New Insights from Aperiodic Variability of Young Stars

Nearly all young stars are variable, with the variability traditionally divided into two classes: periodic variables and aperiodic or "irregular" variables. Periodic variables have been studied extensively, typically using periodograms, while aperiodic variables have received much less attention due to a lack of standard statistical tools. However, aperiodic variability can serve as a powerful probe of young star accretion physics and inner circumstellar disk structure. For my dissertation, I analyzed data from a large-scale, long-term survey of the nearby North America Nebula complex, using Palomar Transient Factory photometric time series collected on a nightly or every few night cadence over several years. This survey is the most thorough exploration of variability in a sample of thousands of young stars over time baselines of days to years, revealing a rich array of lightcurve shapes, amplitudes, and timescales.

I have constrained the timescale distribution of all young variables, periodic and aperiodic, on timescales from less than a day to ~100 days. I have shown that the distribution of timescales for aperiodic variables peaks at a few days, with relatively few (~15%) sources dominated by variability on tens of days or longer. My constraints on aperiodic timescale distributions are based on two new tools, magnitude- vs. time-difference (Δm-Δt) plots and peak-finding plots, for describing aperiodic lightcurves; this thesis provides simulations of their performance and presents recommendations on how to apply them to aperiodic signals in other time series data sets. In addition, I have measured the error introduced into colors or SEDs from combining photometry of variable sources taken at different epochs. These are the first quantitative results to be presented on the distributions in amplitude and time scale for young aperiodic variables, particularly those varying on timescales of weeks to months.

Regional variations in upper mantle structure beneath North America

Several types of seismological data, including surface wave group and phase velocities, travel times from large explosions, and teleseismic travel time anomalies, have indicated that there are significant regional variations in the upper few hundred kilometers of the mantle beneath continental areas. Body wave travel times and amplitudes from large chemical and nuclear explosions are used in this study to delineate the details of these variations beneath North America.

As a preliminary step in this study, theoretical P wave travel times, apparent velocities, and amplitudes have been calculated for a number of proposed upper mantle models, those of Gutenberg, Jeffreys, Lehman, and Lukk and Nersesov. These quantities have been calculated for both P and S waves for model CIT11GB, which is derived from surface wave dispersion data. First arrival times for all the models except that of Lukk and Nersesov are in close agreement, but the travel time curves for later arrivals are both qualitatively and quantitatively very different. For model CIT11GB, there are two large, overlapping regions of triplication of the travel time curve, produced by regions of rapid velocity increase near depths of 400 and 600 km. Throughout the distance range from 10 to 40 degrees, the later arrivals produced by these discontinuities have larger amplitudes than the first arrivals. The amplitudes of body waves, in fact, are extremely sensitive to small variations in the velocity structure, and provide a powerful tool for studying structural details.

Most of eastern North America, including the Canadian Shield has a Pn velocity of about 8.1 km/sec, with a nearly abrupt increase in compressional velocity by ~ 0.3 km/sec near at a depth varying regionally between 60 and 90 km. Variations in the structure of this part of the mantle are significant even within the Canadian Shield. The low-velocity zone is a minor feature in eastern North America and is subject to pronounced regional variations. It is 30 to 50 km thick, and occurs somewhere in the depth range from 80 to 160 km. The velocity decrease is less than 0.2 km/sec.

Consideration of the absolute amplitudes indicates that the attenuation due to anelasticity is negligible for 2 hz waves in the upper 200 km along the southeastern and southwestern margins of the Canadian Shield. For compressional waves the average Q for this region is > 3000. The amplitudes also indicate that the velocity gradient is at least 2 x 10^-3 both above and below the low-velocity zone, implying that the temperature gradient is < 4.8°C/km if the regions are chemically homogeneous.

In western North America, the low-velocity zone is a pronounced feature, extending to the base of the crust and having minimum velocities of 7.7 to 7.8 km/sec. Beneath the Colorado Plateau and Southern Rocky Mountains provinces, there is a rapid velocity increase of about 0.3 km/sec, similar to that observed in eastern North America, but near a depth of 100 km.

