Guest post by Larry Fields
The last Ice Age razed all of the coniferous forests in Finland. After the ice sheet retreated, trees from elsewhere–like the Scots Pine–gradually colonized the vacant niches. On a smaller scale, the same thing happened in many high mountains of the Earth’s temperate regions, including the Sierra Nevada Range of California. We can learn a thing or two about climate history from Alpine dendrology.
Round Top Lake, at 9340 feet elevation in the Northern Sierra near Carson Pass, is my favorite place for informal climate history research. Whitebark Pine trees grow in tight clumps around the North half of the lake.
Other high altitude conifers–like Lodgepole Pine, Mountain Hemlock, and Red Fir–also grow in the Carson Pass area. But Whitebark Pines can grow at slightly high elevations than these other trees.
At Round Top Lake, the Whitebark Pines in any given group are nearly identical genetically, since they reproduce asexually. New tree trunks grow outward from an existing root system. This is called suckering. The seeds that do sprout can’t endure the harsh Winters at that altitude. Walking 100 yards downhill from the lake on the main trail, one can see Whitebark Pines that have grown in a more normal way.
Naturalist Jeffrey P. Schaffer mentioned Round Top Lake in the 1989 edition of his book, The Tahoe Sierra: A Natural History Guide to the 106 Hikes in the Northern Sierra. Here’s a link to a review of a more recent book by Schaffer.
http://www.amazon.com/Tahoe-Sierra-Natural-History-Northern/dp/0899972209
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