Caza y espacios naturales protegidos en Extremadura

La superficie protegida ha crecido, en poco más de un siglo, de forma muy rápida, logrando alcanzar cifras significativas que, no obstante, pueden oscilar de forma muy notable entre unos países y otros. Este interés por proteger los espacios naturales responde, en el contexto actual, a la consecución de una amplia serie de fines de carácter científico, educativo, recreativo y socioeconómico. Como consecuencia de ello, ha surgido un nuevo escenario en el que determinados aprovechamientos tradicionales se están viendo afectados. La caza es, sin duda, uno de los mejores ejemplos de actividad tradicional que se está viendo perjudicada por este proceso. Con estos antecedentes, en el presente trabajo se analiza con carácter general la situación de los espacios naturales protegidos en Extremadura en relación con la actividad cinegética. Este análisis se lleva a cabo teniendo en cuenta que un tercio de la superficie regional está protegida por algunas de las figuras existentes y que, además, estos espacios se distribuyen por áreas en las que la caza ha sido un aprovechamiento tradicional que ha contribuido a mantener los espacios en mejor estado de conservación.

III. Diary, 1799

This diary, which John Henry Tudor titled A Registry of College Adventures, documents his life as a student at Harvard College. The entries describe his daily activities and notable events, including trips to the theater, hunting outings to "shoot Robbins," adventures with other students in local taverns, visits with his family in Boston and at the family estate, Rockwood, and the illumination of Cambridge in honor of George Washington's birthday. Tudor created and recorded a humorous classology, describing his peers at Harvard in a sometimes scathing manner, and also recorded information about those obliged to leave the College, usually following pranks or other unacceptable behavior. He also recounts his own involvement in pranks and other antics, which he believed to be the only antidote to the dullness of college life, and in one entry he describes an evening when he and several friends "disguised [them]selves like Negroes" and wandered into scholars' rooms without detection. Tudor was a member of the Hasty Pudding Club and the Porcellian Club ("the Pig club") while at Harvard and describes club meetings in several entries. There are also more reflective and personal entries, describing Tudor's feelings about his aging grandmother, his brother William's departure for Holland, and his desire for a "wife who shall make [him] happy[,] an affectionate dog [and] a farm & garden."

Traditional beluga drives of the Iñupiat of Kotzebue Sound, Alaska / Charles V. Lucier, James W. VanStone.

n.s. no.25(1995)

Primitive hunters of Australia / by Wilfrid D. Hambly, Assistant Curator of African Ethnology. 12 plates in photogravure and 1 map.

no.32(1936)

III. Diary, 1799

This diary, which John Henry Tudor titled A Registry of College Adventures, documents his life as a student at Harvard College. The entries describe his daily activities and notable events, including trips to the theater, hunting outings to "shoot Robbins," adventures with other students in local taverns, visits with his family in Boston and at the family estate, Rockwood, and the illumination of Cambridge in honor of George Washington's birthday. Tudor created and recorded a humorous classology, describing his peers at Harvard in a sometimes scathing manner, and also recorded information about those obliged to leave the College, usually following pranks or other unacceptable behavior. He also recounts his own involvement in pranks and other antics, which he believed to be the only antidote to the dullness of college life, and in one entry he describes an evening when he and several friends "disguised [them]selves like Negroes" and wandered into scholars' rooms without detection. Tudor was a member of the Hasty Pudding Club and the Porcellian Club ("the Pig club") while at Harvard and describes club meetings in several entries. There are also more reflective and personal entries, describing Tudor's feelings about his aging grandmother, his brother William's departure for Holland, and his desire for a "wife who shall make [him] happy[,] an affectionate dog [and] a farm & garden."

Upper Penobscot Bay, Maine, Nautical Chart, 1776 (Image 2 of 2) (Raster Image)

This layer is a georeferenced raster image of the untitled, historic nautical chart: [A chart of Great Bluehill Bay, Penobscot River &c.] (sheet originally published in 1776). The map is [sheet 41] from the Atlantic Neptune atlas Vol. 3 : Charts of the coast and harbors of New England, from surveys taken by Samuel Holland and published by J.F.W. Des Barres, 1781. Scale [ca. 1:50,000]. This layer is image 2 of 2 total images of the two sheet source map, representing the eastern portion of the map. Covers a portion of Penobscot Bay, including Blue Hill Bay, Deer Island, and Eggemoggin Reach, Maine. The image is georeferenced to the surface of the earth and fit to the 'World Mercator' (WGS 84) projected coordinate system. All map collar information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, or other information associated with the principal map. This map shows coastal features such as harbors, inlets, rocks, channels, points, coves, shoals, islands, and more. Includes also selected land features such as cities and towns, and buildings. Relief is shown by hachures; depths by soundings. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection. The entire Atlantic Neptune atlas Vol. 3 : Charts of the coast and harbors of New England has been scanned and georeferenced as part of this selection.

