The residents of Union City, NJ— a 1.2 square mile metropolis across the Hudson from Manhattan—are fond of taking to the task of adorning their city streets on their own. In the business sector of the city (that is to say, most of it) the business owners garnish their windows with red, white, and blue, and more often than not their decoration is accompanied by the uncomfortably warm smile of a middle-aged bespectacled Irish man. The man, so comically out of place in the majority Spanish-speaking, 82.3% Latino city, is referred to interchangeably as Mayor and State Senator Brian P. Stack. On the city’s border is official proof of his status on the “Welcome to Union City” sign, mirrored by its North Bergen, NJ counterpart and the name Nicholas Sacco: mayor, state senator, assistant superintendent of North Bergen schools, and principal of Horace Mann Elementary. For decades, New Jersey politicians have viewed multiple office holding as an integral part of the urban power structure. To rise up in the totem pole, one must collect public office jobs until rising to one high enough to stand on its own. While not particularly common in the less populated areas of the state, urban centers like the aforementioned Hudson County, Newark, and Camden have a tradition of sending their leaders off to Trenton without making them relinquish their jobs at home. And yet it was these very state legislators that passed a ban on the practice into law in February 2008. Supported by senator-turned-governor Jon Corzine, the ban passed with the support of political leaders like Stack and Sacco. On paper and in the pages of the New York Times it read like a rare and barely believable victory for political morality in what longtime NJ political journalists Bob Ingle and Sandy McClure call “The Soprano State”. If it sounded barely believable, it is probably because in practice it was not. A grandfather clause in the law keeps those currently in two positions of power safe from the wrath of the law. And since elections were held in between the passing of the law and the enacting of it, there are actually more dual office holders in the Legislature today than there were when the law was passed according to state newspaper the Star Ledger. This study intends answer several questions regarding the phenomenon of multiple office holding and its sudden “extinction” in New Jersey. I hypothesize that the introduction of such a law was merely cashing in on a long-standing bit of political credit that, due to the highly salient role of the practice in building machines, could not be touched. As the number of political bosses engaging in this practice diminished, and as the need to hold various offices lessened because of an increase in income and power from other sources, dual office holding became an obsolete relic of the 1990s political machine structures. Thus it became feasible to ban the practice with a grandfather clause for those that had established themselves through this old system, with much credit in the field of ethics to be gained by all involved—every dual office holder, legislator, and the governor himself. On a micro level, it aspires to investigate why early 2008 was an opportune time for such a law and where this grandfather clause arouse from and why. Although the tradition has existed previously in less populated areas of New Jersey, especially in the 1940s, at some point (peaking in the 1990s) dual office holding became an essential component in the structure of an urban political machine. On a macro level, this study seeks to explain the place of such a practice in the creation and maintenance of the traditional urban political machine, a structure with a lush history in New Jersey that is still alive and kicking today. It attempts to begin a dialogue with existing literature on urban politics centered around the practice of dual office holding. To do this, the study needs to paint as vivid a portrait as possible of the modern urban political machine, its bosses, and every gear that moves its structure. For this it will heavily rely on literature describing the initial development of political machines of Tammany Hall and similar structures around the country, paying especial attention to the impact of immigration, given that preliminary research is showing a pronounced impact on the system from the wave of Latino immigrants beginning with the rise of the Cuban Revolution in 1958. This new wave of immigrants appears to have jump-started the machines and replenished them with an entire new wave of fodder ready to be introduced to the patronage system post-naturalization (a matter of five years’ time). Of particular note in this body of urban political research is Steven Erie’s Rainbow’s End, which I have discovered to be the definitive work in the field of immigration and its impact on urban political machines. Working with this broad field of urban politics in mind, I also intend on illustrating in detail the specific political machine structures of the three largest urban communities in New Jersey: Newark, Camden, and the general Hudson County area (as the cities of Hudson County tend to be about 1-2 square miles in area excepting Jersey City, there is little that distinguishes one from another culturally and politically). In order to do this, I must work with data specific to the state, beginning with a database of multiple office holders over time. I have constructed this database over the course of several decades and am currently developing it in the 1930s using biographical sketches in the New Jersey Legislative Manuals published yearly in the New Jersey State Archives of Trenton. Unfortunately, this means that my research is limited to multiple office holders who have one job in the state legislature, but as all signs point to most dual office holders preferring to have a state and local job rather than two of either, I do not believe this will seriously hinder my research. Supplementary research will also come from personal stories, which I plan on gathering from interviews with those deeply involved in urban politics. The study will include interviews with multiple office holders from these regions themselves, as well as those close to them—journalists, chiefs of staff, and those receiving patronage and practicing loyalty to the leaders. The goal of this study is to shed some light on the dark, backroom world of urban politics through the lens of this one common practice among the machine leaders. This one practice, currently a topic of much controversy due to this recent law, could very well be the key to understanding the development of machines, their power over citizens and their ability to maintain themselves over such extended periods of time.

