Alien Invertebrates and Fish in European Inland Waters
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Cladocera: Anomopoda: Daphniidae) from the Lower Cretaceous of Australia
Palaeontologia Electronica palaeo-electronica.org Ephippia belonging to Ceriodaphnia Dana, 1853 (Cladocera: Anomopoda: Daphniidae) from the Lower Cretaceous of Australia Thomas A. Hegna and Alexey A. Kotov ABSTRACT The first fossil ephippia (cladoceran exuvia containing resting eggs) belonging to the extant genus Ceriodaphnia (Anomopoda: Daphniidae) are reported from the Lower Cretaceous (Aptian) freshwater Koonwarra Fossil Bed (Strzelecki Group), South Gippsland, Victoria, Australia. They represent only the second record of (pre-Quater- nary) fossil cladoceran ephippia from Australia (Ceriodaphnia and Simocephalus, both being from Koonwarra). The occurrence of both of these genera is roughly coincident with the first occurrence of these genera elsewhere (i.e., Mongolia). This suggests that the early radiation of daphniid anomopods predates the breakup of Pangaea. In addi- tion, some putative cladoceran body fossils from the same locality are reviewed; though they are consistent with the size and shape of cladocerans, they possess no cladoceran-specific synapomorphies. They are thus regarded as indeterminate diplostracans. Thomas A. Hegna. Department of Geology, Western Illinois University, Macomb, IL 61455, USA. ta- [email protected] Alexey A. Kotov. A.N. Severtsov Institute of Ecology and Evolution, Leninsky Prospect 33, Moscow 119071, Russia and Kazan Federal University, Kremlevskaya Str.18, Kazan 420000, Russia. alexey-a- [email protected] Keywords: Crustacea; Branchiopoda; Cladocera; Anomopoda; Daphniidae; Cretaceous. Submission: 28 March 2016 Acceptance: 22 September 2016 INTRODUCTION tions that the sparse known fossil record does not correlate with a meager past diversity. The rarity of Water fleas (Crustacea: Cladocera) are small, the cladoceran fossils is probably an artifact, a soft-bodied branchiopod crustaceans and are a result of insufficient efforts to find them in known diverse and ubiquitous component of inland and new palaeontological collections (Kotov, aquatic communities (Dumont and Negrea, 2002). -
Further Expansion of the Genus Cercopagis (Crustacea, Branchiopoda, Onychopoda) in the Baltic Sea, with Notes on the Taxa Present and Their Ecology
Hydrobiologia 429: 207–218, 2000. 207 © 2000 Kluwer Academic Publishers. Printed in the Netherlands. Further expansion of the genus Cercopagis (Crustacea, Branchiopoda, Onychopoda) in the Baltic Sea, with notes on the taxa present and their ecology Elena Gorokhova1;∗, Nikolai Aladin2 & Henri J. Dumont3 1Department of Systems Ecology, Stockholm University, 109 61 Stockholm, Sweden Present address: Department of Biology, Arizona State University, Tempe, U.S.A. Fax: [+1] 480-965-2519. E-mail: [email protected] 2Zoological Institute, Russian Academy of Science, 199034 St. Petersburg, Russia 3Laboratory of Animal Ecology, University of Ghent, B-9000 Ghent, Belgium Received 5 May 1999; in revised form 10 September 1999; accepted 20 September 1999 Key words: Cercopagis, invasion, Baltic Sea, depth, temperature, salinity, morphological variations Abstract The onychopod cladoceran Cercopagis that recently invaded the Baltic Sea is reported from new zones of the north- ern Baltic proper. Because of successful survival and an expanding distribution range, the addition of Cercopagis to the Baltic fauna is considered to be permanent. What has previously been cited as Cercopagis pengoi encompasses the morphology of several other species, subspecies and forms. Either a number of morphologically similar species is present, or there is a number of spurious species in Cercopagis. The last hypothesis is favoured. The spatial distribution pattern of Cercopagis, as well as that of total zooplankton, was correlated with depth. Deep (>100 m) and shallow (<10 m) stations had significantly lower abundance than stations of intermediate depth (<100 m). An overview of the distribution of C. pengoi group in fresh and brackish waters suggests a high tolerance to environmental factors, but with differences among taxa. -
Annotated Checklist of Chinese Cladocera (Crustacea: Branchiopoda)
