Recent carbonate sediments from (133-236m) on the northern Jamaican island slope are significantly different from shallower reef zones (l-70m) in grain constituents, textural parameters, and foraminiferal assemblages. The island slope sediment is dominated by coral fragments, calcareous algae, Halimeda plates, and foraminiferal tests. The sediment is characteristically poorly-sorted, nearly-symmetrically skewed, and mesokurtic, with a mean grain size in the fine sand range. Mineralogically, the sediment is predominantly aragonite (66%) and high-Mg calcite (22%), with some calcite (8%), and minor amounts of clays and other insoluble minerals (4%). Q-mode cluster analyses of sediment constituents, textural parameters, and foraminiferal species and larger group abundances were utilized in the delineation of shelf and island slope depositional environments. ineffective for such use. Mineralogy proves No significant differences are observed in sedimentological parameters (textures, constituents, and sedimentation rates) between an island slope traverse located below an area with prominant sill reefs and a traverse below an area lacking well-developed sill reefs. It is suggested that the sill reefs have less effect on off-reef transport than was previously believed. Based on the abundance trends of certain sediment grains and the similarity of sediment grains in island slope and deep fore reef/fore reef slope sediment, it is suggested that the deeper reef zones (>30m) are the source of most sediment transported seaward. Foraminiferal abundances show lateral differences between traverses related to input of shallow water (

Indiana University-Purdue University Indianapolis (IUPUI) / The frequency and magnitude of flooding events on the Lower Ohio River and their relationship with climate are investigated using a ca. 2000-year-long sediment core collected from Goose Pond, Indiana. Using high-resolution radiocarbon dating (n = 25), late Holocene sedimentation rates were calculated for Goose Pond. Changes in sediment accumulation rates are attributed to variations in the frequency of flooding events on the lower Ohio River. Elevated sedimentation rates immediately following the formation of Goose Pond ca. 2000 years ago persisted until 680 CE, suggesting regular flooding during this interval. Between 680 and 1190 CE, sedimentation rates decreased dramatically and abruptly, indicating a reduction in flood frequencies. Sedimentation rates subsequently increased again at ca. 1190 CE and persisted at a similar level until 1850 CE, suggesting that flooding frequencies increased during a time that overlapped with the Little Ice Age (LIA; 1250-1850 CE). Sedimentation rates increased again at ca. 1850 CE, reaching a 2000-year high (3.33 cm/yr) at 1970 CE and indicating a period characterized by frequent flooding and landscape erosion. The flood record from Goose Pond shows similarities with other Lower Ohio River flood reconstructions from Avery Lake, IL, and Hovey Lake, IN, suggesting the Goose Pond record reflects the regional flooding history for the lower Ohio River. Comparison with paleoclimate records from the Midwest supports the idea that lower Ohio River flood frequencies prior to Euro American occupation in the 1800s increased during times when winter precipitation predominated as a result of atmospheric circulation changes resembling the Pacific North vii American mode (PNA) that appear to have been driven in part by the Pacific Decadal Oscillation (PDO). Following Euro-American land clearance, lower Ohio River flooding increased dramatically despite a decrease in winter precipitation. This likely reflects an increase in runoff and erosion as a result of deforestation and landscape conversion to intensive row crop agriculture. As climate continues to change and the Midwestern United States continues to see an increase in precipitation, both winter and summer, flood frequencies could be expected to increase still further.

Isotopic investigations of speleothem CR1 from Cristal Cave in southeastern Brazil have established a high-resolution record of climate change extending 4,100 years prior to sample collection in 2007. A total of 14 subsamples were collected from CR1 for U/Th age determination. ICP-MS analysis yielded very precise ages with analytical errors (2σ) averaging ± 13 years. An initial growth rate of .062 mm y-1 for the first 2860 years is followed by a rate of .08 mm y-1 for the remaining growth period allowing for sampling of δ18O at sub-decadal resolution. Stable isotope analyses show a large range of δ18O values between -7.5 ‰ to -4 ‰. The data show a trend of steadily decreasing values over the past 4,000 y BP. The exception to this trend is the last 150 years BP when some of the least negative and most variable values for the record are observed. Variations in speleothem δ18O in southern Brazil have been shown to reflect changes in rainfall δ18O, which in turn indicate changes in rainfall source or rainfall amount (Cruz et al., 2006). In Southeastern Brazil, δ18O is controlled mainly by moisture source location, in particular South American monsoonal versus extratropical sources (Cruz et al., 2005). The relative contribution of monsoonal and extratropical moisture help to define the δ18O of regional precipitation via the mean location and southward extent of Hadley cell convective activity associated with the South American summer monsoon (Cruz et al., 2005). For example, decreases in precipitation δ18O are often interpreted as a decreased contribution of winter versus summer precipitation (Cruz et al., 2005). Assuming that the modern (observed) relationship between the seasonality and moisture source location effect occurring in southeastern Brazil have functioned for the past ~ 4,100 years, trends of more negative values towards modern day are likely due to increased summer precipitation and/or an overall increase in total yearly precipitation. The more enriched values of the past 100 years suggest a recent decrease in summer and/or total rainfall.

