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Paleolimnology and the Reconstruction of Ancient Environments - Paleolimnology Proceedings of the XII INQUA Congress (Paperback, Softcover reprint of the original 1st ed. 1990)
Loot Price: R5,713
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Paleolimnology and the Reconstruction of Ancient Environments - Paleolimnology Proceedings of the XII INQUA Congress (Paperback, Softcover reprint of the original 1st ed. 1990)
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stable or falling water levels, and permit differen tiation between
gradual and sudden transgression The level of Lake Ontario was long
assumed to of the shoreline. Vegetational succession reflects have
risen at an exponentially decreasing rate shoreline transgression
and increasing water solely in response to differential isostatic
rebound depth as upland species are replaced by emergent of the St.
Lawrence outlet since the Admiralty aquatic marsh species. If
transgression continues, Phase (or Early Lake Ontario) 11 500 years
B. P. these are in turn replaced by floating and sub (Muller &
Prest, 1985). Recent work indicates merged aquatic species,
commonly found in water that the Holocene water level history of
Lake to 4 m depth in Ontario lakes, below which there Ontario is
more complex than the simple rebound is a sharp decline in species
richness and biomass model suggests. Sutton et al. (1972) and
(Crowder et al., 1977). This depth varies with Anderson & Lewis
(1982, 1985) indicate that physical limnological conditions in each
basin. periods of accelerated water level rise followed by Because
aquatic pollen and plant macrofossils are temporary stabilization
occurred around 5000 to locally deposited, an abundance of emergent
4000 B. P. The accelerated water level rise, called aquatic fossils
reflects sedimentation in the littoral the 'Nipissing Flood', was
attributed to the cap zone, the part of the basin shallow enough to
ture of Upper Great Lakes drainage. support rooted vegetation."
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