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Limnol. Ocennogr., 24(e), 1979, 1081-1091 @ 1979, by the American Society of Limnology Effects of temperature (Tunicata, Thaliacea): vertical migration’ and Oceanography, Inc. on the swimming Implications for of salps C. R. Harbison Woods IIole Oceanographic Institution, Woods IIole, Massachusetts 02543 R. B. Campenot IIarvard University Medical School, Boston, Massachusetts 02115 Abstract Salps swim by means of rhythmic contractions of the circular body muscles. In most species, these contractions are regular. At constant temperature, the pulsation rate is inversely related to body length for hand-collected animals. Such a relationship is not seen with trawl-collected salps. When temperature is lowered experimentally, marked differences are seen in the response of individual species. The pulsation rates of Pegeu confederutu, CycZosuZpu poke, and Salpa cylindricu are greatly depressed and cease altogether at low temperatures (response type I). For Pegea so&, CycZosuZpu pinnutu, Cyclosalpu affinis, and SuZpu maxima, the pulsation rates are usually greatly depressed, but do not cease, even at extremely low temperatures (response type II). The pulsation rates of Salpa fusiformis and Salpa usperu are largely insensitive to changes in temperature (response type III). Evidence from net sampling suggests a relationship between these response types and vertical and horizontal distribution patterns. Salps showing response type I are found only in tropical and subtropical surface waters; those showing response type II are more widely distributed or are found in temperate waters; and those showing response type III are vertical migrators. Thus, differences in the temperature response provide clues as to the differing modes of life available to salps in the open sea. Salps are transparent, free-swimming tunicates found primarily in the open ocean, where they arc a widespread and characteristic fauna. They show considerable differences in size and morphology which may reflect different adaptations to life in the open sea. The greatest diversity of species is found in relatively warm tropical and subtropical waters or in temperate waters in the summer (Thompson 1948; Yount 1958; Van Soest 1975), but several forms have been found only in the Southern Ocean and Antarctic waters (Thompson 1948; Foxton 1966; Van Soest 1975). Of particular interest are species in the genus Salpa, some of which are primarily tropical (e.g. Salpa cylindrica), while others occur only in cold waters (e.g. Salpa thompsoni), and yet others are found over a wide range (e.g. Salpa aspera). Salps swim by rythmic contractions of the circular muscles of the body wall (Fedele 1932). This method of swimming sustained swimming is very effective; speeds of 550 me h-l have been measured in the field (Madin 1974). The swimming and feeding processes are closely linked-salps must swim to feed (Madin 1974b). As they are thought to feed primarily on phytoplankton, salps have been regarded as near-surface living animals, restricted to the euphotic zone. There are, however, reports of salps at great depths (Foxton 1966; Caldwell 1966) and an increasing body of evidence that some species migrate over a considerable vertical range on a daily basis. Salpa thompsoni has been reported to undergo a diel vertical migration (Mack* Contribution 4172 of the Woods IIolc Oceanointosh 1934; IIardy and Gunther 1935; graphic Institution. Research supported by the BiFoxton 1966). Foxton (1966) fLirther reological Oceanography Section, National Science ported that S. thompsoni occurred at Foundation, grant OCE 7521715 and OCE 7722511 and by the National Institutes of IIealth, Training depths as great as 1,000 m. Franqueville Grant~NS07009. (1971) showed that Salpa fusiformis, a 1081 1082 Harhison and Campenot closely related species, underwent a diel vertical migration of some 500-800 m in the temperate Mediterranean Sea. Wiebe et al. (1979) gave evidence for vertical migration by yet another related form, S. aspera; they found that the greatest biomass of this species by night was in the upper 25 m, whereas by day, the greatest biomass was in the 700-800-m sample. Although they did not sample below 800 m, prior and subsequent visual observations from the DSRV Alvin indicated that the bulk of the population occurred at a depth of between 800 and 1,200 m during the day (Wiebe et al. 1979). We have also