The history of the genus Eubosmina in Lake Mondsee (Upper Austria)

Nauwerck, Arnold

doi:10.1007/bf00028388

Cited by 13 publications

(8 citation statements)

References 31 publications

(32 reference statements)

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“…Evidences from mtDNA, nuclear DNA, and paleolimnological data are consistent with the hypothesis that the European Eubosmina (Bosmina coregoni included) phylogroup is of post-glacial origin from a Bosmina (Eubosmina) longispina-like ancestor (Haney & Taylor, 2003). Paleolimnological data obtained by Nauwerck (1991) also indicate an ongoing centrifugal spreading from an origin center located in north-eastern Europe. Apart from Northeastern Europe (e.g.…”

supporting

confidence: 74%

“…This species shows higher abundances in lakes in which mean total phosphorous concentrations, mean water conductivity and mean suspended matter were 30 μg/l, 100 μS/cm and 60 mg/l, respectively (Berzins & Bertilsson, 1989). Nauwerck (1991) and Hofmann (1996) also reported that when water conditions shift from eutrophic to oligotrophic, B. (E.) coregoni becomes more prominent.…”

Section: Excepting Valdecañas Reservoir Whichmentioning

confidence: 90%

“…In the area of origin B. (E.) coregoni is typically found in mesotrophic lakes (Nauwerck, 1991;Dimante-Deimantovica et al, 2012). This species shows higher abundances in lakes in which mean total phosphorous concentrations, mean water conductivity and mean suspended matter were 30 μg/l, 100 μS/cm and 60 mg/l, respectively (Berzins & Bertilsson, 1989).…”

Section: Excepting Valdecañas Reservoir Whichmentioning

confidence: 99%

“…Apart from Northeastern Europe (e.g. Kernan et al, 2009) it was mentioned in Poland (Kuczynska-Kippen, 2006;Adamczuk, 2009), Germany (Nauwerck, 1991;Hofmann, 1996;Straile & Müller, 2010), Denmark (Brucet et al, 2009), Belgium (Malbrouck et al, 2005) and in Northern Italy (Margaritora, 1983). In the Iberian Peninsula B.…”

mentioning

confidence: 99%

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Bosmina (Eubosmina) coregoni Baird, 1857 (Crustacea, Branchiopoda, Anomopoda): New planktonic invader in the Iberian peninsula

Geraldes¹,

Alonso²

2014

GRAELLSIA

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Bosmina (Eubosmina) coregoni Baird, 1857 has been recorded for the first time in the Iberian Peninsula. It is a planktonic cladoceran widely distributed in the Holarctic region which was never previously referred in the Iberian Peninsula in spite of the numerous and intensive studies on freshwater planktonic fauna in this geographic area in the last three decades. The species appeared in five reservoirs located in the Northwest quadrant. Excepting Valdecañas reservoir, which can be considered eutrophic, the others (Bárcena, Peares, Belesar and Aguieira) were classified as meso-eutrophic. The only morphotype found corresponds to Bosmina (Eubosmina) coregoni ssp. coregoni. The maximum abundance of this species occurred during the winter period. It is plausible to consider that waterfowl migration and the presence of recreational boats might be the dispersion vector of this species in Iberian Peninsula.Key words: Bosmina coregoni; Reservoirs; Iberian Peninsula. RESUMENBosmina (Eubosmina) coregoni Baird, 1857 (Crustacea, Branchiopoda, Anomopoda): un nuevo invasor planctónico en la península ibérica Se cita Bosmina (Eubosmina) coregoni Baird, 1857 por vez primera en la península ibérica. Se trata de un cladócero planctónico ampliamente distribuido en la región holártica, que no había sido previamente referido en la península ibérica a pesar de los numerosos e intensivos estudios sobre la fauna planctónica de agua dulce realizados durante las últimas tres décadas en este ámbito geográfico. La especie ha aparecido en cinco embalses situados en el cuadrante noroccidental. Con excepción del Embalse de Valdecañas, que se puede considerar eutrófico, los restantes (Bárcena, Peares, Belesar y Aguieira) fueron clasificados como mesoeutróficos. El único morfotipo encontrado corresponde a Bosmina (Eubosmina) coregoni ssp. coregoni. La abundancia máxima de la especie ocurrió durante el período del invierno. Es plausible considerar que las aves acuáticas y la presencia de embarcaciones de recreo pudieron ser un vector importante de la dispersión de esta especie en la península ibérica.Palabras clave: Bosmina coregoni; embalses; península ibérica. Recibido