Zootaxa 3904 (1): 001–027 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2015 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3904.1.1 http://zoobank.org/urn:lsid:zoobank.org:pub:56FD65B2-63F4-4F6D-9268-15246AD330B1 Annotated Checklist of Chinese Cladocera (Crustacea: Branchiopoda). Part I. Haplopoda, Ctenopoda, Onychopoda and Anomopoda (families Daphniidae, Moinidae, Bosminidae, Ilyocryptidae) XIAN-FEN XIANG1, GAO-HUA JI2, SHOU-ZHONG CHEN1, GONG-LIANG YU1,6, LEI XU3, BO-PING HAN3, ALEXEY A. KOTOV3, 4, 5 & HENRI J. DUMONT3,6 1Institute of Hydrobiology, Chinese Academy of Sciences, 7# Southern Road of East Lake, Wuhan, Hubei Province, 430072, China. E-mail: [email protected] 2College of Fisheries and Life Science, Shanghai Ocean University, Shanghai 201306, China 3 Department of Ecology and Institute of Hydrobiology, Jinan University, Guangzhou 510632, China. 4A. N. Severtsov Institute of Ecology and Evolution, Leninsky Prospect 33, Moscow 119071, Russia 5Kazan Federal University, Kremlevskaya Str.18, Kazan 420000, Russia 6Corresponding authors. E-mail: [email protected], [email protected] Abstract Approximately 199 cladoceran species, 5 marine and 194 freshwater and continental saltwater species, live in China. Of these, 89 species are discussed in this paper. They belong to the 4 cladoceran orders, 10 families and 23 genera. There are 2 species in Leptodoridae; 6 species in 4 genera and 3 families in order Onychopoda; 18 species in 7 genera and 2 families in order Ctenopoda; and 63 species in 11 genera and 4 families in non-Radopoda Anomopoda. Five species might be en- demic of China and three of Asia. -
The Zoocenosis of the Aral Sea: Six Decades of Fast-Paced Change
Environmental Science and Pollution Research https://doi.org/10.1007/s11356-018-3807-z REVIEW ARTICLE The zoocenosis of the Aral Sea: six decades of fast-paced change Nikolay Vasilevich Aladin1 & Valentina Ivanovna Gontar1 & Ljubov Vasilevna Zhakova1 & Igor Svetozarovich Plotnikov1 & Alexey Olegovich Smurov1 & Piotr Rzymski2 & Piotr Klimaszyk3 Received: 29 June 2018 /Accepted: 19 November 2018 # The Author(s) 2018 Abstract During the last six decades, the water level of the Aral Sea, once one of the largest lakes in the world, has experienced a major human-driven regression followed by significant changes in salinity. These fast-paced alterations were initiated by the diversion of two rivers—the Amu Darya and Syr Darya—key players in the regulation of the water balance of the Aral Sea. Consequently, biological modifications took place leading to severe changes of the zoocenosis. This paper reviews the changes that have affected communities of fish and aquatic invertebrates in the Aral Sea since the 1950s. The reported alterations in biodiversity not only represent a natural response to a decrease in water level and a subsequent increase in salinity but also effects of non- native species introduction. The future prospects for invertebrates and fish in the Aral Sea, assuming that initiated restoration work is continued, are also discussed in this paper. Keywords Aral Sea . Ecological disaster . Ichthyofauna . Aquatic macroinvertebrates . Aquatic restoration Introduction largelyexceededbyevaporation,bothrivers,theonlysur- face water inflows -
Population Dynamics of Pseudevadne Tergestina (Branchiopoda: Onychopoda) in Guanabara Bay, Brazil
713 Vol.47, n. 5 : pp. 713-723, September 2004 ISSN 1516-8913 Printed in Brazil BRAZILIAN ARCHIVES OF BIOLOGY AND TECHNOLOGY AN INTERNATIONAL JOURNAL Population Dynamics of Pseudevadne tergestina (Branchiopoda: Onychopoda) in Guanabara Bay, Brazil Andrea Marazzo and Jean Louis Valentin* Departamento de Biologia Marinha; Instituto de Biologia; Universidade Federal do Rio de Janeiro; CCS; Bl. A; [email protected]; 21949-900; Rio de Janeiro - RJ - Brazil ABSTRACT Populations of Pseudevadne tergestina were studied in Guanabara Bay, southeastern Brazil, to assess temporal variations in density and population dynamics. Data on temperature, salinity and zooplankton samples were taken from the superficial water of a fixed station, every 3 - 4 days, from February 2 through August 1, 2000. The highest abundance of this species was observed in March, when densities varied widely, from 20 to 600 ind. m-3. Population parameters were calculated, such as birth rate (from 0.25 to 0.90 ind.-1.day-1), growth rate (from -1.30 to 2.09 day-1 ) and death rate ( from -1.6 to 1.9 day-1 ) Start of population could be attributed to the increase of temperature and to the hatching of resting eggs. The population collapsed in fall-winter, as result from the combined effects of different factors: decrease of water temperature (from 27oC to 21oC) influencing egg development time (from 2.27 to 3.28 days); predation pressure by chaetognaths (Max. 100 ind. m-3 ) and switch of population from parthenogenic to sexual reproduction. Horizontal transport of water by tidal currents contributed partially to the reduction of population density. -
