Microscopic timecapsules

Dr. Estella Leopold looks directly into a camera during an interview

"As a youngster, I spent many idyllic weekends getting 'lost in nature' at my family's Sand County farm cabin in Wisconsin... a wonderful place to learn natural history."

Dr. Estella Leopold
 

What can fossil pollen tell us about Florissant's climate 34 million years ago?

Pollen may cause sniffles and sneezes, but ancient pollen preserved in Florissant's rock record provides clues to the ancient climate here. Some of the Eocene trees are known only from fossil pollen instead of leaves.

Pollen provides the only evidence for some plants that frew only on the higher slopes more distant from the lake.

Up Close and Detailed

The size of pollen grains varies between plant species, ranging from about 20 to 150 microns in length. In other words, over a thousand of the smallest pollen grains lined up end to end would only measure about an inch!
 
Conifer pollen and hardwood pollen sizes
 
Residue of pollen, which is then stained red and mounted on a microscope slide

Preserved in Detail

A pollen grain's tough walls allow it to remain well preserved in rock. Florissant's rock record has yielded over 150 different types of pollen and spores, some of which are the only remaining evidence of certain plants/

Dr. Leopold's method of removing the pollen from the shale, isolating it, and comparing it to the modern plant relatives helps us to determine the temperature and rainfall of ancient Florissant.

Retrieving ancient Pollen

Shale is placed into a test tube and dissolved in acids, leaving behind a residue of pollen. The pollen is stained red and mounted onto a microscope slide.

 

Plant Communities of Ancient Florissant

Some of the ancient forest's plants lived far from the lake, making it unlikely that their leaves or fruits would become fossils. However, wind often carried the pollen grains into the lake where they settled. Pollen provides the only evidence that some higher-elevation trees- such as Douglas Fir/ Larch and Hemlock- grew here in the Eocene.

Wet Valley Bottom

Redwood (Sequoia), False Cedar (chamaecyparis), Willow (Salix), Poplar (Populus), Golden-Rain Tree (Koelreuteria), Extinct Birch relative (paracarpinus), Extinct Beech relative (Fagopsis)

Marsh

Cattail (typha), Water lillies (Nymphaeaceae), Water Fern (Azolia) , Pondweed (Potamogeton)

Hillside and Ridges

Pine (Pinus), Oak (quercus), Mountain Mohogany (Cerocarpus)

High Conifer Forest

Fir (Abies), Douglas fir (pseudosugal), Larch (Larix), Pine (Pinus), Spruce (picea), Hemlock (Tsuga)

Transition

Pine (pinus), Rose (Rosa), Serviceberry (Amelanchier), Currant (Ribes), Sumac (rhus)




 
This illustration combines the evidence of pollen with that from leaves and fruits. Descriptions of communities are in the text above.
 

Nearest Living Relative

Dr. Leopold concluded that many of the Florissant fossil plants have close living relatives today. Some of these modern relatives are nowr estricted to far-away parts of the world, yet they lived together here during the late Eocene.
 
Globe map showing where modern relatives of Eocene Florissant plant species now live
 

Dr. Estella Leopold

Estella Leopold is the daughter of Aldo Leopold, who founded the Conservation ethic in America. In 1969, she was the leader in establishing a bold grassroots effort to save the Florissant Fossil Beds from development. She and other scientists and lawyers stopped the development long enough for Congress to create Florissant Fossil Beds National Monument. In 2010, Dr. Leopold received the International Cosmos Prize- the world's highest award for conservation- recognizing her notable achievements at Florissant.

Last updated: November 19, 2022

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