found S. aspera and S. fusiformis at the surface during the night, but we have observed only scattered and obviously dying specimens of these species while SCUBA diving in the upper waters during the day. Therefore, there is evidence that at least three species of the genusS. fusiformis, S. aspera, and S. thompsoni -undergo extensive diel vertical migrations. Vertical migrations of this magnitude are accompanied by temperature changes of about 20°C and pressure changes of about 100 atm. Pressure seems to have complex effects on metabolic processes (e.g. Hochachka 1975), but temperature effects are usually unidirectional-an increase in temperature causes an increase in metabolic rate, unless some compensatory or buffering mechanism is present (Prosser 1973). We here compare the effects of changing temperature on the frequency of the swimming pulsations of migratory and nonmigratory species of salps. There are pronounced differences in the effects of temperature on the pulsation rates of different salps, and these differences may be related to whether a species migrates vertically. Differences in the response to changing temperature can also explain much about the geographic distribution of several species. We thank M. J, Greenberg for loaning us the impedance converter, M. R. Reeve for loaning us the vertically towed plankton net, and V. L. McAlister for preparing the figures, L. P. Madin, V. L. McAlister, N. R. Swanberg, W. E. Cross, and J. E. Craddock helped these experiments. us collect salps for Materials and methods Salps of both the solitary and aggregate generations were used in our experiments. Pegea confederata, Pegea socia, C yclosalpa polae, C yclosalpa pinna ta, Cyclosalpa affinis, Salpa maxima, and Salpa cylindrica were collected with hand-held jars while SCUBA diving during the day. The dives were made on RV Oceanus Cruise 22 (tropical North Atlantic) and RV Atlantis II Cruise 101 (subtropical and temperate North Atlantic). Station data for the dives are given by Harbison et al. (1978) and Swanberg and Harbison (in prep.). Since all our dives were made during the day, salps that rnigrated into the upper waters at night were collected with nets. The nets were of two kinds: a horizontally towed rectangular midwater trawl and a vertically towed plankton net designed for the collection of soft-bodied organisms (Reeve 1977). Species collected with these nets and used in experiments were S. maxima, S. cylindrica, S. fusiformis, and S, aspera. Except for a few hand-collected specimens, salps were used in experiments immediately after collection. To measure the pulsation rate of a salp, the animal was placed in a finger bowl (loo-mm diam) containing seawater, and a pair of fine wires, insulated except at the tips, were sutured to the outside of the tunic on opposite sides of the body. The wires were fixed to the rim of the finger bowl with wax, restraining the salp from touching the walls of the finger bowl. The wires were flexible enough so that they could be pulled toward one another each time the salp contracted, permitting the rhythmic pulses to be timed by observing changes in electrical resistance as the wires changed their relative positions. Electrical resistance was monitored on Oceanus 22 with a Biocom impedance convertor (model 2991), and on Atlantis II 101 with a Harvard Apparatus impedance pneumograph (model 2191), and recorded with a Grass polygraph (model 5B). Ship-roll caused move- Temperature TEMPERATURE 1083 ejyects on salps c°C) Fig. 1. Temperature profiles of four regions in Atlautic Ocean where species were collected (data from Fuglister 1960). O-Equator (OO”lci’S, 37”14’W); H-northern Sargasso Sea in summer (34”04’S, 65”02’W); ~--slope water in summer North Atlantic (38”54’N, 65”OO’W); l -eastern (40”15’N, 33”13’W). mcnt of the electrodes, but it was usually of different form, amplitude, and period from the movement caused by the contractions of the salp, and could be easily distinguished. In questionable cases, it was easy to check by counting the pulses of the salp visually. The finger bowl was placed in a larger container to which ice or warm water was added to change the temperature (Oceanus 22). To attain and maintain lower temperatures, a refrigeration unit was used on Atlantis ZZ 101. The temperature of the seawater bathing the salp was measured with a thermometer, and the pulsations of the salp served to mix the water, so that the temperature was