ERSS-Fishhook Waterflea (Cercopagis Pengoi)
Fishhook Waterflea (Cercopagis pengoi) Ecological Risk Screening Summary U.S. Fish & Wildlife Service, February 2011 Revised, September 2017 Web Version, 11/30/2017 Photo: J. Liebig, NOAA GLERL. 1 Native Range and Nonindigenous Occurrences Native Range From Benson et al. (2017): “Black, Caspian, Azov, and Aral seas of Europe and Asia (Makarewicz et al. 2001)” Status in the United States From Benson et al. (2017): “Great Lakes Region Lake Ontario in 1998, Lake Erie in 2002 (Presque Isle), Lake Huron in 2002 (USEPA 2008), Lake Michigan in 1999 (Charlebois 2001), Finger Lakes et al. (Canandaiga, Cayuga, Keuka, Cross, Otisco, Owasco, and Seneca lakes) of New York. In the summer of 2001, C. pengoi was found in Muskegon Lake east of Lake Michigan (Therriault et al. 2002). A single specimen was collected from Lake Superior in 2003, but the species is not believed to be established there.” “Considered established in Lake Ontario, establishing itself quickly (similar to the invasion patterns in Europe) in the other Great Lakes (except L. Huron and Superior) and other inland lakes due to recreational boat traffic and other human activities (USEPA 2008).” 1 Means of Introduction into the United States From Benson et al. (2017): “Ballast water, boating” From Birnbaum (2011): “The colonization of North America by Cercopagis pengoi appears to be a secondary introduction from the Baltic Sea via ballast water (Cristescu et al. 2001).” Remarks From Benson et al. (2017): “According to the EPA's GARP model, C. pengoi, a free-swimming macroinvertebrate, would likely find suitable habitat throughout the Great Lakes region, except for the deeper waters of Lake Superior. -
Crustacea, Branchiopoda, Onychopoda) in the Baltic Sea, with Notes on the Taxa Present and Their Ecology
Hydrobiologia 429: 207-218,2000. © 2000 Kluwer Academic Publishers. Printed in the Netherlands. Further expansion of the genus Cercopagis (Crustacea, Branchiopoda, Onychopoda) in the Baltic Sea, with notes on the taxa present and their ecology Elena Gorokhova1*, Nikolai Aladin2 & Henri J. Dumont3 1Department of Systems Ecology, Stockholm University, 109 61 Stockholm, Sweden Present address: Department of Biology, Arizona State University, Tempe, U.S.A. Fax: [+1]480-965-2519. E-mail: elenag@ imap1.asu.edu 2Zoological Institute, Russian Academy of Science, 199034 St.Petersburg, Russia 3 Laboratory of Animal Ecology, University of Ghent, B-9000 Ghent, Belgium Received 5 May 1999: in revised form 10 September 1999: accepted 20 September 1999 Key words: Cercopagis, invasion, Baltic Sea, depth, temperature, salinity, morphological variations Abstract The onychopod cladoceran Cercopagis that recently invaded the Baltic Sea is reported from new zones of the northern Baltic proper. Because of successful survival and an expanding distribution range, the addition of Cercopagis to the Baltic fauna is considered to be permanent. What has previously been cited as Cercopagis pengoi encompasses the morphology of several other species, subspecies and forms. Either a number of morphologically similar species is present, or there is a number of spurious species in Cercopagis. The last hypothesis is favoured. The spatial distribution pattern of Cercopagis, as well as that of total zooplankton, was correlated with depth. Deep (> 100 m) and shallow (<10 m) stations had significantly lower abundance than stations of intermediate depth (<100 m). An overview of the distribution of C. pengoi group in fresh and brackish waters suggests a high tolerance to environmental factors, but with differences among taxa. -
Orden ONYCHOPODA Manual
