observations of swarms and associated biological activity in a swarm area, collected oceanographic information, and examined samples from individual swarm patches and plankton collections obtained before, during and after swarm activity. In this paper, we describe our results and discuss the possible adaptive significance of swarming in this species. MATERIALS AND METHODS Swarms were observed and sampled between 1300 and 1530 h on 31 May 1985 in the Gulf of the Farallones(37'48.3'N, 122"56.3'W). Individual patches were sampled usinga hand-helddipnet (mouth area = 0.1 m2, mesh width = 1.0 mm). Each sample came from a discrete patch, the size of which was estimated visually. These samples were then preserved in 10% neutralized formalin and seawater. Water temperature profiles were obtained with an expendable bathythermograph (XBT). We were able to obtain depth-stratified plankton samples in the swarm area before, during, and after surface swarm activity. This was possible because the swarms occurred in the same area (within 1.5 km) in which we had been monitoring T. spinifera springtime relative abundance since A set of horizontal tows of 15-min duration was made at the swarm site 12 h prior to and 12 and 24 h after swarm activity was observed. Each set consisted of tows made at 55,37, and 18 m over bottom depths of m. During the day of swarm activity, one tow at 55 m was completed while dipnet samples were being collected from surface waters. These collections were made with an opening-closing Tucker net (described by Hopkins et al., 1973) with an effective mouth opening of 1 m2 and a mesh size of mm. The net was towed at 1.3 m sec-'. Controlled test runs using a digital flowmeter in the mouth of the net indicated this procedure strained roughly 74 m3 of water per minute, assuming
3 78 BULLETIN OF MARINE SCIENCE, VOL. 42. NO. I. I988 Table 1. Sex ratios, x-square values, and significance levels of Thysanoessa spinifera swarm patch samples collected by dip net from the sea surface Patch samole number Patch area (m') N % Females r1 P o o I I.94 <o.o I N.S. N.S. N.S. the absence of net clogging. Organism counts were standardized for 1,000 m3 of water strained by the net. Swarm samples containing 200 euphausiids or less were examined in their entirety; larger samples were divided with a Folsom plankton splitter. Total length was measured to the nearest millimeter from the tip of the rostrum to the tip of the telson. Body length, from the base of the eye to the junction of abdomen and telson, was also measured to allow comparison with other data. These lengths were highly correlated (r2 = 0.957, P < ). A least-squares fit of 1,304 comparisons gave the equation Y = 0.742X where Y = body length and X = total length. An analysis of variance showed that variation due to regression is significant, and therefore the true slope differs from zero (F = 29,05 1; df = 1,1302; P < 0.001). Females were classified as (1) with spermatophores attached, with ripe or ripening eggs ( mm in diameter); (2) without spermatophores, with ripe or ripening eggs; (3) without spermatophores, with early developing eggs (<0.2 mm); and (4) with spermatophores attached, but with no eggs discernible in the thoracic cavity (spent). Females with spermatophores attached to the thelycum will be termed "fertilized," even though actual fertilization of eggs may not take place at the time of spermatophore transfer. Males were classified as (1) with ripe spermatophores protruding or internal; and (2) without ripe spermatophores. A11 specimens were grossly examined for the presence ofparasites. In addition, the ventral food basket between the thoracic appendages of each specimen was examined, and contents of food boluses were identified to the lowest possible taxonomical level. RESULTS Nine patches, 1-5 m2 in size (Table l), each approximately 137 m apart, were sampled over an area of about 1 km'. The aggregations occurred from the surface to a maximum depth of about 37 m in 71 m of water, based on echosounder readings (Fig. 1A). Weather and sea conditions at the swarm site were seasonally mild: wind speed = 8 knots, wind direction = 270", sea state = 2 on Beaufort scale, swell height = 1 m, swell direction = 255" mag., cloud cover = 2 (YE sky covered). During the cruise period (30 May-5 June), oceanographic conditions were characterized as transitional, marked by persistent south winds, relaxation of upwelling, and warming and stratification of upper surface 1ayers.l Coastal Upwelling Index values (Bakun, 1975) for the central California coast were well below average for the last week in May, indicating an absence of strong upwelling during and preceding swarm activity.2 Observations of swimming behavior and patch shape were made while the ship I K. Brigs. University oisanta Cnrr. Sanla Crur. CA pen. commun. June : Andrew Bakun. Pacific Fisheries Environmental Group. National Manne Firhenes S e~i~e. NOAA. Montere), CA Unpubl. data
