End-of-life (EOL) care decisions present a challenge for family caregivers. Despite the increasing number of terminally ill patients in need of pain management and comfort care, there is limited qualitative data about how populations in the developing world can access culturally appropriate resources and EOL support. In this phenomenological study, 17 Garifuna family caregivers in southern Belize were interviewed about their experience caring for terminally family members. The conceptual frameworks were Kübler-Ross’s hospice approach and Watson’s theory of human caring. The two theories were selected based on their significance to this process: Kübler Ross’s hospice approach and its impact on the family system during the end stage of life and Watson’s theory of human caring for its emphasis on the impact of the importance of meeting the basic needs of individuals. NVivo 12 was used to code and generate themes for further analysis. Caregivers who said they would not utilize support outside of the home were those who were committed not do so at the request of the patient. Caregivers who cared for their family member and those who could financially afford to hire caregivers in their home to assist with their relative said they would not utilize nonfamily support. All others, regardless of relationship to the patient, indicated they would have accepted care if the environment were safe, caring, and culturally sensitive. Additionally, the caregivers saw their needs as secondary and insignificant compared to the comfort and care of the patient. This study may contribute to positive social change by revealing strategies and services that could be included in the design of a health services delivery system to meet the needs of individuals facing EOL decisions.

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This paper examines the archaeological data collected during the 2008 and 2009 seasons at the Maya settlement, Hun Tun, in northwestern Belize. Hun Tun was initially identified in 2008 where preliminary investigations have focused on survey, mapping and testing courtyard spaces. Architectural evidence and material culture will be discussed generally in terms of chronology and possible function. Ceramic analysis suggests a single occupation with a Late Classic hiatus. Analysis of field research will be limited to studies of settlement patterns, chronological sequencing of courtyard spaces and proposed function of limestone features. These initial field seasons have yielded information pertaining to socioeconomic status, sociopolitical interaction and potential hypotheses related to these topics. Future research at Hun Tun is presented with an emphasis on household archaeology. / text

Thesis advisor: Amy E. Frappier / A ~7,000 year stable isotope record from a Central American stalagmite is presented as a record of rainfall and consequently Intertropical Convergence Zone (ITCZ) tropical rain belt strength over the late Pleistocene to mid-Holocene. The "amount effect" explains the well-documented inverse relationship between rainfall amount and stable oxygen isotope values observed in tropical monsoon regions and consequently in stalagmite calcite from those regions. ITCZ rainfall influences much of the Central American tropical region and here a ~7,000 year stable isotope record from stalagmite ATM1 harvested from Actún Tunichil Muknal Cave in Belize is presented as a record of ITCZ influenced rainfall during the late Pleistocene to mid-Holocene (5,561 ± 2,488 BP - 12,605 ± 284 BP). Three major oxygen isotope excursions occur within the record. These excursions correspond to the global cold Younger Dryas and 8.2 ka events and a relatively undocumented wet period around 6,300 bp. The Younger Dryas manifests as a relatively moist period in central Belize while the 8.2 ka event manifests as a relatively dry period. The reason for the opposite responses to cooling elsewhere in the globe is posited to be due to orbital forcings. The 6,300 bp relatively wet period appears to be synoptic in scale and two possible triggers for the isotope excursion are presented: eustatic sea level rise causing lagoonal constriction, warming of water off the coast of Belize, and thus increased evaporation and precipitation over the study region; and hurricane clusters, evidenced in the region in the succeeding 1,000 years, in which the location of the Azores High funnels hurricanes to make landfall near the central Belize region. ATM1 provides evidence for tropical leads and/or lags to global climate events and bolsters the idea that high and low latitude climate relationships are complexly interlinked. / Thesis (MS) — Boston College, 2010. / Submitted to: Boston College. Graduate School of Arts and Sciences. / Discipline: Geology and Geophysics.