probably uniform throughout the finger bowl provided that the salp continued to swim. Temperature was measured with a thermistor (Yellow Springs Instr. Co.) and recorded on the polygraph trace on Atlantis ZZ 101. Figure 1 shows typical summer tcmperature profiles for four regions where we collected salps: Equatorial, Sargasso Sea, slope water off New England, and eastern North Atlantic (Fuglister 1960). The temperature profile of the equatorial water is the same year-round and is almost identical with that of the slope water in summer. A salp migrating to a I 10 I I 20 30 TIME I-I 40 50 60 (mln> Fig. 2. Typical experimental temperature drop (O), compared with time-course of temperature changes that might he experienced in first hour by salps migrating vertically dowu from 100 m in equatorial regions (Fig. 1). Salps wo~lld experience most rapid temperature changes at thermocliue (about 100-200 in). Rate of chauge cxperieuced would depend on swimming speed of salp. We calculated time-course of temperatures that might be experienced by a vertically migrating salp for animals moving vertically at 200 and 800 m *h-’ (see text for justification of these speeds). For slower animal, this means a temperature change of about -0.3”C*min-‘; for faster animal, about -1.3%. min-‘. Experimental temperature drop initially is ahout -0.7”C. min-‘, a compromise between extremes. To compare rates of change more easily, we set all initial tcrnperaturcs at 25°C. depth of 1,000 m in one of these four major regions in the smnmer would undergo a temperature change ranging from 14°C (eastern North Atlantic) to 23°C (Equator). In our experimental setup, we varied temperature between 28” and 2.2”C. We attempted to mimic the temperature changes that might be encountered by vertically migrating salps at the Equator (Fig. 2). Madin (1974a) measured horizontal swimming speeds of several species of salps and found that the slowest species swam about 200 111.h-l, the fastest about three times as fast. When observed in the laboratory, S. aspera appears more active than any of the species timed by Madin, so it is reasonable to as- 1084 Harhison I and Campenot I 0.6 BODY LENGTH Cmm) I 1.0 I I I I 1.4 1.6 2.2 2.6 WEIGHT C mg C 1 Fig. 3. Dependence of swimming rhythm at constant temperature on size for Pegea confederata. O-Solitaries; O-aggregates. a-Beats per minute (bpm) at 25°C vs. length (y = -1.0X + 97, r = 0.89); b-bpm at 25°C vs. weight, as measured by carbon content (y = -0.018X + 77, T = 0.95). Differences between the two generations are slightly reduced when compared on a weight basis. sume that these salps may swim about 800 m. h-l. Although we have no information about the speed at which salps actually migrate, we used these two extremes of swimming speed to calculate the temperature changes that would be encountered by salps swimming straight down, with no pauses, at the Equator (Fig. 2). Our experimental temperature changes represent a compromise between the two extremes. Once the temperature reached its lowest point, it was held there for variable lengths of time (up to 2.5 h) and was then raised to room temperature (23’-28OC). Rewarming was usually faster than cooling. Pulsation rates before cooling were compared with rates after rewarming; if rates after rewarming were significantly lower, the salp was considered to be damaged, and the data were discarded. Results Of the nine species of salps we studied, two (S. aspera and S. fusiformis) have been collected by us and coworkers on only a few of the more than 750 dives we have made in the upper waters of the open ocean during the day. All of the other species are frequently collected by daytime diving. Several species show non-overlapping horizontal ranges. Pegea confederata, C. polae, C. affinis, and S. cylindrica are found in the upper waters of the tropical and subtropical western North Atlantic, while P. socia and C. pinnata are found mainly in the temperate eastern North Atlantic. SaLpa maxima is found in all parts of the North Atlantic, however. For some species pulsation rate is decreased markedly by cooling, others are relatively insensitive. To compare these results, we have calculated the ratio of the pulsation rate at 20°C to the rate at 10°C. In accordance with the established definition (Prosser 1973) we term this ratio the Qlo value. Usually the shape of the temperature response curve was not exponential (see Fig. 5), so our use of the term