Limnological studies of saline lakes in the dry valleys

Author(s):  
Tetsuya Torii ◽  
Noboru Yamagata
Keyword(s):  
Author(s):  
Jill Mikucki ◽  
W. Berry Lyons ◽  
Ian Hawes ◽  
Brian D. Lanoil ◽  
Peter T. Doran

2008 ◽  
Vol 15 (1-2) ◽  
pp. 321-348 ◽  
Author(s):  
William J. Green ◽  
W. Berry Lyons

2002 ◽  
Vol 357 (1423) ◽  
pp. 863-869 ◽  
Author(s):  
Johanna Laybourn-Parry

In Antarctic lakes, organisms are confronted by continuous low temperatures as well as a poor light climate and nutrient limitation. Such extreme environments support truncated food webs with no fish, few metazoans and a dominance of microbial plankton. The key to success lies in entering the short Antarctic summer with actively growing populations. In many cases, the most successful organisms continue to function throughout the year. The few crustacean zooplankton remain active in the winter months, surviving on endogenous energy reserves and, in some cases, continuing development. Among the Protozoa, mixotrophy is an important nutritional strategy. In the extreme lakes of the McMurdo Dry Valleys, planktonic cryptophytes are forced to sustain a mixotrophic strategy and cannot survive by photosynthesis alone. The dependence on ingesting bacteria varies seasonally and with depth in the water column. In the Vestfold Hills, Pyramimonas , which dominates the plankton of some of the saline lakes, also resorts to mixotrophy, but does become entirely photosynthetic at mid–summer. Mixotrophic ciliates are also common and the entirely photosynthetic ciliate Mesodinium rubrum has a widespread distribution in the saline lakes of the Vestfold Hills, where it attains high concentrations. Bacteria continue to grow all year, showing cycles that appear to be related to the availability of dissolved organic carbon. In saline lakes, bacteria experience sub–zero temperatures for long periods of the year and have developed biochemical adaptations that include anti–freeze proteins, changes in the concentrations of polyunsaturated fatty acids in their membranes and suites of low–temperature enzymes.


2016 ◽  
Author(s):  
Devin Castendyk ◽  
◽  
Maciej K. Obryk ◽  
Sasha Z. Leidman ◽  
Michael Gooseff ◽  
...  

2016 ◽  
Author(s):  
Melisa A. Diaz ◽  
◽  
Susan A. Welch ◽  
Kathleen A. Welch ◽  
Alia L. Khan ◽  
...  

2016 ◽  
Author(s):  
Kate M. Swanger ◽  
◽  
Joerg M. Schaefer ◽  
Gisela Winckler

2017 ◽  
Author(s):  
Melisa A. Diaz ◽  
◽  
Byron J. Adams ◽  
Alia L. Khan ◽  
Kathleen A. Welch ◽  
...  

2021 ◽  
Vol 307 (1) ◽  
Author(s):  
Anca M. Şuteu ◽  
Laura Momeu ◽  
Karina P. Battes ◽  
Andreea Baricz ◽  
Adorján Cristea ◽  
...  

1997 ◽  
Vol 66 (4) ◽  
pp. 257-262
Author(s):  
Cristian R. Altaba

The allozyme data base of Arntzen & García-París (1995) on midwife toads (Alytes, Discoglossidae) is reanalysed considering each locus as a discrete character. The phylogeny thus inferred differs from the one obtained with genetic distances in the position of A. dickhilleni from the Betic region – it appears that its sister species is the widespread A. obstetricans, not the Mallorcan endemic A. muletensis. This phylogenetic hypothesis agrees with the taxonomic treatment of the genus based on morphology. A testable biogeographic hypothesis is proposed to account for the diversification of midwife toads in Iberia and the Balearics. The postulated underlying geological changes were the spread of inland saline lakes that divided Iberia (16 mY B.P.), the emergence and break-up of the Betic orogen (14 mY), and the formation of the Betic Strait (8 mY). Dispersal over sea channels or during the Messinian Crisis (6 mY) are deemed unlikely on the basis of ecological and biogeographical data.


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