Eurasian Neogene large herbivorous mammals and climate

The development and changes in the distribution of herbivorous mammal communities during the Neogene is complex. The Eurasian scale environmental patterns reflect the large scale geographical and climatic patterns. The reorganization of these affect the biome distribution throughout the continent. The distribution of mammal taxa was closely associated with the distribution of biomes. In Eurasia the Neogene development of environments was twofold. The early and middle Miocene that seemed to have been advantageous for mammals was followed by drying of environments during the late Neogene. The mid-latitude drying was the main trend, and it is the combined result of the retreat of Paratethys, the uplift of Tibetan Plateau and changes in the ocean currents and temperatures. The common mammals were "driving" the evolution of mammalian communities. During the late Miocene we see the drying affecting more and more regions, and we see changes in the composition of mammalian communities.

Late Pleistocene and Holocene environmental evolution of the Murchisonfjorden area, Nordaustlandet, Svalbard

The purpose of this study was to establish the palaeoenvironmental conditions during the late Quaternary in Murchisonfjorden, Nordaustlandet, based on foraminiferal assemblage compositions, and to determine the onset and termination of the Weichselian glaciations. The foraminiferal assemblage compositions were studied in marine sediments from three different archives, from sections next to the present shoreline in the Bay of Isvika, from a core in the Bay of Isvika and from a core from Lake Einstaken. OSL and AMS 14C age determinations were performed on samples from the three archives, and the results show deposition of marine sediments during ice-free periods of the Early Weichselian, the Middle Weichselian and the Late Weichselian, as well as during the Holocene in the investigated area. Marine sediments from the Early and Middle Weichselian were sampled from isostatically uplifted sections along the present shoreline.Sediments from the transition from the Late Weichselian to early Holocene time intervals were found in the bottom of the core from Lake Einstaken. Holocene sediments were investigated in the sections and in the core from the Bay of Isvika. The marine sediments from the sections are comprised of five benthic foraminiferal assemblages. The Early Weichselian is represented by two foraminiferal assemblages, the Middle Weichselian, the early and the late Holocene each by one. All five foraminiferal assemblages were deposited in glacier-distal shallow-water environments, which had a connection to the open ocean. Changes in the composition of the assemblages can be ascribed to differences in the bottom-water currents and changes in the salinity. The Middle Weichselian assemblage is of special importance, because it is the first foraminiferal assemblage to be described from this time interval from Svalbard. Four benthic foraminiferal assemblages were deposited shortly before the marine to lacustrine transition at the boundary between the Late Weichselian and Holocene in Lake Einstaken. The foraminiferal assemblages show a change from a high-arctic, normal marine shallow-water environment to an even shallower environment with highly fluctuating salinity. The analyses of the core from 100 m water depth in the Bay of Isvika resulted in the determination of four foraminiferal assemblages. These indicated changes from a glacier-proximal environment during deglaciation, to a more glacier-distal environment during the Early Holocene. This was followed by a period with a marked change to a considerably cooler environment and finally to a closed fjord environment in the middle and late Holocene times. Additional sedimentological analyses of the marine and glacially derived sediments from the uplifted sections, as well as observations of multiple striae on the bedrock, observations of deeply weathered bedrock and findings of tills interlayered with marine sediments complete the investigations in the study area. They indicate weak glacial erosion in the study area. It can be concluded that marine deposition occurred in the investigated area during three time intervals in the Weichselian and during most of the Holocene. The foraminiferal assemblages in the Holocene are characterized by a transition from glacier-proximal to glacier-distal faunas. The palaeogeographical change from an open fjord to a closed fjord environment is a result of the isostatic uplift of the area after the LGM and is clearly reflected in the foraminiferal assemblages. Another influencing factor on the foraminiferal assemblage composition are changes in the inflow of warmer Atlantic waters to the study area.

"Oma entinen on palannut takaisin elämään" : Kuntoutuksen vaikuttavuus aikuisena kuuroutuneiden henkilöiden elämänhallintaan ja psykososiaaliseen hyvinvointiin

Objective The objective of this study was to learn about the psychosocial well-being and life management of Finnish adults with late deafness or hearing loss and to observe the effectiveness of the rehabilitation courses they participated in. Methods For my study I used indicators which were suitable for the evaluation of life management and psychosocial well-being of late-deafened adults. The first part of the study was conducted during 2009 as a questionnaire on three rehabilitation courses in Kopola, a course center of the Finnish Federation of Hard of Hearing. The follow-up study was done at the third period of the courses during 2009 2010. The questionnaire contained both open and structured questions. The questionnaire consisted of five areas concerning life management and psychosocial well-being: sense of coherence (life management), human relations and social support, mood, self-esteem and satisfaction with life. I also asked the participants to reflect on their experiences of group rehabilitation. Results and conclusions The participants consisted of seven women and three men. They were approximately 63 years old and were all retired. Loss of hearing was described to have affected their social life, free time, and in general made their lives more difficult. From the course the participants hoped to gain new skills such as signed speech and lip-reading, uplift their mood, accept their loss of hearing and experience peer support. After the courses they replied that they had more close relations with whom they also were a little more in contact with. More participants were satisfied with e.g. their ability to take care of themselves, their free time, financial situation, family life, mental resources and physical shape. Majority of the participants showed symptoms of depression when the courses started, but at the end of the courses these signs had moderated or disappeared for most of them. The participants felt that during the rehabilitation they had been heard, respected, accepted and been taken care of. The course provided the possibility for confiding, and the discussions gave the participants support and consolidation. In conclusion, the course affected positively on the acclimatization to the hearing loss and the empowerment of the participants. The results of this study can be utilized in disability services, the development of rehabilitation and in the social- and health services of senior citizens.