Qlo implies no mechanism. For comparative purposes, we regard any Qla value > 1.4 as high, and any value s 1.4 as low. Because the response to changing temperature is largely species-specific, we will present our results by species. Genus Pegea-The physiological responses of the two species of Pegea that we studied differed greatly, in spite of their close morphological similarity (Table 1). At constant temperature, the pulsation rate of P. confederata was more rapid than that of P. socia. For P. confederata, we observed an inverse relationship between body size and pulsation rate (Fig. 3). The mean pulsation rate at 25°C for all specimens of P. confederata was 48 bpm (beats per minute). This is somewhat lower than the mean value reported by Madin (1974a), but the dis- Temperature 1085 effects on salps b .,, -\-‘ for a Pegea confederutu solitary (length = 51 mm), showing constancy of swimming Fig. 4. a-Record rhythm of this species. Chart speed, 5 s. div- ‘; temperature, 23.5%; mean pulsation rate, 44 bpm. Most salps we studied showed a constant pulsation rate such as this. b--Record for a Salpa cylindricu solitary (length = 17 mm), showing irregular swimming rhythm characteristic of this species. Chart speed, 5 se div-‘; temperature, 25.5%; mean pulsation rate, 96 bpm. crepancy may be due to differences in the average size or differences in the temperature. The swimming rhythm of P. confederata was extremely regular (Fig. 4a), while that of P. socia consisted of bursts of activity and periods of quiescence. Both species usually showed a marked sensitivity to changes in temperature (Table 1). QIo values for P. confederata -, 10 TEMP CoC) TEMP Fig. 5. a-Effect of temperature on pulsation rate at 23.5”C), showing typical type I response. Pulsation on ordinate indicates temperature at which pulsations on pulsation rate of a S&pa maxima solitary (initial response. c-Effect of temperature on pulsation rate 25”C), showing a typical type III response. All panels: <oCI TEMP 20 30 C°C) of a Pegeu confederutu solitary (initial rate, 44 bpm rates expressed as percentages of initial rate. Arrow resumed after warming. b-Effect of temperature rate, 47 bpm at 24”(Z), showing a typical type II of a Salpa usperu solitary (initial rate, 60 bpm at O-cooling curve; O-warming curve. 1086 Harbison and Campenot Table 1. Effects of temperature on pulsation rate of salps in genus Pegeu. Pulsation rate at 25°C in beats per minute (bpm). Qlo values are for interval of cooling between 20” and 10°C. In most cases, temperature response curve was linear, rather than exponential, between these temperatures (see Fig. 5), so a least-squares regression line for data points was calculated, and values for pulsation rates at 10” and 20°C were used to determine Qlo. With P. confederutu, salps stopped swimming at low temperatures. Point at which salp stopped is given below, as well as temperature at which it started up again. In some cases, experimental temperature was not low enough to cause salp to stop, so lowest temperature obtained in a given experiment is also shown. Length of salp is given, since there is an inverse relationship between pulsation rate (bpm) and size (Fig. 3). Symbols for collection method on all tables: H-hand-collected; Mmidwater trawl-collected; V-collected with the vertically towed plankton net. Length (mm) bpm at 25°C QlO stop temp CC) Restart yL;p P. confederutu 30 33 50 47 51 60 60 62 67 51 38 43 46 35 31 30 2.75 5.17 3.67 3.24 2.00 29 38 45 60 72 63 59 45 2.78 4.35 - 23 24 24 26 28 29 37 40 41 35 2.02 1.97 1.58 2.10 1.32 * Restart temperahlre Collection method solitaries s.0 ca. 5.0 7.5 19.0 8.3 P. confederutu Lowest T attained (“C) aggregates 10.0 6.0 - P. sociu aggregates - 19.0 * 13.0 20.0 12.0 20.5 14.5 - - 12.5 5.0 14.0 5.0 7.5 11.0 19.0 6.0 II II II H II H H l-1 10.0 6.0 16.0 16.0 H H H H 2.2 7.7 6.0 3.2 3.5 H H H H H not recorded. were higher than for P. socia, but the greatest difference between the two species was that all P. confederata ceased pulsating at low experimental temperatures (< 10°C) whereas none of the P. socia did. When specimens of P. confederata were rewarmed, there was always a marked lag before pulsations resumed (Fig. 5a). This lag may be due to an actual physiological effect or to uneven warming. Since the salp was not swimming, the interior of the animal may have been cooler than the water in the finger bowl (see methods). Once the animal resumed beating, the