1. Introduction
Temperature extremes are becoming increasingly common in unstable climates [
1,
2,
3]. This is a public health concern [
4], but for biota in general, global warming is even more dangerous and unpredictable [
5,
6,
7], especially for polar ecosystems including the Arctic [
1,
8,
9], where climate change is predicted to be stronger than at low latitudes [
10].
The response to an extreme increase in environmental temperature is not known for most species [
6,
11]. For a number of species, a few studies identified a critical temperature at which death occurs [
12], but the exposure to extreme heat was short-lived. How quickly do changes in vital activity appear with a prolonged increase in temperature? To what extent are these vital reactions reversible? Is it possible to adapt to extreme conditions of existence? These and similar questions are directly related to the response of ecosystems to possible climate warming. So far, the scientific literature has been dominated by only the most general assumptions about changes in ecosystems; these assumptions are often based on biogeographic data. However, the methods of biogeography can reliably determine only the established correspondences between habitat conditions and ecosystems. In such cases, the ecological preferences of species are judged using the typical characteristics of the biotopes in which these species live within their ranges. Obviously, this method is not enough to determine the response of a species to an ongoing change in habitat indicators [
13].
Therefore, we undertook an experimental study on colonial hydroids in order to determine the immediate and prolonged response of some key vital signs to a significant increase in seawater temperature.
This article presents the results of studying the reaction of
Dynamena pumila (L., 1758 to an increase in water temperature from 14–15 °C to 24–25 °C, as well as a subsequent decrease in temperature to a normal value of 15 °C, using the species’ growth and the pulsations of the body of the colony. Few studies of this kind have been performed in hydroids, all of which were scattered and gave only a general idea of the reaction of the colonies to a slight increase in water temperature [
14,
15,
16,
17,
18,
19,
20,
21,
22,
23,
24]. Only recently was a study performed on the instantaneous reaction of the colonial hydroid
D. pumila to various temperature increases, and it was found that 25 °C was the limiting temperature at which the hydroid did not die [
25].
However, this is not enough to accurately determine the upper temperature limit of the survival of individuals. Now, we have determined how constant the hydroid’s negative reaction to an increasing temperature is. Does adaptation to that temperature occur over a few days following a significant and rapid increase in temperature to the upper limit?
The White Sea population of
D. pumila lives in the upper sublittoral zone and even in the drying zone during regular low tides. Only a small part of the White Sea invertebrate fauna survives such conditions. Therefore,
D. pumila can rightfully be classified as a eurybiont. Without an accurate idea of how much sea surface temperatures will increase with the predicted warming of the global climate, it seems advisable to at least learn about the reaction of the most resilient eurybiont species to the upcoming ordeal. The first question that must be answered is what is the thermal tolerance limit of the species? Therefore, in our study, we focused on determining the upper temperature limit of the White Sea population of
D. pumila. The most severe exposure conditions were chosen: a rapid and significant change in temperature. Having previously established [
25] the upper temperature limit for
D. pumila under such extreme conditions in an experiment on the response of the species’ growth and stolon pulsations in colonies in the first hours of a sharp change in temperature, in this study, we wanted to determine how stable the cessation of growth and changes in stolon pulsations are within five days. We were also interested in the possibility of restoring the normal life activity of
D. pumila with a subsequent decrease in water temperature and the speed of this process.
2. Materials and Methods
The object of study: the colonial hydroid
Dynamena pumila (L., 1758), a representative of the Sertulariidae family of the Leptothecata suborder of the Hydrozoa class, was chosen for this study (
Figure 1). Many studies on growth, colony integration, feeding, etc., have been carried out on this hydroid [
26,
27].
This study was carried out on colonies grown from individual shoots. All colonies included, in addition to the initial shoot, a short stolon less than 10 mm long with one or two young shoots on it (
Figure 2). We call such colonies juvenile, contrasting them with branched–developed colonies with many stolons and shoots.