Revista IDE@ - SEA, nº 70 (30-06-2015): 1–6. ISSN 2386-7183 1 Ibero Diversidad Entomológica @ccesible www.sea-entomologia.org/IDE@ Clase: Branchiopoda Orden ONYCHOPODA Manual CLASE BRANCHIOPODA Orden Onychopoda Jordi Sala1, Juan García-de-Lomas2 & Miguel Alonso3 1 GRECO, Institut d’Ecologia Aquàtica, Universitat de Girona, Campus de Montilivi, 17071, Girona (España). [email protected] 2 Grupo de Investigación Estructura y Dinámica de Ecosistemas Acuáticos, Universidad de Cádiz, Pol. Río San Pedro s/n. 11510, Puerto Real (Cádiz, España). 3 Departament d'Ecologia, Facultat de Biologia, Universitat de Barcelona, Avda. Diagonal 643, 08028, Barcelona (España). 1. Breve definición del grupo y principales caracteres diagnósticos El orden Onychopoda es un pequeño grupo de crustáceos branquiópodos que habitan principalmente el medio marino, aunque existen algunas especies de aguas dulces. Se caracterizan por su pequeño tama- ño (aunque algunas especies pueden presentar expansiones abdominales extraordinariamente largas, pudiendo llegar a tamaños totales mayores de 15 mm), con tagmosis poco aparente, cabeza relativamen- te grande y prácticamente ocupada por el ojo compuesto, un caparazón muy reducido formando la cáma- ra incubadora (y por tanto no cubriendo completamente la región postcefálica), unos toracópodos heteró- nomos (o sea, con una diferenciación marcada entre ellos) y estenopodiales (apéndices tubulares, en contraposición a los apéndices filopodiales o aplanados de los Anomopoda Sala et al., 2015a o Ctenopo- da Sala et al., 2015b), y por no presentar efipio para proteger los huevos gamogenéticos (al contrario que los Anomopoda). 1.1. Morfología El cuerpo de los Onychopoda es corto, con una forma más o menos globular, aunque algunas especies (no presentes en la fauna ibérica o macaronésica) pueden tener un pedúnculo caudal que puede llegar ser 2,5 veces la longitud corporal. -
Comparative Phylogeography of Marine Cladocerans
Mar Biol (2008) 155:1–10 DOI 10.1007/s00227-008-0996-x ORIGINAL PAPER Comparative phylogeography of marine cladocerans Alan Durbin · Paul D. N. Hebert · Melania E. A. Cristescu Received: 25 July 2007 / Accepted: 2 May 2008 / Published online: 10 June 2008 © Springer-Verlag 2008 Abstract We examined the population genetics of six the Wrst genetically documented cases of exotic or invasive species of marine cladocerans, using a »600 bp fragment marine zooplankton, likely an underreported group. of the cytochrome oxidase subunit I gene sequence. Phylo- genetic analysis revealed signiWcant intraspeciWc, semi- allopatric phylogenetic breaks in four out of Wve species Introduction belonging to the Podonidae, supporting an ancient radiation and oceanic expansion for this group. By contrast, Penilia Although there are over 600 described species of cladocer- avirostris (Sididae) displayed no phylogeographic structure ans, only 8 are truly marine. The relative scarcity of marine across a global sampling, suggesting a recent worldwide cladocerans compared to the high diversity of their fresh- expansion. Our results also show a transoceanic distribution water and brackish relatives has been remarked as curious of identical or very similar haplotypes in several species of (Rivier 1998) and has been attributed to their high dispersal marine Cladocera, which may be interpreted as either natu- ability which may inhibit vicariant speciation by enhancing ral transport or evidence of recent anthropogenic transport. genetic connectivity between distant populations (EgloV If the latter is the case, marine cladocerans represent one of et al. 1997). On the other hand, the very broad distribution range of marine cladocerans suggests them as good candi- dates for phylogeographic and population genetic investi- gations. -
Diversity and Zoogeography of the Fairy Shrimps (Branchiopoda: Anostraca) on the Indian Subcontinent
Hydrobiologia DOI 10.1007/s10750-017-3122-6 CHALLENGES IN ANOSTRACAN RESEARCH Diversity and zoogeography of the fairy shrimps (Branchiopoda: Anostraca) on the Indian subcontinent Sameer M. Padhye . Mihir R. Kulkarni . Henri J. Dumont Received: 21 December 2016 / Revised: 1 February 2017 / Accepted: 11 February 2017 Ó Springer International Publishing Switzerland 2017 Abstract The Indian subcontinent has a specific two zoogeographic ‘‘zones,’’ viz., a Northern (NZ) biogeographical history, but has remained understud- zone and the rest of the subcontinent (RS) comprising ied with respect to invertebrates like the Anostraca. In the Central (CZ) and South (SZ) zones by Unweighted this study, we discuss the anostracan diversity and Pair-Group Method using arithmetic averages cluster- zoogeography on the subcontinent. We collected all ing and Analysis of Similarity. Complementarity pertinent literature and considered nineteen biocli- index shows that no fauna is shared between NZ and matic variables along with altitude and its terrestrial RS, while CZ and SZ share 50% of the species. ecoregions. The study area was overlaid with Principal Component analysis shows that NZ and RS 10,000 km2 grids, and five hundred random GIS data differ somewhat from one another climatically. NZ points per grid were extracted for analysis besides the and RS have different ecoregions with montane and species locality data. Species richness estimators temperate grasslands commonly observed in NZ while predict at least 3–4 more species to the existing list the latter comprising tropical forests, implying differ- of 19 species. The beta diversity measure bsim reveals ences in soil geochemistry which is crucial for anostracan distribution. -
