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Research Training Program
Highlights from 2006

Updated: 6 June 2006
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Smithsonian Institution
National Museum of Natural History

Research Training Program

Schedule of Events
Field Trips



Scientist Cliffs
Paleobiology Field Trip

Location: Scientist Cliffs, Maryland

Host: Matthew Oreska

Guides: Dave Bohaska and Bob Purdy

Topic: Paleobiology - Calvert Cliffs formation

Itinerary:

7:30 a.m. Meet

8:00 a.m.
Depart

9:30 a.m. Arrive Scientists Cliffs, Maryland
Meet at the "Chestnut Cabin" parking lot.


9:30 - 9:45 a.m.
Site Orientation

10:00 a.m. - noon.
Site Exploration

noon - 1:00 p.m. Lunch Break - Bring your own lunch.

Notes:

    • Bring sunscreen.
    • Plan on getting wet and walking in the water (you can even swim at the beach, if you want.).
    • Bring drinking water.
    • Bring your lunch.
    • Bring a towel, or something to dry off with.
    • No digging in the cliff.

Participants:

Elisa Maldonado
Jorge Alvarez
Emily Armgardt
Dave Bohaska
Terry Chesser
Malcolm Collins
Megan Ennis & guest
Katie Faust
Paige Hamilton
Gene Hunt & guest
Jayme Job
Sara Marsteller
Juan Andrea Martinez
Caleb McMahan
Sylvia Moses
Alisa O'Connor
Matthew Oreska
Bob Purdy
Nick Rassmusen
Erin Saup
Ashleigh Smythe & guest
Maya Strahl
Kim Vann

 

About the Scientists Cliffs Site:

Located on the western side of the Chesapeake Bay, the "Calvert Cliffs" were formed over 15 million years ago when all of Southern Maryland was covered by a warm, shallow sea.

The cliffs dominate the shoreline of the Chesapeake Bay extending for more than thirty miles; from Fairhaven (Anne Arundel County, MD) to near Drum Point (Calvert County, MD).

Know Before You Go

Maryland State Fossil, Ecphora garderae garderae Wilson, an extinct gastropod (snail). This fossil snail was one of the first fossils from the New World to be illustrated and published in the scientific literature, dating to about 1770. It was officially named Maryland's state fossil 1 October 1994.

They are considered the best marine Miocene (Miocene Epoch, 25 million to 6.5 million years ago) deposit in the world.

Three formations are recognized in the cliffs; from oldest to youngest, the Calvert, Choptank, and St. Marys Formations. These have been further subdivided into Members and Beds.

Because of the gentle dip (about 11 feet per mile) of the deposits to the southeast, different Beds are exposed at different localities, containing different sediment types and fossils.

The cliffs and beaches have been collected and studied from Colonial times to the present.

Over 600 species of fossils have been identified from these cliffs including the "Maryland State Fossil" Ecphora gardnerae gardnerae Wilson.

The most visible fossils are mollusk shells, with some beds so densely packed that they are described as "shell beds."

The most popular fossils are the sharks' teeth.

Other fossils include microscopic plants and animals, macroscopic plants, corals, barnacles, crabs, sand dollars, sea urchins, bony fish, rays, crocodiles, turtles, birds, terrestrial mammals, and marine mammals. Many fossils have Calvert Cliffs as their type locality and some have been found nowhere else.

The Calvert Cliffs region is also home to two Federally threatened species of tiger beetle; Cicindela dorsalis dorsalis (Northeastern Beach Tiger Beetle) and Cicindela puritana (Puritan Tiger Beetle) which live on the broad, sandy beaches at approximately ten locations in Virginia and Maryland including four populations in Calvert County.

Check out more:


Most popular finds include shark teeth and ray teeth. Here in the left photo, a complete Spotted Eagle Ray tooth, Aetobatus sp. (far left) and Requien Shark tooth, Carcharhinus sp. (upper center). Lower right is an example of ray teeth. The most ray teeth found are form are from the spotted eagle ray, Aetobatus sp.
In the photo on the right you see a variety of common finds, including a Mako Shark tooth, Isurus hastalis, (lower right).


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