4 SMITH AND ADAMS: EUPHAUSIID DAYTIME SURFACE SWARMS 19 TEMPERATURE ("C) 8 IO n $ - c E" 40- I I- n - w n t - 40 I I- n 8 6o t I 1- --_- I I Figure 1A. Echogram (38 khz) and XBT temperature profile obtained at the surface swarm site on the day of swarm observations. 31 May 1985; Figure 1B. Echogram and XBT temperature profile obtained at the surface swarm site the night following swarm activity, 1 June drifted into the swarming area and during sampling. Some of the patches were roughly circular and contained tightly spaced individuals without parallel orientation. Others were ribbonlike streams of individuals, which swam parallel to each other at an estimated 0.3 m sec-i. The animals often sounded rapidly as a group when disturbed, and some individuals even vaulted from the water in an effort to escape the dip net or the samplers' boat. Isolated individuals were also observed swimming at the surface outside the dense patches. Although feeding activity of fishes has been associated with surface swarming of T. spinifera in Monterey Bay (Harvey3) and in the Gulf of the Farallones (by the salmon sportfishing fleet4), we saw no evidence of this at the swarm site. The Harvey. J T Daytime surface rwarmlng ofeuphausuds in Monlere) Bay. Callfomla. Unpubl. manuscr.. Halfield Mannc Science Ccnicr. Oregon Stale Unwenn?. Nrupon. OR ' Roger Thomas. Caplain Sdn. Lad!.. Harbor Drive. Sausallto. CA pen. commun. May 1985.
5 80 BULLETIN OF MARINE SCIENCE. VOL. 42. NO. I, 1988 Table 2. Estimated number per 1,000 m3 (N) and percent sample volume (%) of T. spinifem eggs, nauplii, and adults taken in plankton tows at the swarm site before, during, and after swarm activity Toul Tow Tow QS Nauplii Adults snmpk depth duration volume (m) (min) N 96 N % Ripca Fen. Q 94 (ml) Night before swarm activity (015CL1340 hr) 18 I5 19, I5 689 <O.OI Day of swarm activity (1400 hr) 55 IS 3, * Night following swarm activity hr) , IS 28, , Day after swarm activity ( 124&1400 hr) 18 I5 4, , I5 24, , *A single. unfmilized female with early stags was lakm in this colkction only predators evident in the area were western gulls (Lam occidentalis) which were observed on the water singly or in pairs, feeding on individual patches. There was no evidence, either in our plankton collections (Table 2) or in echosounder tracings (Fig. lb), that the surface swarming persisted after nightfall. Euphausiid eggs, however, were numerous in plankton collections taken that night and the next day (Table 2). Although positive identification could not be made of the eggs or of the Stage 1 nauplii found in near-surface samples the following day, the size of the egg embryos and the shape of the nauplii differed from those of Euphausia pacifica, the only other abundant euphausiid in the area.5 We therefore assume that the eggs and nauplii were those of T. spingera. Egg numbers may have been underestimated because of possible extrusion through the net meshes (mean egg diameter = 0.41 mm; mesh width = mm; mean diagonal mesh width = 0.42 mm). Analyses of sex and maturity stage of the dipnetted samples from surface patches showed that 94% of all euphausiids were either males with fully developed spermatophores or fertilized females with ripe or ripening eggs. The sex ratio, however, differed from patch to patch. Six of the nine collections differed significantly from the expected 1: 1 male : female ratio, with males dominating in four collections and females dominating in two collections (Table 1). Analyses of length frequencies by maturity stage helped to distinguish major components of the swarms (Fig. 2). Overall, sexually mature males (TL mean = 20.7 mm) and large fertilized females with eggs (TL mean = 25.4 mm) comprised 55.7% and 38.0%, respectively, of the sampled population. A third, lesser group (4.8% of individuals), which occurred strongly only in patch sample 2, was composed of smaller developing females (TL mean = 19.9 mm). The remainder (1.5%) consisted of unfertilized ripe females (8 individuals), spent females (6), and males without spermatophores (5). ' Margaret Knight. Scripm Instltutlon of Oceanography. La Jolla. CA 92093, prs. commun. March 1986.
