SPATIAL VARIATION AND DISTRIBUTION OF PHOSPHORUS FORMS IN BOTTOM SEDIMENTS OF TWO CANADIAN SHIELD LAKES

Nutrient dynamics in lake systems are influenced by the loading of sediment-associated phosphorus (P) from both internal and external sources. Despite efforts to control lake productivity through reductions in external P loading, water quality problems persist in some lakes due to high internal loading of P from bottom sediment. The present study examines the spatial distribution of chemically defined P forms (NH₄Cl-RP, BD-RP, NaOH-RP, HCI-RP, and NaOH_(S5)-RP) in bottom sediments of two noncalcareous Canadian Shield Lakes. Sediment P data are related to some of the physical and chemical variables that control internal P loading in lakes. The BD-RP and NaOH-RP forms are related to water depth and nonresidual iron and aluminum content of sediment. Approximately 80% of the total extractable P in the Muldrew Lakes sediment was bioavailable P (NH₄Co-RP + BD - RP + NaOH - RP), which is about twice that reported in the literature for calcareous lakes. In order to model P cycling in the Muldrew Lakes, further research is required to determine the internal supply of P from the lakes' sediments and potential anthropogenic inputs ofP from private sewage disposal systems. La dynamique des nutriments dans un lac est influenceé par I'apport en phosphore (P) provenant de sources internes et externes. Malgré les efforts déployés pour contrôler le taux de P par réduction de I'apport externe, la qualityé de I'eau demeure un problème dans certains lacs à cause de la contribution interne provenant de la sédimentation de fond. Cette étude examine la distribution spatiale de formes chimiquement définies de P (NH₄CI-RP, BD-RP, NaOH-RP, HCI-RP, and NaOH₍₈₅₎-RP) présentes dans les sédiments de fonds de deux lacs non-calcaires du Bouclier Canadien. Les contenus en P des sediments sont reliés à certaines variables physiques et chimiques qui contrôlent I'apport interne des lacs. Le Bd-RP et le NaOH-RP sont reliés à la profondeur de I'eau ainsi qu'aux contenus non-résiduels de fer et d'aluminium du sédiment. Environ 80% du P pouvant être extrait du sédiment des lacs Muldrew éait du P (NH₄Cl-RP + BD-RP + NaOH-RP) biodisponible. Ceci représente le double de ce qui est rapporté dans la littéature pour des lacs calcaires. Afin de construire un modèle du cycle du P dans les lacs Muldrew, il est important de déterminer I'apport interne de P provenant de la sédimentation et les sources anthropiques potentielles provenant des systèmes d'égouts privés.     

Editorial Introduction 35(3)

Sherzer, Joel. Kuna Ways of Speaking: An Ethnographic Perspective. Austin: University of Texas Press, 1983. xii + 260 pp. including bibliography and guide to pronunciation. $22.50 cloth.     

The graptolite Glossograptus Emmons and its proximal structure

Ni Yunan & Cooper, R. A., 1994:03:28. The graptolite Glossograptus Emmons and its proximal structure. Alcheringa 18, 161–167. ISSN 0311-5518.

New specimens of Glossograptus acanthus from the Ningkuo Shale of China, preserved in relief, help to resolve the much debated problem of the structure of Glossograptus. A model for the proximal structure of the genus is proposed, based on the new material and on Finney's (1978) Athens Shale specimens. The model confirms that Glossograptus has homologous structure and development with Pseudisograptus, and isograptid development type is primitive for the group containing both genera. A cladogram is presented in which the suborder Glossograptina Jaanusson (with families Glossograptidae and Cryptograptidae) together with family Corynoididae Bulman are subsumed within a redefined family Glossograptidae.