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                  <text>Kyoto University</text>
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                <text>Changes in Developmental Trends of Caregiver-Child Interactions among the San: Evidence from the !Xun of Northern Namibia</text>
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                <text>The San have been the subject of extensive research with respect to their foraging lifestyle that is assumed to date back to antiquity. I conducted field research among the !Xun San, who have had close associations with the neighboring agro-pastoralists, in order to deepen understanding in this area. As anticipated by previous studies on the influence of sedentarization, !Xun children were increasingly engaged in the care of their younger siblings or cousins. These studies also predicted early weaning from breastfeeding. Indeed, the transition from breastfeeding to solid baby food occurred primarily during the second year after birth, regardless of the mother's next pregnancy, among the present-day !Xun. However, several findings did not meet the expectations raised by previous studies. Despite the difference in subsistence patterns, the trend toward parity among sedentary !Xun women was quite similar to that of nomadic Ju|'hoan women. The developmental transition involving touching and holding by the mother was similar among the Ju|'hoan and the !Xun. Gymnastic behavior preceding unaided walking of children persisted, even among the sedentary !Xun, mediated by differences in folk knowledge regarding such gymnastic behavior. Based on this evidence, I reconsidered the relationships among ecology and subsistence patterns, parental ideology, and patterns of caregiver-child interactions.</text>
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                <text>Akira TAKADA</text>
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                <text>African study monographs. Supplementary issue (2010), 40: 155-177</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/96291</text>
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                  <text>Kyoto University</text>
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                <text>Ethnohistory and Archaeology of the Ju/'hoansi Bushmen</text>
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                <text>The 'Great Kalahari Debate' which revolved around the degree of isolation of the Ju/'hoansi Bushmen failed to adequately interrogate the Bushmen on what they knew of their own history. A combination of interviews with respected Ju/'hoansi elders and archaeological excavation indicates that those Bushmen living in the Sandveld of north-eastern Namibia, although in contact with Kavango farmers, would use them as a convenient source of hxaro exchange items only when needed. This meant only a limited number of exotic pieces were found in the excavations at the hxaro exchange place of Cho/ana in the Kaudom Reserve, suggesting that the Bushmen retained their independence. By way of contrast, hunters living in small rock shelters on the edge of Tswana settlements around Gaberone in Botswana gradually saw their cultural material being completely replaced by exotic goods and food, indicating encapsulation by the dominant society.</text>
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                <text>Andrew B. Smith</text>
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                <text>African study monographs. Supplementary issue (2001), 26: 15-25</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/68410</text>
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        <name>Andrew B. Smith</name>
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        <name>Encapsulation</name>
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                  <text>Kyoto University</text>
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                <text>Interactions between Termite Mounds, Trees, and the Zemba People in the Mopane Savanna in Northwestern Namibia</text>
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                <text>Termite mounds comprise a significant part of the landscape in northwestern Namibia. The vegetation type in this area is mopane vegetation, a vegetation type unique to southern Africa. In the area where I conducted research, almost all termite mounds coexisted with trees, of which 80% were mopane. The rate at which trees withered was higher on the termite mounds than outside them, and few saplings, seedlings, or grasses grew on the mounds, indicating that termite mounds could cause trees to wither and suppress the growth of plants. However, even though termite mounds appeared to have a negative impact on vegetation, they could actually have positive effects on the growth of mopane vegetation. Moreover, local people use the soil of termite mounds as construction material, and this utilization may have an effect on vegetation change if they are removing the mounds that are inhospitable for the growth of plants. Consequently, both termite mounds and human activities should be taken into account as factors affecting mopane vegetation.</text>
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                <text>Chisato YAMASHINA</text>
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                <text>African study monographs. Supplementary issue (2010), 40: 115-128</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/96293</text>
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        <name>Chisato YAMASHINA</name>
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        <name>Himba</name>
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        <name>Kaoko</name>
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        <name>Mopane vegetation</name>
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        <name>Termite mounds</name>
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        <name>Utilization of termite mounds</name>
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        <name>Vegetation change</name>
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              <name>Title</name>
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                  <text>Kyoto University</text>