2.1. The Morphology of the Colonies
D. pumila colonies are characterised by filamentous stolons creeping along the substrate. From them, at approximately equal distances from each other (on average, 3 mm), shoots depart with a two-row opposite arrangement of hydranths in hydrothecas (
Figure 1). New shoots are formed within the top of the stolon but never between shoots. The growth zones are located proximally from the apex of the stolon or shoot at a distance of approximately 0.3 mm from the apical end of the stolon/shoot (apex) [
25,
26].
2.2. Colony Mapping Technique
After selecting the colonies for the experiment, the registration of their sizes began: the length of the stolon, the number of shoots, the size of the shoots (expressed as the number of internodes—pairs of hydrothecas), the formation of lateral branches of the stolon, the number of active hydranths, the resorption of hydranths, and the areas of the maternal shoot coenosarc were determined. All these indicators were obtained using a simple method of “mapping” the colonies under a binocular microscope [
28], i.e., drawing up schemes of the colonies on which measurements and calculations are recorded (
Figure 2).
When drawing up regular diagrams (“maps”) of the colonies, we noted active hydranths, i.e., those which were not hiding in hydrothecas but had opened their tentacles. Such observations are not enough for a quantitative account; however, we used the appearance of active hydranths in colonies after they experienced unfavourable conditions as a marker for the onset of the recovery stage.
2.3. Terminology and Parameters
The text of this article uses several little-known terms and parameters which are defined below.
Colonial organism—usually called a colony, but the term colony is polysemantic; it is used to refer to both a colony of gulls or bees and to refer to modular colonial invertebrates, hydroids, corals, bryozoans, etc., although modular organisms are not communities of individuals. However, the term “colony” has become so entrenched that it is easier to use than “colonial organism”. In this article, these terms are used as synonyms.
The shoot module is a part of the shoot, which in D. pumila includes two oppositely located hydrothecas and a section of the trunk between them. The boundaries between the modules are conditional and are “tied” to the narrowest places on the runoff between pairs of hydrothecas.
The stolon module is the part of the stolon between two successive shoots.
The growing tip is the apical (terminal) part of the coenosarc of the shoot or stolon, due to the pulsations of which this part moves forward with the stretching of the thin perisarc and the release of a new perisarc. Growing tips are morphologically different from tubular coenosarcs, which they crown.
Growth per cycle of pulsation—the distance that the top of the growth moves forward for each cycle of longitudinal pulsation.
2.4. The Collection of Colonies at Sea
D. pumila colonies live on the border of the littoral and sublittoral zones. They can be found on the macrophytes Fucus and Ascophyllum, as well as on rocks in areas of constant water movement due to regular tides [
26]. In summer, the water temperature at the sea surface reaches 16 °C, and in the apexes of bays, it reaches up to 18 °C and higher, depending on the shallowness of the water and warming up. In winter, the sea is covered with ice, and the water temperature drops to a minimum of −1.3–−1.7° C on average. The salinity of the water at the surface varies between 26‰ and below. The average daily production of phytoplankton in the White Sea is 250 mg C/m
2, and the average biomass of zooplankton is about 200 mg/m
3 [
29,
30].
Material was collected from a dense population of
D. pumila on the Yeremeevsky threshold (66°33.3′ N 33°08′ E) in the Great Salma Strait of the Kandalaksha Bay, near the White Sea Biological Station of Lomonosov Moscow State University, where this study was carried out [
31].
During the low water phase on 2 June 2022, one bush of
Fucus serratus on the Yeremeevsky threshold, with clean, slightly overgrown colonies of
D. pumila was selected, and medium-sized shoots were cut from it, i.e., from 13 to 20 internodes of the shoot trunk. The shoots were fixed one by one under transverse threads on slides according to the method described earlier [
32,
33].
2.5. The Cultivation of Colonies
Individual shoots were placed on glass slides or on photographic plates without an emulsion (9 cm × 12 cm in size) [
34,
35]. The slides with
D. pumila shoots attached to them were placed in a ten-litre aquarium placed in a large, opaque container filled with water. Water was constantly pumped (300 L/h) through a flow cooler (Resun CL–200). So, in a container with an aquarium, a predetermined temperature of 14–15 °C was maintained, which is optimal for the rapid growth of this species [
25]. With the help of a microcompressor, the water in the aquarium was constantly aerated, mainly in order to set it in motion, simulating a flow.
