Issue
Knowl. Manag. Aquat. Ecosyst.
Number 422, 2021
Topical issue on Crayfish
Article Number 27
Number of page(s) 7
DOI https://doi.org/10.1051/kmae/2021026
Published online 07 July 2021

© M.-I. Groza et al., Published by EDP Sciences 2021

Licence Creative CommonsThis is an Open Access article distributed under the terms of the Creative Commons Attribution License CC-BY-ND (https://creativecommons.org/licenses/by-nd/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. If you remix, transform, or build upon the material, you may not distribute the modified material.

Freshwater crayfish are an old group of invertebrates, with different adaptive potentials (Reynolds et al., 2013). They generally inhabit fresh waters with heterogeneous substrate that provides shelters (Füreder et al., 2006), and are mostly negatively influenced by organic and inorganic pollutants (Reynolds et al., 2013). Climate change, deforestation, habitat deterioration and introduction of the alien invasive crayfish species to their environment negatively affect their chances of survival (Holdich et al., 2009).

The stone crayfish (Austropotamobius torrentium) is one of the most threatened crayfish species in Europe (Streissl and Hodl, 2002), mostly due to human impact onto their natural habitats (Maguire et al., 2018). This species is a complex of genetically divergent phylogenetic groups (Klobučar et al., 2013; Pârvulescu et al., 2019; Lovrenčić et al., 2020), with typically high environmental requirements. It is most commonly present in cold (Souty-Grosset et al., 2006), well-oxygenated waters (Pârvulescu et al., 2011), with moderate current velocities (Pockl and Streissl, 2005). It mostly prefers habitats with hard substrate (Bohl, 1988) and a high number of suitable stone shelters (Vlach et al., 2009; Pârvulescu et al., 2016). Due to their environmental requirements and negative anthropogenic pressure onto their habitats, this species has a fragmented dispersal across its distribution range (Kouba et al., 2014). According to recent studies (Klobučar et al., 2013; Pârvulescu et al., 2019, Lovrenčić et al., 2020), A. torrentium most likely began its spread from the Dinarids (in early Miocene) towards eastern and southern Europe via pre-glacial and post-glacial dispersal routes, later linked to the Danube River and its tributaries that enabled its dispersal into central Europe (Klobučar et al., 2013), reaching its northernmost limits of distribution in the Rhine and Elbe River Basins (Petrusek et al., 2017).

Previous molecular studies established that the population of the stone crayfish in the south-western part of the Carpathians in Romania belongs to the central-south European (CSE) phylogroup sensu Klobučar et al. (2013). Stone crayfish migrated to that region via the Danube River system (Pârvulescu et al., 2019; Lovrenčić et al., 2020), and survived Pleistocene glaciations due to suitable refuge habitats (Pârvulescu et al., 2013). Currently, these populations' distribution is limited to mountainous and sub-mountainous karstic regions (Pârvulescu et al., 2013, 2020). Presently, their survival is confined by the presence of co-occurring species: Astacus astacus and recently introduced Faxonius limosus (Pârvulescu et al., 2009, 2011). The later species, is also a carrier and a spreading vector of the pathogen Aphanomyces astaci that is a causative agent of crayfish plague (Kozubíková et al., 2011), disease that is most frequently lethal for native crayfish species and subsequently poses one of the most serious threats to their survival (Jussila et al., 2017). Faxonius limosus carrying the pathogen has colonised a long stretch of the Danube River in Romania (Pârvulescu et al., 2012), but, to our knowledge, there is no published evidence about its contact with the populations of A. torrentium in the small tributaries of the Danube, nor is there any mention of the A. astaci infection within the stone crayfish populations from the aforementioned streams.

