Trees and Paleoclimate
Part B: Where Were the Trees of the Past?
At the end of the last ice ageapproximately 21,000 years agoEarth's climate began a dramatic warming, causing the retreat of the great ice sheets across North America (and the rest of the globe). The emerging climate launched a major re-organization of both plant and animal species. This process of change, which lasted tens of thousands of years, is recorded in pollen sediment cores from lakes and other shallow and still bodies of water. You will learn more about these cores in Lab 6C, but first you will use an interactive map interface to step through the past.
Before you begin your journey, recall the biomes and climate zones that you studied in Lab 4. Two factors are important in determining where a tree or other plant species can exist: climate and soil type.
As the climate changed over the past 21,000 years, so did the abundance and distribution of tree and plant species. In this lab, you will observe the "migration" of the trees and consider how past tree distributions compare to modern tree distributions. Using this information, you will hypothesize the past climatic conditions of regions.
Introduction to Pollen Viewer
Take a moment to study the legend below the map. The number ranges shown in the legend indicate the percent of all fossil pollen (from the highlighted species) that was collected from the region during the given time period. For example, in the image left, the locations of 21,000 year-old fossilized pollen from (Picea) spruce is displayed, illustrating where spruce trees lived in this period of time, the end of the last Ice Age.In the case of the spruce, the blue color represents the ice sheet. Grey shading indicates 0-5% of the total pollen found is spruce; dark green indicates 40-100% of the pollen is from spruce trees. Note that as you select different species the numbers in the legend may vary.
Click the Play button to watch the change in fossil pollen distribution across a 21,000 year time period. The fossilized pollen is evidence of the presence of actual trees. These trees would have been present in the highlighted locations during the particular period of time. Notice the "migration" of spruce trees northward as the ice sheet retreats.
Use the Forward and Back arrows to move through the animation manually. Notice the change in the coastline as the North American ice sheet melts and the sea level rises. To examine this more closely select "Paleogeography with Ice Sheets" from the drop down menu.
Follow the migration of the Maple
Choose the maple (Acer) tree species from the drop down menu. Play the animation and watch how the maple tree abundance changed as the ice sheet retreated to Canada. As you view the map, answer the Stop and Think questions below.
You may want to refer to this online Atlas of the United States or your maps from Lab 3, to help you locate geographic boundaries.
Stop and Think
- Observe the image from 21,000 years ago. In what region of the country was the sugar maple tree located?
- In the years between 12,000 and 8,000 years ago the maple tree gained abundance in the Midwest and Great Lakes region. Based on what you know about the climate of present day Vermont, what does that tell you about the climatic conditions of the time in this region?
- Consider the change in the maple concentration in the past 500 years. What factors, other than climate, may have altered its abundance?
Explore the change in several other plant species over time. Examine the similarities and differences of their behavior with respect to changing climatic conditions across North America. Do some trees move more than others?