Milwaukee County, Wisconsin, 1858 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of the county of Milwaukee, Wisconsin, from surveys under the direction of H.F. Walling ; engraved, printed, colored & mounted at H.F. Wallings Map Establishment. It was published by M.H. Tyler in 1858. Scale [1:31,680]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Wisconsin South State Plane NAD 1983 coordinate system (in Feet) (Fipszone 4803). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This cadastral map shows features such as roads, railroads and stations, drainage, city wards, selected buildings, property lots, and names of landowners, and more. Includes insets: City of Milwaukee -- Humboldt (Milwaukee) -- Franklin -- Oak Creek -- Wauwatosa. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Milwaukee and vicinity, Wisconsin, 1962 (Image 1 of 4) (Raster Image)

This layer is a georeferenced raster image of the historic, topographic paper map entitled: Milwaukee and vicinity, Wisconsin, 1959, mapped, edited and published by the Geological Survey. It was published by U.S. Dept. of the Interior, Geological Survey in 1962. Scale 1:24,000. Compiled from 1:24,000-scale maps of Thiensville, Menomonee Falls, Wauwatosa, Milwaukee, South Milwaukee, Greendale 1958, and Hales Corners 1959 7.5 minute quadrangles. Selected hydrographic data compiled from U.S. Lake Survey Charts 74 and 743 (1957). This layer is image 1 of 4 total images of the four sheet source map representing the northwest portion of the map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Wisconsin South State Plane NAD 1927 coordinate system (Fipszone 4803). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This is a typical topographic map portraying both natural and manmade features. It shows and names works of nature, such as mountains, valleys, lakes, rivers, vegetation, etc. It also identify the principal works of humans, such as roads, railroads, boundaries, transmission lines, major buildings, etc. Relief shown by contours (interval 10 feet) and spot heights. Depths shown by contours and soundings. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Milwaukee and vicinity, Wisconsin, 1962 (Image 2 of 4) (Raster Image)

This layer is a georeferenced raster image of the historic, topographic paper map entitled: Milwaukee and vicinity, Wisconsin, 1959, mapped, edited and published by the Geological Survey. It was published by U.S. Dept. of the Interior, Geological Survey in 1962. Scale 1:24,000. Compiled from 1:24,000-scale maps of Thiensville, Menomonee Falls, Wauwatosa, Milwaukee, South Milwaukee, Greendale 1958, and Hales Corners 1959 7.5 minute quadrangles. Selected hydrographic data compiled from U.S. Lake Survey Charts 74 and 743 (1957). This layer is image 2 of 4 total images of the four sheet source map representing the northeast portion of the map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Wisconsin South State Plane NAD 1927 coordinate system (Fipszone 4803). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This is a typical topographic map portraying both natural and manmade features. It shows and names works of nature, such as mountains, valleys, lakes, rivers, vegetation, etc. It also identify the principal works of humans, such as roads, railroads, boundaries, transmission lines, major buildings, etc. Relief shown by contours (interval 10 feet) and spot heights. Depths shown by contours and soundings. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Local community perception towards bats (Mammalia: Chiroptera) in Caves in South central Mindanao, Philippines: Threats and Implication for conservation

In the tropics, bats are an essential component of many native ecosystems, through providing various ecological services including pollination and insect pest control, in addition to seed dispersal. Many Philippine bat species roost in caves and underground habitats. However, many caves are disturbed by people, to exploit resources for food, recreation, and mineral and guano extraction. The misunderstanding of the importance of bats to the ecosystem is also considered a threat to many cave roosting species. Understanding the conflicts between humans and ecosystems which provide essential services is important to maintain ecosystem service provision. A total of 100 local respondents from the village of Pisan, Kabacan North Cotabato in south central Mindanao were interviewed through semi-structured interviews and focus group discussions. Respondents were asked about their views, levels of knowledge, use, interaction, and awareness towards both the caves and bats in their locality. Our survey found that most of the respondents are aware of the presence of bats from the caves in their locality. Unfortunately, a large proportion of the respondents noted that bats are hunted in caves for bush meat and trade, and most people perceived bats as pest to fruit crops such as durian. These factors are among the main factors of the execution of many bat colonies in caves of south central Mindanao. In general, cave bats are under appreciated species in caves. The unregulated tourism, hunting for bush meat and trade, and guano extraction are among the alarming threats occurring for both caves and bats in the locality and possibly to other localities in the country. Furthermore, the establishment of strong and effective model conservation education programs and the strengthening the participation of local government, academic, and community are essential steps to preserve the current state of cave bats in the area.