6 SMITH AND ADAMS: EUPHAUSIID DAYTIME SURFACE SWARMS o Q Q wi I n=239 n:136 n:l67 I 1 u 1 d n:l67 I n =154 tq d u n TOTAL LENGTH (mm) Figure 2. Length frequency histograms of the nine sampled swarm patches of Thysunoessu spingem. Crosshatching = unfertilized developing females; open = fertilized females with ripe or ripening eggs and males with spermatophores; solid = other (males without spermatophores, fertilized females without eggs, and ripe, unfertilized females). Q Examination of food baskets of swarm individuals indicated little feeding activity, but some cannibalism was evident. The only recognizable items were euphausiid ommatidia and other optic material. Of the 1,304 specimens examined, '0 had empty food baskets, 17.6% contained euphausiid ommatidia, and the remainder contained unrecognizable material. Suctorian protozoans infested the exoskeletons of 75.2% of the euphausiids examined.6 The thoracic cavity of three female individuals each contained a single larval nematode, identified as Anisakis SP.~ DISCUSSION The results provide evidence of sexual segregation in T. spinifera and strongly indicate that swarming is related to reproduction. It is unlikely that the euphausiids were transported to the surface by some physical force, judging from the stratified temperature profiles and mild oceanographic conditions, and we found no evidence that they were there to feed or avoid predators. Some of these findings are very similar to those of others who have recently studied daytime swarming of temperate water euphausiids on other coasts. Nicol (1 984a) found that reproductive adults dominated swarms of Meganyctiphanes norvegica in the Bay of Fundy, and that sex ratios from patch to patch were highly skewed. He also found a high degree of suctorian infestation in swarm samples identified by S. K. Johnson. Texas A&M Universtl). I I I Nagle Hall. College Stallon. Texas pen. commun. May 1986 ' Ideniificd b) Mike Mow. Univcnll). of California. Sam CNZ. CA pen. commun. April 1986.
7 a2 BULLETIN OF MARINE SCIENCE. VOL. 42. NO. I, 1988 compared to those taken at depth offshore (Nicol, 1984b). Endo (1 984) and Endo et al. (1 985) concluded that swarming of Euphausia pacifica in Sendai Bay, Japan, was related to reproduction, although the majority of ripening females they sampled were as yet unfertilized. They also found a predominance of euphausiid spines and eye parts in guts of swarm individuals and a similar infestation of suctorian epibionts. Adult male euphausiids and the larger adult females may segregate by sex to facilitate schooling (Nicol, 1984a). Those patches in which the sexual segregation was not pronounced may represent the convergence of male and female aggregations and, indeed, swarm patches have been seen to merge and separate.8 The fertilized mature females and sexually mature males are assumed to represent the 1983 year class because they correspond to individuals classified as Age 2 by Nemoto ( 1957). If so, the smaller developing females are likely sexually precocious individuals of the 1984 year class. Their association with the more sexually advanced males may be based on corresponding size and therefore swimming efficiency, rather than corresponding reproductive stage. Surface swarming may relate to reproduction in one or more of the following ways: (1) for more effectual transfer of spermatophores from males to females, (2) for release of eggs at the surface, or (3) for maturation of sexual products in adults and/or incubation of eggs in warm surface layers. There are arguments for and against all of these possibilities. Swarming for the purpose of spermatophore transfer seems likely, considering the range of sex ratios in individual patches and observations of swarms merging. But the virtual absence in our samples of mature but as yet unfertilized females suggests otherwise. We have also found a similar absence of unfertilized females in plankton samples and chinook salmon (Oncorhynchus tshawytscha) gut contents collected throughout the swarm season. This suggests that the bulk of spermatophore transfer takes place prior to the surface swarming season, and that refertilization of molted females, if it does occur, takes place in areas less accessible to our collecting gear and to salmon predation. Nicol(l984a) also found very few unfertilized mature females in swarming Meganyctiphanes norvegica in the Bay of Fundy. Although the intermolt period for nonreproductive T. spinifera has been estimated at 5 to 6 days (Jerde and Lasker, 1966), molting may be delayed or suspended during the reproductive period or upon reaching sexual maturity (Dexter, 1977; Nicol, 1984b). This would further explain why an overwhelming majority of females carry intact spermatophores throughout the