The colonies were fed daily with freshly hatched Artemia salina nauplii for one hour in a separate feed tank. The water in the aquarium was renewed daily, and the aquarium was rinsed with fresh water before it was filled with fresh sea water. Artemia nauplii were added to the fresh water. After feeding, the concentration of nauplii was 0.6–1.7 ind./mL.
A few days after the start of cultivation, from the bases of some cut-off shoots, which we call “mother” shoots, stolons began to grow which spread along the surface of the substrate and were firmly attached to it. After another day or two, one daughter shoot appeared on the stolons. Not all colonies were suitable for detailed study. First of all, they differed in their similarity to each other in size, depending on the date of the initiation of stolon growth. However, all grown colonies were in the experiment. From these, if necessary, it was possible to choose a replacement for a damaged colony.
2.6. The Main Stages of the Experiment
This experiment consisted of six main stages.
Stage 1: The completion of colony cultivation at 14 °C, drawing up colony diagrams, and obtaining time-lapse photographs of the pulsations of the stolon tips;
Stage 2: Increasing the water temperature to 25 °C in 2–3 h to simulate thermal shock “in its pure form”, not smoothed out via a slow transition and without an adaptation to changes in temperature conditions;
Stage 3: Drawing up diagrams of the colonies and obtaining time-lapse photographs of the pulsations of the tops of the stolons immediately after increasing the water temperature to record the rapid responses of the growth and pulsations of the coenosarcs of the colonies to thermal shock;
Stage 4: Drawing up diagrams of the colonies and obtaining time-lapse photographs of the pulsations at the tops of the stolons twice over five days to detect a possible adaptation to elevated water temperatures;
Stage 5: Reducing the water temperature from 25 °C to 15–16 °C within 2–3 h, recording changes in the structure of the colonies and obtaining time-lapse photographs of the pulsations of the tops of the stolons to determine the immediate reaction of the colonies to the restoration of growth conditions typical for this species in the White Sea;
Stage 6: Recording changes in the structure of colonies and conducting time-lapse photography of pulsations at the tops of stolons on the fifth day of keeping colonies under normal cultivation conditions to determine the degree of restoration of the growth and pulsations of stolons after a five-day thermal shock.
2.7. Time-Lapse Microvideo Recording Technique
Time-lapse microvideos were filmed to register the vital signs of the D. pumila colonies. For this, an Arecont AV3100M video camera was fixed on a microscope tube and connected to a personal computer. Filming was carried out frame by frame with a frequency of 4 frames/s. A transparent cuvette with double walls and a bottom was placed on the working table of the microscope. The inner volume was a working space filled with fresh sea water in which to place glass with colonies to videorecording, and the outer space between the two walls and two bottoms was used to achieve a constant flow of water of a certain temperature which was pumped through the flow cooler. Taking into account the size of the cuvette, it was the most convenient to use the simplest microscope, an MBI-1 with a straight tube, on which a video camera was fixed. The object was illuminated using a separate illuminator, the beam of which was directed into the field of view through a mirror. This helped avoid overheating the working area during filming. For microscopy, an 8× microscope objective without an eyepiece was used. Due to the tube, the overall increase was approximately 100-fold. Before shooting the object, a scale microline was taken which was used to calibrate the on-screen ruler for subsequent measurements during the cameral processing of the video recordings.
Time-lapse photography makes it possible to register (1) growth of the stolon apex, (2) the pulsations of the apex, and (3) coenosarc walls in any transparent place of the stolon, as well as (4) the movement of particles in the gastrovascular cavity of the stolon which are carried by hydroplasma (internal fluid filling the cavity).
The pulsations of the coenosarc can be express indicators of the state of a colonial organism of hydroids. The most sensitive and reliable among all indicators of coenosarc pulsation are the regular successive protrusions and contractions of the terminal end of the apex of a stolon or shoot, which are usually called growth pulsations or pulsations of the growth apex [
34,
35]. Normally, growth pulsations are rhythmic and can be characterised by several indicators, including their period, amplitude, and growth per pulsation cycle. Although these indicators do not remain strictly constant, they are nevertheless convenient for comparison, including graphical comparisons. The growth pulsation plots clearly show differences in detail. More information can be extracted from them than from averaging, but to achieve this, it is necessary to analyse growth pulsations individually for colonies.