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                <text>FARMER'S SELECTION OF LOCAL AND IMPROVED PEARL MILLET VARIETIES IN OVAMBOLAND, NORTHERN NAMIBIA</text>
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                <text>A new and improved cultivar of pearl millet (Pennisetum glaucum), Okashana-1, was released in Namibia in 1990 and was rapidly adopted in Ovamboland. However, as most farmers do not buy new seeds each year, any genetic trials of the cultivar on actual farms would be affected by cross-pollination. The present study clarified the characteristics of Okashana-1, as found on actual farms. In addition, this research also examined the interrela- tionships between the environmental status, traditions, livelihood, and subsistence activities in the study area and the cultivar characteristics.</text>
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                <text>Daisuke Uno</text>
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            <description>An entity responsible for making the resource available</description>
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                <text>African study monographs. Supplementary issue (2005), 30: 107-117</text>
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                <text>2005</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/68457</text>
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        <name>Agriculture</name>
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        <name>Daisuke Uno</name>
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        <name>Farming</name>
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        <name>Mahangu</name>
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        <name>Millet</name>
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        <name>Oshana</name>
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        <name>Ovamboland</name>
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                  <text>Kyoto University</text>
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                <text>OBSERVATION OF RIPARIAN VEGETATION IN WESTERN NAMIBIA BY USING NDVI AND NDWI DERIVED FROM SPOT-VEGETATION</text>
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                <text>Ephemeral rivers in western Namibia are unique entities that support both natural vegetation and human activities. This paper presents an approach for observing riparian vegetation along them synoptically using remotely sensed datasets, derived from a satellite borne sensor named SPOT-VEGETATION. The most commonly used vegetation index, the Normalized Difference Vegetation Index (NDVI), certainly delineates the overall distribution of vegetation, but not without errors. A vegetation index that was designed as a supplement for NDVI, the Normalized Difference Water Index (NDWI), showed some interesting features, but again, with faults. By synthesizing the two indices, the scarce and sparse vegetation in coastal deserts and the relatively dense vegetation in inland highlands could be effi ciently observed. Furthermore, by introducing a fl ow accumulation model produced from a digital elevation model (DEM), it became possible to observe such riparian vegetation quantitatively and systematically.</text>
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                <text>Hiroyuki Yoshida</text>
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                <text>The production of grass was investigated on the gravel plains of the Central Namib Desert, Namibia, during 10 rainfall seasons sampled between 1989-2003. The aim was to evaluate the rainfall-productivity relationship, to elucidate the relationship between temporal and spatial variability, and to examine the spatial scale of patchiness. We compared two different methods and found that a less accurate rapid assessment of grass cover correlat- ed well with measurements of biomass. Our data were in agreement with previous determina- tions of the desert end of the curve of grassland productivity, and productivity was closely related to the rainfall of the particular season. There was high variability between years at study sites, especially in the west (CV=279%), where it rained more seldom than in the east (CV=86%). During all years rainfall was very patchy at a spatial scale of 5 km, which appar- ently reflected the storm path of individual rain clouds. Long-term monitoring should be continued in order to detect changes of pattern in this rainfall-driven system.</text>
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                <text>Environmental Change and Vegetation Succession along an Ephemeral River: The Kuiseb in the Namib Desert</text>
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                <text>Forests line the course of the Kuiseb River, an ephemeral river in the Namib Desert, and several areas of these forests are characterized by high concentrations of tree death (Mizuno, 2005; Mizuno &amp; Yamagata, 2005). We sought to clarify the relationship between recent environmental changes and such tree deaths in the region. In November 2007, we examined the roots of a seedling of Acacia erioloba that was germinated by rainfall beginning in January 2006. The Acacia erioloba had grown to a height of 10cm and its roots to over 230cm, within two years. In the sapling (seedling) stage, Acacia erioloba extends its main roots deeply until it reaches a moist, fine-grained soil layer (sandy silt) and can absorb water through lateral roots. When it reaches the stage at which the water supply from the moist, fine-grained soil layer is insufficient for its growing size, the tree extends innumerable lateral roots within a 50cm depth from the land surface, where they absorb water that has been transported to a shallow depth by fog and other sources. Acacia erioloba dies when its lateral roots are unable to absorb water. Until the mid-1970s, successive floods repeatedly deposited fine-grained materials (e.g., sandy silt) that create water-bearing sediments for the growth of Acacia erioloba, and the trees died only rarely. However, from 1980 to 1985 these materials became increasingly scarce due to the decreasing occurrence of flooding, and consequently many trees died. It is reasonable to infer that the trees died because fine sediments were no longer being regularly deposited, and because of the drawdown of the groundwater level, both of which are making it difficult for the shallow roots of the trees to absorb the water necessary to survive.</text>