breeding season, and may account for the high incidence of exoskeleton infestation by suctorians. Suspension of ecdysis would seem an adaptive means to alleviate the need for segregated males to relocate and refertilize females with each molt. The presence of eggs in the swarm area suggests that egg release may be an important function of swarming. This hypothesis is supported by the reports of swarms composed entirely of spent female T. spinifera (Boden et al., 1955; Pearcy and Hosie, 1985). Egg incubation, however, is probably not a factor, since euphausiid eggs, being denser than seawater, tend to sink when broadcast freely in the sea (Mauchline and Fisher, 1969). Even so, neritic species such as T. spinifera would benefit from releasing eggs high in the water column, thus providing more time for eggs to develop and hatch before reaching the sea floor. After hatching, the larvae are thought to ascend to surface waters where food supplies are abundant a Pea) Gamin. vessel Sabr Lodr. Harbor Drive. Sausahlo. CA pen. commun. May 1985.
8 SMITH AND ADAMS: EUPHAUSIID DAYTIME SURFACE SWARMS 83 (Mauchline and Fisher, 1969) and the greater average velocity of surface currents can disperse them away from the area and potential cannibalism by adults. But the advantage gained by suspending or reversing normal diel migratory behavior by aggregating at the surface during daylight hours is still not clear. As with other breeding-related activity, egg release could occur during crepuscular or nocturnal periods, presumably with the same benefits mentioned above with the added protection from diurnal predators that darkness would provide. In addition, less than 1% of females in our swarm samples were spent, which indicates that egg release may not be the primary swarm activity during the day, or at least during the afternoon period that we sampled. Perhaps one of the functions of daytime surface swarming is to prolong exposure of reproductive individuals to the warmer surface layers, where maturation of sexual products would be accelerated. Lindley (1 978), working with Thysanoessa longicaudata, found that timing of reproduction in spring was correlated with sea surface temperature, and concluded that the rate of sexual maturation is controlled mainly by temperature. The animals may take advantage of interim warming periods between upwelling events to accelerate gonadal development in the warm surface layers. But again, the advantage gained by this strategy would have to outweigh the disadvantage of being highly vulnerable to predation at the sea surface during the day. Most likely, the adaptive significance of Thysanoessa spinifera surface swarming encompasses more than just one factor, since the selective forces acting upon breeding adults would differ from those acting upon eggs and larvae (Dingle, 1980). Both the timing of sexual maturation and the timing of egg release and subsequent larval dispersal would seem crucial, since these events occur during the upwelling season when water temperature and sea surface current velocity and direction can change over a short period of time. Success, however, would seem to depend largely on the rapid behavioral responses of breeding adults. Swarming may be such a response. Although the cost of being at the surface in daylight would seem high for adults because of their greater visibility, the intermittent formation of dense schools, and the rapid response to stimuli that schooling facilitates, may offer the needed edge over predators to ensure that sufficient numbers of adults survive to breed and release their eggs under favorable environmental conditions. The small-scale patchiness revealed by this study re-emphasizes the importance of direct sampling of these reproductive swarms, the dynamics of which may be masked by more conventional sampling with towed plankton nets. ACKNOWLEDGMENTS We are grateful to D. Ainley and R. Fems of the Point Reyes Bird Observatory for their help in obtaining surface swarm samples, and to D. Ainley, E. Brinton, J. Chess, Y. Endo, J. Harvey, E. Hobson. M. Knight, and S. Nicol for their constructive comments on earlier drafts of the manuscript. LITERATURE CITED Aitken, J. J Swarming in Meganycriphanes norvegica (M. Sars) in Strangford Lough, Co. Down. Ir. Nat. J. 13: Alton, M. S. and C. J. Blackburn Diel changes in the vertical distribution of the euphausiids, Thysanoessa spinifera Holmes and Euphausia pacijca Hansen, in coastal waters of Washington. Calif. Fish Game 58: Bakun, A Daily and weekly upwelling indices, West Coast of North America, U.S. Dep. Commer., NOAA Tech. Rep. NMFS SSRF pp. Barham, E. G The ecology of sonic scattering layers in the Monterey Bay area, California. Ph.D. Thesis, Stanford Univ., Palo Alto, Calif. 182 pp.