This dissertation is a palynological examination of the Mayan archaeological site at Blue Creek, northwestern Belize. This study uncovers more than 4,500 years of environmental and agricultural history of the region, which can be related to human incursion, habitation and plant use, abandonment, and reoccupation of the region. After an historical and ecological overview of the study site, there follows an explanation of procedures for collecting, sampling, processing, identifying, and counting the fossil pollen from the area. Evidence from archaeology, paleoecology, and physical anthropology is used to construct a model for the first entry of humans into the Maya area. Examinations are made of Archaic Period paleoecology and the cultural developments that set the stage for the advancement of Maya culture. Next, the physical environment of Blue Creek is explored, and its stability is assessed. This information leads to an assessment of the possibility of drought or soil degradation during the height of Mayan civilization, and contributes to the current understanding of the Maya Collapse at Blue Creek. Mayan agricultural methodologies are explained, and the changes to traditional production systems that resulted from European colonization are described. A model of agricultural development is proposed. The plant taxa identified in the Laguna Verde pollen core are listed and described. Finally, the Laguna Verde pollen core is interpreted in terms of the vegetation associations and environmental conditions represented by each stratum. This dissertation is a palynological examination of the Mayan archaeological site at Blue Creek, northwestern Belize. This study uncovers more than 4,500 years of environmental and agricultural history of the region, which can be related to human incursion, habitation and plant use, abandonment, and reoccupation of the region. After an historical and ecological overview of the study site, there follows an explanation of procedures for collecting, sampling, processing, identifying, and counting the fossil pollen from the area. Evidence from archaeology, paleoecology, and physical anthropology is used to construct a model for the first entry of humans into the Maya area. Examinations are made of Archaic Period paleoecology and the cultural developments that set the stage for the advancement of Maya culture. Next, the physical environment of Blue Creek is explored, and its stability is assessed. This information leads to an assessment of the possibility of drought or soil degradation during the height of Mayan civilization, and contributes to the current understanding of the Maya Collapse at Blue Creek. Mayan agricultural methodologies are explained, and the changes to traditional production systems that resulted from European colonization are described. A model of agricultural development is proposed. The plant taxa identified in the Laguna Verde pollen core are listed and described. Finally, the Laguna Verde pollen core is interpreted in terms of the vegetation associations and environmental conditions represented by each stratum.

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The following dissertation outlines historical-archaeological research focused on the nineteenth-century, British plantation settlement at Lamanai, Belize. Archaeological data presented here include recent archaeological excavations (2014) and a study of previously excavated archaeological materials recovered at the site over the past 30 years (2009), conducted by this author. The study's archaeological data are synthesized in tandem with historical and documentary sources, comparative site data, and oral histories. Even though the study data span more than thirty years of recovery, it must be noted that very little research has focused on the late-colonial period at Lamanai to date. The most recent phase of archaeology is a foundational effort, which aims to set the stage for future late-colonial period, historical-archaeological studies. To this end, a great deal of effort has been spent here outlining the project's core theoretical and methodological foundations with which frame the current study and inform future research endeavors. Little is known about the eighteenth- and nineteenth- centuries at Lamanai, and to this end, the project aimed to answer questions regarding how life (residential, industrial, and administrative) was structured. While the archaeological and historical records have elucidated much about the plantation settlement at Lamanai to date, that data have also been frustratingly oblique and obfuscating with regard to intra-site variability among known British colonial activity and habitation areas.

This thesis explores the connections that the Garifuna indigenous group of Belize has with their former homeland, the island of St. Vincent. After emerging as a distinct ethnic group during the 17th century, the Garifuna were exiled from St. Vincent by British colonial rulers in 1797. For the Garifuna people, the connection to the island is more than historical. It is also spiritual. Interviews were conducted in July 2006 in Belize with members of the Garifuna community who have made the journey back to the island. In addition to presenting the results of those interviews, this thesis will also provide a history of the Garifuna people, describe some of the spiritual aspects of the culture, and a discussion of the current literature on pilgrimage.

No description available.