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supporting

confidence: 74%

Section: Excepting Valdecañas Reservoir Whichmentioning

confidence: 90%

Section: Excepting Valdecañas Reservoir Whichmentioning

confidence: 99%

mentioning

confidence: 99%

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Bosmina (Eubosmina) coregoni Baird, 1857 (Crustacea, Branchiopoda, Anomopoda): New planktonic invader in the Iberian peninsula

Geraldes¹,

Alonso²

2014

GRAELLSIA

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“…In particular, in CAZ III B-D-F, the simultaneous presence of the planktonic species E. coregoni and B. longirostris indicate an increase in the trophic level (Boucherle and Zullig, 1983;Szeroczyńska, 1985Szeroczyńska, , 1991Frey, 1986;Nauwerck, 1991;Dimante-Deimantovica et al, 2012), which is also confirmed by the presence of M. dispar and A. exigua. Moreover the identification of C. rectirostris, P. uncinatus and G. testudinaria reveals an increase in water temperatures (Szeroczyńska, 1985;Hofmann, 2000), while remains of A. harpae, A. quadrangularis and L. leydigi suggest a continuous development of the macrophyte zone.…”

Section: Late Eemianmentioning

confidence: 89%

The Eemian/Early Vistulian development of the Solniki paleolake (north-eastern Poland) as shown by subfossil Cladocera

Niska

2016

Adv Ocean Limnol

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This work presents results of a paleolimnological study focussed on subfossil Cladocera analysis and on different aspects of the evolution of the Solniki paleolake during the Eemian/Early Vistulian period. The study aimed at the reconstruction of the long-term dynamics of this paleoecosystem and at defining the conditions (e.g., water level, trophic status and water temperature) of the ancient lake. Paleolacustrine deposits of ca. 10 m thickness were discovered at Solniki during cartographic works for the Trześcianka sheet of the Detailed Geological Map of Poland. This archives recorded one full-interglacial sequence (Eemian Interglacial), one interstadial warming (Brørup) and two stadial coolings (Herning and Rederstall) stages, which were confirmed by palynological analyses. The subfossil Cladocera fauna from the Solniki paleolake consisted in 17 species belonging to the families Bosminidae, Chydoridae, Sididae and Daphniidae. Littoral species were dominant (52%), the most frequent of which were Alona affinis and Camptocercus rectirostris. The most abundance pelagic species were Eubosmina coregoni and Bosmina longirostris. The sediment species composition was quite similar to that of contemporary Central European lakes. The early and the late stages of Eemian Interglacial were likely the most favourable periods for the Cladocera development in the paleolake, in relation to higher water level, moderate water temperature and the mesotrophic state of water. A further ecologically favourable period was the Brørup Interstadial. The highest species richness, abundance, and diversity during the whole paleolake existence were recorded during these three periods. Surprisingly, the middle of the Middle Eemian Interglacial climate optimum appeared as an unfavourable period for the Cladocera growth as it was associated with decreasing water level and pronounced climate fluctuations. This sequence was also recorded by other studies of Eemian lakes in Central Europe.

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Postglacial Succession in the Subgenus Eubosmina (Crustacea: Cladocera) in the Region of the Unterhavel River (near Berlin, Germany) — Type Changes or Species Immigration?

Günther

Lieder

1993

Intl Review of Hydrobiology

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Analyses were made of subfossil Eubosmino remains from two Berlin Lakes. The first postglacial eubosminid was B. (E.) longispinu. In Tegeler See it occurred from the Allerod to Atlantic 2. In Lake Unterhavel it disappeared earlier in the Boreal. Bosmina (E.) longicornis occurred in early Atlantic I resp. at the end of Atlantic 2 (Tegeler See). Bosmina (E.) c. coregoni appeared in Lake Unterhavel at the end of the Boreal, in Lake Tegeler See at early Boreal. Bosmina (E.) c. thersitrs occurred only in sediments of Lake Unterhavel beginning in Atlantic 2.No sign of a "morphological transition" between taxa found by HOFMANN could be found in the two investigated lakes. The succession of Eubosmina taxa seems to be mainly the result of immigration.

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The history of the genus Eubosmina in Lake Mondsee (Upper Austria)

Cited by 13 publications

References 31 publications

<em>Bosmina (Eubosmina) coregoni</em> Baird, 1857 (Crustacea, Branchiopoda, Anomopoda): New planktonic invader in the Iberian peninsula

<em>Bosmina (Eubosmina) coregoni</em> Baird, 1857 (Crustacea, Branchiopoda, Anomopoda): New planktonic invader in the Iberian peninsula

The Eemian/Early Vistulian development of the Solniki paleolake (north-eastern Poland) as shown by subfossil Cladocera

Postglacial Succession in the Subgenus Eubosmina (Crustacea: Cladocera) in the Region of the Unterhavel River (near Berlin, Germany) — Type Changes or Species Immigration?

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