9 84 BULLETIN OF MARINE SCIENCE, VOL. 42. NO, I Boden. B. P., M. W. Johnson and E. Brinton The Euphausiacea (Crustacea) of the North Pacific. Bull. Scripps Inst. Oceanogr. Univ. Calif. 6: Bolin. R. L. and D. P. Abbot Studies on the marine climate and phytoplankton of the central coastal area of California, Calif. Coop. Ocean. Fish. Invest. Rep. IX: Brinton, E The distribution of Pacific euphausiids. Bull. Scripps Inst. Oceanogr. Univ. Calif. 8: Brown, R. G. B., S. P. Parkerand D. E. Gaskin Daytime surface swarming by Meganyctiphanes norvegica (M. Sars) (Crustacea, Euphausiacea) off Briar Island, Bay of Fundy. Can. J. Zool. 57: I. Dexter, B. L The molting biology and molting behavior of two species of euphausiids off Oregon. M.S. Thesis, Oreg. State Univ., Corvallis. 158 pp. Dingle, H Ecology and evolution of migration. Pages in S. A. Gauthreaux, Jr., ed. Animal migration, orientation, and navigation. Academic Press, Inc., New York. Endo, Y Daytime surface swarming of Euphausia pacifica (Crustacea: Euphausiacea) in the Sanriku coastal waters off northeastern Japan. Mar. Biol. (Berl.) 79: Y. Hanamura and A. Taniguchi In situ observations on the surface swarm of Euphausiu puci~cu in Sendai Bay in early spring with special reference to their biological characteristics. Mer (Tokyo) 23: Forsyth, D. C. T. and L. T. Jones Swarming of Thysanoessu longicaudata (Kroyer) (Crustacea, Euphausiacea) in the Shetland Islands. Nature (Lond.) 212: Hatheld, S. E Distribution of zooplankton in association with Dungeness crab, Cancer magister, larvae in California. Pages in P. w. Wild and R. N. Tasto, eds. Life history, environment and mariculture studies of the Dungeness crab, Cancer magister, with emphasis of the central California fishery resource. Calif. Dep. Fish Game Fish Bull Hopkins, T. L., R. C. Baird and D. M. Milliken A messenger-operated closing trawl. Limnol. Oceanogr. 18: Jerde, C. W. and R. Lasker Molting of euphausiid shrimps: shipboard operations. Limnol. Oceanogr. 1 1: Komaki, Y On the surface swarming of euphausiid crustaceans. Pac. Sci. 21: Lindley. J. A Population dynamics and production of euphausiids. I. Thysunoessa longicaudata in the North Atlantic Ocean. Mar. Biol. (Berl.) 46: Marr, J. W. S The natural history and geography of the Antarctic krill (Euphausia superbu Dana). Discovery Rep. 32: Mauchline, J The biology of mysids and euphausiids. Adv. Mar. Biol pp. - and L. R. Fisher The biology of euphausiids. Adv. Mar. Biol pp. Nemoto, T Foods of baleen whales in the northern Pacific. Sci. Rep. Whales Res. Inst. Tokyo 12: Nicol, S. 1984a. Population structure of daytime surface swarms of the euphausiid Meganyctiphanes norvegica in the Bay of Fundy. Mar. Ecol. Prog. Ser. 18: b. Ephelota sp., a suctorian found on the euphausiid Meganyctiphanes norvegica. Can. J. Zool. 62: Paulsen, Plankton investigations in the waters around Iceland and the North Atlantic in Medd. Komn Havunders., Ser. Plankton l(18): Pearcy, B. and M. Hosie Mass stranding of krill off Bandon. Oregon Wildlife. p. 14. Ponamareva, L. A The euphausiids of the North Pacific, their distribution and ecology. Doklady Akad. Nauk. SSSR, Israel Programme for Scientific Translation, Jerusalem. Terazaki, M Surface swarms of a euphausiid Euphausia pacifica in Otsuchi Bay, Northern Japan. Bull. Plankton SOC. Jpn. 27(1): DATE ACCEPTED: March 2, ADDRESS: National Marine Fisheries Service, South west Fisheries Center, NOM, 3150 Paradise Drive. Tiburon, Cullfornia
