We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.
To save content items to your account,
please confirm that you agree to abide by our usage policies.
If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account.
Find out more about saving content to .
To save content items to your Kindle, first ensure no-reply@cambridge.org
is added to your Approved Personal Document E-mail List under your Personal Document Settings
on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part
of your Kindle email address below.
Find out more about saving to your Kindle.
Note you can select to save to either the @free.kindle.com or @kindle.com variations.
‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi.
‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.
Salt works along the Yucatan coasts of Mexico and Belize provide a record of salt production for inland trade during the height of Late Classic Maya civilisation (AD 550–800). At the Paynes Creek Salt Works in Belize, production focused on the creation of salt cakes by boiling brine in pots supported over fires in dedicated salt kitchens. Underwater excavations at the Early Classic (AD 250–550) site of Jay-yi Nah now indicate there was a longer and evolving tradition of salt making in the area, one that initially employed large, incurved bowls to meet local or down-the-line trade needs before inland demand for salt soared.
Sea-level rise and settlement are investigated at Ta'ab Nuk Na, an ancient Maya salt works in Belize, by examining samples from wooden posts and marine sediment. The samples included Post 145 of Building B and the Nunavut beam, along with marine sediment columns cut from beside both wooden posts. The sediment columns were sampled at 2 cm intervals. Loss-on ignition confirmed the presence of organic material. Identifying the organic content involved removing nonorganic material from the sediment and sorting the organic material under magnification. This procedure established that most of the organic material was red mangrove (Rhizophora mangle). Red mangroves tolerate salt water, but under conditions of sea-level rise, the plants grow vertically to keep their leaves above water. Sediment, leaves, and detritus trapped in the prop roots form mangrove peat, which serves as a proxy for sea-level rise. AMS dating of fine red mangrove roots determined that the local sea levels rose at Ta'ab Nuk Na throughout the Late Classic period and continued into the Postclassic period. Radiocarbon dates obtained from the wood-post samples yielded Late Classic–period dates. Comparing the radiocarbon dates from the wooden posts and the sediment core samples determined that the site was abandoned before the rising seas flooded the area. Evidently, sea-level rise did not play a role in site abandonment.
Salt is an essential commodity; archaeological remains around the world attest to the importance of its production, exchange and consumption. Often located in coastal locations, many production sites were submerged by rising seas, including the Paynes Creek Salt Works on the southern Belize coast. Survey and excavation of these sites has identified ‘kitchens’ for brine boiling, as well as Terminal Classic residential structures at Ek Way Nal. The authors report the discovery of an earlier residential building alongside salt kitchens at the nearby site of Ta'ab Nuk Na. This finding indicates that surplus household production began during the Late Classic, when demand for salt from inland cities was at its peak.
Systematic flotation survey and spatial analysis of artifacts at the submerged salt work of Ek Way Nal reveal evidence of a residence, salt kitchens, and additional activities. Ek Way Nal is one of 110 salt works associated with a Late to Terminal Classic (A.D. 600–900) salt industry known as the Paynes Creek Salt Works. Wooden posts that form the walls of 10 buildings are remarkably preserved in a peat bog below the sea floor providing an opportunity to examine surface artifacts in relation to buildings. Numerous salt kitchens have been located at the Paynes Creek Salt Works by evidence of abundant briquetage—pottery associated with boiling brine over fires to make salt. As one of the largest salt works with 10 buildings, there is an opportunity to examine variability in building use. Systematic flotation survey over the site and flagging and mapping individual artifacts and posts provide evidence that the Ek Way Nal salt makers had a residence near the salt kitchens, along with evidence of salting fish for subsistence or surplus household production. The results are compared with ethnographic evidence from Sacapulas and other salt works.
