On the relationship between the Bosmina taxa coregoni and thersites (Cladocera), as indicated by subfossil remains

A succession of morphs from Bosmina coregoni f. coregoni to B. c. f. thersites, which vary in shell and antennule characters, occurred in an undated 176 cm long sediment core from the Neversdorfer See (N. Germany).     

Morphological variation and population dynamics of Bosmina (E.) longicornis kessleri Uljanin (Crustacea: Anomopoda: Bosminidae) in the Bukovec Reservoir (S.E. Slovakia)

Bosmina (Eubosmina) longicornis kessleri and B. (Bosmina) longirostris are minor components among the crustacean zooplankton in the pelagial of Bukovec Reservoir. B. (E.) l. kessleri is a recent colonist in the Carpathian region and was first found in the Bukovec reservoir in 1986. The present study gives some information about the niche occupied by B. (E.) l. kessleri in the zooplankton community; the seasonal abundance of zooplankton and phenotypic variability (cyclomorphosis) of B. (E.) l. kessleri are also examined.     

The food preference of vendace (Coregonus albula) in South Swedish forest lakes including the predation effect on zooplankton populations

Vendace (Coregonus albula, L.) is in the southern part of its distribution area during the summer period restricted to hypolimnion. Food is dominated by Bosmina coregoni and Daphnia sp. The selectivity index is highest for large cladocerans and large copepods.The pelagic crustacean fauna in vendace lakes is dominated by small species like Bosmina coregoni, Daphnia cristata, Thermocyclops and Mesocyclops sp. and Eudiaptomus sp. During periods of maximum vendace abundance only Bosmina coregoni is left of the cladocerans, while the abundance of cyclopoid copepods increases.     

Late-Pleistocene and early Holocene history of the canid fauna of Europe (Canidae)

In the sub-fossil assemblages of Europe the red fox is clearly the most frequent carnivorous mammalian species with a total of 1553 records. In depositions from the Weichselian Glacial the red fox Vulpes vulpes is, a typical representative of the Holocene fauna, already recorded in 100 assemblages. The Iberian peninsula, Italian peninsula and Balkans were theorised as glacial refugia. Well-founded facts give reason to believe that V. vulpes was also distributed in the Carpathian refuge. Later on, the Crimean peninsula would also appear to be a possible glacial refuge of the red fox.In the last warmer complex of interstadials during the Pleni-Glacial (Hengelo-Denekamp, 38,000–25,000 BC) the red fox was distributed in central Europe. Its distribution during this epoch extended at least in part to southern England. The earliest well-dated records of V. vulpes in central Europe after the Maximum Glaciation lie between 14,000 and 13,500 BC. Already during the early Late-Glacial (13,500 BC) the red fox appeared in typical glacial faunal communities. A separation to glacial refugia was only possible for 10,000 years.During the last warmer Pleni-Glacial complex of interstadials (38,000–25,000 BC) in central Europe a sympatric distribution of the arctic fox (Alopex lagopus) and the red fox probably existed. During the Last Glacial Maximum (22,000–18,000 BC) the arctic fox was exclusively distributed in central Europe, outside of the refuges. The combined distribution of A. lagopus and V. vulpes during the Late-Glacial (15,000–9500 BC) in central Europe, with the probable exception of the Allerød, is precisely documented by sub-fossil assemblages.In the Pleni-Glacial the wolf Canis lupus was distributed in geographic regions that served as glacial refugia of more warm-climate adapted species. Concerning the wolf no drastic decrease of the distribution is assumed. The Holocene presence of C. lupus is probably not caused by recolonisation.

