CC BY
80
Arctic
Environmental Research
Arctic Environmental Research 18(2): 76-81
UDC 594. 1
DOI 10.3897/issn2541-8416.2018.18.2.76
Research Article 3
Molluscan fauna of the lower reaches of the Syoyakha River (Yamal Peninsula)
YuV Bespalaya1, OV Aksenova1, NA Zubriy1
1 N. Laverov Federal Center for Integrated Arctic Research, Russian Academy of Sciences, Severnaya Dvina Emb. 23, 163000 (Arkhangelsk, Russian Federation)
Corresponding author: Yulia Vladimirovna Bespalaya (jbespalaja@yandex.ru)
Academic editor: Aleksandr P. Novoselov ♦ Received 14 May 2018 ♦ Accepted 24 July 2018 ♦ Published 3 August 2018
Citation: Bespalaya YuV, Aksenova OV, Zubriy NA (2018) Molluscan fauna of the lower reaches of the Syoyakha River (Yamal Peninsula). Arctic Environmental Research 18(2): 76-81. https://doi.org/10.3897/issn2541-8416.2018.18.276
Abstract
The molluscan fauna of the Syoyakha (Zelenaya) River remain poorly explored even though the Syoyakha is one of the biggest rivers on the Yamal Peninsula. The Syoyakha River is remarkable for its high fish stocking capacity and it plays an important role in the seasonal distribution and migration of commercial fish species. Freshwater mollusks are known to be a major component of freshwater ecosystems and they make up a part of the diet of many commercially important fish species. The species composition of the mollusks inhabiting the lower reaches of the Syoyakha River has been studied. Five bivalve species of the family Sphaeriidae were found, namely Sphaerium corneum (Linnaeus, 1758), Pisidium casertanum (Poli, 1791), P. globulare (Clessin in Westerlund, 1873), P. lilljeborgi (Clessin in Esmark et Hoyer, 1886) and P. dilatatum (Westerlund, 1897). In general, the molluscan fauna of the lower reaches of the Syoyakha River are taxonomically poor, which can be considered typical of freshwater invertebrate communities living at high latitudes. Another reason for the decline in species diversity may lie in the absence of any large transit watercourse in the basin in question allowing northward dispersion of the mollusks. The average density of mollusks in the watercourse stretch under study varied from 98.9 ind./m2 to 620.5 ind./m2. P. globulare settlements had the highest recorded density of 1,442.9 ind./m2. The mollusks are confined to clayey, silty and sandy substrates with remnants of vegetation. The fauna is basically formed by widespread Palearctic and Holarctic mollusk species that have adapted to the extreme conditions of the Arctic. The findings may be used for hydrobiological and fishery characterization of the watercourse given that the recorded species of S. corneum, P. globulare, P. lilljeborgi, and P. dilatatum are a major food item for important fish species, such as cisco, vendace, char, muksun, etc.
Keywords
Yamal Peninsula, freshwater mollusks, Sphaeriidae, species diversity, Syoyakha River, Arctic.
Introduction
The ecosystems of the Yamal Peninsula are subject to an intensive anthropogenic influence connected with construction and operation of gas fields (Golovatin et al. 2010), hence there is a need to perform environmental monitoring in order to control these negative effects on water ecosystems (Bogdanov et al. 2012). Freshwater
mollusks are an important component of freshwater ecosystems and they often dominate in benthic communities (Sousa et al. 2011). Further, mollusks also make up a part of the diet of many commercially important fish species (Leshko 1998).
The first data concerning the composition of the molluscan fauna of water reservoirs on the Yamal Peninsula come from materials collected by the expedition that was
Copyright Bespalaya YuV et al. This is an open access article distributed under the terms of the Creative Commons Attribution License (CC-BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
organized by the Kuznetsov brothers in 1909 (Lindholm 1919). In the summer of 1964, the scientific research expedition of the ichthyological team of the Biology Institute of the Urals Branch of the USSR Academy of Sciences collected mollusks in the basin of the Syoyakha River (Khokhutkin 1966). New data on the species composition of freshwater mollusks were obtained later, during the study of the diet of fish species inhabiting the Yarroto, Neito and Polkurto water reservoirs (Khokhutkin 1969). A total of 16 species of freshwater mollusks were recorded on the peninsula (Khokhutkin 1969).
Many years of research studies of the freshwater mollusks of the Yamal Peninsula inhabiting the Yuribei River and Lake Yarroto that were undertaken by V.N. Dolgin (2001) are noteworthy among contemporary works in the literature. The gastropod fauna of the Schuchya River were studied in 2011 (Palatov and Vinarski 2012). The macro-zoobenthos, including the freshwater mollusks inhabiting a number of watercourses in Southern Yamal, has been evaluated (Palatov and Chertoprud 2012). The zooben-thos of water reservoirs and watercourses of the Setnaya, Ngoyakha and Yaroyakha Rivers that are located on the south-eastern part of the peninsula has been studied. The taxonomic composition of the invertebrate bottom fauna has been analyzed (Stepanov 2016, 2017).