(Table 2) Radiocarbon ages of lake sediments from Boresø, East Greenland

This chapter provides a review of proxy data from a variety of natural archives sampled in the Wollaston Forland region, central Northeast Greenland. The data are used to describe long-term environmental and climatic changes. The focus is on reconstructing the Holocene conditions particularly in the Zackenberg area. In addition, this chapter provides an overview of the archaeological evidence for prehistoric occupation of the region. The Zackenberg area has been covered by the Greenland Ice Sheet several times during the Quaternary. At the Last Glacial Maximum (LGM, about 22,000 years BP), temperatures were much lower than at present, and only very hardy organisms may have survived in the region, even if ice-free areas existed. Marked warming at around 11,700 years BP led to ice recession, and the Zackenberg area was deglaciated in the early Holocene, prior to 10,100 years BP. Rapid early Holocene land emergence was replaced by a slight transgression in the late Holocene. During the Holocene, summer solar insolation decreased in the north. Following deglaciation of the region, summer temperatures probably peaked in the early to mid-Holocene, as indicated by the occurrence of a southern beetle species. However, the timing for the onset of the Holocene thermal maximum is rather poorly constrained because of delayed immigration of key plant species. During the thermal maximum, the mean July temperature was at least 2-3°C higher than at present. Evidence for declining summer temperatures is seen at around 5500, 4500 and 3500 years BP. The cooling culminated during the Little Ice Age that peaked about 100-200 years ago. The first plants that immigrated to the region were herbs and mosses. The first dwarf shrubs arrived in Northeast Greenland prior to 10,400 years BP, and dwarf birch arrived around 8800 years BP. The first people arrived about 4500 years BP, but the region was depopulated several times before the last people disappeared some time after 1823 AD, perhaps as a consequence of poor hunting conditions during the peak of the Little Ice Age.

Pollen profiles from a Late Palaeolithic site in the community of Bad Buchau-Kappel, Baden-Wuerttemberg, Germany

Excavations were carried out in a Late Palaeolithic site in the community of Bad Buchau-Kappel between 2003 and 2007. Archaeological investigations covered a total of more than 200 m**2. This site is the product of what likely were multiple occupations that occurred during the Late Glacial on the Federsee shore in this location. The site is situated on a mineral ridge that projected into the former Late Glacial lake Federsee. This beach ridge consists of deposits of fine to coarse gravel and sand and was surrounded by open water, except for a connection to the solid shore on the south. A lagoon lay between the hook-shaped ridge and the shore of the Federsee. This exposed location provided optimal access to the water of the lake. In addition, the small lagoon may have served as a natural harbor for landing boats or canoes. Sedimentological and palynological investigations document the dynamic history of the location between 14,500 and 11,600 years before present (cal BP). Evidence of the deposition of sands, gravels and muds since the Bølling Interstadial is provided by stratigraphic and palynological analyses. The major occupation occurred in the second half of the Younger Dryas period. Most of the finds were located on or in the sediments of the ridge; fewer finds occurred in the surrounding mud, which was also deposited during the Younger Dryas. Direct dates on some bone fragments, however, demonstrate that intermittent sporadic occupations also took place during the two millennia of the Meiendorf, Bølling, and Allerød Interstadials. These bones were reworked during the Younger Dryas and redeposited in the mud. A 14C date from one bone of 11,600 years ago (cal BP) places the Late Palaeolithic occupation of the ridge at the very end of the Younger Dryas, which is in agreement with stratigraphic observations. Stone artifacts, numbering 3,281, comprise the majority of finds from the site. These include typical artifacts of the Late Palaeolithic, such as backed points, short scrapers, and small burins. There are no bipointes or Malaurie-Points, which is in accord with the absolute date of the occupation. A majority of the artifacts are made from a brown chert that is obtainable a few kilometers north of the site in sediments of the Graupensandrinne. Other raw materials include red and green radiolarite that occur in the fluvioglacial gravels of Oberschwaben, as well as quartzite and lydite. The only non-local material present is a few artifacts of tabular chert from the region near Kelheim in Bavaria. A unique find consists of two fragments of a double-barbed harpoon made of red deer antler, which was found in the Younger Dryas mud. It is likely, but not certain, that this find belongs to the same assemblage as the numerous stone artifacts. Although not numerous, animal bones were also found in the excavations. Most of them lay in sediments of the Younger Dryas, but several 14C dates place some of these bones in earlier periods, including the Meiendorf, Bølling, and Allerød Interstadials. These bones were reworked by water and redeposited in mud sediments during the Younger Dryas. As a result, it is difficult to attribute individual bones to particular chronological positions without exact dates. Species that could be identified include wild horse (Equus spec.), moose or elk (Alces alces), red deer (Cervus elaphus), roe deer (Capreolus capreolus), aurochs or bison (Bos spec.), wild boar (Sus scrofa), as well as birds and fish, including pike (Esox Lucius).

University of Michigan Women's Cross Country Team, 1982

Back Row: Holly Hunting, Melanie Weaver, Lisa Larsen-Weidenbach, Judy Yuhn, coach Francie Kraker Goodridge

Front Row: Sue Schroeder, Carol Lam, Patty Shanahan, Sue Frederick-Foster