The video recordings were decoded using the following method. In order to register the processes in an accelerated mode corresponding to a half-minute interval, every 30 s, three indicators were measured on a computer monitor with a screen microline: (1) the position of the apical edge of the stolon apex, (2) the size of the coenosarc lumen, and (3) the displacement of any distinct particles in the colony cavity within the field of view. The results of registering the speed of particle movement are not given in this article. Based on the measurements of the position of the apical point of the apex of the stolon coenosarc, the increase in one cycle of pulsations was determined. With the degradation of the apex and its departure from the perisarc, the growth rate turned out to be conditional because while pulsing, the stolon did not grow, and the tip only moved forward inside the empty space in the perisarc from time to time.
2.8. Statistical Processing
Since the distribution of quantitative data often differs from a normal distribution, we used the median to estimate the average values, and the quartiles Q1 and Q3 were used to determine the degree of deviation from the average values. The significance of differences between samples was determined using the Mann–Whitney U test.
The samples depended on the number of pulsations taken into account, and they, in turn, depended on the pulsation frequency and the total recording time. The standard shooting time was 90 min, but nighttime was also used, so individual episodes lasted from seven to nine hours.
2.9. The Number of Colonies in the Experiment
Our experience, gained from many years of research, suggests that the samples in the study of the growth, resorption, and functioning of the distribution system should be small in order to be able to individually analyse the processes studied in each colony, along with statistical processing [
25,
27,
35]. Modular and especially branched organisms differ from each other incomparably more than unitary (single) organisms [
27]. These differences are not limited to age and environmental factors. For example, the intensity of the branching of shoots and stolons affects the growth rate and the nature of the functioning of the distribution system. No less influence is exerted by the processes of the resorption of hydranths, depending on a set of circumstances. Therefore, during a study, one should strive not to increase the sample and limit the parameters but to ensure a comprehensive individual consideration of a variety of indicators, using the example of the optimal number of individuals. This approach is called “idiographic” [
35].
Of the several dozen cut-off shoots of
D. pumila, only a third attached to glass and produced a stolon, and not all of them began to grow stolons convenient for subsequent observations, i.e., stolons which were straightforward and without branching. Therefore, the experimental sample included colonies in which the formation of stolons was not delayed and the direction of their growth was convenient for observation. There were no other criteria for selecting colonies for this experiment. Therefore, the colonies were not uniform, although they were similar to each other (
Figure 2). Such limited heterogeneity is best suited to an individual analysis of the dynamics of indicators over the course of an experiment within a small group of related research objects.
Initially, there were five D. pumila colonies in the experiment, but over the course of the experiment, one colony dropped out, and the second was replaced with an identical colony in the first days of the experiment. The limitation of the number of colonies allows for replacement, if necessary, since all results are tracked and compared with each other for each colony separately and not just on average. Therefore, the idiographic approach expands the possibilities of statistically processing quantitative data, especially when tracking changes that occur in objects over the course of monitoring.
4. Discussion
In connection with global climate change and increases in the temperature of the upper water layer recorded in a number of locations [
36,
37], the timely determination of changes in species’ ranges is especially important [
38]. Understanding and scientific forecasts of the biological consequences of climate warming should be based on fundamental information about the responses of biological species to changes in environmental temperature. However, thermotolerance, the range of allowable temperature values in which the viability and temperature optimum of a species is maintained, is far from known for all species. In addition, indicators of ecological tolerance and the temperature optimum should be tested for different life cycle stages, as well as in combination with other environmental factors; this significantly increases the amount of information needed and reduces the number of species for which all or at least a significant part of this information is already available. Such species include representatives of the class Hydrozoa: freshwater hydras [
39,
40,
41,
42] and marine colonial hydroids [
14,
15,
17,
18,
31].
