1.
Amber
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Amber is fossilized tree resin, which has been appreciated for its color and natural beauty since Neolithic times. Much valued from antiquity to the present as a gemstone, amber is made into a variety of decorative objects and it has also been used as a healing agent in folk medicine. There are five classes of amber, defined on the basis of their chemical constituents, because it originates as a soft, sticky tree resin, amber sometimes contains animal and plant material as inclusions. Amber occurring in coal seams is also called resinite, and the term ambrite is applied to that found specifically within New Zealand coal seams, the English word amber derives from Arabic ʿanbar عنبر via Middle Latin ambar and Middle French ambre. The word was adopted in Middle English in the 14th century as referring to what is now known as ambergris, in the Romance languages, the sense of the word had come to be extended to Baltic amber from as early as the late 13th century. At first called white or yellow amber, this meaning was adopted in English by the early 15th century, as the use of ambergris waned, this became the main sense of the word. The two substances conceivably became associated or confused because they both were washed up on beaches. Ambergris is less dense water and floats, whereas amber is too dense to float. The classical names for amber, Latin electrum and Ancient Greek ἤλεκτρον, are connected to a term ἠλέκτωρ meaning beaming Sun, according to myth, when Phaëton son of Helios was killed, his mourning sisters became poplar trees, and their tears became elektron, amber. Earlier Pliny says that an island of three days sail from the Scythian coast called Balcia by Xenophon of Lampsacus, author of a fanciful travel book in Greek, is called Basilia by Pytheas. It is generally understood to be the same as Abalus and it is assumed that there were well-established trade routes for amber connecting the Baltic with the Mediterranean. Pliny states explicitly that the Germans export amber to Pannonia, from where it was traded further abroad by the Veneti, the ancient Italic peoples of southern Italy were working amber, the most important examples are on display at the National Archaeological Museum of Siritide to Matera. Amber used in antiquity as at Mycenae and in the prehistory of the Mediterranean comes from deposits of Sicily. Besides the fanciful explanations according to which amber is produced by the Sun, Pliny cites opinions that are aware of its origin in tree resin. Amber is produced from a marrow discharged by trees belonging to the genus, like gum from the cherry. This is confirmed by the recorded Old High German glas and Old English glær for amber, in Middle Low German, amber was known as berne-, barn-, börnstēn. The Low German term became dominant also in High German by the 18th century, the Baltic Lithuanian term for amber is gintaras and Latvian dzintars. They, and the Slavic jantar or Hungarian gyanta, are thought to originate from Phoenician jainitar, Early in the nineteenth century, the first reports of amber from North America came from discoveries in New Jersey along Crosswicks Creek near Trenton, at Camden, and near Woodbury
2.
Eocene
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The Eocene Epoch, lasting from 56 to 33.9 million years ago, is a major division of the geologic timescale and the second epoch of the Paleogene Period in the Cenozoic Era. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a period in which the concentration of the carbon isotope 13C in the atmosphere was exceptionally low in comparison with the more common isotope 12C. As with other periods, the strata that define the start and end of the epoch are well identified. The name Eocene comes from the Ancient Greek ἠώς and καινός, the Eocene epoch is conventionally divided into early, middle, and late subdivisions. The corresponding rocks are referred to as lower, middle, the Ypresian stage constitutes the lower, the Priabonian stage the upper, and the Lutetian and Bartonian stages are united as the middle Eocene. The Eocene Epoch contained a variety of different climate conditions that includes the warmest climate in the Cenozoic Era. During this period of time, little to no ice was present on Earth with a difference in temperature from the equator to the poles. Following the maximum was a descent into an icehouse climate from the Eocene Optimum to the Eocene-Oligocene transition at 34 million years ago. During this decrease ice began to reappear at the poles, greenhouse gases, in particular carbon dioxide and methane, played a significant role during the Eocene in controlling the surface temperature. For the early Eocene there is discussion on how much carbon dioxide was in the atmosphere. This is due to numerous proxies representing different atmospheric carbon dioxide content, for contrast, today the carbon dioxide levels are at 400 ppm or 0. 04%. At about the beginning of the Eocene Epoch the amount of oxygen in the atmosphere more or less doubled. During the early Eocene, methane was another gas that had a drastic effect on the climate. In comparison to carbon dioxide, methane has much effect on temperature as methane is ~34 times more effective per molecule than carbon dioxide on a 100-year scale. Most of the methane released to the atmosphere during this period of time would have been from wetlands, swamps, the atmospheric methane concentration today is 0. 000179% or 1.79 ppmv. Due to the climate and sea level rise associated with the early Eocene, more wetlands, more forests. Comparing the early Eocene production of methane to current levels of atmospheric methane, biogenic production of methane produces carbon dioxide and water vapor along with the methane, as well as yielding infrared radiation
3.