Complicated travel time curves observed on profiles with stations in both eastern and western North America can be explained in detail by a model taking into account the lateral variations in the structure of the low-velocity zone. These variations involve primarily the velocity within the zone and the depth to the top of the zone; the depth to the bottom is, for both regions, between 140 and 160 km.

The depth to the transition zone near 400 km also varies regionally, by about 30-40 km. These differences imply variations of 250 °C in the temperature or 6 % in the iron content of the mantle, if the phase transformation of olivine to the spinel structure is assumed responsible. The structural variations at this depth are not correlated with those at shallower depths, and follow no obvious simple pattern.

The computer programs used in this study are described in the Appendices. The program TTINV (Appendix IV) fits spherically symmetric earth models to observed travel time data. The method, described in Appendix III, resembles conventional least-square fitting, using partial derivatives of the travel time with respect to the model parameters to perturb an initial model. The usual ill-conditioned nature of least-squares techniques is avoided by a technique which minimizes both the travel time residuals and the model perturbations.

Spherically symmetric earth models, however, have been found inadequate to explain most of the observed travel times in this study. TVT4, a computer program that performs ray theory calculations for a laterally inhomogeneous earth model, is described in Appendix II. Appendix I gives a derivation of seismic ray theory for an arbitrarily inhomogeneous earth model.

Legitimaciones sociales de las políticas patrimoniales y museísticas

Cap. 1. Proyectos patrimoniales y museísticos en las sociedades democráticas y capitalistas: entre la legitimación formal y la vinculación social. Iñaki Arrieta Urtizberea. Cap. 2. Musées et patrimoine immatériel au Québec : enjeux politiques et sociaux. Laurier Turgeon. Cap. 3. “El patrimonio pertenece a todos”. De la universalidad a la identidad, ¿cuál es el lugar de la participación social? Victoria Quintero Morón. Cap. 4. La legitimación social y política de los museos: dos casos del estado de Oaxaca, México. Teresa Morales Lersch y Cuauhtémoc Camarena Ocampo. Cap. 5. Reinterpretaciones de la misión social de los museos: políticas de la cultura en la red de museos de Loures, Portugal. Marta Anico. Cap. 6. La comunicación de los museos y sus relaciones con las políticas culturales de las ciudades. Entre la repetición de estrategias y la innovación. Daniel Paül i Agustí. Cap. 7. El Patrimonio de la Guerra Civil como útil de concienciación social al amparo de la Ley de la Memoria Histórica. Óscar Navajas Corral y Julián González Fraile. Cap. 8. Política y planificación museística, y participación social en Cataluña: un breve recorrido histórico y algunas reflexiones. Daniel Solé i Lladós. Cap. 9. Diagnóstico de las acciones de los museos catalanes como parte de las políticas de integración. Fabien Van Geert. Cap. 10. Los inexistentes alcornocaleños y las experiencias museísticas etnográficas en el Parque Natural Los Alcornocales. Agustín Coca Pérez.

Using Earth Deformation Caused by Surface Mass Loading to Constrain the Elastic Structure of the Crust and Mantle