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Life in the Deep Sea Angler fish photo The Deep Sea Environment 200-11000 m depth Largest environment on earth 80% of ocean floor =2X total land area above sea level Extremely poorly known even today S
JA/J05/JR9 Yearly trend of blubber thickness in the Antarctic minke whale Balaenoptera bonaerensis in Areas IV and V KENJI KONISHI 1), TSUTOMU TAMURA 1) AND LARS WALLØW 2) 1)The Institute of Cetacean Research,
Canadian Science Advisory Secretariat Science Advisory Report 2009/078 SCIENCE ADVICE FROM THE RISK ASSESSMENT OF THE INVASIVE BLOODY RED SHRIMP (HEMIMYSIS ANOMALA) IN CANADA Photo credit: Kelly Bowen,
UC San Diego Library Scripps Collection UC San Diego Title: Fish Bulletin No. 121. The California Marine Fish Catch For 1961 and Catch Localities for Dover Sole, Microstomus pacificus (Lockington), Landed
Integrating Near Real-Time Data for Coral Reef Ecosystem Forecasting NOAA s Integrated Coral Observing Network (ICON) Atlantic Oceanographic and Meteorological Laboratory Laboratory Review, March 18, 2008
MS-ESS2-6 Develop and use a model to describe how unequal heating and rotation of the Earth cause patterns of atmospheric and oceanic circulation that determine regional climates. [Clarification statement:
Cost Recovery Annual Report March 2014 Trawl Rationalization Program Fishing Year 2013 and Calculation for 2014 U.S. Department of Commerce National Oceanic and Atmospheric Administration National Marine
ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 9 May 2011 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index (ONI)
10. NEAR-SURFACE VELOCITY AND TEMPERATURE STRUCTURE OF THE PERU CURRENT AT ODP SITES 685, 686, AND 688 1 Dean L. Merrill 2 INTRODUCTION The Peru Current has been studied frequently as the classic example
Project information Keywords Carbon flux, Biological carbon pump, sea ice cover Project title Carbon flux dynamics in ice-free versus ice-covered Svalbard fjords-exploring the effects of sea ice variability
Chapter 1 General introduction Several aspects of the natural history of the rocky intertidal barnacle can explain why it has long been exploited as an example of marine animal recruitment. The adult barnacle
Title Acoustic monitoring of Japanese anchovy Engraulis japonicus post larvae shirasu K. Miyashita,, A. Watanabe, S. Morioka, Y. Ikewaki,, R. Matsukura,, and H. Yasuma Engraulis japonicus Shirasu fishery
Extra-Tropical Cyclones in a Warming Climate: Observational Evidence of Trends in Frequencies and Intensities in the North Pacific, North Atlantic, & Great Lakes Regions David Levinson Scientific Services
May 29, 2015 Mr. Tom Howard Executive Director State Water Resources Control Board P.O. Box 100 Sacramento, CA 95812-0100 Mr. Ron Milligan Operations Manager, Central Valley Project U.S. Bureau of Reclamation
Grass Shrimp Background When studying estuarine ecosystems, students can learn about the animals found in this environment including grass shrimp, some of which are in the genus Palaemonetes and include
Title: Water density and marine organisms Summary: Students expand on concepts they have previously learned about seawater density, ocean stratification, and density-driven circulation by connecting these
