Michigan Forest Communities - Michigan Association of ...
Michigan Forest Communities - Michigan Association of ...
Michigan Forest Communities - Michigan Association of ...
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A SHORT HISTORY<br />
OF MICHIGAN FORESTS<br />
T<br />
he diverse forests that cover much<br />
<strong>of</strong> the <strong>Michigan</strong> landscape are the<br />
culmination <strong>of</strong> many thousands <strong>of</strong> years<br />
<strong>of</strong> development. Their history begins<br />
with the slow melting and retreat <strong>of</strong> the<br />
Wisconsin glacier, a portentous event<br />
that marked the end <strong>of</strong> the great<br />
Pleistocene Ice Age. The spoil left<br />
behind by the retreating glacier represented<br />
a biological vacuum; plants and<br />
animals that had marked time for millennia<br />
in ice-free areas south <strong>of</strong> the glacier<br />
lost no time in moving north to<br />
invade the vacated landscape. Among<br />
these first plants were several types <strong>of</strong><br />
trees, the ancestors <strong>of</strong> today’s <strong>Michigan</strong><br />
forests.<br />
The glacier began its retreat about<br />
14,000 years ago. Most <strong>of</strong> the Lower<br />
Peninsula was ice-free about 2,000<br />
years later (Kapp 1999). At this time a<br />
narrow belt <strong>of</strong> tundra and scattered<br />
clumps <strong>of</strong> spruce and tamarack occupied<br />
much <strong>of</strong> the northern Lower<br />
Peninsula, with closed boreal forests <strong>of</strong><br />
spruce, fir, birch, and poplar to the<br />
south. After the passage <strong>of</strong> another<br />
2,000 years, the glacial margin had<br />
receded almost to the shore <strong>of</strong> Lake<br />
Superior in the Upper Peninsula. Boreal<br />
conifers still dominated in the north,<br />
but now the southern part <strong>of</strong> the state<br />
was occupied by more complex pine-<br />
Spruce and tamarack forests were among the first to establish after the Wisconsin glacier receded.<br />
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