Block & Bridle Annual 1959-1960

President Roger Wehrbein Vice President Ted Klug Secretary George B. O'Neal Treasurer Ralph Hazen Marshal Bud Reece Historian Tom Kraeger Co-Historian John Zauha Ag. Executive Representative Larry Williams Faculty Advisor Dr. E. B. Peo, Jr. George Ahlschwede Richard Hahn Henry Beel Ralph Hazen Gary Briggs Gary Heineman Leslie Cook Max Hauser Richard Eberspacher Buce Jameson Russ Edeal Leon Janovy William Ehresman Alan Jorgensen Rolland Eubanks John Joyner Mickey Evertson Marshall Jurgens Jesse Felker Ron Kahle Mylon Filkins Donald Kavan Richard Frahm Max Keasling Roger French Ronald Kennedy Angus Garey Ted Klug Ed Gates Herb Kraeger Gerald Gogan Tom Kraeger Gerald Goold Fernando Lagos Jay Graf Gerald Lamberson Lloyd Langemeier Ralph Langemeier Gerald Loseke Donald Meiergerd Lowell Minert John Oeltjen George B. O'Neal Don Ormesher Larry Ott Bud Reece Ron Sabatka Keith Smith Ronald Smith Donn Simonson Daryl Starr Galen Stevens Eugene Turdy Ernest Thayer Charles Thompson Jerry Thompson Eli Thomssen William Watkins Allen Trumble Robert Weber Lawrence Turner Dan Wehrbein Reginald Turner Roger Wehrbein Vance Uden Dick White Max Waldo Billy Williams Blair Williams Larry Williams D. Patrick Wright John Zauha

Radiocarbon Dating, Chronologic Framework, and Changes in Accumulation Rates of Holocene Estuarine Sediments from Chesapeake Bay

Rapidly accumulating Holocene sediments in estuaries commonly are difficult to sample and date. In Chesapeake Bay, we obtained sediment cores as much as 20min length and used numerous radiocarbon ages measured by accelerator mass spectrometry methods to provide the first detailed chronologies of Holocene sediment accumulation in the bay. Carbon in these sediments is a complex mixture of materials from a variety of sources. Analyses of different components of the sediments show that total organic carbon ages are largely unreliable, because much of the carbon (including coal) has been transported to the bay from upstream sources and is older than sediments in which it was deposited. Mollusk shells (clams, oysters) and foraminifera appear to give reliable results, although reworking and burrowing are potential problems. Analyses of museum specimens collected alive before atmospheric nuclear testing suggest that the standard reservoir correction for marine samples is appropriate for middle to lower Chesapeake Bay. The biogenic carbonate radiocarbon ages are compatible with 210Pb and 137Cs data and pollen stratigraphy from the same sites. Post-settlement changes in sediment transport and accumulation is an important environmental issue in many estuaries, including the Chesapeake. Our data show that large variations in sediment mass accumulation rates occur among sites. At shallow water sites, local factors seem to control changes in accumulation rates with time. Our two relatively deep-water sites in the axial channel of the bay have different long-term average accumulation rates, but the history of sediment accumulation at these sites appears to reflect overall conditions in the bay. Mass accumulation rates at the two deep-water sites rapidly increased by about fourfold coincident with widespread land clearance for agriculture in the Chesapeake watershed.