In this study, we present the first report of an A. torrentium population in the lowlands of Romania (an altitude of 40–50 m/asl). This population was discovered in 2018 in a small stream, in the Blahnița Plain, near Țigănași Village, approximately 50 km away from the mountains and the karstic habitats (Fig. 1). This stream is a small tributary of the Danube River and is connected to a series of irrigation channels. It flows into the Danube River 2.2 km downstream from Țigănași Village (Fig. 2). The last 500 m of the stream (section WSWC in Fig. 2), close to its mouth, possess conditions similar to typical stone crayfish habitat, with coarse sand and gravel, small to medium sized stones as a substrate and many larger stones, randomly spread throughout the stream. Upstream part of this stream is different (section WSHC in Fig. 2); a smoother substrate of sand with silt and steeper banks with tree roots rising from the water. This, approximately 4.5 km stretch of the stream (sections: WSWC, WSHC, Fig. 2), is surrounded by an alder grove. The crayfish searches were made only in the last two downstream sections (WSWC, WSHC) because section BSWC, situated upstream from WSWC and WSHC, was lacking tree coverage and was vastly affected by agriculture. Crayfish were caught only in the WSHC section of the stream with no recorded findings in the WSWC section, even though the conditions in WSWC section seem to be more suitable for this species. Five, apparently healthy looking, individuals and nine in poor health condition (limp or dead), were caught. The crayfish were captured by hand and were 7–10 cm long (total length, from the tip of the rostrum until the end of telson).

Samples (the distal segment of pereiopod five) for mtDNA COI analysis were taken from the healthy crayfish. Since crayfish in the poor health condition showed gross signs of crayfish plague (numerous melanisations on the carapace and pereiopods), we also sampled them/removed them from the stream for later laboratory analyses. Both sample types were preserved in the 95% alcohol until laboratory processing.

In order to establish crayfish phylogenetic position samples were processed and analysed according to procedure described in Lovrenčić et al. (2020). Obtained COI sequences were collapsed into already described haplotype AT108 that belongs to CSE phylogroup sensu Klobučar et al. (2013) (Appendix 1).

In order to test sampled tissues for A. astaci we followed procedure of Pavić et al. (2020). Analysis showed that sampled stone crayfish were infected by A. astaci and their poor health status and observed mass mortality was a consequence of crayfish plague outbreak. The pathogen load was level A2 what disabled genotyping (Vrålstad et al., 2009).

The search for this A. torrentium population was repeated twice during October (mating time/period of crayfish high activity) 2020, but not a single crayfish was captured. Furthermore, 4 similar looking streams in the proximity were also thoroughly searched for the presence of the crayfish (Fig. 1), with the same outcome. Even though, three out of the four additional streams run directly into the Danube River (where F. limosus was observed ‑ personal observations), there were no records of this invasive species within any of them. This absence of crayfish in all of these four additional streams is most probably linked to the fine grain substrate, the high velocity shallow water throughout most of the watercourses and the lack of suitable shelters or banks suitable for burrowing. Also, crayfish absence could have been a consequence of anthropogenic pressure onto the habitat since these streams are surrounded by settlements and agriculture land.

Guarding in mind previously adduced, a question that arises is: How did the population of A. torrentium get to the stream near Țigănași? Their presence in Romania is related to their past migrations in the Miocene-Pleistocene period, when they also colonised the southern part of the Carpathians through the Danube River and its tributaries (Lovrenčić et al., 2020; Pârvulescu et al., 2020). Thus, the most probable explanation for their discovery away from the expected areas could be the close relation of this species to the Danube River system. Stone crayfish populations might have been widespread in the streams of this area, but only the Țigănași population survived.

