Redescription 3: The Pacification of the Primitive Tribes of Lake Geneva (Nacirema Ethnography)

2020 ◽  
pp. 29-40
Keyword(s):  
1989 ◽  
Vol 93 (3-4) ◽  
pp. 345-358 ◽  
Author(s):  
J. Dominik ◽  
Ch. Schuler ◽  
P.H. Santschi
Keyword(s):  

2013 ◽  
Vol 76 (S1) ◽  
pp. 7-19 ◽  
Author(s):  
Corinne C. Hoerger ◽  
Yosef Akhtman ◽  
Lorenzo Martelletti ◽  
Rebecca Rutler ◽  
Florence Bonvin ◽  
...  

2016 ◽  
Vol 79 (2) ◽  
pp. 249-263 ◽  
Author(s):  
Nicole Gallina ◽  
Martin Beniston ◽  
Stéphan Jacquet

Crustaceana ◽  
2014 ◽  
Vol 87 (8-9) ◽  
pp. 1095-1123 ◽  
Author(s):  
Laurent Decrouy ◽  
Torsten W. Vennemann

Because environmental conditions within a given basin are different for each season and at different water depth, knowledge of the life history and depth distribution of target species is important for environmental and palaeoenvironmental interpretations based on ostracod species assemblages and/or the geochemical compositions of their valves. In order to determine the distribution of species with depth as well as the life history of species from Lake Geneva, a one-year sampling campaign of living ostracods was conducted at five sites (2, 5, 13, 33 and 70 m water depth) on a monthly basis in the Petit-Lac (western basin of Lake Geneva, Switzerland). Based on the results, the different species can be classified into three groups. Littoral taxa are found at 2 and 5 m water depth and include, in decreasing numbers of individuals,Cypridopsis vidua(O. F. Müller, 1776),Pseudocandona compressa(Koch, 1838),Limnocythere inopinata(Baird, 1843),Herpetocypris reptans(Baird, 1835),Potamocypris smaragdina(Vávra, 1891),Potamocypris similis(G. W. Müller, 1912),Plesiocypridopsis newtoni(Brady & Robertson, 1870),Prionocypris zenkeri(Chyzer & Toth, 1858) andIlyocyprissp. Brady & Norman, 1889. Sublittoral species are found in a majority at 13 m water depth and to a lesser extend at 33 m water depth and include, in decreasing numbers of individuals,Fabaeformiscandona caudata(Kaufmann, 1900),Limnocytherina sanctipatricii,Candona candida(O. F. Müller, 1776) andIsocypris beauchampi(Paris, 1920). Profundal species are found equally at 13, 33 and 70 m water depth and includes, in decreasing numbers of individuals,Cytherissa lacustris(Sars, 1863),Candona neglectaSars, 1887 andCypria lacustrisLilljeborg, 1890. The occurrence ofLimnocytherina sanctipatricii(Brady & Robertson, 1869) is restricted from late winter to late spring when temperatures are low, whileC. vidua,L. inopinata,P. smaragdina,P. similis,P. newtoniandIlyocyprissp. occur predominantly from spring to early autumn when temperatures are high. Individuals ofC. neglecta,C. candida,F. caudata,P. compressa,C. lacustris,H. reptansandCp. lacustrisoccur throughout the year with juveniles and adults occurring during the same period (C. neglectaat 70 m,C. lacustrisat 13, 33 and 70 m, andH. reptansat 2, 5 and 13 m water depth) or with juveniles occurring during a different period of the year than adults (C. neglectaat 13 and 33 m andC. candida,F. caudataandP. compressaat their respective depth of occurrence). Among the environmental parameters investigated, an estimate of the relationship between ostracod autoecology and environmental parameters suggests that in the Petit-Lac: (i) water temperature and substrate characteristics are important factors controlling the distribution of species with depth, (ii) water temperature is also important for determining the timing of species development and, hence, its specific life history, and (iii) water oxygen and sedimentary organic matter content is less important compared to the other environmental parameter monitored.


1893 ◽  
Vol 10 (10) ◽  
pp. 454-455
Author(s):  
Charles Davison
Keyword(s):  

Though the observations described in this note are not conclusive, they seem to me to show that the lake of Geneva is probably growing at the present time, and that a similar growth, if taking place beneath an ice-covering on nearly level ground, would in time produce a true rock-basin. Unfortunately, the instruments used were very delicate levels, and experiments with such instruments prove that they are not to be trusted entirely for measurements of very small angles continued over a long interval of time.


1983 ◽  
Vol 109 (10) ◽  
pp. 1285-1297 ◽  
Author(s):  
Sebastian W. Bauer ◽  
Klaus D. Schmidt

2008 ◽  
Vol 99 (15) ◽  
pp. 7122-7131 ◽  
Author(s):  
John Poté ◽  
Laurence Haller ◽  
Jean-Luc Loizeau ◽  
Andrea Garcia Bravo ◽  
Vincent Sastre ◽  
...  

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