However, the molluscan fauna of the Syoyakha (Zelena-ya) River remain poorly explored even though the Syoyak-ha is one of the largest rivers of the Yamal Peninsula. The watercourse is 165 km long and the watershed covers an area of 4,400 km2 (Bolshakov et al. 1995). The Syoyakha River is remarkable for its high fish capacity and plays an
important role in the seasonal distribution and migration of commercial fish species (Bogdanov et al. 2000).
The goal of this research was to study the fauna and to analyze the zoogeographical structure of the molluscan fauna in particular in the lower reaches of the Syoyakha (Zelenaya) River.
Materials and methods
The Yamal Peninsula is located the Northern part of Western Siberia in the central part of Russia. The Yamal Territory refers to the West Siberian plain (Morozova and Magomedova 2004). The surface dismembered quite strongly by valleys of the rivers, streams and lake hollows (Golovatin et al. 2009). The summers are short and cold, and the winters are windy and frosty. The average annual temperature in the South of Yamal (Salekhard) is -6.6 °C, and on the northern side it is -10.2 °C (Morozova and Magomedova 2004). The peninsula is located in the permafrost zone (Dobrinsky 1995).
The mollusk samples of the Yamal Peninsula were collected in the lower reaches of the Syoyakha (Zelenaya) River in July-August 2014 (Fig. 1). The Syoyakha is a plain river type with a low flow rate and its bed meanders strongly in the shallow and broad valleys (Dobrinsky 1995). The river originates from Lake Yambuto and runs into Obskaya Bay of the Kara Sea. Ice on most Yamal rivers is most likely to form in the second week of October (Do-brinsky 1995). The temperature dynamics in the Syoyakha River were measured at 60-minute intervals using TP-1
35°E 45°E 55°E 65°E 75°E 85°E 95°E
Fig. 1. The schematic sampling site map of the study area: A - the schematic study area map, B - sampling sites (the white markers correspond to blank samples (no mollusks found), the grey marker corresponds to samples in which mollusks were found), C - view of the Syoyakha River
temperature data loggers (TermoReg version 2.01.) between July 15, 2014 and August 30, 2014.
The benthic samples were collected using standard methods (Mordukhay-Boltovskoy 1975). Samples were washed using a hydrobiological sieve. The mollusks were fixed in 96% ethanol (Mordukhay-Boltovskoy 1975). A total of 1,886 mollusk specimens were collected.
The mollusks were identified according to a number of keys (Korniushin 1996, 2001; Gloer and Meier-Brook 2003). The justification of applying the traditional approach to determining genera within the Sphaeriidae family is provided by Bespalaya et al. (2017). Five major monophyletic lineages were originally assigned by Lee and O Foighil (2003) as genera: Sphaerium, Pisidium s. str., Cyclocalyx, Odhneripisidium, and Afropisidium. These were subsequently adopted by other phylogenetic studies on Sphaeriidae, but us subgenera (e.g., Clewing et al. 2013; BoEneck et al. 2016; Bespalaya et al. 2017). In some works, the phylogeny of Lee and O'Foighil (2003) was taken into account, but the genus Cyclocalyx Dall, 1903 has been replaced by Euglesa, Jenyns, 1832 following the principle of priority of publication (Gargominy et al. 2011; Bogatov and Prozorova 2017).
The specimens are kept in the collection of the Russian Museum of Biodiversity Hotspots (RMBH) of the N. La-verov Federal Center for Integrated Arctic Research, Russian Academy of Sciences (FCIARtic).
Results
The hydrochemical characteristics of the waters in the Syoyakha River are presented in Table 1. The waters in the river are weakly mineralized; the basic ion concentration is low. The average water temperature in the Syoyakha
River during the study period varied between 6.9 °C and 11.9 °C.
Fives mollusk species of the Sphaeriidae family were found in the lower reaches of the Syoyakha River during the present study (Fig. 2). The bivalve community was dominated by Pisidium globulare (Westerlund, 1873) (36.9%), P. lilljeborgi ranked second (Clessin in Esmark et Hoyer, 1886) (31.9%). The average density of mollusks varied between 98.9 ind./m2 and 620.5 ind./m2 (Table 2). The P. globulare settlements had the highest recorded density of 1,442.9 ind./m2. The mollusks are confined to clayey, sil-ty and sandy substrates with remnants of vegetation. The fauna of mollusks of the lower reaches of the Syoyakha River include the European and Western Siberian, Pale-arctic, Holarctic, and Cosmopolite species (Table 2).