Pleistocene New Jersey shelf sedimentology is strongly influenced by glacially driven sea level changes. A combination of regressive shoreline processes, subaerial exposure, fluvial downcutting, and deposition and reworking during transgression has influenced the NJ shelf sediment composition. Sediment provenance and transport history may be determined on a shelf environment through analysis of grain size distribution, heavy mineral content, magnetic mineral concentrations, and isotopic dating methods. A combination of surface grab and stratigraphic samples were analyzed within the study area. Relatively high percentages of heavy minerals were found in the 2 phi and 3 phi size fractions and hornblende grains provided K-Ar age values indicating two groups of sediment sources. The first source is Grenville with apparent ages above 900 Ma deposited during marine OIS 1. The second source is a mixed assemblage of Grenvillian and Paleozoic sources deposited during marine OIS 3, with apparent ages of approximately 850 ± 20 Ma.

The goal of this thesis was to test the applicability of biomarker analyses to better understand the glacial stratigraphic record of the Hudson Bay Lowlands and Oak Ridges Moraine. A biomarker analysis conducted on three geologic deposits from the Hudson Bay Lowlands showed that they can be differentiated based on organic matter (OM) inputs and stage of diagenesis, relating to paleoclimate and depositional environments. In the second study, a biomarker analysis was applied to samples from ten deposits in the Oak Ridges Moraine. These deposits were differentiated based on OM inputs relating to paleovegetation. Additionally, reincorporation and post-deposition alteration led to sample heterogeneity confirming the current understanding of glacial depositional processes and environments. This thesis shows that biomarker analyses can effectively differentiate and contextualize geologic deposits based on OM inputs and stage of diagenesis. This in turn will provide a more robust understanding of the stratigraphic record.

The goal of this thesis was to test the applicability of biomarker analyses to better understand the glacial stratigraphic record of the Hudson Bay Lowlands and Oak Ridges Moraine. A biomarker analysis conducted on three geologic deposits from the Hudson Bay Lowlands showed that they can be differentiated based on organic matter (OM) inputs and stage of diagenesis, relating to paleoclimate and depositional environments. In the second study, a biomarker analysis was applied to samples from ten deposits in the Oak Ridges Moraine. These deposits were differentiated based on OM inputs relating to paleovegetation. Additionally, reincorporation and post-deposition alteration led to sample heterogeneity confirming the current understanding of glacial depositional processes and environments. This thesis shows that biomarker analyses can effectively differentiate and contextualize geologic deposits based on OM inputs and stage of diagenesis. This in turn will provide a more robust understanding of the stratigraphic record.

In 2005, box cores were collected throughout the Hudson Bay and Strait. A detailed micropaleontological data set has been generated from these cores for this study and is combined with geochemical and geochronological data to observe temporal and spatial oceanographic changes throughout the bay and strait. All of the cores show an increase in tintinnid species and agglutinated foraminifera, and coincident decreases in calcareous foraminifera in younger core sections. In general, these microfossil trends are correlated with higher organic matter content of the younger core sections. This results from a more extensive freshwater plume that causes lowered pH in the superficial sediments and conditions less favourable for the preservation of calcareous tests. Furthermore, with a 14C age constraint in one of the cores, the mid-Holocene depositional and paleoceanographic history is represented, and provides evidence of marine invasion by 7100 cal yrs BP.