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                <text>Kazuharu MIZUNO</text>
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                <text>African study monographs. Supplementary issue (2010), 40: 3-18</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/96301</text>
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                  <text>Kyoto University</text>
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                <text>ENVIRONMENTAL CHANGES IN RELATION TO TREE DEATH ALONG THE KUISEB RIVER IN THE NAMIB DESERT</text>
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                <text>The Namib Desert is located along the western coast of Namibia and is affected by the cold Benguela Current. Although forest is distributed along the Kuiseb River in the Namib Desert, many trees are almost dead in some areas. The aim of this research was to clarify the relationship between environmental changes and tree death. The results of the survey are summarized as follows: (1) Many dead trees are located on the riverbanks made of dune sand, which are about 1 m high. (2) Dead trees are located in transitional areas where a northward protrusion of the southern shore is followed by a southward protrusion of the northern shore along the course of the river, in proximity to a sand dune. (3) Floods have eroded the noses of advancing sand dunes of the upper stream and have caused tree death by depositing sand. (4) The date of tree death has been estimated between the late 1970s and the early 1980s by 14C dating. (5) Flood days numbered 33 per year from 1962 to 1975 and 2.7 from 1976 to 1985. The remaining thick sand layer, deposited by the last flood, may be the cause of tree death, given that there was drastic decrease in fl oods since 1976. (6) Tree death has greatly affected people's lives along the Kuiseb River because they depend on riverside forests as a source of shade, shelter, fuel, and food for humans and livestock.</text>
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                <text>African study monographs. Supplementary issue (2005), 30: 27-41</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/68463</text>
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                <text>VEGETATION SUCCESSION AND PLANT USE IN RELATION TO ENVIRONMENTAL CHANGES ALONG THE KUISEB RIVER IN THE NAMIB DESERT</text>
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                <text>The aim of this study was to clarify the relationship between environmental change and vegetational succession in the Kuiseb River area of the Namib Desert. The results reveal the following: 1. About 5000–7000 years ago, wetter conditions prevailed in the Kuiseb River basin, forming a wider riverbed than at present. 2. About 600 years ago, a low terrace formed. The low terrace was characterized by the growth of acacia trees and other vegetation, which trapped and accreted aeolian sand. 3. About 400 years ago, the trapped and accumulated sand began to form a sand dune, eventually killing the tree population. 4. At the present time, all of the buried acacia trees have died and have been replaced by salvadora bushes, which continue to trap sand and increase the size of the dune. 5. Plants such as Acacia erioloba, Faidherbia albida, and Acanthosicyos horridus are very important food sources and shade plants for the local Topnaar people and their livestock. The succession of vegetation in response to environmental change has a profound impact on life in the Kuiseb River area, owing to the harsh environmental conditions and scarce plant life in the region.</text>
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                <text>Kazuharu MIZUNO, Kotaro YAMAGATA</text>
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                <text>African study monographs. Supplementary issue (2005), 30: 3-14</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/68465</text>
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                  <text>Kyoto University</text>
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                <text>Among the Central Kalahari San, hunting with dogs was once only of secondary importance to that with traps or bows and arrows. In recent years, hunting with bows and arrows has declined, whereas that with dogs has become more common. Dogs play an important role when the San hunt large antelopes with spears, or medium-sized animals with sticks. Hunting success depends on the hunter's skill in identifying footprints and timing for throwing the spear, and the chasing and fighting abilities of the dog. The owners of the dogs participating in a hunt share the game. Three factors can be identified for the increase in dog hunting. Firstly, dogs have increased dramatically. Secondly, dog hunting does not require hunters to learn new skills, and convenient for the San who travel long distance on foot. Thirdly, hides of medium-sized animals and dried gemsbok meat have become important source of cash in a developing commercial economy.</text>
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                <text>Kazunobu IKEYA</text>
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                <text>African Study Monographs (1994), 15(3): 119-134</text>
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                <text>1994</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/68123</text>
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        <name>Kazunobu IKEYA</name>
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        <name>San</name>
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                  <text>Kyoto University</text>
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                <text>ORIGIN OF THE FOG IN NAMIB DESERT IN DRY SEASON</text>