This claim is also supported by the molecular phylogenetic analysis (Appendix 1). This population is part of the CSE clade sensu Klobučar et al. (2013), together with all the stone crayfish populations within the southern Carpathians, in Romania (Pârvulescu et al., 2020), and are also closely related to some populations in Croatia (Lovrenčić et al., 2020). The Danube River changed its course throughout the Pleistocene period, starting from its most north-eastern location in the Gȕnz ice age and reaching its most south-western position (the current location) after the last glaciation (Würm) (Răducă et al., 2019). The Danube might have played an essential dualistic role in the spread of the crayfish, firstly, by acting as a refuge during the glaciations and secondly, by being a strong barrier in the migration path of the animals coming from the Carpathians, in the north. Thus, the A. torrentium population near Țigănași might have been a relic of the past populations that found refuge in the lower and probably warmer area, of southern Romania. Similar patterns of settling into lower elevations with a milder climate, during the ice ages as a survival mechanism/strategy, were also recorded for numerous plant and animal taxa. For example, trees from genus Fagus can be found here, at lower altitudes than expected (Paşcovschi, 1967). Also, species classified as mountainous, like some terrestrial isopods, Hyloniscus transsilvanicus and Ligidium germanicum (Ferenţi and Covaciu-Marcov, 2014) and Salamandra salamandra (Covaciu-Marcov et al., 2017), were also found in the Blahnița Plain region. Another important finding that supports our hypothesis is the presence of Mesoniscus graniger (Ferenți and Covaciu-Marcov, 2018) in the Blahnița Plain. This isopod species was thought to be related only to the caves in the mountainous karstic region, until it was discovered in the lowlands. The presence of Darevskia praticola in the open areas near streams of this region (Covaciu-Marcov et al., 2009), is also very important, proving that these areas used to be covered with forests, that are known as factors that enable stable conditions in freshwater habitats (Beschta, 1991).

And yet we cannot rule out possibility that the Țigănași population was of anthropogenic origin, but we could not find any written evidence in the literature that would support this hypothesis.

The presence of A. astaci in the studied stream was established, but pathogen level was too low and we could not determine its genotype. We can only presume that it belongs to Or genotype (haplogroup E) that is connected to the spiny-cheek crayfish (Kozubíková et al., 2011) distributed in the vicinity (the Danube River). Infection could only have occurred recently, since F. limosus was seen in 2015 (Covaciu-Marcov, personal communication) at Portile de fier II, a village located on the bank of the Danube River, 13 km downstream from the studied stream. Aphanomyces astaci have reached Drobeta-Turnu Severin in 2014 (Pârvulescu et al., 2015), and although there are no recently published updates on the plague spread/distribution, based on the distribution of the spiny-cheek crayfish, we can assume that the plague occurred at the same time as the invader near Țigănași. The spread of the infection into the tributaries is not unexpected (Jussila et al., 2015), taking into consideration that contact with any carrier of A. astaci zoospores (crayfish or fish) or fishing equipment could cause a crayfish plague outbreak (Schrimpf et al., 2012; Maguire et al., 2016).

A. torrentium individuals from the mouth of the stream, into the Danube River, might have come into contact with crayfish or other pathogen carriers and become infected first. Consequently, they also died first, explaining the lack of the crayfish in the WSWC section of the stream. The explanation for the lack of F. limosus in the stream may be linked to the size of the waterbody, as these crayfish were rarely seen entering and spreading upstream small tributaries (Petrusek et al., 2006).

Our data indicated that A. torrentium probably had a historically wider distribution in Romania. Thus, we can infer that the populations here did not only survive in areas with limestone or karst during the Pleistocen glaciations (Pârvulescu et al., 2013). It is possible that the studied population survived until 2018 only by chance, as they only occupied a segment of the stream (4.5 km long) that was not heavily affected by agricultural activity. But unfortunately, isolation, all the outside pressures and lastly, the crayfish plague have led to their demise.

Our report highlights the vulnerability of isolated relic populations in the face of outside stressors, both biotic (A. astaci) and abiotic (anthropogenic pressure onto the freshwater habitats) that frequently lead to their demise.

