Thesis advisor: Noah P. Snyder / Nitrogen is an important component in the biogeochemical processes of freshwater systems. Likewise, it is unknown if, and to what magnitude, changes in land use in the watersheds of New England lakes have affected nitrogen availability. This study examines the effects of land-use change on the present and historic isotopic signatures of nitrogen in three New England lakes of varied histories, Lower South Branch Pond, Little Kennebago Lake, and Sennebec Pond. The histories of all three sites indicate minimal discernible disturbance before the onset of Euro-American-induced land use change. For two sites, the dominant mechanism of change was timber harvest, which began in the latter half of the 19th century. Sediment cores for each site were examined and variations in geochemical and sedimentological indicators were evaluated in the context of changes within respective basins. Statistical analysis indicates significant shifts in the means and variance of the geochemistry within the Little Kennebago Lake and Sennebec Pond watersheds after the incursion of Euro-American settlers, while the Lower South Branch Pond watershed displays similarities to a more widespread signal of anthropogenic nitrogen that has been deposited remotely. The record of magnetic susceptibility in Little Kennebago Lake displays the largest variation compared to the other two lakes, which may indicate that the magnitude of land-use change within the basin was more impactful relative to Lower South Branch Pond and Sennebec Pond. This is significant in that all three sites experienced some level of land-clearance. / Thesis (MS) — Boston College, 2023. / Submitted to: Boston College. Graduate School of Arts and Sciences. / Discipline: Earth and Environmental Sciences.

Yes / Sampling of dentine for stable carbon (δ13 C) and nitrogen (δ15 N) isotope ratios in the direction of tooth growth allows the study of temporal changes to the diet and physiological stress of an individual during tooth formation. Current methods of sampling permanent teeth using 1mm increments provide temporal resolution of six - nine months at best depending on the tooth chosen. While this gives sufficient sample sizes for reliable analysis by mass spectrometry, sectioning the dentine across the incremental structures results in a rolling average of the isotope ratios. A novel method of incremental dentine collagen sampling has been developed to decrease the collagen increment size to 0.35mm along the incremental structures thus reducing averaging and improving the temporal resolution of short-term changes within the δ13 C and δ15 N values. This study presents data for a MicroMill-assisted sampling method that allows for sampling at 0.35mm width x 1mm depth increments following the incremental growth pattern of dentine. A NewWave MicroMill was used to sample the demineralised dentine section of modern donated human third molars from Sudan and compared to data from the same teeth using the 1mm incremental sectioning method 2 from Beaumont et al. (2013). The δ13 C and δ15 N isotopic data showed an increased temporal resolution, with each increment providing data for two-four months of dentine formation. The data show the potential of this method for studying dietary reconstruction, nutritional stress, and physiological change with greater temporal resolution potentially to seasonal level and with less attenuation of the δ13 C and δ15 N values than was previously possible from human dentine.

The work presented in this dissertation explores the nature of agro-pastoral strategies developed by Neolithic farmers as a way to understand how early food production was inter-twined with environmental and socio-economic opportunities and constraints. Towards this end, a multi-isotope approach is used to address questions of scale and intensity of crop cultivation and animal management at the archaeological sites of Kouphovouno, southern Greece, Makriyalos, northern Greece, and Çatalhöyük, south-central Turkey. Measurements of stable carbon, nitrogen, oxygen and strontium isotope values of carbonized plant remains, human and animal bone collagen and animal tooth enamel are used to examine the similarities and differences in the types of treatments that individual species of plants and animals received during the agricultural cycle at the distinct locations. The results show that farmers at the three sites developed variable methods for exploiting the arable and pastoral landscape and catering to their economic and culinary needs. The discussion considers the implications of these findings to our understanding of the complexity and adaptability of early farming systems.

Long-term diet patterns based on stable isotope analysis may be helpful to understand changes in food selection of black bears (Ursus americanus) over time and guide management programs to reduce human-bear conflicts. An enriched stable carbon isotope signature indicates an anthropogenic food source in the diet and an enriched nitrogen signature indicates a higher tropic level for a species. I examined longitudinal feeding patterns from 117 hair samples of black bears live captured in Great Smoky Mountains National Park during 1980–2001 using stable carbon and nitrogen isotope analysis from hair samples. I developed a set of a priori models to examine if sex, age class, year, weight class, total hard mast index, white oak index (Quercus spp.), red oak index (Quercus spp.), nuisance status and hog harvest (Sus scrofa) affected stable isotope signatures. I used model averaging and an estimator of the unconditional variance was used to account for model uncertainty. The δ[delta]13C signatures differed by weight class with above average weight, (ß[Beta] = 0.76‰; 95% CI = 0.28 to 1.23) and average weight (ß[Beta] = 0.42‰; CI = 0.06 to 0.78) showing enriched values compared to below average bears. Bears had enriched δ[delta]15N signatures in years with low white oak mast production (ß[beta] = -0.19, CI = -0.34 to -0.03) and depleted when white oak hard mast was abundant. Sub adult bears had enriched δ[delta]15N signatures compared to adult and older adult bears. Variation of nitrogen values was small during 1980–1991 ( = 2.57, SD = 0.28) but increased substantially during 1992–2000 ( = 2.29, SD = 0.71) when there was substantial variation in hard mast production. Bears in better physical condition appear more likely to access anthropogenic food sources. In years of low white oak acorn production, the larger bears and sub adult bears are more likely to turn to alternative food sources. The long term variation detected in this study is important in identifying which bears are potentially more likely to seek out the anthropogenic food sources when changes occur in availability of natural foods.

