Ancient Environments

PALEOECOLOGY 442
A long-term perspective on ecology and environmental issues
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Tree Rings | Lake Sediments | Ancient Environments | Mass Extinctions 

In Paleo 442 we spend a lot of time learning to see ancient history embedded in the landscapes around us. Glaciations, sea level changes, megafloods, erosion, deposition, wind-blown dust, fires, ecological succession, and human activity all leave signs clearly visible to the trained eye. Reconstructing the ecological history of a site can tell a great deal about why an ecosystem looks and operates the way it does.

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From the air, it's easy to see that the sandy ridge running down the middle of Rainbow Lake, near campus, is an "esker," the former bed of a meltwater river that ran through a tunnel in/under the great glacier that buried this region under a mile or more of ice until about 12,500 years ago. Houses built on such porous material can cause septic wastes to seep into and pollute lakes.

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The Spring, 2001, Paleo class took a field trip to the Champlain Valley where we found marine mollusc shells that were left behind when Lake Champlain was a fjord-like arm of the Atlantic Ocean at the close of the last Ice Age. Talk about environmental change: the lake was first fresh with meltwater, then salty with seawater, then fresh again when the Valley rose above sea level about 10,000 years ago.

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