Zusammenfassung

Die Entwicklung der Canidenfauna Europas im Spätpleistozän und frühen HolozänIn den subfossilen Ablagerungen ist Vulpes vulpes in Europa mit 1553 Nachweisen das mit Abstand am häufigsten nachgewiesene Raubsäugetier. Allein in den Ablagerungen des Weichselglazials konnte der Rotfuchs bereits in 100 Fundkomplexen nachgewiesen werden. Als Glazialrefugium des Rotfuchses wird die Iberische Halbinsel sicher identifiziert. Eine Verbreitung der Art während des Kältemaximums wird außerdem auf der Apenninen-Halbinsel sowie der Balkan- Halbinsel vermutet. Außerdem liegen fundierte Fakten für die Annahme vor, dass V. vulpes im Karpatenrefugium verbreitet war. Auf der Halbinsel Krim scheint ein Glazialrefugium für des Fuchses möglich.Während des letzten wärmeren Interstadial-Komplexes im Hochglazial (Hengelo-Denekamp, ca. 38.000–25.000 v. Chr.) war Mitteleuropa vom Rotfuchs besiedelt. Die nördliche Arealgrenze der Art war innerhalb dieses Klimaabschnitts mindestens zeitweise bis nach Südengland ausgedehnt. Die frühesten, zeitlich relativ gut abgesicherten Nachweise von V. vulpes nach der Weichsel-Maximalvereisung in Mitteleuropa liegen etwa zwischen 14.000–13.500 v. Chr. Schon im frühen Spätglazial (ca. 13.500 v. Chr.) kam der Rotfuchs im nördlichen Mitteleuropa in typischen glazialen Faunengemeinschaften vor. Eine Disjunktion des Areals während der letzten Vereisung kann für höchstens 10.000 Jahre stattgefunden haben. Es wird angenommen, dass während des Hengelo-Deenekamp Interstadials ein sympatrisches Vorkommen von Eisfuchs Alopex lagopus und Rotfuchs V. vulpes in Mitteleuropa existierte. Nur zur Zeit des absoluten Kältemaximums (ca. 22.000–18.000 v. Chr.) war außerhalb der Refugialgebiete in Mitteleuropa ausschließlich A. lagopus verbreitet. Das gemeinsame Vorkommen (von A. lagopus und V. vulpes) während des gesamten Spätglazials in Mitteleuropa, wahrscheinlich mit Ausnahme des Allerød-Interstadials, ist präzise belegt.Während des Hochglazials war Canis lupus auch in geografischen Regionen verbreitet, die für an wärmeres Klima gebundene Tierarten den Charakter von Glazialrefugien hatten. Beim Wolf C. lupus kann keine extreme Arealverringerung während der Weichseleiszeit angenommen werden. Das holozäne Vorkommen von C. lupus in Mitteleuropa dürfte daher nicht generell auf eine Rekolonisation zurückzuführen sein.     

The long-term succession of cladoceran fauna and palaeoclimate forcing: A 14,600-year record from Plešné Lake,the Bohemian Forest

A sediment record of cladoceran remains was analysed in a 543 cm long core from Ple?né jezero (Ple?né Lake), the Bohemian Forest, Czech Republic. The core covered the time period from the Oldest Dryas to the present. Littoral and benthic Cladocera included 11 species of the family Chydoridae while three species (Bosmina longispina, Daphnia cf. pulicaria and D. cf. longispina) lived in the open water. Remains of Alona quadrangularis and Chydrous sphaericus occurred in the oldest sediment layers from the beginning of the Bølling chronozone. Bosmina longispina and Daphnia cf. pulicaria appeared about 400 years later. Inorganic sediment accumulated at a relatively high rate of ～ 90 mg cm^?2 yr^?1 at that time, diluting cladoceran remains and organic matter. Remains of Cladocera accumulated at 0.1 to 0.01 of the Holocene rate, making it difficult to observe effects of climate variation on the species structure of Cladocera in the Late-Glacial. Production of remains increased after warming during the Younger Dryas-Preboreal transition at ～11.6 kyr BP, and the proportion of littoral species increased. The most important change in cladoceran fauna occurred at ～10.5 kyr BP and culminated with afforestation of the catchment around 10.3 kyr BP. The domaination of Bosmina longispina lasted for ～250 years. The afforestation occurred concurrently with a decrease in lake water pH. Bosmina longispina and Daphnia cf. pulicaria disappeared, production of cladoceran remains decreased, but biodiversity increased. Planktonic Cladocera were represented by Daphnia cf. longispina during most of the rest of the Holocene. The production of Cladocera never reached the Preboreal level. Since ～ 5 cal. kyr BP, the inferred pH continuously decreased. The final decline was likely caused by cooling during the Little Ice Age and by sulphur emissions from ore smelting. The recent acidification of lake water and impoverishment of aquatic fauna was brought about by emissions of sulphur and nitrogen compounds in the 20^th century.     