resultant warming curve was usually identical to the cooling curve, showing complete reversibility (Fig. 5a). Genus Cyclosalpa-C yclosalpa polae showed a temperature response similar to that of P. coqfederata: a high QlO, with pulsations ceasing altogether at low temperatures (Table 2). In contrast, none of the specimens of C. pinnata or C. affinis stopped, although Qlo values were usually high. In one case, a very low Q10 was observed with a C. affinis solitary. Both C. polae and C. pinnata showed regular swimming rhythms at constant temperature, but C. af$nis did not. For example, for one specimen, pulsation rates at 25°C for 40 successive 5-s intervals ranged from 30 to 63 bpm (mean rate = 53 bpm). We used the highest rate sustained over 5 s for each temperature in our calculations of Qro values. We reason that this maximal rate shows the maximal capability at each temperature. We could associate no change in gross behavior with changes in pulsation rate, as we were able to do with S. aspera (see below). Genus Salpa-At constant temperature, Temperature 1087 effects on salps the swimming rhythm of S. cylindrica was irregular (Fig. 4b), and we saw no differences in behavior to account for it. Fpr example, for one specimen of S. cylid&a, rates ranged from 61 to 110 bpm (mean rate = 87 bpm). For this species, as for others that had irregular swimming rhythms, we have used the highest rate sustained over a 5-s interval as representing the actual capability of the salp. Use of the highest rate seemed preferable to averaging because salps have been observed to pulsate at submaximal rates during “escape responses” (Madin 1974a) II--I 10 30 20 BODY IL-40 LENGTH I-_ 50 80 8 TO Cmml Fig. 6. Dependence of pulsation rate (bpm at 25°C) on body length for four species of S&m-S. cylindrica, S. maxima, S. fusiformis, and S. aspera. We used this relationship to assess effects of collection method on experimental results. l Hand-collected S. cylindrica and S. maxima; Aindividuals (S. usperu and S. fusiformis) collected with vertically towed plankton net; O-individuals (S. cylindrica, S. maxima, S. aspera, and S. fusiformis) collected with midwater trawl. Solid line is least-squares regression line for data points obtained with hand-collected individuals (y = -0.98X + 110, r = 0.85); stippled area defines 95% conficlencc limits for these data points. All data points Table 2. Effects nation of quantities of temperature listed. on pulsation for individuals collected with vertically towed plankton net lie within or above stippled area. Least-squares regression line (y = - l.lX + 120, r = 0.78) through these data points does not differ significantly from line through data points for handcollected individuals. In contrast, most data points for trawl survivors lie below 95% confidence limits. Least-squares regression line (y = 0.079X + 50, r = 0.034) through these data points does not show relationship observed with animals collected by other two methods. WC conclude that data obtained from trawl-collected animals are variably depressed. rate of salps in genus Cyclosalpa. stop Lfxgth (mm) %Yt 0 1 70 21 Q*0 28.33 C. polae solitary ca. 10.0 C. polae 28 28 30 32 14.34 3.53 60 64 72 38 37 31 3.22 2.17 2.77 50 52 23 23 1.68 1.75 36 50 21 45 1.05 1.62 28 36 60 33 2.93 2.01 Collection method 6.0 II 23.5 ca . 14 .0 5.0 5.5 II H - E 5:o II H II - 3.5 3.0 l1 II - - 5.0 10.0 H II aggregates - - 5.0 4.8 II II solitaries - C. pinnata aggregates - C. affinis C. uffznis Lowest 7 attained (“C) 1 gives expla- 18.0 aggregates 11.0 8.5 C. pinnata , Restart temp r-C) temp (“a Table solitaries 1088 Harbison Table 3. of quantities Effects listed. of temperature on pulsation and Campenot rate of species in genus Salpa. Table stop Length (mm) QlO 17 19 24 25 - 92 102 76 83 110 1.95 2.24 2.59 2.35 2.67 38 54 55 60 65 75 77 62 66 48 46 35 1.94 1.60 1.64 4.31 1.54 1.26 40 42 46 52 55 60 62 52 53 38 66 55 1.58 1.60 1.45 1.60 - 22 23 24 55 108 84 11 20 21 26 28 27 53 98 34 72 0.812 2.03 1.67 0.864 1.37 15 26 30 30 39 48 50 58 62 73 131 31 38 80 47 23 60 63 69 49 1.51 1.54 1.17 1.12 1.24 1.35 1.28 1.42 1.44 1.26 19 27 28 60 125 60* 64 53 Restart S. maxima Collection method ‘g t;Fy S. cylindrica 5.5 6.0 4.5 6.0 5.0 1 gives explanation solitaries 21.3 ca. 18.0 17.0 15.0 18.0 5.5 6.0 4.5 5.5 5.0 H II M V H M H H H H H solitaries - - 10.0 - 1G - 7.0 8.0 5.0 8.0 5.0 10.0 - 5.0 4.0 3.0 7.5 13.0 15.0 H H H H H H - 14.0 5.0 5.0 M V V - 10.5 4.0 