Among colonial hydroids, the reaction to water temperature is best studied in three species: Cordylophora caspia (Pallas, 1771), Clava multicornis (Forsskål, 1775), and Dynamena pumila (L., 1758).
The response of marine cnidarians to temperature depends on the salinity of the water. Therefore, most studies compare combinations of given temperature and salinity series [
18,
43,
44]. For example, in a study of
Clava multicornis, a hydroid’s response was compared to 12 different combinations of constant temperature and salinity levels: temperatures of 12, 17, and 22 °C and salinity levels of 16, 24, 32, and 40‰.
At 12 °C and 17 °C, the colonies survived in water at any of the four salinities, and at 22 °C, most colonies survived no more than one week at 16 °C and 40 ‰ salinity.
Optimal conditions were determined using the following indicators: (a) the length and width of the body of the hydranth, (b) the number and length of tentacles, and (c) the rate of digestion. In water with a salinity of 16‰, the length of the hydranth in
C. multicornis reached its maximum at 12 °C, at a higher level of salinity (24‰) at 17 °C, and at a salinity of 32‰ at 22 °C. The number of tentacles on the hydranth decreased with increasing temperature and depending on salinity. The maximum number of tentacles was observed at 12 °C and 16‰, at 17 °C and 24‰, and at 22 °C and 32‰ [
17]. As a result, the optimal conditions for different criteria could differ somewhat. Thus, the growth of stolons was the fastest at 12 °C and 32‰, and the highest rate of increase in the number of hydranths occurred at temperatures of 17 °C and 22 °C and a salinity of 32‰.
Cordylophora caspia grows in a wide range of aquatic environments varying in salinity, temperature, currents, oxygen, etc. Survival resistance among populations varies greatly as a result of both genetics and acclimatisation [
45].
The optimal temperatures for the asexual growth of
Cordylophora caspia were found to be 11–18 °C for populations in Germany [
14,
15], 18–26 °C for populations from Massachusetts, USA [
46], 16–25 °C for populations in San Francisco [
47], and 23–30 °C for colonies from Iraq [
45]. The upper temperature limit was established in experiments to determine a means of eliminating this species in the biofouling of TPP pipelines.
C. caspia colonies were harvested from the Des Plaines River in Joliot, Illinois, cultured under laboratory conditions in the same water, and then exposed to elevated temperatures of 35 °C for 2, 4, 6, and 8 h; 36.1 °C for 1, 3, 5, and 7 h; and 37.7 °C and 40.5 °C for 1 and 2 h. It is important that the temperature was raised at a rate of 2 °C over 15 min, i.e., not all at once, but rather quickly. At the end of the thermal shock, the colonies were transferred into an aquarium with room-temperature water (19.4 °C), and further growth or recovery was monitored by changing the number of hydranths after 7 and 12 days. In all variants of thermal shock, the colonies stopped growing, and some of the hydranths were absorbed. Only when exposed to 35 °C for several hours did regeneration occur in room-temperature water, which was noted after 7 and 12 days, but after 8 h of thermal shock at 35 °C, the colonies could not recover. After exposure to 36.1 °C, the colonies regenerated only in a series with a thermal shock duration of 1 h. In longer series, no regeneration of the colonies was observed. From the data presented, it appears that for a population of
C. caspia from the Des Plaines River in Illinois, the upper temperature limit for short-term exposure does not exceed 35 °C [
48].
When studying the thermotolerance of the colonial hydroid
Dynamena pumila (L., 1758), the temperature limits of survival were the focus of attention [
25,
49,
50]. The lower temperature limit can be determined biogeographically from the temperature in winter in the habitats of the
D. pumila population. Thise research was carried out in the White Sea.
The lower water surface temperature during winter drops to (−)1.3 °C-…(−)1.7 °C. However, when the water drained during low tides,
D. pumila colonies living on fucus and stones in the zone of the boundary of the lower littoral and sublittoral can also be exposed to lower air temperatures. Usually, the inhabitants of the lower littoral are protected from freezing by thick ice covering the White Sea, but in bare areas of the littoral on rapids (for example, on the Yeremeevsky threshold in the Great Salma of the Kandalaksha Bay), the colonies remain drained at air temperatures down to −20 °C [
51].