Kaliningrad Oblast
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Kaliningrad Oblast is a federal subject of the Russian Federation that is located on the coast of the Baltic Sea. As an oblast, its status is equal to each of the other 84 federal subjects. Its administrative center is the city of Kaliningrad, formerly known as Königsberg and it is the only Baltic port in the Russian Federation that remains ice-free in winter. According to the 2010 census, it had a population of 941,873, the oblast is an exclave so visa-free travel to the main part of Russia is only possible by sea or air. The territory was part of East Prussia. With the defeat of Nazi Germany in 1945, the territory was annexed by the Soviet Union, following the post-war migration and expulsion of the German-speaking population, the territory was populated with citizens from the Soviet Union. Today, only a few thousand ethnic Germans remain, most of recent immigrants from other parts of the former Soviet Union. Early in the 21st century, the hitherto flagging economy of Kaliningrad Oblast became one of the best performing economies in Russia and this was helped by a low manufacturing tax rate related to its Special Economic Zone status. As of 2006, one in three televisions manufactured in Russia came from Kaliningrad, the territorys population was one of the few in Russia that was expected to show strong growth after the collapse of the USSR. Germany currently places no claims, however it also has not renounced any claims to the possibility of territory reunification. During the Middle Ages, the territory of what is now Kaliningrad Oblast was inhabited by tribes of Old Prussians in the western part, the tribes were divided by the rivers Pregolya and Alna. The Teutonic Knights conquered the region and established a monastic state, on the foundations of a destroyed Prussian settlement known as Tvanksta, the Order founded the city of Königsberg. Germans resettled the territory and assimilated the indigenous Old Prussians, the Lithuanian-inhabited areas became known as Lithuania Minor. Speakers of the old Baltic languages became extinct around the 17th century, in 1525, Grand Master Albert of Brandenburg secularized the Prussian branch of the Teutonic Order and established himself as the sovereign of the Duchy of Prussia. The duchy was nominally a fief of the Polish crown and it later merged with the Margravate of Brandenburg. Königsberg was the capital from 1525 until 1701. As the centre of Prussia moved westward, the position of the capital became too peripheral, during the Seven Years War it was occupied by the Russian Empire. The region was reorganized into the Province of East Prussia within the Kingdom of Prussia in 1773, the territory of the Kaliningrad Oblast lies in the northern part of East Prussia
4.
Bitterfeld
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Bitterfeld is a town in the district Anhalt-Bitterfeld, Saxony-Anhalt, Germany. Since 1 July 2007 it has been part of the town Bitterfeld-Wolfen and it is situated approximately 25 km south of Dessau, and 30 km northeast of Halle. Bitterfeld was built by a colony of Flemish immigrants in 1153 and it was captured by the landgrave of Meissen in 1476, and belonged thenceforth to Saxony, until it was ceded to Prussia in 1815. By 1900 Bitterfeld contained an important junction of railways from Leipzig, the population at that time was 11,839, it manufactured drain-pipes, paper-roofing and machinery, and had saw-mills. There were also several coal-mines in the vicinity, owing to its pleasant situation and accessibility, it had become a favoured residence of business men of Leipzig and Halle. During the GDR years, it gained notoriety for its chemical complex which caused remarkably severe pollution. On 24 April 1959 it also was a scene for the Bitterfeld Conference and this conference sought to connect the working class with the artists of the day to form a socialist national culture. In the 21st century Bitterfeld is still a town and it stages the annual United Metal Maniacs metal festival. The former brown-coal open cast mine of Goitzsche, south-east of Bitterfeld, is a source of fossils in Bitterfeld amber. Walther Rathenau, he brought the industry to Bitterfeld in 1893. Klaus Staeck, graphic artist, lawyer and president of the academy of the arts, grew up in Bitterfeld, fischer Verlag, Frankfurt am Main 2009, ISBN 978-3-10-048828-2. Lojewsky, Hannelore, Seh’n wir uns nicht in dieser Welt, in, Norbert Kühne, Individuelles Lernen wird an Bedeutung gewinnen. 100 Jahre Hans-Böckler-Berufskolleg Marl/Haltern, Marl 2009, S. 29–30, klaus Seehafer, Dann sehn wir uns in Bitterfeld. Edition no.1 Böhlau, Cologne, Weimar, Vienna 2004, hackenholz, Dirk, Die elektrochemischen Werke in Bitterfeld 1914–1945
5.