Perm/Trias-Grenzprofile in den Regionen von Julfa (NW-Iran) und Abadeh (Zentral-Iran) zeigen eine Abfolge von drei charakteristischen Gesteinseinheiten, (1) den Paratirolites Limestone mit dem end-permischen Massensterbehorizont an seiner Oberkante, (2) den Boundary Clay und (3) die untertriassische Elikah-Formation mit der mit Conodonten definierten Perm/Trias-Grenze an seiner Basis. Die Karbonatmikrofazies zeigt eine Veränderung in den Profilen bei Julfa; innerhalb des Paratirolites Limestone ist eine zunehmende Anzahl von Intraklasten, Fe-Mn-Krusten und biogenen Verkrustungen erkennbar. Die Karbonatproduktion des späten Perms wurde mit der Ablagerung von mikrobiellen Karbonaten an der Basis der Elikah-Formation in Julfa erneuert. Die in den Profilen von Baghuk (Abadeh-Region) vorkommenden Mikrobialite sind vielfältig; es gibt groß-und kleinskalige, arboreszierendende Mikrobialit-Ansammlungen mit auffälliger Morphologie und innerer Struktur. In den Regionen von Julfa (NW-Iran) und Abadeh (Zentral-Iran) deutet eine deutliche und weltweit nachvollziehbare negative Kohlenstoffisotopenexkursion hin. Die rasche Exkursion der Kohlenstoffisotopenexkursion unterhalb des Aussterbehorizonts im obersten Bereich des Paratirolites Limestone wird durch eine stratigraphische Kondensation, die ein Defizit der Karbonatproduktion/Akkumulation und/oder eine schnelle geochemische Veränderung in Richtung Karbonatuntersättigung spiegelt, verstärkt. Dies deutet darauf hin, dass ein länger andauernder Mechanismus, wie die thermische Metamorphose von an organischem Material reicher Sedimente, und/oder verstärkte Verwitterung auf den Kontinenten, die negative Perm/Trias- Kohlenstoffisotopenexkursion verursacht haben könnte. Die Stickstoffisotopenwerte zeigen keinen Trend unterhalb des Aussterbehorizonts, was auf eine Kombination verschiedener Prozesse (Stickstofffixierung und ein Gleichgewichtszustand zwischen Nitratassimilation, Stickstoff-Fixierung und Denitrifikation) hinweist. / Permian-Triassic boundary sections in the Julfa (NW Iran) and Abadeh (Central Iran) regions display a succession of three characteristic rock units, (1) the Paratirolites Limestone with the end-Permian mass extinction horizon at its top, (2) the Boundary Clay, and (3) the Early Triassic Elikah Formation with the conodont Permian-Triassic boundary at its base. The carbonate microfacies reveals a change, in the sections near Julfa, within the Paratirolites Limestone with an increasing number of intraclasts, Fe-Mn crusts, and biogenic encrustation. A decline in carbonate accumulation occurs towards the top of this unit, finally resulting in a complete demise of the carbonate factory. The skeletal carbonate factory was restored with the deposition of microbial carbonates at the base of the Elikah Formation at Julfa. At Baghuk Mountain (Abadeh region) large- and small-scale, arborescent microbialite buildups with conspicuous morphology and internal structure occur. In the Julfa and Abadeh regions, a prominent and globally traceable negative carbon isotope excursion indicates major perturbations of the carbon cycle around the P-Tr boundary. The sudden carbonate carbon isotope decrease below the extinction horizon is triggered by stratigraphic condensation that mirrors a deficit of the carbonate production/accumulation and/or a rapid geochemical change towards carbonate undersaturation. The negative carbon isotope trend before extinction horizon is gradual, suggesting that a longer lasting mechanism, such as thermal metamorphism of organic-rich sediments, and/or enhanced weathering on the continents may have caused the negative Permian-Triassic stable carbon isotope excursion. The bulk nitrogen isotope values in the sections of the Julfa region do not show any trend below the extinction horizon, pointing to rather mixing of different processes (nitrogen fixation and an equilibrium state between nitrate assimilation, nitrogen fixation, and denitrification).