When keeping
D. pumila colonies in the laboratory at temperatures from (−)1 °C to +1 °C, and from +1 °C to +4 °C, it was found that only a part of the hydranths remained active in winter colonies. Their size was about two times smaller than that of summer colonies, and the diameter of the corolla of the tentacles was three times smaller. With an increase in water temperature, the growth of stolons began, regardless of the amount of food received. At the same time, shoot growth under these conditions began only in the presence of food [
52]. With daily feeding in water at different temperatures in four parallel series, 20 °C (13 colonies), 12 °C (10 colonies), 6 °C (18 colonies), and from −1 °C to +1 °C (5 colonies), the average growth rate of the shoots and stolons was determined via regular colony mapping. The appearance of gonophores was also recorded. The dependence of the average growth rate of shoots and stolons on the temperature in the range of 6–20 °C was close to directly proportional, while the growth rate of stolons differed when comparing colonies from different temperature conditions and was twice as fast as the growth rate of shoots. At temperatures below 2 °C, there were few growing tops in the colonies, both in the lab and in the sea. The temperature in the area drained at low tide did not remain constant. At temperatures close to 0 °C, growing stolons elongated very slowly (0.04 mm/day), and shoots behaved similarly (0.04–0.05 mm/day) [
19].
The upper temperature limit for the normal life activity of
D. pumila was established using time-lapse microvideo recording by analysing the growth pulsations of the stolon coenosarc [
25]. This method is so sensitive that it allows for the registration of changes in the growth of the coenosarc in less than two hours after the onset of exposure to environmental factors; in this case, after an increase in water temperature. It turned out that the optimal range, in which a high growth rate, intense movement of hydroplasma, and the largest volume of transferred hydroplasma are observed, is limited by the interval from 10 °C to 20 °C. At 28 °C, the pulsations of the stolon coenosarc became unstable, growth, as a rule, slowed down, and the movements of the hydroplasma were less active [
25]. Therefore, the upper temperature limit of the normal life activity of White Sea
D. pumila colonies, according to the results of the analysis of coenosarc pulsations, can be within 25–28 °C. In the natural habitat of
D. pumila in the White Sea, the temperature of the surface meter layer of the water does not exceed 18 °C. It is under these conditions that the population of this species lives, and these conditions were used for cultivating colonies in the laboratory at 14–16 °C.
Our new experiment aimed to elucidate the possibility of the
D. pumila colonies adapting to a rapid increase in environmental temperature within five days. If, in the previous study [
25], the majority of attention was paid to the possibility of quickly registering the reaction of the colony to temperature changes, we are now interested, first of all, in the degree of sufficiency of express diagnostics for determining the long-term response of the body to the temperature increase produced in the experiment.
In all colonies that were tested using a significant increase in water temperature (an increase of 10–11 °C), growth pulsations and growth as a whole in the first hours of thermal shock were preserved, although the pulsation indexes immediately changed (
Figure 3). Starting from the second or third day, the increase decreased and stopped, and the terminal pulsations of the stolon tips ceased to be regular (
Figure 5). The amplitude of the growth pulsations was not strictly constant in the norm, and now it changed significantly. Also, the gain per pulsation cycle varied from normal to zero or even became negative.
Already at this phase, in some colonies, the growth of the stolon stopped. The coenosarc of the growing tip of the stolon lost its strong connection with the perisarc, and since there was often tension in the coenosarc behind the growing tip, the tip was pulled back as soon as it became thinner and shorter. Then, a gap was formed between the apex of the perisarc and the coenosarc of the stolon which was minimal in some colonies and significant in others. The change in the position of the stolon apex was now determined via two factors: the force of forward movement during the pulsations of the growth apex and the tension force of the coenosarc of the stolon which, apparently, was determined by a lack of cells in the epithelium of the walls of the body [
53].