THE HEIGHT OF the Classic Maya civilization and its demise in the tropical landscape of Central America occurred during the Early Middle Ages. The Classic period is defined as the time when the Maya erected carved monuments in the centre of cities with dates in the Maya long count between about 300 and 900 CE. The dates recorded the dynastic histories of kings and queens of city-states. Accompanying hieroglyphs on stone monuments describe events in the lives of the dynastic leaders about marriage and other alliances, warfare with other polities, and battles won. The hieroglyphic record is limited by its focus on major historical events of dynastic leaders while providing virtually no information on the lives of the bulk of the Maya population, which consisted of farmers, artisans, and other non-elites. Commercial transactions, so well documented among, for instance, ancient Mesopotamian civilizations, are not found in the Maya glyphs, although pictorial depictions on painted pottery vessels include scenes featuring dynastic leaders and visitors, including feasting events and offerings or tribute payment. Most information about the ancient Maya derives from survey and excavation of sites that lack written records. This evaluation of the Early Middle Ages in the Maya area focuses on the Late Classic period (600– 800 CE), the slow collapse of the southern lowland civilization that began about 750 and continued through the Terminal Classic period (800– 900 CE), and the role of trade, migration, warfare, climate change, population increase, and ecological balance in the rise and fall of the Maya civilization.
With the fall of Teotihuacan by 600, the Late Classic Maya flourished, with a focus on trade within the Maya area. This included long-distance trade from the highlands to the lowlands in obsidian, jadeite, pottery, and various perishable goods that have not preserved. The collapse of the lowland city-states between 750 and 900 and the movement of people to the coast and the northern Maya lowlands, occurred during the time of ascendancy of Chichen Itza in the northern lowlands and the Toltec state north of Mexico City with its capital at Tula.
Jadeite artefacts at Maya sites are normally associated with ritual and ceremonial locations, with high-quality jadeite reserved for elite objects. The discovery of a jadeite gouge with a wooden handle at a Classic Maya salt-working site submerged by sea-level rise—Ek Way Nal, Belize—is therefore unexpected and provides new information about the utilitarian use of this stone. The extremely high quality of this jadeite tool is particularly surprising, offering new insight into the Classic Maya exchange systems and the role of salt makers such as those based at Ek Way Nal.
ABSTRACT. The author underlines the importance of Maya navigation around the Yucatan Peninsula. The discovery by underwater archeologists of canoes, paddles, and pottery in Maya settlements shows the importance of salt, obsidian, precious stones, gold, and copper trade that made ports such as Moho Cay or Wild Cane Cay prosperous.
RÉSUMÉ. L'auteur souligne l'importance de la navigation maya autour de la péninsule du Yucatan. La découverte de canoës, de pagaies, de poteries par l'archéologie sous-marine dans les établissements mayas montre l'importance du commerce du sel, de l'obsidienne, de pierres rares, d'or et de cuivre, qui a fait la prospérité de ports comme Moho Cay ou Wild Cane Cay.
Maritime navigation was important to the ancient Maya for trade, fishing, and transportation. Best known from the Classic period (AD 300–900) city-states that flourished in Guatemala, Belize, the Yucatan peninsula of Mexico, and western El Salvador and Honduras, Central America, Maya culture originated about 1800 BC and continues to the present (Figure 1). Interest in ancient Maya sea trade has focused on Columbus' encounter with an alleged Maya trading canoe off the north coast of Honduras during his fourth voyage to the New World in 1502. The large ocean-going wooden dugout canoe held several passengers and was laden with trade goods such as copper, woven cotton, and honey. Evidently, the arrival of the Spaniards disrupted active circum-Yucatan sea trade bringing exotic materials and goods from distant and nearby locations. In this paper, I examine evidence for Maya navigation – both direct evidence of canoes and paddles, and indirect evidence in terms of artistic depictions of boat travel, settlement of offshore islands, maritime trade, seafood and other marine resources at inland settlements, and the ritual importance of the sea to the ancient Maya. I focus on my archaeological field research on offshore islands and underwater sites along the coast of Belize to evaluate what role Maya canoe trade played in the political and economic course of Maya prehistory.
Annectina viriosa, a new species of Ammodiscidae (Foraminiferida), is described from Recent brackish ponds on a salt flat adjacent to Lake Winnipegosis, Manitoba. Colonization of the ponds was probably by avian transport. The distinct morphotype is either the result of an allopatric speciation event within the last 5,000 years or it is a previously undescribed species of shallow-water Annectina from nearby Hudson Bay. It is also possible that recovered specimens are previously unrecognized ecophenotypic variants of some known species produced by unknown hostile environmental factors within the pond ecosystem. The latter hypothesis is difficult to test without extensive biological culturing. The large number of phenotypically stable specimens living in these ponds warrants recognition of these populations as a distinct taxon.
