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- W2767310236 abstract "The Macquarie Harbour water column is highly stratified due to the significant freshwater inputs from the Gordon and King Rivers, deep central basin (maximum depth ~ 50m) and shallow sill at its mouth (<5 m) that restricts exchanges with the ocean. This isolation of deep waters in the Harbour has resulted in a naturally low dissolved oxygen (DO) environment (Creswell et al., 1989; Koehnken 1996). The dark tannin rich freshwater layer limits light penetration and as a consequence productivity is low; the sediments are naturally depauperate of fauna (O’Connor et al. 1996; Talman et al. 1996; Edgar et al. 1999)" @default.
- W2767310236 created "2017-11-17" @default.
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- W2767310236 date "2017-01-01" @default.
- W2767310236 modified "2023-09-24" @default.
- W2767310236 title "Environmental research in Macquarie Harbour: interim synopsis of benthic and water column conditions" @default.
- W2767310236 hasPublicationYear "2017" @default.
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