Melting ice in the Greater Yellowstone Ecosystem of the Rocky Mountains exposes an ancient, mature stand of whitebark pine from the Holocene, 180 m in elevation above the modern treeline. Findings suggest it is possible the treeline may expand upslope with climate change.
Melting ice in the Greater Yellowstone Ecosystem of the Rocky Mountains exposes an ancient, mature stand of whitebark pine from the Holocene, 180 m in elevation above the modern treeline. Findings suggest it is possible the treeline may expand upslope with climate change.