Bosmina (Eubosmina) longicornis longicornis SCHOEDLER, 1866 (Crustacea,Cladocera: Bosminidae) from the Postglacial Sediments of the Neuendorfer See,East-Germany

Analyses were made of subfossil Eubosmina remains from the Lake Neuendorfer See, a lake in the middle part of the river Spree in the “Urstromtal” of Baruth situated in the eastern part of Germany. In addition to Bosmina (Bosmina) longirostris (O. F. M., 1785) Bosmina (Eub.) longicornis longicornis Schoedler, 1866 occured in the lake from the Boreal (sediment depth 15.85 m) to the recent surface layers of the core. Other eubosminids did not occur during the history of the Lake Neuendorfer See with the exception of few remains of B. (Eub.) longispina, which were detected in the lowermost layers of the core during the late Pleistocene. In the present-day plankton, Bosmina (Eub.) l. longicornis was the only eubosminid found in the Lake Neuendorfer See. During the long period between colonization during the Boreal to the present, no changes were detected in typical morphological features of B. (Eub.) l. longicornis. All remains of Eubosmina in the layers above 15.85 m belong undoubtedly to the same taxon. No signs of any morphological instability (other then ontogenetic and cyclomorphic formchanges) or “morphological transition” (Hofmann, 1977) to other taxa could be found. By using paleolimnological analyses, the named taxon has proven to be a “good” entity within the group of long-spined taxa of the subgenus Eubosmina.     

Fine sediment effects on feeding and growth in the invertebrate grazers Potamopyrgus antipodarum (Gastropoda,Hydrobiidae) and Deleatidium sp. (Ephemeroptera,Leptophlebiidae)

The influence of fine sediment (<63 m diameter) upon the assimilation rates of the snail Potamopyrgus antipodarum, and the mayfly Deleatidium sp. were determined by allowing individuals to feed upon ¹⁴C radiolabelled periphyton which had been contaminated with varying quantities of sediment (sediment:food ratios of: 0:1, 1:1, 5:1, 10:1, 50:1, 100:1 [dry weight]). For both grazers, the assimilation rate falls in direct proportion to the sediment fraction in the (sediment+food) matrix. In a second experiment the growth of P. antipodarum was monitored over 3 months when fed organic matter that had been contaminated with fine sediment at ratios of 0:1, 1:1, 5:1, 10:1, 50:1, 100:1, 500:1. In contrast to the monotonic relation between sediment and short-term assimilation, growth rates (mm shell height d^–1) were highest at intermediate levels of sediment contamination (5:1 and 10:1 by dry weight) and lowest in the treatment with no sediment added. Growth rates were significantly lower, and mortality high, at sediment:food contamination ratios above 50:1. The reasons for the contrast between the results from the short-term and the long-term experiments are unknown at present, but the fact that snail growth was greatest at intermediate levels of sediment contamination might indicate that they derive trace nutrients from ingested sediment.     

Origin and formation of the Spanish Imperial Eagle ( Aquila adalberti )

A review of the paleontological records of the Eastern Imperial Eagle (Aquila heliaca) and the Spanish Imperial Eagle (Aquila adalberti) in the context of the paleoecological environment in Eurasia during the Pleistocene and Holocene epochs is presented. The Eastern Imperial Eagle expanded its range in Eurasia during the last Pleistocenic glaciation favoured by the expansion of the steppes. The first records of Spanish Imperial Eagles are from the Late Pleistocene and Early Holocene in the eastern Iberian Peninsula, and their distribution seems to have been limited to the distribution areas of Mediterranean vegetation and the European rabbit. Individuals of migrant A. heliaca could have reached the Iberian Peninsula at the end of the Pleistocene–beginning of the Holocene. These individuals could have adapted to the Mediterranean ecosystem, subsequently specializing in a diet of rabbit, a prey which is in abundance all year round. Due to the availability of such prey, A. heliaca would become more sedentary. These individuals may have overcome their breeding phenology and paired up assortatively, becoming genetically separate from the migrant populations and initiating the speciation mechanisms for sympatry or parapatry that resulted in A. adalberti. This is one possible mechanism. These findings reported here support the recent age of divergence between both taxons, and the incipient speciation supports its taxonomical considerations as a semi-species. The study reported here complies with the current laws of Spain.     