Approximately 5,000 years ago, eastern hemlock (Tsuga canadensis) experienced a sudden, rapid, range-wide decline most probably due to pest, disease, or climate change. An aphid-like defoliating insect, the hemlock woolly adelgid (Adelges tsugae), recently (1950’s) introduced to eastern North America has been spreading across the eastern United States. The adelgid attacks all size and age classes of hemlocks causing up to 95% mortality in affected stands. The potential for another range-wide hemlock decline has raised a number of concerns including the increased threat of wildfire. Altered fuel loadings in modern adelgid-affected stands and the effects of presumably similar changes in fuels and subsequently altered fire regimes following the prehistoric decline are examined. Fuels data from an adelgid-infested stand in Connecticut and an uninfested stand in Massachusetts were used to generate custom fuel models and predict fire behavior in each stand. Sediment cores were extracted from three sites in western Massachusetts and analyzed for fossil pollen and charcoal around the period of the prehistoric decline. Fossil data from two previously studied sediment cores from coastal Maine are included in the analysis. Results demonstrate a clear and highly significant increase in both fuel loadings and predicted fire behavior in the modern, adelgid-affected stand. Three of the coring sites reflect distinct, significant, short-lived increases in charcoal associated with the prehistoric decline; two do not. Results from the first three sites suggesting increased fire activity also were associated with changes in vegetation which indicate disturbance. Increased fire activity after the decline seems most pronounced in areas where fire was common before the decline. Results indicate that fire was not universally a significant factor driving post-decline succession. Research across a broader geographic area is needed to clarify the relationship between fire and hemlock following the mid-Holocene decline, but the results presented here suggest that managers of modern stands affected by the adelgid should include the possibility of intense fires as a threat to landscapes heavily affected by hemlock decline.

The small number and diffuse distribution of sites with intact Late Pleistocene/Early Holocene occupations in the Southeastern United States consequently makes examining Late Pleistocene/Early Holocene settlement patterning in the region difficult (Goodyear 1999). The Hester Site (22MO569), located in northeastern Mississippi, contains intact Late Pleistocene/Early Holocene deposits that can potentially afford archaeologists with a better understanding of late Pleistocene/early Holocene settlement in the region (Brookes 1979; Goodyear 1999:463-465). Investigations at Hester by Brookes (1979) revealed a stratified site containing artifacts that represented the late Paleoindian through Woodland periods in the Southeastern United States. Burris (2006) developed an alternative typology by re-analyzing the Hester biface assemblage, which demonstrated four discrete occupations at the Hester site. I use formation theory to evaluate the degree to which post-depositional processes have impacted the deposits at the Hester site. I have determined that the Hester site has not been significantly altered by post-depositional processes.

Big Bone Lick (BBL) is a late Pleistocene and Holocene fossil locality in the Ohio River valley of Kentucky. This study utilized stable isotopes (δ13C, δ18O, and 87Sr/86Sr) in tooth enamel to reconstruct mobility and diet in Bison, as well as diet in Bootherium bombifrons. Isotopic results from seven Bison and two B. bombifrons are reported. Results suggest Pleistocene Bison and Bootherium occupied different dietary niches. Although both had C3-dominated diets, Bison occupied more open environments than B. bombifrons. Two bison from the late Holocene deposit had diets that consisted of more C3 vegetation than Pleistocene bison, which may indicate these individuals occupied a closed C3 landscape. However, one specimen previously identified as late Holocene had diet and mobility patterns consistent with Pleistocene bison, which could indicate temporal mixing. Pleistocene and Holocene Bison have 87Sr/86Sr values that suggest they spent most of their time in places other than BBL.

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No description available.

<p>Ancient DNA has the power to elucidate ecological and evolutionary relationships that were previously only quantifiable by proxy. This work details both a metagenetic and a targeted metagenomic study of ancient sedimentary DNA. By using DNA to investigate the plants and animals present in twelve different time points, we describe the nature of the ecological change over the Pleistocene-Holocene transition. We show that as the stability of the habitat degraded due to climate change, the dominant plant communities exhibited a shift from functional groups such as forbs to shrubs and trees. As this cascading change consequently affected the animal communities, we demonstrate the decline, extinction, and replacement of a variety of megafaunal species and mammoths. As well, we provide a proof-ofconcept for the targeted oligonucleotide enrichment for ancient sedimentary DNA. By processing the same DNA extracts with targeted enrichment, we show that metagenomic soil DNA can provide the same taxonomic fingerprint unique to each time period even using different genetic loci. This unique pattern can be used as a reference in future studies. Although the oligonucleotide baits did not yield the composition of taxa that we expected, the oligonucleotide baits did increase the eukaryotic fraction of DNA extracts by up to 50%. Overall, this technique is open to further study and has fantastic potential to redefine the metagenomic work of ancient DNA soil cores.</p> / Master of Science (MSc)

The thesis is compilation of four manuscripts discussing the stable isotope analysis modem and archaeological faunal material from Namu, British Columbia. These studies concentrate on the application of stable isotopic analysis of biogenic material for paleonvironmental interpretation over the Holocene. The first study addresses the use of phosphate and carbonate associated oxygen isotopes in bioapatites (Sebastes spp. vertebrae) as a proxy for the isotopic composition of water from approximently 6,000 to 2,000 years before present (BP). The second study evaluates sclerochronological sampling strategies as applicable to the study of bivalves with implications for sampling fragmented material such as that found in archaeological deposits. The third study investigates stable isotopes composition of estuarine bivalve carbonate (Saxidomus gigantea) and the controlling environmental and biological factors. Finally, the fourth study uses a 5,000 year record of archaeological S. gigantea to provide a paleoclimatic record at Namu over the mid-late Holocene. / Thesis / Master of Science (MS)