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                <text>The origin of the fog in the Namib Desert was generally considered the westerly advection fog over the Benguela cold current. When the author went to the Namib Desert in dry seasons in 2003 and 2004, the fog in the early morning, however, moved easterly from the inland to the Atlantic Ocean. It was the opposite direction of so called the sea fog. In addition to that, the fog in the Namib Desert showed the diurnal change: the fog arises in the early morning and disappeared before noon. The fog was usually driven easterly to the Atlantic Ocean. Through the climatic observation, the following were found for consideration of the origin of the fog on early August, 2004: it is not advection fog but that it is radiation fog. In the daytime, the air which is comparatively moist because of sea breeze moved to the inland, and it is solidified by radiative cooling in the night. Thus, the water vapor runs the fog and it is blown by the land wind to the westward.</text>
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                <text>Keiji KIMURA</text>
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                <text>African study monographs. Supplementary issue (2005), 30: 57-64</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/68461</text>
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        <name>Keiji KIMURA</name>
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              <name>Title</name>
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                  <text>Kyoto University</text>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Soil Clay Minerals in Namibia and their Significance for the Terrestrial and Marine Past Global Change Research</text>
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                <text>We delineated seven soil clay mineral provinces in Namibia. Many individual clay mineral assemblages occur in fluvial, pan, cave and other environments. Previous researchers have used clay mineral compositions as evidence for palaeoenvironmental reconstructions, often without analyzing the formation, the transport and the deposition of these clay minerals. In Namibia, rates of erosion and denudation by water and wind have been very small since early Quaternary times. During the Quaternary, the clay mineral assemblages of the seven provinces and of individual clay mineral deposits did not change significantly. Palaeoenvironmental reconstructions have to consider these small rates of erosion, especially if clay minerals were transported by water and/or wind from their source area to distant regions (e.g., the ocean). Changes in marine clay mineral compositions may not reflect climate change, but can be caused by changes in the ratio of fluvial to aeolian transport. If the changes in the transport mode are known, these changes can be interpreted palaeoenvironmentally. Future researchers have to decipher quantity and quality of the fluvial and aeolian dust transport (clay minerals, pollen, etc.) over southwestern Africa and the Benguela Current area.</text>
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                <text>Klaus HEINE, Jörg VÖLKEL</text>
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                <text>African study monographs. Supplementary issue (2010), 40: 31-50</text>
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              <elementText elementTextId="2995">
                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/96299</text>
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        <name>Clay minerals</name>
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        <name>Jörg VÖLKEL</name>
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        <name>Klaus HEINE</name>
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        <name>Namibia</name>
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        <name>Quaternary palaeoclimate</name>
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        <name>Terrestrial and marine geoarchives</name>
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                  <text>Kyoto University</text>
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          <element elementId="50">
            <name>Title</name>
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                <text>Influence of Geomorphology on the Physiognomy of Colophospermum mopane and its Effect on Browsing in Central Namibia</text>
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            <description>An account of the resource</description>
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                <text>Colophospermum mopane is a characteristic tree species indigenous to Southern Africa, where it forms 'mopane vegetation.' Mopane plays an important role in livestock farming, and the physiognomy of mopane influences the availability of feed. This study clarified the relationship between the difference in mopane physiognomy and the browsing activity of goats with reference to geomorphology. The physiognomy of mopane corresponded to geomorphological characteristics of surface structures and soil layer thickness. Consequently, the landscape based on the physiognomy of mopane was more diverse in the mountainous study area. Short, multi-stemmed mopane dominated the pediment and crest surface, while tall, single-stemmed mopane trees dominated the flood plain and ephemeral river bed. We determined that people recognize the differences in vegetation and geomorphology and use this knowledge to ensure good browsing for their goats. Most browsing occurred on pediment, where many short, multi-stemmed mopane plants, an important browsing resource for goats, can be found. The physiognomy of mopane at the study site corresponded to geomorphology and was related to browsing activity.</text>
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                <text>Koki TESHIROGI</text>
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              <elementText elementTextId="3039">
                <text>African study monographs. Supplementary issue (2010), 40: 103-114</text>
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                <text>2010</text>
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              <elementText elementTextId="3043">
                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/96294</text>
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        <name>Browsing activity</name>