We set the duration of the thermal shock to only 5 days, during which no adaptation to a temperature of 25 °C occurred. This means that the changes in the growth indicators and the pulsations of the stolon apex obtained immediately after the increase in water temperature via the express method of time-lapse recording the stolon growth pulsations [
25] can be extrapolated to at least the next 5 days (
Figure 3,
Table 2). Therefore, this method is quite suitable for the rapid monitoring of the effect of water warming on the state of bioassay objects such as the colonial hydroid
D. pumila.
However, it should be taken into account that all colonies survived at 25 °C for five days, and with the subsequent cooling of the water in which they were kept, they were able to quickly recover. We did not expect recovery to begin immediately after the water temperature dropped and kept the colonies at 15–16 °C for the next five days before resuming the time-lapse recording of coenosarc pulsations. By this time, the tops of the stolons had all returned to their normal state, the coenosarc moved close to the previously formed perisarc, and the growth of stolons resumed (
Table 2). Therefore, even with prolonged exposure to elevated temperatures (up to 25 °C), the
D. pumila population retained the ability to quickly recover when the temperature dropped.
Is this enough for the White Sea population of D. pumila to withstand climate warming? Currently, the maximum annual summer water temperature in the surface layer in the habitat of the White Sea population of D. pumila reaches 17–18 °C in July–August in some years, according to long-term measurement data.
Unfortunately, for the vast majority of species, the maximum water temperatures in their habitats are still not known. It is possible to approximately determine the living conditions of species using only the geography of their distribution.
D. pumila is an Atlantic high boreal species [
54]. The range of
D. pumila includes the entire Atlantic coast of Europe north of the Bay of Biscay, the White and Barents Seas, the coast of the British Isles, Iceland and southern Greenland, and the Atlantic coast of Canada, i.e., waters with cold currents and summer surface temperatures that are about the same (less than 19 °C) as in the White Sea [
55,
56].
Previously, we experimentally established that when
D. pumila was cultivated at 15 °C in White Sea water and the water temperature was increased rapidly for several hours, the maximum level of thermotolerance in this species did not exceed 25 °C [
25]. We judged this using the change in the indicators of stolon coenosarc and shoot pulsation.
This time, when investigating the reaction of
D. pumila colonies to prolonged exposure to elevated temperature for five days, we found that immediately after the temperature was raised from 14 °C to 25 °C, the growth of colonies even increased, but not for long. The frequency of the growth pulsations of the stolon immediately increased, while the amplitude of the pulsations and the growth per cycle remained the same, which caused an acceleration in growth. A day later, and possibly earlier—during the following hours—the period of the pulsations remained reduced, and the amplitude of the pulsations decreased. The main factor is that the stolons almost stopped growing within a day after the water temperature rose to 25 °C. The pulsations became less regular, and the stolon apex coenosarc began to lose contact with the perisarc, due to which the apex “moved back”. Normally, the top of the coenosarc tightly adjoins the perisarc and, pulsing, moves forward, pulling the coenosarc behind it. When growth stops and the contact surface of the coenosarc of the apex with the perisarc decreases, the coenosarc stretched behind the apex pulls it back (
Figure 5). During eight and a half hours of video recording, the apex either moved forward inside the perisarcal tube or sharply moved back. Apparently, the tension of the coenosarc behind the apex became greater in these short time intervals. On the third or fourth day, the apex pulsations weakened and ceased to be regular (
Figure 7). On the fifth day, the terminal pulsations became even less clear. Consequently, after five days of exposure to an elevated temperature (25 °C), adaptation did not occur in the
D. pumila colonies.
We determined that the restoration of the pulsations and growth of colonies is possible even after five days of exposure to thermal shock. Recovery after the termination of the thermal shock occurred in just a few days. The nature of the pulsations became full-fledged in terms of their period and amplitude, and the growth rate of the stolons corresponded to the norm.
Answering the question formulated in the title of this article, it can be stated that in the stage of vegetative growth, the colonial hydroid D. pumila can adapt to the predicted increase in environmental temperature in the Arctic region, provided that a sufficient amount of small zooplankton, which the hydroids feed on, remains in the ecosystem. However, this conclusion is not final because the survival of the species and its ability to adapt to changing environmental conditions are not limited to the growth stage. So far, there are no data on the possibility of sexual reproduction with an increase in water temperature.