Surface mass loads come in many different varieties, including the oceans, atmosphere, rivers, lakes, glaciers, ice caps, and snow fields. The loads migrate over Earth's surface on time scales that range from less than a day to many thousand years. The weights of the shifting loads exert normal forces on Earth's surface. Since the Earth is not perfectly rigid, the applied pressure deforms the shape of the solid Earth in a manner controlled by the material properties of Earth's interior. One of the most prominent types of surface mass loading, ocean tidal loading (OTL), comes from the periodic rise and fall in sea-surface height due to the gravitational influence of celestial objects, such as the moon and sun. Depending on geographic location, the surface displacements induced by OTL typically range from millimeters to several centimeters in amplitude, which may be inferred from Global Navigation and Satellite System (GNSS) measurements with sub-millimeter precision. Spatiotemporal characteristics of observed OTL-induced surface displacements may therefore be exploited to probe Earth structure. In this thesis, I present descriptions of contemporary observational and modeling techniques used to explore Earth's deformation response to OTL and other varieties of surface mass loading. With the aim to extract information about Earth's density and elastic structure from observations of the response to OTL, I investigate the sensitivity of OTL-induced surface displacements to perturbations in the material structure. As a case study, I compute and compare the observed and predicted OTL-induced surface displacements for a network of GNSS receivers across South America. The residuals in three distinct and dominant tidal bands are sub-millimeter in amplitude, indicating that modern ocean-tide and elastic-Earth models well predict the observed displacement response in that region. Nevertheless, the sub-millimeter residuals exhibit regional spatial coherency that cannot be explained entirely by random observational uncertainties and that suggests deficiencies in the forward-model assumptions. In particular, the discrepancies may reveal sensitivities to deviations from spherically symmetric, non-rotating, elastic, and isotropic (SNREI) Earth structure due to the presence of the South American craton.

Calidad de vida de las mujeres en America Latina. Ecuador y Bolivia

El presente trabajo pretende abordar la situación actual de las mujeres de América Latina centrándose en su calidad de vida como forma de argumentar la desigualdad en la que viven con respecto a los hombres. Para ello, se analizará los entornos en los cuales las mujeres latino americanas experimentan un sentimiento de inferioridad con respecto a los hombres. Como forma de dar veracidad y buscar la conexión con estos argumentos, previamente se expondrán tres conceptos teóricos relativos al enfoque de las capacidades, la agencia de las mujeres y el empoderamiento de las mismas puesto que resultan conceptos muy importantes y necesarios para entender las condiciones de inferioridad en las que se sitúan las mujeres de estas regiones. Por último y con el objetivo de buscar posibilidades de cambio, se presentan dos ejemplos de proyectos por la igualdad de género protagonizados por Bolivia y Ecuador, países que por diversos factores como son los cambios de gobierno que han experimentado o la incidencia de los movimientos feministas, se han encaminado hacia la labor de la lucha por la igualdad. Tanto los desafíos a los que ambos países han de enfrentarse como la importancia de los levantamientos feministas por el cambio serán también abordados aunque de forma más breve.

Inversion extranjera directa en America Latina y el Caribe: el caso de Brasil

[ES] Evolución de la inversión extranjera directa en América Latina y el Caribe, con especial interés en el caso de Brasil

Otolith morphometrics and population structure of Pacific sardine (Sardinops sagax) along the west coast of North America

The broad distribution of Pacific sardine (Sardinops sagax) along the Pacif ic coast of North America makes it difficult for fisheries managers to identify regional stocks of this dominant small pelagic species. An investigation of morphometric characteristics of otoliths of Pacific sardine across most of their range revealed regional differences in populations. In a survey of over 2000 otoliths, all ages (with an emphasis on age-1 recruits) were compared. Principal components analysis, multivariate analysis of variance, and a novel method derived from regression and residuals calculations, termed perimeter-weight profiles (PWPs), revealed otolith similarities and differences. The results of the different approaches to statistical comparisons did not always agree. Sardine otoliths from Mexican waters were generally lighter and more lobate than those from U.S. and Canadian populations. Age-1 otoliths from northern California in 2006–07 tended to be heavier and smoother than those from other areas, including year-class cohorts from southern California. Comparisons of age-groups and year-classes of northern California otoliths with the use of the PWP models indicated signif icant trends in year-to-year patterns. In conjunction with other established indices of population structure, otolith PWPs are a useful tool for identifying local and regional stocks of Pacific sardine and may help distinguish populations of other fish species as well.