Acknowledgements

This work was funded by Project 123008, “SmartDoct − High quality programmes for doctoral and post-doctoral students of Oradea University, for the increase of relevance in research and innovation, in the context of the regional economy”, project financed by Human Capital Operational Programme 2014‑2020 (for the research carried out by the Romanian team: Marius-Ioan Groza, Diana Cupșa), also it was partially funded by the Croatian Science Foundation (for the research carried out by the Croatian team: CLINEinBIOta − IP-2016-06-2563 to Ivana Maguire, ESF − DOK-2018-01-9589 to Leona Lovrenčić). We would like to thank Adam Peter Maguire for English language editing, and anonymous reviewers for their constructive criticisms.

Appendix 1

thumbnail Appendix 1

Phylogenetic tree of A. torrentium based on COI data obtained through Bayesian analysis performed in MrBayes 3.2.6 (Ronquist et al., 2012). The optimal model of nucleotide evolution for COI data set was HKY + I + G, selected under the Bayesian information criterion (BIC) using the jModelTest 2.1.10. (Darriba et al., 2012). The BA priors were set according to the suggested model; two separate runs with four Metropolis-coupled Monte Carlo Markov chains (MMCM) were performed for 10,000,000 generations, and trees were sampled every 1,000 generations. After checking congruence (ESS values > 200) with Tracer v1.7.1 (Rambaut et al., 2018), the first 25% of sampled trees were eliminated as burn-in, and a tree was constructed, with nodal values representing the posterior probabilities. Numbers at the nodes indicate Bayesian posterior probabilities (values > 0.91 are indicated). New Romanian sequences belonging to haplotype AT108 are indicated in red colour. Phylogroups are represented by different colour: black − central and south-eastern Europe (CSE), blue − Gorski Kotar (GK), purple − Lika and Dalmatia (LD), orange − Žumberak, Plitvice and Bjelolasica (ŽPB), pink − southern Balkans (SB), green − Banovina (BAN), red − Zeleni Vir (ZV), gray − Apuseni Mountain (APU) and turquoise blue − Kordun (KOR).

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Cite this article as: Groza M-I, Cupșa D, Lovrenčić L, Maguire I. 2021. First record of the stone crayfish in the Romanian lowlands. Knowl. Manag. Aquat. Ecosyst., 422, 27.

All Figures

thumbnail Fig. 1

The map was made using QGIS 3.16.1-Hannover version and GIMP 2.10.22 version. It was designed by the superimposition of the A. torrentium distribution map from Pârvulescu et al. (2020) and the karstic structures map from Onac and Goran (2019).

In the text
thumbnail Fig. 2

The map of the studied stream containing the most important roads that pass over it and the manmade artificial channels it connects with; WSWC − wooded section without crayfish; WSHC − wooded section harbouring crayfish; BSWC − barren section without crayfish.

In the text
thumbnail Appendix 1

Phylogenetic tree of A. torrentium based on COI data obtained through Bayesian analysis performed in MrBayes 3.2.6 (Ronquist et al., 2012). The optimal model of nucleotide evolution for COI data set was HKY + I + G, selected under the Bayesian information criterion (BIC) using the jModelTest 2.1.10. (Darriba et al., 2012). The BA priors were set according to the suggested model; two separate runs with four Metropolis-coupled Monte Carlo Markov chains (MMCM) were performed for 10,000,000 generations, and trees were sampled every 1,000 generations. After checking congruence (ESS values > 200) with Tracer v1.7.1 (Rambaut et al., 2018), the first 25% of sampled trees were eliminated as burn-in, and a tree was constructed, with nodal values representing the posterior probabilities. Numbers at the nodes indicate Bayesian posterior probabilities (values > 0.91 are indicated). New Romanian sequences belonging to haplotype AT108 are indicated in red colour. Phylogroups are represented by different colour: black − central and south-eastern Europe (CSE), blue − Gorski Kotar (GK), purple − Lika and Dalmatia (LD), orange − Žumberak, Plitvice and Bjelolasica (ŽPB), pink − southern Balkans (SB), green − Banovina (BAN), red − Zeleni Vir (ZV), gray − Apuseni Mountain (APU) and turquoise blue − Kordun (KOR).

In the text

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