ISSN:
1573-5117
Keywords:
Antarctic pond
;
Labyrinth
;
chemical element
;
stable isotopic ratio
;
water source
;
salt origin
Source:
Springer Online Journal Archives 1860-2000
Topics:
Biology
Notes:
Abstract A large number of fresh water and saline ponds are located in the Labyrinth (77° 33′ S, 160° 50′ E) of the upper Wright Valley in the Dry Valleys region of southern Victoria Land, Antarctica. It is situated near the terminus of the Wright Upper Glacier between 800–1000 m above sea level. From a limnological point of view, the most interesting problems concerning these saline ponds are the origin of their salts and their evolutional history. Chloride ion contents vary remarkably among the ponds ranging from 0.0049 to 52.4 g kg−1. Surprisingly, more than a half of the ponds are saline with the highest chloride ion content being 2.7 times greater than that of seawater. The δD and δ18O values of the pond waters indicate a snow and/or glacial meltwaters origin, and that the ponds underwent subsequent alteration due to evaporation or freezing. The composition of chemical components reveal no evidence of trapped seawater. Thus the salt concentrations in the Labyrinth pond waters must be explained principally by the accumulation of atmospheric salts and subsequent repeated cycles of evaporation and freezing of the pond waters over considerable time periods.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF00031626
Permalink