Ocean distribution of the American shad (Alosa sapidissima) along the Pacific coast of North America

We examined the incidental catches of American shad (Alosa sapidissima) taken during research cruises and in commercial and recreational landings along the Pacific coast of North America during over 30 years of sampling. Shad, an introduced species, was mainly found over the shallow continental shelf, and largest catches and highest frequency of occurrences were found north of central Oregon, along the coasts of Washington and Vancouver Island, and in California around San Francisco Bay. Migrations to the north off Washington and Vancouver were seen during spring to fall, but we found no evidence for large-scale seasonal migrations to the south during the fall or winter. The average weight of shad increased in deeper water. Sizes were also larger in early years of the study. Most were caught over a wide range of sea surface temperatures (11–17°C) and bottom temperatures (6.4–8.0°C). Abundance of shad on the continental shelf north of 44°N was highly correlated with counts of shad at Bonneville Dam on the Columbia River in the same year. Counts were negatively related to average weights and also negatively correlated with the survival of hatchery coho salmon (Oncorhynchus kisutch), indicating that survival of shad is favored by warm ocean conditions. Examining the catch during research cruises and commercial and recreational landings, we concluded that American shad along the Pacific coast have adapted to the prevailing environmental conditions and undertake only moderate seasonal migrations compared with the long seasonal migrations of shad along the Atlantic coast of North America. We suggest that the large spawning populations in the Columbia River and San Francisco Bay areas explain most of the distributional features along the Pacific coast.

Day and night abundance, distribution, and activity patterns of demersal fishes on Heceta Bank, Oregon

Most shallow-dwelling tropical marine fishes exhibit different activity patterns during the day and night but show similar transition behavior among habitat sites despite the dissimilar assemblages of the species. However, changes in species abundance, distribution, and activity patterns have only rarely been examined in temperate deepwater habitats during the day and night, where day-to-night differences in light intensity are extremely slight. Direct-observation surveys were conducted over several depths and habitat types on Heceta Bank, the largest rocky bank off the Oregon coast. Day and night fish community composition, relative density, and activity levels were compared by using videotape footage from a remotely operated vehicle (ROV) operated along paired transects. Habitat-specific abundance and activity were determined for 31 taxa or groups. General patterns observed were similar to shallow temperate day and night studies, with an overall increase in the abundance and activity of fishes during the day than at night, particularly in shallower cobble, boulder, and rock ridge habitats. Smaller schooling rockfishes (Sebastes spp.) were more abundant and active in day than in night transects, and sharpchin (S. zacentrus) and harlequin (S. variegatus) rockfish were significantly more abundant in night transects. Most taxa, however, did not exhibit distinct diurnal or nocturnal activity patterns. Rosethorn rockfish (S. helvomaculatus) and hagfishes (Eptatretus spp.) showed the clearest diurnal and nocturnal activity patterns, respectively. Because day and night distributions and activity patterns in demersal fishes are likely to influence both catchability and observability in bottom trawl and direct-count in situ surveys, the patterns observed in the current study should be considered for survey design and interpretation.