KEY CONCEPT Climate is a long-term weather pattern. BEFORE, you learned The Sun s energy heats Earth s surface unevenly The atmosphere s temperature changes with altitude Oceans affect wind flow NOW, you
VOCALS-CUpEx: The Chilean Upwelling Experiment René D. Garreaud 1, José Rutllant 1,2, Ricardo Muñoz 1, David Rahn 1, Marcel Ramos 2 and Dante Figueroa 3 (1) Department of Geophysics, Universidad de Chile;
Blue sky Workshop: new ways of thinking about the West Coast ecosystem and how penguins interact with other elements Friday 28 August 2015, Velddrif Background The marine ecosystem of the West Coast has
Snow and fee Covers: Interactions with the Atmosphere and Ecosystems (Proceedings of Yokohama Symposia J2 and J5, July 1993). IAHS Publ. no. 223, 1994. 29 Radiative effects of clouds, ice sheet and sea
Daily High-resolution Blended Analyses for Sea Surface Temperature by Richard W. Reynolds 1, Thomas M. Smith 2, Chunying Liu 1, Dudley B. Chelton 3, Kenneth S. Casey 4, and Michael G. Schlax 3 1 NOAA National
UNITED STATES DEPARTMENT DF COMMERCE National Oceanic and Atmoapharic Administration NATIONAL MARINE FISHERIES SERVICE Silver Spring, MD 20910 Incidental Harassment Authorization Washington State Department
Report EU BASIN Kickoff Meeting, Copenhagen, Denmark February 22 25, 2011, Meng Zhou Table of Contents Summary... 1 1. Highlights... 2 1) EU BASIN cruises... 2 2) Regional comparative studies and end to
Sardines Return to British Columbia Waters G.A. McFarlane and R.J. Beamish Pacific Biological Station Hammond Bay Rd. Nanaimo, B.C. V9R 5K6 Canada e-mail: firstname.lastname@example.org The Indians have told
PRESENTING GRAPHS WHICH TYPE OF GRAPH SHOULD YOU CHOOSE? CHOOSING THE RIGHT TYPE OF GRAPH You will usually choose one of four very common graph types: Line graph Bar graph Pie chart Histograms LINE GRAPHS
Tsunami Practice Questions and Answers Revised November 2008 1. What happened on 26 December 2004 off the west coast of Sumatra? 2. What is the final estimate of the magnitude of the Sumatra 26 December
Whale Jenga Food Web Game Baleen whales feed on crustaceans such as amphipods, copepods,and krill, as well as small fish. With changes in ocean temperature, upwelling, acidification and other urban influences,
PROJECT STATUS REPORT Development of microhabitat suitability criteria for fry and juvenile salmonids of the Trinity River Prepared for: Trinity River Restoration Program P.O. Box 13 1313 South Main St.
Ecological Roulette: The Global Transport of Nonindigenous Marine Organisms James T. Carlton 1 and Jonathan B. Geller 2 1 Maritime Studies Program, Williams College, Mystic Seaport, Mystic, CT 06355, and
Mytilus californianus - this mussel is a filter feeder, feeding on plankton. They are the main source of food for both the Ochre Sea Star (Pisaster Ochracus) and the rock whelk (Nucella emarginata). They
Section 3 What Is Climate? Key Concept Earth s climate zones are caused by the distribution of heat around Earth s surface by wind and ocean currents. What You Will Learn Climate is the average weather
The Weather of Pemba 3 years of SUN hours, winds & precipitation A unique weather system Pemba Island has a tropical monsoon climate with high precipitation figures all year round. Pemba Island has two
Grade Level: 6-8 Next Generation Sunshine State Standards SC.6.E.7.3 SC.7.E.6.6 SC.8.L.18.1 Program Overview Explore the ocean s diverse ecosystems from the shallow coral reefs to the deep ocean trenches.