5.5 8.0 7.0 M M V M M - 5.0 8.5 8.0 9.0 8.0 9.5 5.0 3.0 4.0 5.0 V M M M V M V V V V - 2.5 6.0 7.2 3.0 V M V V S. maxima aggregates S. fusiformis solitaries S. fusiformis aggregates S. asperu solitaries * Rate at 25°C chosen 1.32 1.36 1.27 S. aspera aggregates - - arbitrarily. and while swimming backward (see below). Salpa maxima always showed a regular rhythm at constant temperature. If pul- sation rate vs. length is plotted for all hand-collected S. cylindrica and S. maxis found ima, an inverse relationship (Fig. 6). The swimming rhythms of S. ju- Temperuture effects on salps siformis and S. asperu were always regular. However, reverse swimming in S. aspera showed a slower pulsation rate than forward swimming. For example, one S. usperu had a forward rate of 63 bpm at 25”C, a reverse rate of 51 bpm. We have presented only the forward rates in tables and figures. The temperature responses of the four species of Sulpu differed markedly (Table 3). Salpa cylindricu gave a response similar to those of P. confederutu and C. po2ue. The temperature response of S. muximu usually resembled that of P. sociu, C. pinnutu, and C. uf$nis (Fig. 51~). However, the pulsation rates for S. fusi*formis and S. usperu were affected very little by changing temperatures. We could not detect an unequivocal response to changes in light intensity ranging from total darkness to full daylight illumination. In seven experiments with S. usperu, we found a response to changes in light intensity in only two. In one, the amplitude, but not the frequency, decreased at high light intensities. In the other, the frequency decreased at low light levels. Thus, although S. usperu can detect low levels of light, the nature of the responses is not predictable. Our observations contrast with the results of Mackie and Bone (1977) for S. fusiformis; they saw a decrease in pulsation rate at high light intensities. Effects of net truumu on experimental results-Collection by hand should be the best method. All of the animals collected with the vertically towed net also appeared to bc in good condition, so we judged that this method caused little injury. In contrast, most salps collected with the horizontally towed midwater trawl were dead or grossly damaged. A small proportion appeared to be in good condition, and only these were used in experiments. To evaluate the collection methods, we plotted the prllsation rate at 25”~ as a function of body length for hand-collectec3 S. muximu and S. cylindricu (Fig. 6). An inverse relationship is observed, as with P. confederutu (Fig. 3). This relationship probably holds for all’ salps. We 1089 calculated a least-squares regression line and 95% confidence belts for these data points (Fig. 6).Because all of the data points for animals collected by vertically towed nets lie within or above these belts (Fig. 6), we conclude that the vertically towed net causes as little injury as hand collection. In contrast, most (8 of 13) of the data points for the trawl survivors (S. maxima, S. cylindricu, S. usperu, S. fus<formis) lie below the lower 95% confidence limit (Fig. 6). We conclude that, in spite of their appearance, even the healthy-looking trawl survivors were damaged, resulting in a variable depression of the pulsation rates. Absolute rate measurements on other organisms collected with horizontally towed nets are likely to be similarly affected. Although collection with the midwater trawl caused a depression in the absolute rates, there was little effect on the Qlo values. There appears to be no relationship between collection method and the magnitude of the temperature effect (Table 3). Although relative rate mcasurements may not be affected, we recommend a skeptical attitude toward absolute rate measurements made on net-collected specimens. Discussion The species we studied can be divided into three categories, based on their responses to changing temperature. The pulsation rates of those in the first category (response type I) are markedly affected by changing temperature (Qlo values >1.4), and these animals stop pulsating at low temperatures. Pegeu confederutu, C. polue, and S. cylhdricu all show the type I response. The second category (response type II) is characterized by a marked sensitivity to changing temperature (Qlo values >1.4), but the salps do not stop pulsating. Most P. sociu, C. pinnutu, C. affinis, and S. muximu show the type II response. The third category (response type