Atividade in vitro da pterocarpanoquinona LQB-118 sobre o Trypanosoma cruzi

A doença de Chagas é endêmica na América Latina sendo considerada uma doença negligenciada com grande impacto socioeconômico. A infecção é causada pelo protozoário Trypanosoma cruzi que é transmitido pela forma vetorial, entre outros mecanismos. O tratamento consiste basicamente no uso de dois fármacos, o benznidazol e o Nifurtimox que apresentam uma série de efeitos colaterais e atuam muito pouco nas formas amastigotas intracelulares o que faz com que o tratamento atual seja restrito e insatisfatório.Várias atividades farmacológicas foram atribuídas ao lapachol e a pterocarpanos, tais como atividade antitumoral e antiparasitária. Devido a esse potencial foi sintetizado uma molécula híbrida, a pterocarpanoquinona LQB-118, e algumas moléculas derivadas. A LQB-118 mostrou anteriormente atividade antitumoral e anti-Leishmania. O objetivo do presente trabalho foi investigar a atividade in vitro da LQB-118 e suas moléculas derivadas sobre o Trypanosoma cruzi clone Dm28c. Para avaliação inicial do efeito anti-parasitário das moléculas, amastigotas intracelulares, tripomastigotas metacíclicos e epimastigotas foram incubados com 20 M das LQBs 118, 168, 187, 182 e 236. A LQB-118 demonstrou atividade antiparasitária nas três formas evolutivas (90% na forma amastigota, 44% na forma tripomastigota e 70% na forma epimastigota) do parasito, enquanto as moléculas derivadas não mostraram atividade significativa. Sendo assim os estudos foram continuados com a molécula LQB-118. A ação da LQB-118 sobre as amastigotas intracelulares foi dose dependente, com redução do índice de infecção em 81% e 88% nas concentrações de 20 e 30 M respectivamente. Já sobre tripomastigotas, a LQB-118 foi menos ativa reduzindo a mobilidade dessas formas em até 45% a 30 M. Sobre a forma epimastigota a ação foi dose-dependente chegando a inibir 96% o crescimento dos parasitos a 20 M, com alterações da morfologia tais como arrendondamento do corpo celular e perda do flagelo. A dose capaz de inibir 50% foi de 4,2 M para amastigota intracelular e 38,1 M para tripomastigotas. Para macrófagos, a LC50 ficou em 40 M, uma concentração quase dez vezes maior que a IC50 para amastigotas. A capacidade das formas amastigotas intracelulares se diferenciarem em tripomatigotas e lisar os macrófagos foi avaliada após o tratamento com a LQB-118 por 72h. Observou-se um atraso do ciclo intracelular do parasito de modo dose-dependente, onde na concentração de 30 M o surgimento de tripomastigota foi no 9 dia enquanto nos controles foi no 5 dia de cultura. Para delinear o mecanismo de ação, foi avaliado o efeito direto sobre o parasito como a indução da fragmentação de DNA. A análise de indução da fragmentação do DNA feita pela marcação pelo TUNEL mostrou que o tratamento com a LQB-118 induziu seletivamente a fragmentação do núcleo das amastigotas enquanto o núcleo dos macrófagos se mantiveram íntegros. Macrófagos peritoneais pré-tratados com LQB-118 por 24 horas foram capazes de reduzir o número de amastigotas após 72h de cultivo na ausência da molécula, mas sem alteração na produção de óxido nítrico. Esses resultados mostram que a LQB-118 é ativa contra o T. cruzi, principalmente sobre a forma amastigota intracelular, que é a forma presente na fase crônica da infecção. O mecanismo de ação sugere que a LQB-118 é capaz de ser seletivamente tóxica para o parasito e também ativar os mecanismos microbicidas dos macrófagos de modo independente da produção de óxido nítrico.

Efeito antimutagênico, antigenotóxico, antiobesidade e antioxidante da Ilex paraguariensis (erva-mate)