Frequently descriptive entomology suffers from a lack of precise data on specimen colour. Since colour is rarely defined and since an effective technique is available, the authors suggest that greater consideration be given colour analysis. A simple procedure is outlined in relation to colour analysis of specimens undergoing degreasing.
Preston and Westwood (1981) reported on the distribution of Thymelicus lineola (Ochsenheimer) in Manitoba. They suggested that the species arrived here about 1970 by way of northwestern Ontario. At that time the population in central Winnipeg was the most western known in the Prairie region and they suggested that the spread of the species might be impeded by the arid nature of the Great Plains to the west. Klassen et al. (1989) noted that specimens subsequently had been taken 70 km west of Winnipeg at Rathwell(49°39'N; 98°33'W) near the western edge of the Red River Valley soils on the eastern edge of the Prairie. In 1986 Preston and McKillop collected the European Skipper at Eriksdale (50°52'N; 98°06'W) 100 km to the northwest of Winnipeg in the marginal lands of the interlake region (Klassen et al. 1989).
Vapour degreasing and cleaning of entomological specimens proved to be a viable alternative to standard methods. Defined change in colour upon degreasing clearly portrayed the effectiveness of this new technique.
The aim of this study was to explore the realities of everyday nursing practice associated with the implementation of a guideline for the assessment and management of cardiovascular risk.
Background
The use of clinical practice guidelines is pivotal to improving health outcomes. However, the implementation of guidelines into practice is complex, unpredictable and, in spite of much investigation, remains resistant to explanation of what works and why. Exploration of the nature of guideline implementation has the potential to illuminate the complexities of guideline implementation by focussing on the nature of practice. Nurses are well placed at the front line of primary health care to contribute to an understanding of how guideline implementation plays out in their everyday practice.
Methods
Qualitative description was used, involving focus groups and interviews with 32 participants (20 nurses, four doctors, five managers and three funder/planners), to explore the use of a guideline in everyday primary health-care practice. Thematic analysis of data was managed through an inductive process of familiarisation, coding, categorising and generation of themes.
Findings
Four themes were generated from the data portraying the realities of guideline implementation for primary health-care nurses: self-managing patient, everyday nursing practice, developing new relationships in the health team and impact on health-care delivery. The findings reveal that, even with the best of intentions to implement the guideline, health professionals were frustrated and at a loss as to how to achieve that in practice. Consequently, cardiovascular risk assessment and management was uneven and fragmented. Primary health-care practice environments vary so much that solutions to the difficulties of implementing evidence into practice requires context-specific solution-finding through collaborative teamwork. Furthermore, the attention of guideline developers, health-care policymakers, funders and researchers requires direct focus on the ‘how’ and the ‘what’ of evidence implementation.
1. An examination of eighty-nine samples of uncooked and thirty-eight samples of cooked food purchased by one particular hospital showed that the purchased food was bacteriologically clean.
2. A similar examination of 173 samples of food after it was cooked and prepared for serving in the hospital kitchens showed that, with the exception of cold chicken, the bacterial flora was greatly reduced by cooking. Ten of forty-six samples of cold chicken, however, were contaminated with fairly large numbers of Cl. welchii.
3. An investigation into the cooking and handling of the fowls indicated that contamination of the cooked fowls with kitchen dust was a probable explanation for the presence of Cl. welchii.
4. Immediate refrigeration of the fowls, well separated on shallow trays, was shown to be a satisfactory method of preventing the growth of contaminating Cl. welchii to any dangerous extent.
5. Six outbreaks of food poisoning, in which there was an association between cold chicken and the clinical symptoms of Cl. welchii food poisoning, are reported and discussed.
I have pleasure in thanking Dr Betty Hobbs of the Food Hygiene Laboratory of the Public Health Laboratory Service at Colindale for the serological typing of numerous strains of Cl. welchii; Mr D. B. Colquhoun for assistance with the phage-typing of the staphylococci; Mr G. Kerr for the photography; and the kitchen staff in the hospital concerned for making possible the numerous samplings of food and the other inquiries into the day-to-day affairs of the hospital catering department.