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        <name>Colophospermum mopane</name>
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        <name>Feed resource</name>
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        <name>Koki TESHIROGI</name>
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        <name>Land unit</name>
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        <name>Namibia</name>
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        <name>Tree shape</name>
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                  <text>Kyoto University</text>
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                <text>Recent Grain-Size Coarsening of Floodplain Deposits and Forest Decline along the Kuiseb River, Namib Desert, Namibia</text>
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                <text>We investigated the flood plain deposits of the middle reach of the Kuiseb River in order to reveal the recent fluvial environment changes and forest decline. For the conservation of watershed environments, it is important to examine the relationship between environmental and hydrological changes. Fluvial deposits are useful for this as they record the past environmental changes in a catchment. Grain size coarsening was seen in the upper flood plain deposits in many places. The cause of the deposit coarsening was considered to be a relative increase in the supply of coarse material. The frequency of floods seems to have been decreased by the construction of many dams in the upper stream area, but sand dunes continue to advance on the river bed, increasing the relative supply rate of coarse material (dune sand). Notable forest declines were observed at the places where marked deposition of coarse sand had occurred, as such coarse deposits cannot retain water and are desiccated rapidly. The subsequent severe dry conditions at the roots induce tree death.</text>
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                <text>Kotaro YAMAGATA</text>
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            <name>Publisher</name>
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              <elementText elementTextId="2935">
                <text>African study monographs. Supplementary issue (2010), 40: 19-30</text>
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                <text>The hyperarid to arid Namib Desert extends along the west coast of southern Africa. The Kuiseb River is one of the major ephemeral rivers originating in the interior highland, and crosses the Namib Desert. Fluvial terraces are well developed along the middle reaches of the Kuiseb River near Gobabeb, and are classified into four surfaces: upper (H), middle 1 (M1), middle 2 (M2), and lower (L). Layers of calcrete are founded on the M1 and M2 surfaces, and gypcrete layers are founded on the H surface. Dead tree matter, buried by dune sand on the L surface, dates to 300±60 years BP and 550±50 years BP. The calcareous crusts on the M1 surface date to 5, 300±60 years BP and 6, 450±50 years BP, and those of the M2 surface date to 22, 070±260 years BP. The presence of calcrete suggests that the ground water level was higher when the M1 and M2 surfaces were formed than it is at the present time. Tree size distribution on the L surface demonstrates that the L surface was also formed during a relatively wet period. It may be concluded, therefore, that these fluvial terraces record the humid periods of ca 22 ka, 5–6.5 ka, and 300–600 years BP in the catchment area of the Kuiseb River. The presence of a water-soluble gypsum crust on the H surface suggests that the paleohydrologic environment of these terrace-forming periods probably involved increased rainfall in the interior highland east of the desert.</text>
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                <text>African study monographs. Supplementary issue (2005), 30: 15-25</text>
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                  <text>Kyoto University</text>
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                <text>San Cross-border cultural heritage and identity in Botswana, Namibia and South Africa</text>
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                <text>The aim of this paper is to examine the indigenous San cultural identity that transcends ecological zones across the borders of Botswana, Namibia and South Africa respectively. The paper explores the representation of borders and boundaries within traditional culture, dance and music. Dance, music, material art and craft, if broadly defined, become a medium through which San women and men narrate their experiences to a broader audience. The paper contends that giving voice to the San: in the many forms that such voice is captured, will significantly enhance our understanding of indigenous knowledge systems and thus better guide strategies towards transformation of modern southern African societies. The discussion aims to showcase San indigenous knowledge systems and creativity, and shift the discourse from a 'marginalised and suffering only' sphere to appreciation of their voices through culture, art, music and dance. The article suggests that the San artistic contribution, the articulation of their specific experiences and traditional knowledge enjoy significant attention across political boundaries.</text>
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                <text>Maitseo BOLAANE</text>
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                <text>African Study Monographs (2014), 35(1): 41-64</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/187748</text>
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                  <text>Kyoto University</text>
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                <text>CHANGES IN THE DISTRIBUTION OF THE !NARA PLANT THAT AFFECT THE LIFE OF THE TOPNAAR PEOPLE IN THE LOWER KUISEB RIVER, NAMIB DESERT</text>