O extrato aquoso de erva-mate, obtido a partir de folhas secas de Ilex paraguariensis, é uma bebida amplamente consumida na América do Sul. Inicialmente, nosso objetivo foi caracterizar os compostos presentes nas amostras de erva-mate disponíveis no mercado brasileiro (CH: chimarrão; T: chá mate torrado; G: chá mate torrado, comercialmente acondicionado em garrafas ou C: em copos; TS: chá mate torrado solúvel A mutagenicidade, citotoxicidade e antimutagenicidade de todas as amostras também foram avaliadas atavés do Teste de Ames na presença e na ausência de ativação metabólica. Em seguida, analisamos a amostra TS (2,5, 5,0 e 10 mg/mL) quanto a sua atividade antioxidante e antigenotóxica. Além disso, avaliamos também os efeitos da amostra TS sobre a sinalização da leptina e da insulina no hipotálamo e o estresse oxidativo hepático de ratos adultos obesos programados pela superalimentação neonatal (S). Para induzir S, o tamanho da ninhada foi reduzido a três filhotes por lactante e as ninhadas com número padrão de filhotes (dez/lactante) foram utilizadas como controle. Aos 150 dias de vida, as proles S foram subdivididas em: TS - tratados com extrato aquoso de erva-mate (1g/kg de peso corporal/dia, por gavagem) e S - recebendo água por gavagem durante 30 dias. A prole controle (C) também recebeu água nas mesmas condições do grupo S. Em nossos resultados, verificamos a presença de ácido clorogênico, cafeína e teobromina em todas as amostras analisadas. O conteúdo de compostos fenólicos nas infusões estudadas foram CH: 5,140,23; T: 4,330,01; G: 0,930,25; C: 0,800,3 e TS: 8,350,5 mg/ml. Não observamos efeito mutagênico ou citotóxico nas amostras analisadas. Um efeito antimutagênico significativo foi observado para a cepa TA97 (pré-, co- e pós-tratamento), na presença de ativação metabólica, em todas as amostras testadas. A amostra TS também apresentou um efeito antimutagênico significativo para a TA102 (pré-, co-e e pós-tratamento), na presença de ativação metabólica. Na análise exclusiva da amostra TS, observamos uma atividade antioxidante quando utilizado o ensaio de DPPH, apresentando IC50 69,3+3,1 μg/ml. Além disso, a amostra TS apresentou um efeito protetor sobre a quebra do DNA plasmidial induzida por radicais superóxido e hidroxila, de maneira dose dependente. No teste do cometa, detectamos um efeito antigenotóxico induzido pelo TS em cultura primária de células epiteliais de esôfago. Em nossos testes in vivo observamos que os animais TS não desenvolveram sobrepeso, obesidade visceral e hiperfagia. A resistência hipotalâmica à leptina não foi significativamente revertida, porém a resistência à insulina foi minimizada pelo tratamento com TS no grupo programado pela S. No fígado, TS normalizou as atividades das enzimas antioxidantes (SOD, GPx e CAT) e diminuiu os marcadores de estresse oxidativo, MDA e 4-HNE. O tratamento com TS também reduziu o conteúdo de glicogênio e triglicerídios hepáticos. Nossos resultados sugerem que a erva-mate foi capaz de proteger o DNA contra danos oxidativos, aumentou as defesas antioxidantes, melhorou a função hepática em ratos superalimentados na lactação, talvez através da modulação da sinalização hipotalâmica da insulina podendo ser, portanto, uma importante ferramenta para prevenção e tratamento de doenças relacionadas ao estresse oxidativo.

History of the Bay Scallop, Argopecten irradians, Fisheries and Habitats in eastern North America, Massachusetts through northeastern Mexico

This is a broad historical overview of the bay scallop, Argopecten irradians, fishery on the East and Gulf Coasts of North America (Fig. 1). For a little over a century, from about the mid 1870’s to the mid 1980’s, bay scallops supported large commercial fisheries mainly in the U.S. states of Massachusetts, New York, and North Carolina and on smaller scales in the states in between and in western Florida. In these states, the annual harvests and dollar value of bay scallops were far smaller than those of the other important commercial mollusks, the eastern oysters, Crassostrea virginica, and northern quahogs, Mercenaria mercenaria, but they were higher than those of softshell clams, Mya arenaria (Table 1). The fishery had considerable economic importance in the states’ coastal towns, because bay scallops are a high-value product and the fishery was active during the winter months when the economies in most towns were otherwise slow. The scallops also had cultural importance as a special food, an ornament owing to its pretty shell design, and an interesting biological component of