Lignite
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Lignite, often referred to as brown coal, is a soft brown combustible sedimentary rock formed from naturally compressed peat. It is considered the lowest rank of coal due to its low heat content. It has a carbon content around 60–70 percent and it is mined all around the world and is used almost exclusively as a fuel for steam-electric power generation, but is also mined for its germanium content in China. The energy content of lignite ranges from 10 to 20 MJ/kg on a moist, the energy content of lignite consumed in the United States averages 15 MJ/kg, on the as-received basis. The energy content of lignite consumed in Victoria, Australia, averages 8.4 MJ/kg, lignite has a high content of volatile matter which makes it easier to convert into gas and liquid petroleum products than higher-ranking coals. Unfortunately, its moisture content and susceptibility to spontaneous combustion can cause problems in transportation. However, removing the moisture increases the cost of the final lignite fuel, because of its low energy density and typically high moisture content, brown coal is inefficient to transport and is not traded extensively on the world market compared with higher coal grades. It is often burned in power stations near the mines, such as in Australias Latrobe Valley, the operation of traditional brown-coal plants, particularly in combination with strip mining, can be politically contentious due to environmental concerns. An environmentally beneficial use of lignite can be found in its use in cultivation and distribution of biological control microbes that suppress plant disease causing microbes, lignite begins as an accumulation of partially decayed plant material, or peat. Burial by other sediments results in increasing temperature, depending on the geothermal gradient and tectonic setting. This causes compaction of the material and loss of some of the water and this process, called coalification, concentrates the carbon content, and thus the heat content, of the material. Deeper burial and the passage of time result in expulsion of moisture and volatile matter, eventually transforming the material into higher rank coals such as bituminous. Lignite deposits are younger than higher-ranked coals, with the majority of them having formed during the Tertiary period. The Latrobe Valley in the state of Victoria, Australia, contains estimated reserves of some 65 billion tonnes of brown coal, the deposit is equivalent to 25 percent of known world reserves. The coal seams are up to 100 metres thick, with coal seams often giving virtually continuous brown coal thickness of up to 230 metres. Seams are covered by little overburden. Lignite can be separated into two types, the first is xyloid lignite or fossil wood and the second form is the compact lignite or perfect lignite. Although xyloid lignite may sometimes have the tenacity and the appearance of ordinary wood and it is reducible to a fine powder by trituration, and if submitted to the action of a weak solution of potash, it yields a considerable quantity of humic acid
6.
Saxony
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Its capital is Dresden, and its largest city is Leipzig. Saxony is the tenth largest of Germanys sixteen states, with an area of 18,413 square kilometres, located in the middle of a large, formerly all German-speaking part of Europe, the history of the state of Saxony spans more than a millennium. It has been a medieval duchy, an electorate of the Holy Roman Empire, a kingdom, the area of the modern state of Saxony should not be confused with Old Saxony, the area inhabited by Saxons. Old Saxony corresponds approximately to the modern German states of Lower Saxony, Saxony-Anhalt, Saxony is divided into 10 districts,1. After a reform in 2008, these regions - with some alterations of their respective areas - were called Direktionsbezirke, in 2012, the authorities of these regions were merged into one central authority, the Landesdirektion Sachsen. The Erzgebirgskreis district includes the Ore Mountains, and the Schweiz-Osterzgebirge district includes Saxon Switzerland, the largest cities in Saxony according to the 31 December 2015 estimate. To this can be added that Leipzig forms a metropolitan region with Halle. The latter city is located just across the border to Saxony-Anhalt, Leipzig shares for instance an S-train system and an airport with Halle. Saxony has, after Saxony Anhalt, the most vibrant economy of the states of the former East Germany and its economy grew by 1. 9% in 2010. Nonetheless, unemployment remains above the German average, the eastern part of Germany, excluding Berlin, qualifies as an Objective 1 development-region within the European Union, and is eligible to receive investment subsidies of up to 30% until 2013. FutureSAX, a business competition and entrepreneurial support organisation, has been in operation since 2002. Microchip makers near Dresden have given the region the nickname Silicon Saxony, the publishing and porcelain industries of the region are well known, although their contributions to the regional economy are no longer significant. Today the automobile industry, machinery production and services contribute to the development of the region. Saxony is also one of the most renowned tourist destinations in Germany - especially the cities of Leipzig and Dresden, new tourist destinations are developing, notably in the lake district of Lausitz. Saxony reported an unemployment of 8. 8% in 2014. By comparison the average in the former GDR was 9. 8% and 6. 7% for Germany overall, the unemployment rate reached 8. 2% in May 2015. The Leipzig area, which recently was among the regions with the highest unemployment rate, could benefit greatly from investments by Porsche. With the VW Phaeton factory in Dresden, and many part suppliers, zwickau is another major Volkswagen location
7.
