The purpose of this study was to apply oxygen and carbon stable isotope microsampling techniques to the seasonal banding of the otoliths of the Atlantic cod, Gadus morhu~ in order to determine their potential use in reconstructing the environmental conditions experienced by cod. A reconstruction of the changes in environmental temperature is seen as particularly applicable to the determination of cod migration routes based on the known temperature profile of the North Atlantic. Transverse thin sections of six otoliths from cod taken off the coast of Atlantic Canada were prepared using standard methods. Material was sampled from each semiannual band of the otoliths and run on a Finnigan MAT 251 ratio mass spectrometer to determine 0180 and 013C. The results for 0180 indicated that the otoliths had an approximate initial value of either 1.4%o or l.O%o for sample material taken from the nucleus. The 0180 signal was characterized by oscillating values in which sample material from hyaline bands corresponded predominantly with the troughs and sample material from the opaque bands corresponded with the peaks. The average range of 0180 was found to be 0.87%o corresponding to a temperature range of 3.6°C which was within the expected 3 to 4 °C seasonal average temperature shift experienced by cod. Seasonal cycling was apparent in three of the otoliths, with semi-annual values alternating between high opaque bands and low hyaline bands. It was concluded that seasonal temperature changes due to migration from offshore to inshore waters are recorded in the 0180 signal and that future sampling should attempt to resolve several samples within each seasonal band in order to resolve the migratory changes in temperature on an sub-annual basis. It is also suggested that experiments be carried out to determine the species specific 0180 versus temperature relationship for cod to make accurate interpretation of the data possible. The o13C signal was found to be characterized by an increasing logarithmic trend in o13C. The 013C signal was observed to increase over the first three years of growth and to level off at age 4 and fluctuate at a value close to O%o. The otoliths of cod were found to contain a high proportion of inorganic carbon with a minimum 013C value of -4.53%o and a maximum of 0.23%o. It was suggested that the initial increase in 013C was a product of a combination of factors affecting metabolic rate and therefore, indirectly, the amount of metabolically derived carbon circulating in the blood. It was concluded that further research into the growth and development of cod was necessary in order to reach a comprehensive understanding of the biological processes responsible for the observed trends in 013C. 0180 was plotted against 013C for samples from growth bands of age four or greater and found to have a positive correlation with a slope of 0.269 (S.E. 0.049) and an r-squared of 0.537, P < 0.0001 when the results for otolith 176 were excluded due an anomalous trend in that data set. Two hypotheses were suggested to account for the observed positive correlation, a metabolic/temperature effect, and a depth/temperature effect. It was concluded that, with further research into the controlling factors behind the fluctuations in 013C, the 013C signal may provide a second source of information with regards to changes in habitat and environmental characteristics over the life time of the cod. It is suggested that a study be carried out to determine the amount of metabolic carbon incorporated into the otolith in order to clarify the observed trends. / Thesis / Candidate in Philosophy

Thesis (Ph. D.)--University of California, Irvine, 2005. / Chair: Ralph J. Cicerone. Includes bibliographical references.

名古屋大学年代測定総合研究センターシンポジウム報告

Thesis (Ph.D.) -- McMaster University, 1997. / Includes bibliographical references. Also available via World Wide Web.

The aim of this work was to characterize the diet of a Merovingian population sample and examine if apparent differences in grave good assemblages of Merovingian burials and transfromation of this funerary rite during 6th and 7th centuries were reflected in diet. Dietary composition was assessed using a carbon and nitrogen stable isotope analysis of 74 bone collagen samples from adults buried at an early medieval cemetery of le-Norroy-le-Veneur, France. Results showed diet based primarily on C3 plants, supplemented with animal protein in a range similar to other contemporary sites. No significant contribution of C4 plants (e.g. millet) or marine-derived protein has been detected and neither has δ15 N dependency on status, sex or datation been found. However, persons with rich grave good assemblages had significantly higher δ13 C than low-ranking individuals. Also, during the time of use of the cemetery there has been a population-wide decrease of 0,33 ‰ in mean value of δ13 C, independent of social status or sex. Results indicate that dietary differentiation steaming from social stratification was only in its early phase of formation, slowly following a progressive rise in power of the Merovingian nobility, and the general subsistence was affected by another independent change in society, most...

New Zealand forests have been reduced and degraded by gross removal, logging, and the effects of mammals introduced by Polynesian and European settlers. These changes increase the value of the remaining forests, so information on the effects of these disturbances will be useful to inform the management of forest protection. Integrated measurements of C and N cycling within forests can be obtained using foliar stable isotope ratios, which may detect differences between forests resulting from natural or anthropogenic disturbances. This thesis characterises the stable isotopic composition distribution and likely drivers of isotopic variation of vegetation in several central South Island forests, and provides a baseline for future ecological New Zealand studies of present and pre-human vegetation. The largest detected stable isotope variation in modern leaf material was that of δ15N values between the eastern and western podocarp-broadleaf forests. This variation was probably controlled by the lower soil N availability associated with the high rainfall of western forests causing low δ15N values (-8.5 ± 3.5 ‰) relative to an eastern forest (+1.6 ± 1.3 ‰) and global temperate forests (average -2.8 ± 2.0 ‰ (Martinelli et al. 1999)). The significant but slightly higher mean δ15N (0.6 ‰) of a historically selectively logged forest (Saltwater Forest) in comparison to the mean in an unlogged forest (Okarito Forest), on the West Coast, could be attributed to either alteration to N cycling from logging, site differences in topography, or local soil N differences between the forests. Although δ13C showed no significant geographical variation, the well-described ‘canopy effect’ was observed in all modern forests, manifested as a positive covariation between δ13C and vegetation height. Similarly, large taxon-specific differences were observed between δ15N and δ13C values in both modern and fossil leaves. Well-preserved fossil leaves, from sediments c. 4500 years B.P in Pyramid Valley, North Canterbury, had higher δ13C (4.2 ‰) and δ15N (2.5 ‰) values than modern vegetation from Riccarton Bush, Christchurch. The difference between ecosystems spanning several millennia probably reflects ecosystem-scale changes in C and N cycling within New Zealand forests following human arrival, particularly from the degradation caused by invasive animals.

科学研究費補助金 研究種目:基盤研究(B) 課題番号:06554036 研究代表者:吉岡 崇仁 研究期間:1994-1996年度