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                <text>The !Nara plant is endemic to the central Namib Desert. The Topnaar people, who live along the Kuiseb River, use this plant in their daily lives, as it serves as a vital source of income, nutrition, and traditional culture. !Nara is virtually the only food source of the Topnaar during harvest time, and cash can be obtained by selling the seeds of the !Nara fruit. In fact, 40% of Topnaar harvesters have no other source of income. A fl ood protection wall was built in 1961 to protect Walvis Bay from flood damage, and a tributary that once flowed to the town was dammed as a result. A large percentage of !Nara was killed, and the crop yield decreased dramatically. The loss of floodwaters following the construction of the wall likely resulted in a decreased moisture supply, causing !Nara vegetation to suffer. It is probably difficult for seeds to germinate owing to the decreased flooding erosion, the increased accumulation of sand, and the lowered groundwater table.</text>
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                <text>Masaaki ITO</text>
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                <text>African study monographs. Supplementary issue (2005), 30: 65-75</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/68460</text>
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        <name>Nama</name>
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                  <text>Kyoto University</text>
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                <text>REFUGEES, RESETTLEMENT, AND LAND AND RESOURCE CONFLICTS: THE POLITICS OF IDENTITY AMONG !XUN AND KHWE SAN IN NORTHEASTERN NAMIBIA</text>
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                <text>This study examines land use, natural resource, and development conflicts, and the effects of government policies in a remote area in northeastern Namibia, known formerly as West Bushmanland, now Tsumkwe West. !Xun and Khwe San who had been soldiers of the South African Defense Force in the Angolan and Namibian wars of independence in the 1970s and 1980s were resettled in this area along with their families. Namibian government resettlement and development projects were planned and implemented in the Tsumkwe West in the early 1990s. In part because of the ways in which !Xun and Khwe San identities were constructed over time by settlers, academics, policy-makers, the South African Defense Force, the colonial and post-colonial state, and San themselves, the people of Tsumkwe West, later, the N≠a Jaqna Conservancy, have had to struggle against other groups and the state for the stake in their land and resources. Drawing on anthropological research, work of non-government organizations, and interviews of people in the area over a period of two and a half decades, this study assesses some of the ways in which resettlement and land and resource policies have mutually affected the Namibian government, the military, private companies, donor agencies, non-government and community-based organizations, and a diverse set of peoples in northeastern Namibia.</text>
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                <text>African Study Monographs (2012), 33(2): 73-132</text>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/159000</text>
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        <name>Communal land tenure</name>
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        <name>Ju/’hoansi San</name>
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        <name>Resource rights</name>
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        <name>Robert K. Hitchcock</name>
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        <src>https://namibiadigitalrepository.com/files/original/d5a9d42c98f4907abf63c71265b85d33.pdf</src>
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                  <text>Kyoto University</text>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>CHANGE IN POPULATION AND LAND-USE INTENSITIES IN SEVERAL VILLAGES OF THE FOUR NORTHERN REGIONS OF NAMIBIA</text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
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                <text>Demographic changes in several rural areas in the four northern regions of Namibia were traced from 1991 to 2001 using national census data. On average, the population growth rate of the surveyed area was 2.77% per year. Although this rate approximated the country's mean growth rate of 2.64%, the surveyed areas showed significant differences from the mean, ranging from 3.4% to 7.2% per year. A combination of demographic and land use data collected from four representative villages in the study region revealed that rural-to-urban migration on a micro-scale is a significant process in the control of the area's ecology and economy, and that the percentage of cultivated land is closely tied to population density.</text>
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            <name>Creator</name>
            <description>An entity primarily responsible for making the resource</description>
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                <text>Shigeru Araki</text>
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          <element elementId="45">
            <name>Publisher</name>
            <description>An entity responsible for making the resource available</description>
            <elementTextContainer>
              <elementText elementTextId="3103">
                <text>African study monographs. Supplementary issue (2005), 30: 77-88</text>
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            </elementTextContainer>
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            <name>Format</name>
            <description>The file format, physical medium, or dimensions of the resource</description>
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            <name>Date</name>
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                <text>2005</text>
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            <name>Language</name>
            <description>A language of the resource</description>
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                <text>English</text>
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            <name>Source</name>
            <description>A related resource from which the described resource is derived</description>
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                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/68459</text>