Quahogs in Eastern North America: Part II, History by Province and State

The northern quahog, Mercenaria mercenaria, ranges along the Atlantic Coast of North America from the Canadian Maritimes to Florida, while the southern quahog, M. campechiensis, ranges mostly from Florida to southern Mexico. The northern quahog was fished by native North Americans during prehistoric periods. They used the meats as food and the shells as scrapers and as utensils. The European colonists copied the Indians treading method, and they also used short rakes for harvesting quahogs. The Indians of southern New England and Long Island, N.Y., made wampum from quahog shells, used it for ornaments and sold it to the colonists, who, in turn, traded it to other Indians for furs. During the late 1600’s, 1700’s, and 1800’s, wampum was made in small factories for eventual trading with Indians farther west for furs. The quahoging industry has provided people in many coastal communities with a means of earning a livelihood and has given consumers a tasty, wholesome food whether eaten raw, steamed, cooked in chowders, or as stuffed quahogs. More than a dozen methods and types of gear have been used in the last two centuries for harvesting quahogs. They include treading and using various types of rakes and dredges, both of which have undergone continuous improvements in design. Modern dredges are equipped with hydraulic jets and one type has an escalator to bring the quahogs continuously to the boats. In the early 1900’s, most provinces and states established regulations to conserve and maximize yields of their quahog stocks. They include a minimum size, now almost universally a 38-mm shell width, and can include gear limitations and daily quotas. The United States produces far more quahogs than either Canada or Mexico. The leading producer in Canada is Prince Edward Island. In the United States, New York, New Jersey, and Rhode Island lead in quahog production in the north, while Virginia and North Carolina lead in the south. Connecticut and Florida were large producers in the 1990’s. The State of Tabasco leads in Mexican production. In the northeastern United States, the bays with large openings, and thus large exchanges of bay waters with ocean waters, have much larger stocks of quahogs and fisheries than bays with small openings and water exchanges. Quahog stocks in certified beds have been enhanced by transplanting stocks to them from stocks in uncertified waters and by planting seed grown in hatcheries, which grew in number from Massachusetts to Florida in the 1980’s and 1990’s.

Quahogs in Eastern North America: Part I, Biology, Ecology, and Historical Uses

The northern quahog, Mercenaria mercenaria, ranges along the Atlantic Coast of North America from the Canadian Maritimes to Florida, while the southern quahog, M. campechiensis, ranges mostly from Florida to southern Mexico. The northern quahog was fished by native North Americans during prehistoric periods. They used the meats as food and the shells as scrapers and as utensils. The European colonists copied the Indians treading method, and they also used short rakes for harvesting quahogs. The Indians of southern New England made wampum from quahog shells, used it for ornaments and sold it to the colonists, who, in turn, traded it to other Indians for furs. During the late 1600’s, 1700’s, and 1800’s, wampum was made in small factories for eventual trading with Indians farther west for furs. The quahoging industry has provided people in many coastal communities with a means of earning a livelihood and has provided consumers with a tasty, wholesome food whether eaten raw, steamed, cooked in chowders, or as stuffed quahogs. More than a dozen methods and types of gear have been used in the last two centuries for harvesting quahogs. They include treading and using various types of rakes and dredges, both of which have undergone continuous improvements in design. Modern dredges are equipped with hydraulic jets and one type has an escalator to bring the quahogs continuously to the boats. In the early 1900’s, most provinces and states established regulations to conserve and maximize yields of their quahog stocks. They include a minimum size, now almost universally a 38-mm shell width, and can include gear limitations and daily quotas. The United States produces far more quahogs than either Canada or Mexico. The leading producer in Canada is Prince Edward Island. In the United States, New York, New Jersey, and Rhode Island lead in quahog production in the north, while Virginia and North Carolina lead in the south. Connecticut and Florida were large producers in the 1990’s. The State of Campeche leads in Mexican production. In the northeastern United States, the bays with large openings, and thus large exchanges of bay waters with ocean waters, have much larger stocks of quahogs and fisheries than bays with small openings and water exchanges. Quahog stocks in certifi ed beds have been enhanced by transplanting stocks to them from stocks in uncertified waters and by planting seed grown in hatcheries, which grew in number from Massachusetts to Florida in the 1980’s and 1990’s.