Communities, Biomes, and Ecosystems Section 1: Community Ecology Section 2: Terrestrial Biomes Section 3: Aquatic Ecosystems Click on a lesson name to select. 3.1 Community Ecology Communities A biological
Tilapia production in shrimp ponds: Salinity tolerance and polyculture Dan Cohen and Eran Lahav 2 Aquaculture Production Technology (Israel) Ltd., P.O.Box 4330, Jerusalem, Israel Abstract A special genetic
Chatham Rock Phosphate Marine Consent Application P Kennedy - Environmental Impact Assessment Evidence Summary My evidence and this summary cover the following matters: Seabed and sediment Discharge and
Ch. 7 - Geographical Ecology, Climate & Biomes Weather - the short term properties of the troposphere at a given place and time. Climate - the average long-term weather of an area. averaged over a long
Hydroacoustic surveys of Otsego Lake, 2007 Thomas E. Brooking 1 and Mark D. Cornwell 2 INTRODUCTION In 2007, we sampled Otsego Lake (Otsego County, NY) with acoustics to estimate abundance of pelagic fishes
GEOPHYSICAL RESEARCH LETTERS, VOL. 38,, doi:10.1029/2010gl046376, 2011 Underwater gliders reveal rapid arrival of El Niño effects off California s coast Robert E. Todd, 1 Daniel L. Rudnick, 1 Russ E. Davis,
Documenting Whale Migration off Virginia s Coast Virginia CZM Cooperative Agreement with the Virginia Aquarium October 2012 through March 2014 PROJECT DESCRIPTION This project is collecting aerial survey
Long-term Marine Monitoring in Willapa Bay WA State Department of Ecology Marine Monitoring Program Ecology s Marine Waters Monitoring Program Goal: establish and maintain baseline environmental data Characterize
Animal Reproductive Strategies The ultimate goal of each species is to produce the maximum number of surviving offspring using the least amount of energy. This is called the reproductive effort. Asexual
Slack water (slack tide): The state of a tidal current when its velocity is near zero, especially the moment when a reversing current changes its direction and its velocity is zero. The term is also applied
CONVENTION ON THE PROTECTION OF THE MARINE ENVIRONMENT OF THE BALTIC SEA AREA HELSINKI COMMISSION - Baltic Marine HELCOM 19/98 Environment Protection Commission 15/1 Annex 3 19th Meeting Helsinki, 23-27
Heat Transfer Tab: (Use the textbook or the ScienceSaurus book) Box 1: Radiation: (on the colored tab) Draw a picture (on the white tab directly below it) Box 2: Convection: (on the colored tab) Draw a
Reprint 829 Objective Verification of Weather Forecast in Hong Kong Y.K. Leung Fourth International Verification Methods Workshop, Helsinki, Finland, 4-10 June, 2009 Objective Verification of Weather Forecast
BEST OF COSEE HANDS-ON ACTIVITIES Activity Title: How is Coastal Temperature Influenced by the Great Lakes and the Ocean? Learning Objectives The ocean is a major influence on weather and climate. With
42 Working to Conserve Key Species: EWS-WWF s Marine Turtle Conservation Project Envirocities emagazine 43 Issue 6, Sep 2013 Emirates Wildlife Society - WWF Dubai United Arab Emirates Marine turtles are
Biology 103 A Method of Population Estimation: Mark & Recapture Objectives: 1. Learn one method used by wildlife biologists to estimate population size of wild animals. 2. Learn how sampling size effects
International Journal of Research Studies in Biosciences (IJRSB) Volume 3, Issue 1, January 2015, PP 104-109 ISSN 2349-0357 (Print) & ISSN 2349-0365 (Online) www.arcjournals.org Aspects of Reproduction
Monitoring of sea trout post-smolts, 213 A report to the West Sutherland Fisheries Trust, Report No. WSFT2/14 January 214 Shona Marshall Fisheries Biologist West Sutherland Fisheries Trust Gardeners Cottage
Song Characteristics of Different Baleen Whales : A New Approach to Sound Analysis Pranab Kumar Dhar, Jong-Myon Kim 90 > Abstract This paper presents the characteristics of different baleen whale songs
Thermal Ecology of Lakes In this section, we begin to consider the flow of energy. We will look at lakes and the role that energy flow plays in lake ecology. Ultimately, we will be interested in questions
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