Late-Glacial and Holocene Environmental History of an Oxbow Wetland in the Polabí Lowland (River Elbe,Czech Republic); a Context-Dependent Interpretation of a Multi-Proxy Analysis

This study presents a palaeoenvironmental reconstruction of an oxbow wetland covering the past 11,500 years. The origin of the oxbow lake and development of the floodplain wetland and changes of the surrounding vegetation are reconstructed using palaeobotanical analyses, radiocarbon dating, detailed sediment stratigraphy and micromorphology of samples taken from a former palaeomeander of the river Elbe in the Czech Republic. The sedimentary record of the section Chrast was chosen due to its exceptional position within the area of former oxbow lakes. Using a multi-proxy approach, we investigated how this environment reflected climatic changes during the Holocene. Our results show that the Chrast section covers the Late-Glacial to the Middle Holocene period, which is climatically very unstable and characterized by extensive vegetation and sedimentological changes. The macrofossil record provides detailed evidence of Allerød vegetation. The sedimentological record reflects changes in fluvial activity (meandering-braided transition in the channel pattern) during Late-Glacial/Holocene and postsedimentological changes (occurrence of a doplerite layer) in the middle Holocene. We follow three independent lines of interpretation: (a) a local autogenic environmental-succession process, (b) a regional process driven by climate change, and (c) the role of stochastic and indeterministic processes.     

Population dynamics of Bosmina longirostris (Crustacea: Cladocera) in Lake Kariba,Zimbabwe

The population dynamics of Bosmina longirostris in a large tropical reservoir, Lake Kariba, Zimbabwe, are described. Population density showed two peaks associated with periods of high nutrient fluxes. Fecundity was always low. Two eggs per female was the maximum ever recorded. Instantaneous rates of birth, death and population growth calculated from field data using the egg ratio method are discussed. The rate of biomass change fluctuated in a regular pattern, probably linked to food availability or predation by a clupeid, Limnothrissa miodon.     

Abrupt Changes in Bosmina (Cladocera,Crustacea) Assemblages During the History of the Ostrowite Lake (Northern Poland)

During the 10000-year history of the Ostrowite Lake, there have been several episodes of change in dominance amongst species of the genus Bosmina. The dominants were alternately B.longirostris and Eubosmina spp. Amongst the subgenus Eubosmina, two species prevailed in different periods:Bosmina coregoni and Bosmina reflexa. The first species, Bosmina coregoni, is characterized by long antennae and short carapace mucrones, while the second one, Bosmina reflexa, by short antennae and very long mucrones. Bosmina reflexa was dominant at the beginning of the lake's history (Preboreal, 10000--9000 BP) and during the early Subboreal Period (5000–3500 BP). Only a small number of remains of Bosmina longispina(Eubosmina spp.) were present along the entire profile. Such strong changes in the domination of Bosmina species were observed for the first time in the sediments of Polish lakes. A similar transition from one species to another has been described in a few German lakes and was linked to climate changes. However, the changes in the Ostrowite Lake do not correlate with climate changes, but most probably, with changes in the lake's trophic level. This is suggested by the simultaneous increase of Bosmina reflexa and a good indicator of eutrophy, Bosmina longirostris.     

Feeding habits of larval Mirogrex terraesanctae (Steinitz, 1952) in Lake Kinneret (Israel) I. Field study

Analysis of the food composition, distribution, lengths and dry weights of larval bleak, Mirogrex terraesanctae (Steinitz, 1952) in Lake Kinneret, Israel was conducted. Indices of electivity of ingested prey organisms were also determined. Larvae were surveyed throughout the 1989–90 reproductive seasons (Dec–Mar). Small larvae (<10.28 mm SL) preferentially select prey items smaller than 180 µ. Dominant zooplankters in the larval guts included: Bosmina longirostris, Ceriodaphnia reticulata and C. rigaudi, Asplanchna priodonita, Synchaeta oblonga, S. pectinata and juvenile cyclopoid copepods. Diaphanosoma brachiurum was rarely found (instars only) and no adult copepods were observed in larval guts. Some larvae specimens were found with up to 500 undigested (intact) accidentally ingested cells of Peridinium spp. per gut.     