The objectives of this study were to test for the feasibility of satellite radio-tracking of golden eagles (Aquila chrysaetos) breeding in the Grande-Baleine hydro-electric study area, to assess the size of their home-ranges, to determine their food habits during the nesting season, and to describe migration routes and wintering grounds of these birds. / In June and August 1992, six golden eagles, of which 5 adults (4$ rm sp{o}$ + 1 sex unknown), were caught and fixed with transmitters in order to follow their movements over one year. / The golden eagles fed on various animal species, i.e. 8 mammals, 15 birds and one fish, during the breeding season, however Canada geese (Branta canadensis) were the main item in their diet. / Four of the adult eagles undertook their fall migration in October 1992. The other adult eagle died of an unknown cause while the fate of the nestling could not be determined. All the migratory birds moved south to the United States, but they used different migration routes. The four golden eagles reached their wintering grounds in November and December, 1992. / After a three to four month stay in the wintering area, three eagles undertook their spring migration in March 1993. When returning to the breeding area, two of the eagles followed the same migration routes used in fall, while the third one flew off course to the west into Ontario. The first two birds reached their former territories in March and April while the third eagle only arrived in mid-May 1993.

This study looks at characterizing the terrigenous OC sources, like permafrost, of POC and DOC through 17 rivers and six soils of the Hudson Bay (HB) using lignin biomarkers, and Δ14C. Our findings show the dominance of the OC flux (89%) from the southwest Hudson Bay Rivers, especially from DOC (93%), shedding light on the sources and fate of OC in HB sediments. With warming, organic cryosols, with high OC content in the Cz horizon, have the potential to release as much as 1.5 gOC/m2 for every cm increase in active layer depth. The [Ad/Al] ratios, when combined with 14C ages of DOM, show that older SOC is being released in some rivers and is fresher than expected due to its preservation within permafrost. S/V and C/V ratios, are well correlated to latitude in DOM, reflecting the vegetation in their drainage basins and can be used to indicate OC sources.

The repercussions of climate change are felt worldwide, but Arctic and subarctic regions, where climate warming is expected to be amplified, are especially vulnerable. An episode of mass fish mortality in the Sutton River in the Hudson Bay Lowlands (HBL) of Northern Ontario has elicited the interest of the scientific community. Several lakes were sampled over three years in an effort to better understand and document the changes that may be occurring in these lakes. This study uses sediment cores to assess the history of mercury (Hg) deposition and to assess changes occurring in autochthonous productivity in these lakes. Sediments deposited after the onset of the industrial revolution contained significantly higher concentrations of Hg, with the highest concentrations found in the most recently deposited sediments. Hg concentrations in these pristine lakes rival those of lakes in heavily urbanized areas, indicating that they are in fact subjected to atmospheric deposition of Hg. There was a large variation in [Hg] of the surface sediments of 13 lakes; underscoring the importance of in situ processes in the fate of atmospherically deposited Hg. Methylmercury (MeHg) concentrations were not correlated with total mercury concentrations (THg), demonstrating how THg is a poor predictor of MeHg; the bioaccumulative neurotoxic form of mercury. The S2 fraction of Rock-Eval® Pyrolysis, C:N ratios and ∂13C signatures were used as proxies of autochthonous carbon and all indicated that the lakes have become increasingly productive, presumably due to warmer water temperatures and longer ice-free seasons. Additionally, I use molecular techniques to detect and quantify the merA gene in the sediment; a proxy of bacterial mercury resistance involved in redox transformations. In Aquatuk, Hawley and North Raft Lakes, I observed a subsurface increase in merA genes in the sediment core, independently of a control gene and the [THg]. While I have not been able to explain the driving variables of this subsurface increase, I believe that the role of merA within remote lake sediments deserves further work. Lastly, microcosms were used to measure the production of volatile elemental mercury (Hg(0)) from surface sediments of Aquatuk Lake. I used a combination of analytical and molecular techniques to show that the production of Hg(0) is biogenic and tested the effect of nutrients, pH and ionic strength on the Hg(0) production rates. Ionic strength alone had the greatest impact on Hg(0) production rates, with increased Hg(0) production as ionic strength increases.

Thesis (Ph. D.)--New York University, 1974. / eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 113-125).

Thesis (Ph. D.)-- State University of New York at Binghamton, Department of Geological Sciences and Environmental Studies, 2009.