Master of Science, University of Akron, 2017, Geology-Environmental Geology
Lake sediment can provide records of past changes in climate, water budget and lake level, ecosystems, and human impacts to the environment. This study uses the sediment from Brady Lake, a kettle lake in northeastern Ohio, to determine Late Holocene natural and anthropogenic environmental variability. Because no bathymetric map of the lake was available, one was created in ArcMap by collecting 7,507 latitude, longitude, and water depth measurements with a Garmen 125 fathometer and GPS unit. Sediment dispersal processes were studied by collecting surface samples throughout Brady Lake. Dense, sandy sediment, having low organic content (<5%), were present in water less than 1.5 m deep where wind-wave orbital motion prevents muds from accumulating. Low density, porous muds, having high organic content (30%), accumulate below 1.5 m due to sediment focusing. A 4.13-m-long Livingston piston core was collected from the central deep-water basin to evaluate 2840 Cal yr of environmental change. Age control was determined through radiocarbon dating and correlating event stratigraphy datums to other dated Ohio kettle lake sediment records. Between 4.13 and 1.9 m core depth (2840-210 Cal yr BP), low density gyttja having 70% organic content and a C/N ratio of ~13.7 is present. These sediment characteristics are interpreted as the pre-Euro American settlement period when the watershed was forested and sediment yield was low. Within this interval, five lows in organic content, having increased sediment density, suggests a decrease in vegetation and increased watershed erosion. These changing watershed conditions may reflect fluctuations in atmospheric circulation and moisture balance during the Late Holocene. Furthermore, these lows agree with the timing of globally distributed rapid climate change occurring between 3500-2500; 1200-1000; and 600-150 Cal yr BP identified by Mayewski et al. (2004). At 1.9 m core depth, the gyttja abruptly changes to bedded mud having increased concen (open full item for complete abstract)
Committee: John Peck (Advisor); John Senko (Committee Member); Linda Barrett (Committee Member)
Subjects: Environmental Geology; Environmental Science; Geochemistry; Geology; Limnology; Paleoclimate Science; Sedimentary Geology