The Noncosmopolitanism Paradigm of Freshwater Zooplankton
Molecular Ecology (2009) 18, 5161–5179 doi: 10.1111/j.1365-294X.2009.04422.x The noncosmopolitanism paradigm of freshwater zooplankton: insights from the global phylogeography of the predatory cladoceran Polyphemus pediculus (Linnaeus, 1761) (Crustacea, Onychopoda) S. XU,* P. D. N. HEBERT,† A. A. KOTOV‡ and M. E. CRISTESCU* *Great Lakes Institute for Environmental Research, University of Windsor, Windsor, ON, Canada N9B 3P4, †Biodiversity Institute of Ontario, University of Guelph, Guelph, ON, Canada N1G 2W1, ‡A. N. Severtsov Institute of Ecology and Evolution, Leninsky Prospect 33, Moscow 119071, Russia Abstract A major question in our understanding of eukaryotic biodiversity is whether small bodied taxa have cosmopolitan distributions or consist of geographically localized cryptic taxa. Here, we explore the global phylogeography of the freshwater cladoceran Polyphemus pediculus (Linnaeus, 1761) (Crustacea, Onychopoda) using two mitochon- drial genes, cytochrome c oxidase subunit I and 16s ribosomal RNA, and one nuclear marker, 18s ribosomal RNA. The results of neighbour-joining and Bayesian phylogenetic analyses reveal an exceptionally pronounced genetic structure at both inter- and intra- continental scales. The presence of well-supported, deeply divergent phylogroups across the Holarctic suggests that P. pediculus represents an assemblage of at least nine, largely allopatric cryptic species. Interestingly, all phylogenetic analyses support the reciprocal paraphyly of Nearctic and Palaearctic clades. Bayesian inference of ancestral distribu- tions suggests that P. pediculus originated in North America or East Asia and that European lineages of Polyphemus were established by subsequent intercontinental dispersal events from North America. Japan and the Russian Far East harbour exceptionally high levels of genetic diversity at both regional and local scales. -
Practical Guide to Identifying Freshwater Crustacean Zooplankton
Practical Guide to Identifying Freshwater Crustacean Zooplankton Cooperative Freshwater Ecology Unit 2004, 2nd edition Practical Guide to Identifying Freshwater Crustacean Zooplankton Lynne M. Witty Aquatic Invertebrate Taxonomist Cooperative Freshwater Ecology Unit Department of Biology, Laurentian University 935 Ramsey Lake Road Sudbury, Ontario, Canada P3E 2C6 http://coopunit.laurentian.ca Cooperative Freshwater Ecology Unit 2004, 2nd edition Cover page diagram credits Diagrams of Copepoda derived from: Smith, K. and C.H. Fernando. 1978. A guide to the freshwater calanoid and cyclopoid copepod Crustacea of Ontario. University of Waterloo, Department of Biology. Ser. No. 18. Diagram of Bosminidae derived from: Pennak, R.W. 1989. Freshwater invertebrates of the United States. Third edition. John Wiley and Sons, Inc., New York. Diagram of Daphniidae derived from: Balcer, M.D., N.L. Korda and S.I. Dodson. 1984. Zooplankton of the Great Lakes: A guide to the identification and ecology of the common crustacean species. The University of Wisconsin Press. Madison, Wisconsin. Diagrams of Chydoridae, Holopediidae, Leptodoridae, Macrothricidae, Polyphemidae, and Sididae derived from: Dodson, S.I. and D.G. Frey. 1991. Cladocera and other Branchiopoda. Pp. 723-786 in J.H. Thorp and A.P. Covich (eds.). Ecology and classification of North American freshwater invertebrates. Academic Press. San Diego. ii Acknowledgements Since the first edition of this manual was published in 2002, several changes have occurred within the field of freshwater zooplankton taxonomy. Many thanks go to Robert Girard of the Dorset Environmental Science Centre for keeping me apprised of these changes and for graciously putting up with my never ending list of questions. I would like to thank Julie Leduc for updating the list of zooplankton found within the Sudbury Region, depicted in Table 1.