Newsletter of the Biological Survey of Canada (Terrestrial Arthropods)

Volume 22, No. 1, Spring 2003


 

Quips and Quotes

 

General information and editorial notes

News and Notes

Spread your word

Label data brief translated

Biodiversity research website

Benthic invertebrate monitoring

Activities at the Entomological Societies' meeting

Summary of the Scientific Committee meeting

The Quiz Page

Project Update: Insects of Keewatin and Mackenzie

Web Site Notes

Opinion Page: The real costs of insect identifications

Database updated

Arctic Corner

Arctic research notes

Funding for arctic studies

Selected future conferences

Quips and Quotes

List of Requests for Material or Information

 

"Micromalthus debilis LeConte (1878), has one of the most bizarre life cycles of any metazoan. Reproduction is typically by thelytokous, viviparous, larviform females, but there is also a rare arrhenotokous phase. The active first-instar (triungulin) larva develops into a legless, feeding (cerambycoid) larva. This form either pupates, leading to a diploid adult female, or develops into any of three subsequent types of reproductive paedogenetic forms: (1) a thelytokous female that produces triungulins via viviparity; (2) an arrhenotokous female that produces a single egg that develops into the short-legged (curculionoid) larva, eventually devouring its mother and becoming a haploid adult male; or (3) an amphitokous female that can follow either of the two above reproductive pathways."

From D.A. Pollock and B.B. Normark. 2002. J. Zool. Syst. Evol. Res. 40(2): 105–112.

 

Walker Lake is a monomictic, nitrogen-limited, terminal lake located in western Nevada. . . As a result of anthropogenic desiccation, between 1882 and 1996 the lake's volume has dropped from 11.1 to 2.7 km3 and salinity has increased from 2.6 to 12–13 g l-1. . . If desiccation continues unabated, the lake will be too saline (>15–16 g l-1) to support trout and chub fisheries in 20 years, and in 50–60 years the lake will reach hydrologic equilibrium at a volume of 1.0 km3 and a salinity of 34 g l-1.

From M.W. Beutel, A.J. Horne, J.C. Roth and N.J. Barratt. 2001. Hydrobiologia 466(1–3): 91–105.

 

"It is not necessary to understand things in order to argue about them." Caron de Beaumarchais

 

Terminological exactitude
"In some cases, the difficulty observed by experimentalists is a kinetic problem. Water in a very narrow, viscous layer is hard to remove even if the attraction to the hydrophilic surface is only modest. This is particularly the case at low temperatures because of the strong dependence of viscosity on temperature. Such water would fail to freeze not because it is in equilibrium with ice, but rather because it can remain in disequilibrium for a time exceeding the patience (or even the lifetime) of the experimentalist. In such cases, ‘bound’ water may be not so much tied up as unavoidably detained."

From J. Wolfe, G. Bryant and K.L. Koster. 2002. CryoLetters 23(3): 157–166.

 

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