Discussion
In general, the molluscan fauna of the lower reaches of the Syoyakha River are taxonomically poor compared to the watercourses in both the southern part of Western Siberia (Palatov and Vinarski 2012) and the subarctic zones of the tundra (Bolotov et al. 2014, Bespalaya et al. 2017). The environmental conditions in the Arctic are extreme for invertebrates (Chernov 2012). This is due to the low temperatures, high level of UV radiation and a content of organic and mineral substances that is often insufficient (Samchyshyna et al. 2008, Rautio et al. 2011). Another reason for the decline of the species diversity may lie in "the absence of any large transit watercourse in the basin in question allowing northward dispersion of the mollusk-cs" (Palatov and Vinarski 2012: p.160). It is noteworthy that, in our samples no gastropod species were found. Our data are in accordance with Khokhutkin (1966), who also
Table 1. Species composition and relative abundance of mollusk species in the Syoyakha River samples (Yamal Peninsula). Geographic distribution: PA - Palaearctic, H - Holarctic, C - Cosmopolite, EWS - Europe, Western Siberia.
Geographic Syoyakha River
distribution Average density (ind./m2)±SD Density, (ind./m2) min-max N, ind. N, %
Sphaerium corneum (Linnaeus, 1758) PA 164.8±125.3 14.3-435.7 300 15.9
Pisidium casertanum (Poli, 1791) C 257.1±175.4 107.1-450.0 108 5.7
P. globulare (Clessin in Westerlund, 1873) EWS 620.5±504.1 71.4-1442.9 695 36.9
P. lilljeborgi (Clessin in Esmark et Hoyer, 1886) H 391.6±419.4 7.1-978.6 603 31.9
P. dilatatum (Westerlund, 1897) PA 98.9±119.4 14.3-450.0 180 9.5
Total 1.886
Note: N, ind. - number of individuals representing the species in the collection, N, % - proportion of individuals representing the species in the collection, SD - standard deviation.
Table 2. Hydrochemical characteristics of the Syoyakha River (Yamal Peninsula, July-August 2014)
Parameters Syoyakha River
K+ (mg/l) 0.53±0.08
Na+ (mg/l) 2.8±0.2
Mg2+ (mg/l) 1.2±0.09
CI- (mg/l) 3.54±0.3
SO42- (mg/l) 1.12±0.08
Ca2+ (mg/l) 2.2±0.2
Fig. 2. The external morphology of the shell (left), beak and hinge of the right and left valves (right) of mollusks from the lower reaches of the Syoyakha River: A - Sphaerium corneum, B - Pisidium casertanum, C - P globulare, D - P lilljeborgi, E - P dilatatum
did not discover mollusks of this class in the Syoyakha River. At the same time and by the same author the Gy-raulus acronicus and Aplexa elongata were recorded in the swamps of the Syoyakha River basin (Khokhutkin 1966). As a whole, several species of gastropod were registered in the reservoirs of Middle and Northern Yamal (Dolgin 2001, Stepanov 2016, 2017) and twenty species were registered on the Southern Yamal (Palatov and Vinarski 2012).
The reasons for the absence of the gastropod species in the investigated part of the river will require additional studies. It can be assumed that in the lower reaches of the Syoyakha River provide an unsuitable habitat for gastropods.
In general, the bivalves from Syoyakha River are widespread in the Holarctic and Palearctic regions (Table 1). According to data in the literature, the Sphaeriidae family often dominate in high-latitude water reservoirs (Ash-worth and Preece 2003, Bespalaya 2014). Consequently, it was established that P. casertanum and P. globulare were dominated in the lakes of the Vaigach Island (Bespalaya 2014, Bespalaya et al. in press). The data also conform to the observations of Dolgin (2001), who notes that P. dilatatum, P. globulare and P. lilljeborgi are most abundant in the Arctic. Some authors believe that the Sphaeriidae are adapted to low temperatures (Ashworth and Preece 2003,
Guralnick 2005), which is why they inhabit the Arctic water reservoirs.
Conclusion
According to our records, the molluscan fauna of the Syoyakha River are represented by five species of freshwater bivalves of the Sphaeriidae family. The bivalves of the Syoyakha River are widespread Palearctic and Holarctic mollusk species that have adapted to the conditions at high latitudes. The results of research may be used for hydrobiological and fishery characterization of
the watercourse given that the recorded species of Sp-haerium corneum, Pisidium globulare, P. lilljeborgi, and P. dilatatum are a major food item for commercially important fish species, such as cisco, vendace, char, muksun, etc. (Dolgin 2001).
Acknowledgements
This research was supported by the Program of the Presidium of the Urals Branch of the Russian Academy of Sciences No. 0409-2018-0148) and grant No. 17-44-290016 р_а of the Russian Foundation for Basic Research.
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