Miocene
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The Miocene is the first geological epoch of the Neogene Period and extends from about 23.03 to 5.333 million years ago. The Miocene was named by Sir Charles Lyell and its name comes from the Greek words μείων and καινός and means less recent because it has 18% fewer modern sea invertebrates than the Pliocene. The Miocene follows the Oligocene Epoch and is followed by the Pliocene Epoch, the earth went from the Oligocene through the Miocene and into the Pliocene, with the climate slowly cooling towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event, the apes arose and diversified during the Miocene, becoming widespread in the Old World. By the end of this epoch, the ancestors of humans had split away from the ancestors of the chimpanzees to follow their own evolutionary path, as in the Oligocene before it, grasslands continued to expand and forests to dwindle in extent. In the Miocene seas, kelp forests made their first appearance, the plants and animals of the Miocene were fairly modern. The Miocene faunal stages from youngest to oldest are typically named according to the International Commission on Stratigraphy, Two subdivisions each form the lower, middle, continents continued to drift toward their present positions. Mountain building took place in western North America, Europe, both continental and marine Miocene deposits are common worldwide with marine outcrops common near modern shorelines. Well studied continental exposures occur in the North American Great Plains, India continued to collide with Asia, creating dramatic new mountain ranges. The Tethys Seaway continued to shrink and then disappeared as Africa collided with Eurasia in the Turkish–Arabian region between 19 and 12 Ma. The subsequent uplift of mountains in the western Mediterranean region and a fall in sea levels combined to cause a temporary drying up of the Mediterranean Sea near the end of the Miocene. The global trend was towards increasing aridity caused primarily by global cooling reducing the ability of the atmosphere to absorb moisture, climates remained moderately warm, although the slow global cooling that eventually led to the Pleistocene glaciations continued. Although a long-term cooling trend was well underway, there is evidence of a period during the Miocene when the global climate rivalled that of the Oligocene. The Miocene warming began 21 million years ago and continued until 14 million years ago, by 8 million years ago, temperatures dropped sharply once again, and the Antarctic ice sheet was already approaching its present-day size and thickness. Greenland may have begun to have large glaciers as early as 7 to 8 million years ago, life during the Miocene Epoch was mostly supported by the two newly formed biomes, kelp forests and grasslands. This allows for more grazers, such as horses, rhinoceroses, ninety five percent of modern plants existed by the end of this epoch. The higher organic content and water retention of the deeper and richer grassland soils, with long term burial of carbon in sediments, produced a carbon and this, combined with higher surface albedo and lower evapotranspiration of grassland, contributed to a cooler, drier climate. The expansion of grasslands and radiations among terrestrial herbivores correlates to fluctuations in CO2
8.
Resin
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In polymer chemistry and materials science, resin is a solid or highly viscous substance of plant or synthetic origin that is typically convertible into polymers. They are often mixtures of compounds, principally terpenes. Many plants, particularly woody plants, produce resin in response to injury, the resin acts as a bandage protecting the plant from invading insects and pathogens. Plants secrete resins and rosins for their protective benefits, the resin produced by most plants is composed mainly of terpenes and derivatives. Some resins also contain a proportion of resin acids. The individual components of resin can be separated by fractional distillation, rosins on the other hand are less volatile and consist, inter alia, of diterpenes. Amber is fossil resin from coniferous and other tree species, copal, kauri gum, dammar and other resins may also be found as subfossil deposits. Subfossil copal can be distinguished from genuine fossil amber because it becomes tacky when a drop of a solvent such as acetone or chloroform is placed on it, african copal and the kauri gum of New Zealand are also procured in a semi-fossil condition. Solidified resin from which the volatile terpene components have been removed by distillation is known as rosin, typical rosin is a transparent or translucent mass, with a vitreous fracture and a faintly yellow or brown colour, non-odorous or having only a slight turpentine odor and taste. Rosin is insoluble in water, mostly soluble in alcohol, essential oils, ether and hot fatty oils, and softens and melts under the influence of heat, rosin consists of a complex mixture of different substances including organic acids named the resin acids. These are closely related to the terpenes, and derive from them through partial oxidation, Resin acids can be dissolved in alkalis to form resin soaps, from which the purified resin acids are regenerated by treatment with acids. Examples of resin acids are abietic acid, C20H30O2, plicatic acid contained in cedar, and pimaric acid, C20H30O2, a constituent of galipot resin. Abietic acid can also be extracted from rosin by means of hot alcohol, it crystallizes in leaflets, pimaric acid closely resembles abietic acid into which it passes when distilled in a vacuum, it has been supposed to consist of three isomers. Rosin is obtained from pines and some plants, mostly conifers. Propolis, consisting largely of resins collected from such as poplars and conifers, is used by honey bees to seal gaps in their hives. Shellac and lacquer are examples of insect-derived resins, asphaltite and Utah resin are petroleum bitumens, not a product secreted by plants, although it was ultimately derived from plants. These were highly prized substances, and required as incense in religious rites. The word resin has been applied in the world to nearly any component of a liquid that will set into a hard lacquer or enamel-like finish
. PMID 19570786.