Investigations into the late Pleistocene and Holocene history of vegetation and climate in Santa Catarina (S Brazil)

Palynological studies have been carried out on three highland peat bogs, and one situated on the Atlantic coastal plain. In the highlands, the late Pleistocene (14,000 - 10,000 uncal B.P.) vegetation was dominated by campos (grassland). Scattered stands of Araucaria forests were preserved in deep valleys. In the region of the sites at Morro da Igreja and Serra do Rio Rastro, the dominance of campos vegetation continued until about 1000 B.P. while at the Serra da Boa Vista site there was an expansion of Atlantic pluvial forest elements followed by Araucaria forests at the beginning of the Holocene. A general expansion of A. angustifolia, clearly related to a change towards an increasingly moist climate, can be dated to the present millenium. On the coastal plains, the late Pleistocene vegetation was dominated by Myrtaceae which were replaced by tropical taxa in the Holocene. The lowland profile (Poço Grande) also covers part of the upper Holocene, where the rich flora of the Atlantic pluvial forests can be characterized by taxa including Alchornea, Urticales and Rapanea. Close to the coring site, there was a repeated alternation between two different dune communities (4840 - 4590 B.P.), followed by a lake stage with aquatic plant succession (4590 - 4265 B.P.), plant communities dominated by Rapanea (4265 - 4230 B.P.) and the spread of Alchornea (4230 - 3525 B.P.). Late Pleistocene climate conditions (14,000 - 10,000 B.P.) can be described as cold and relatively dry, possibly including an equivalent of the Younger Dryas period. In the Holocene, there were changes from a warm and drier climate (10,000 -3000 B.P.) to a cool and more moist regime (ca. 3000 -ca. 1000 B.P.) and finally to a cool and very moist period (from around 1000 B.P.).     

Selective zooplankton predation by pre-adult roach (Rutilus rutilus): The size-selective hypothesis versus the visibility-selective hypothesis

Prey selection mechanisms of juveniles of the particulate feeding roach (Rutilus rutilus) were tested in bag experiments in lake Gjersjøn.Cladocerans and large developmental stages (cop. IV-ad.) of copepods were consumed in large numbers both in the bags added fish and in lake, while rotifers increased in numbers in bags added fish.The effect of fish predation on the small cladoceran Bosmina longirostris was tested by comparing morphological structures in fish-free bags and bags added fish.The results strongly support the visibility selective hypothesis, as eye-diameter became significantly smaller in bags added fish (P < 0.05, T-test), while body-size, length of antennae and mucro, frequency and number of eggs were slightly or unsignificantly correlated with presence or absence of fish.Further, while roach was found to consume large numbers of Bosmina longirostris, the far greater but nearly unpigmented Asplanchna priodonta was never consumed. Additionally, other data further supporting the visibility-selective hypothesis are discussed.     

Contaminated sediments in the Elbe estuary: Ecological and economic problems for the Port of Hamburg

The effects of food density on competition between Bosmina longirostris and Bosmina fatalis from Lake Kasumigaura were examined in the laboratory. When the animals were reared with a high concentration of Chlorella, B. fatalis, which is slightly larger than B. longirostris in body length, had larger brood sizes and a higher rate of population growth than B. longirostris. When the species were reared together at high food density, B. fatalis overcame B. longirostris. But B. longirostris won the competition at low food density.The effects of Microcystis on the competition were also examined. When the two species of Bosmina were reared in a mixture of Chlorella and Microcystis, the populations of both species hardly increased, although individual B fatalis showed slightly better individual growth and reproduction than B. longirostris. Decomposed Microcystis, however, was utilized well by both species.In Lake Kasumigaura, the decomposition of abundant Microcystis seemed to raise the food level, favouring B. fatalis over B. longirostris.     

The late Pleistocene/Holocene and recent Bosmina (Eubosmina) fauna (Crustacea: Cladocera) of the pre-alpine Starnberger See (FRG)

An analysis of the remains of Bosmina (Eubosmina) in a sedimentcore from the pre-alpine, mesotrophic Starnberger See showedthat the lake was inhabited by B. longispina since the OldestDryas. In the Subatlantic- -1900 years ago — the kesslerimorph of B. coregoni invaded the lake and both taxa have sinceco-existed. Although there was considerable morphological variation,B. longispina clearly differed from Circumbaltic populationsthrough most of the late Pleistocene and Holocene periods. Inthe recent Bosmina fauna of the lake two morphologically wellseparated taxa (B. longispina ruehei and a morph of B. coregoni)occur which differ clearly from the Bosmina remains found inthe core up to the uppermost sample from 7 cm sediment depth.B. coregoni f. kessleri appeared in the lake in a period whenit was supposedly still oligotrophic. The Bosmina successionobserved in the Starnberger See resembles the pattern foundin deep north German lakes.     