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        <name>Four northern regions</name>
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        <name>Land use intensity</name>
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        <name>Namibia</name>
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      <tag tagId="137">
        <name>Ovamboland</name>
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      <tag tagId="1195">
        <name>Population census</name>
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      <tag tagId="1196">
        <name>Shigeru Araki</name>
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        <src>https://namibiadigitalrepository.com/files/original/57bc348bbfc72e16741a364115d377da.pdf</src>
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              <name>Title</name>
              <description>A name given to the resource</description>
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                  <text>Kyoto University</text>
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      <name>Text</name>
      <description>A resource consisting primarily of words for reading. Examples include books, letters, dissertations, poems, newspapers, articles, archives of mailing lists. Note that facsimiles or images of texts are still of the genre Text.</description>
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      <elementSet elementSetId="1">
        <name>Dublin Core</name>
        <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Late Pleistocene Sedimentary Environment of the "Homeb Silts" Deposits, along the Middle Kuiseb River in the Namib Desert, Namibia</text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
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                <text>In the Namib, the tectonic and geographic setting of the area means that there are no large lake basins, and relict aeolian deposits appear to be quite rare. This has posed severe problems for reconstructing palaeoclimates in this region. In addition, there are significant problems with developing a well-dated chronology of events, as well as in the interpretation of the dated evidence for hydrologic and climatic changes. The Late Pleistocene "Homeb Silts" have been interpreted in previous studies as follows: (1) dunedamed lake sediments indicating an arid environment; (2) river end-point deposits indicating arid conditions; (3) flood plain sediments of an aggrading river indicating a semi-arid environment and (4) river flood slack water sediments indicating a wet environment and intense precipitation events in the headwaters. In this present study, sedimentary facies of the "Homeb Silts" were re-described and interpretation of the sedimentary environment changes that resulted in their deposition re-assessed. The conclusions are as follows: (1) The "Homeb Silts" were deposited during ca. 26 to 19 k yrs BP (ca. 25 to 19 k cal yrs BP) as indicated by eleven AMS 14C measurements; (2) Almost all of the "Homeb Silts" were deposited under wet conditions by fluvial floods, except during the early depositional phase; (3) The "Homeb Silts" have recorded some detailed environmental changes during ca. 26 to 19 k yrs BP (ca. 25 to 19 k cal yrs BP); and, (4) Depositional events caused by similar climatic events in recent years have occurred, like heavy rains and flood events in the headwaters.</text>
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          <element elementId="39">
            <name>Creator</name>
            <description>An entity primarily responsible for making the resource</description>
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                <text>Shinji MIYAMOTO</text>
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            <name>Publisher</name>
            <description>An entity responsible for making the resource available</description>
            <elementTextContainer>
              <elementText elementTextId="3055">
                <text>African study monographs. Supplementary issue (2010), 40: 51-66</text>
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            </elementTextContainer>
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            <name>Format</name>
            <description>The file format, physical medium, or dimensions of the resource</description>
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                <text>PDF</text>
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            <name>Date</name>
            <description>A point or period of time associated with an event in the lifecycle of the resource</description>
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                <text>2010</text>
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            </elementTextContainer>
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          <element elementId="44">
            <name>Language</name>
            <description>A language of the resource</description>
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              <elementText elementTextId="3058">
                <text>English</text>
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          </element>
          <element elementId="48">
            <name>Source</name>
            <description>A related resource from which the described resource is derived</description>
            <elementTextContainer>
              <elementText elementTextId="3059">
                <text>http://repository.kulib.kyoto-u.ac.jp/dspace/handle/2433/96298</text>
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    <tagContainer>
      <tag tagId="1157">
        <name>AMS radiocarbon dating</name>
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      <tag tagId="1090">
        <name>Kuiseb River</name>
      </tag>
      <tag tagId="1158">
        <name>Last Glacial Maximum (LGM)</name>
      </tag>
      <tag tagId="630">
        <name>Namib Desert</name>
      </tag>
      <tag tagId="1159">
        <name>Palaeohydrology</name>
      </tag>
      <tag tagId="1160">
        <name>Sedimentary environment</name>
      </tag>
      <tag tagId="1161">
        <name>Shinji MIYAMOTO</name>
      </tag>
      <tag tagId="1162">
        <name>Slack water sediments</name>
      </tag>
    </tagContainer>
  </item>
</itemContainer>