III) is characterized by very little sensitivity to changing temperature (Q,,, values ~1.4). Most S. fusiformis and S. usperu show the type III response. Although the correspondence Hurbison und Cumpenot RESPONSE TYPE S. fusiformis S. aspera I I I I I I 2 4 6 2 4 6 I 2 4 6 Fig. 7. Histogram summarizing our classification of species on basis of response types for all salps of solitary individuals; exposed to experimental temperatures of 10°C or lower. Open bars-number hatched bars-number of aggregate individuals. Three species (P. con&Aeruta, C. poke, and S. cy2inckica) always showed the type I response, accounting for 14 of the 15 times (93%) we observed it. Two species (S. fusi~ornzis and S. usperu) accomlted for 86% of the times we observed the type III response (see text for definition of response types). between response type and species is not perfect (Fig. 7), we conclude that insensitivity of pulsation rate to experimental cooling is associated with absence from surface waters during daylight. Salps are found primarily in the open sea-an environment characterized by great thermal stability (Fuglister 1960). Therefore, one would expect to find physiological adaptations to rapidly changing temperature only in species that migrate vertically. Indeed, this should be true of all other oceanic organisms as well. Our experimental results support the present sampling evidence that S. fusiformis and S. usperu do migrate vertically (Franqueville 1971; Wiebe et al. 1979). We do not know whether the effects of temperature on pulsation rate mirror comparable effects on metabolism. Mackie and Bone (1977) confirmed the finding of Fedele (1932) that there is a neural pacemaker for the swimming rhythm in the brain. The effects we see may be acting only on the pacemaker or may reflect a more general effect on metabolism. Our results are also in accord with present zoogeographic information. Species limited to tropical and subtropical waters all show the type I response. P. confederutu has not For example, been found in waters colder than 16°C (1Madin and Harbison 1978), and S. cylindricu has not been found in waters colder than 17°C (Van Soest 1975). In contrast, the species showing response type III are either widely distributed (S. muximu, S. usperu, S. fusiformis) or are found ex- Temperuture effects on sulps elusively in temperate waters (P. sociu, C. pinnutu) (Madin and Harbison 1978; Harbison and Madin unpubl.). Zoogeographic information on C. uffinis (Van Soest 1975; Harbison and Madin unpubl,) is not in accord with its response type classification; its distribution is similar to that of the type I species. However, it might be predicted that it, as well as other response type II species, could range to greater depths. Present zoogeographic information on salps is very liinited, and fLirther data, incorporating the most recent taxonomic revisions, are needed before our classification of physiological response types can be adequately tested. References CALDWELL, M. C. 1966. The distribution of pelagic tunicates, family Salpidae in Antarctic and subantarctic waters. Bull. So. Calif. Acad. Sci. 65( 1): 1-16. FEDELE, M. 1932. Muscoli ed attivita muscolare nei Thuliuceu. Boll. Sot. Nat. Napoli 44: 237250. FoxroN, P. 1966. The distribution and life history of Salpa thornpsoni Foxton, with observations on a related species, S&m gerluchei Foxton. Discovery Rep. 34: 1-116. FFMNQUEVILLE, C. 1971. Macroplancton profound (Invertebrks) de la Meditcrran& nord-occidentale. Tethys 3: 11-55. FUGLISTER, F. C. 1960. Atlantic Ocean atlas of temperature and salinity profiles and data from the International Geophysical Year of 19571958. Woods IIole Oceanogr. Inst. Atlas Ser. 1. 209 p. IIARBISON, G. IX., L. P. MADIN, AND N. R. SWANBERG. 1978. On the natural history atid distribution of oceanic ctenophores. Deep-Sea Rcs. 25: 233-256. 1091 HARDY, A. C., AND E. It. GUNTEIER. 1935. The plankton of the South Georgia whaling grounds Discovery and adjacent waters, 1926-1927. Rep. 8: l-456. HOCIIAC~IKA, I’. W. 1975. Why study proteins of abyssal organisms ? Camp. Biochcm. Physiol. 52B: l-2. I~ACKIE, G. O., AND Q. BONE. 1977. Locomotion and propagated skin impulses in salps (Tunicata: Thaliacea). Biol. Bull. 153: 180-197. MACKINTOSH, N. A. 1934. Distribution of the macroplankton in the Atlantic sector of the Antarctic. Discovery Rep. 9: 65-160. MADIN, L. P. 1974a. 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