Holocene forest development in the central Scandes Mountains, Sweden

Pollen analyses of sediment cores from two small lakes within the boreal forest in the central Scandes Mountains help to elucidate the Holocene forest dynamics of the region. Analyses of pore/pollen grain diameter ratios of Alnus grains indicate the early Holocene presence of Alnus glutinosa in the study area. The results are discussed in conjunction with available pollen records to evaluate the importance of thermophilous trees during the early Holocene and to deduce the regional spread of Picea abies. Corylus avellana, Alnus glutinosa and Ulmus glabra were probably common constituents of the early Holocene forest. Tilia cordata may have occurred there as a rare tree. Pollen stratigraphies from the region do not indicate the occurrence of Quercus robur. The regional spread of Picea abies can be separated into two phases: a mid-Holocene establishment or first expansion of small outpost populations and a late-Holocene population expansion. The mid-Holocene shift in vegetation composition may have been caused by changes in the westerly airflow.     

The estimation of production and mortality ofBosmina longirostris (O. F. Müller) in the River Danube (Danubialia Hungarica,CIX)

Produced and eliminated biomass ofBosmina longirostris in the River Danube (Hungary) was estimated in 1982. An attempt was made to calculate the rate of immigration and mortality, taking into consideration the hydrological characteristics of the river. Production and immigration influence population change to about the same extent.     

Morphological variation in Bosmina longirostris (O.F. Müller, 1785) (Crustacea: Cladocera): consequence of cyclomorphosis or indication of cryptic species?

Samples of the polymorphic cladoceran Bosmina longirostris were collected in several lakes and ponds in Western Germany between 1993 and 1999. The shape of the first antennule was used as a qualitative criterion to classify 1241 individuals to three morphs (`longirostris', `cornuta', `pellucida') according to Lieder (Crustacea: Cladocera: Bosminidae. Stuttgart, Germany: Gustav. Fischer Verlag, 1996). Eight morphometric variables were subsequently measured in each individual to quantify size‐ and shape‐related features. Principal component and discriminant analyses were used to describe the morphological variation within and among the three morphs. Seasonal environmental changes modified several traits and thus, cyclomorphosis accounted for a high proportion of within‐morph variation. However, there was no gradual change from one morph to another. As well among‐morph variation was considerably greater than within‐morph variation. Consequently, the disagreement between the qualitative pre‐classification and the assignment basing on morphometric discriminant functions was low (4.6–12.0%). Considering that each morph is morphologically well‐defined, and that the different morphs coexisted over several generations in the same lake we conclude that they represent different species rather than variants of one polymorphic species. Therefore, we recognize beside the nominal taxon Bosmina longirostris ( 26 ) two more species: Bosmina cornuta ( 10 ) and Bosmina pellucida 30 .     

Effects of large Saduria entomon (Isopoda) on spatial distribution of their small S. entomon and Monoporeia affinis (Amphipoda) prey

We performed laboratory experiments to investigate the effects of predator avoidance and numerical effects of predation on spatial distribution of small Saduria entomon (Isopoda) and Monoporeia affinis (Amphipoda), with large S. entomon as predators. The horizontal distribution and mortality of the prey species, separately and together, were studied in aquaria with a spatial horizontal refuge. We also estimated effects of refuge on mortality of small S. entomon and M. affinis by experiments without the refuge net. In addition, we investigated whether predation risk from large S. entomon influenced the swimming activity of M. affinis, to clarify the mechanisms behind the spatial distribution. Both small S. entomon and M. affinis avoided large S. entomon. The avoidance behaviour of M. fffinis contributed about 10 times more to the high proportion in the refuge than numerical effects of predation. Due to the low mortality of small S. entomon the avoidance behaviour of this species was even more important for the spatial distribution. The combined effect of avoidance behaviour and predation in both species was aggregation, producting a positive correlation between the species in density. M. affinis showed two types of avoidance behaviour. In the activity experiments they reduced activity by 36% and buried themselves in the sediment. In the refuge experiments we also observed avoidance behaviour with the emigration rate from the predator compartment being twice the immigration rate. The refuge did not lower predation mortality in M. affinis, probably due to the small scale of the experimental units in relation to the mobility of the species. Predation mortality in small S. entomon was higher in absence of a refuge and especially high in absence of M. affinis.