From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #4864 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Sunday, August 30 2020 Volume 14 : Number 4864 Today's Subjects: ----------------- Green Veggie Causes Diabetes Type 2 in Millions ["Beat Blood Sugar" ] #1 Greatest Danger in the American Diet ["**Keto Bread**" Subject: Green Veggie Causes Diabetes Type 2 in Millions Green Veggie Causes Diabetes Type 2 in Millions http://eyesighton.buzz/_9ZnBy9IEvaDmzvTaGBpgNv9EdmoGrbg7HlBaTA_zZaL7vEP http://eyesighton.buzz/3_Xkgjzf8yRvf-ZYteO7fwEOSacRd8_OvDpFjdzOoky6iAbN Serbian population to help the authorities in every way in their struggle against the communist rebels, and called for loyalty to the Germans, condemning the Partisan-led resistance as unpatriotic. The Serbian Bar Association unanimously supported the Appeal, but some notable personalities, such as the writers Isidora Sekuli? and Ivo Andri? and university professor MiloE! N. ?uri?, refused to sign. The A?imovi? administration also appealed for rebels to return to their homes and announced bounties for the killing of rebels and their leaders. In addition, A?imovi? gave orders that the wives of communists and their sons older than 16 years of age be arrested and held, and the Germans burned their houses and imposed curfews. Replacement The German occupation authorities considered A?imovi? and his administration incompetent due to their failure to suppress the uprising, and had been considering sacking A?imovi? since mid-July. To strengthen the puppet government, Danckelmann wanted to find a Serb who was both well-known and highly regarded by the population who could raise some sort of Serbian armed force and who would be willing to use it ruthlessly against the rebels whilst remaining under full German control. In response to a request from Benzler, the Foreign Office sent SS-StandartenfC Subject: Everyone at some point has suffered pain in their neck Everyone at some point has suffered pain in their neck http://relaxical.buzz/g9fl8vMFTCHug67tshBC2YcCH1eAMPMdb2QETzwXCW5B6ap_ http://relaxical.buzz/c_yyDzoMNf5_jjxOpGVDhYJEMnnwlidXHC2Q7zV0LSpngknx Clark's reports about the finds rekindled interest in the bird. Sir Richard Owen and Alfred Newton both wanted to be first to describe the post-cranial anatomy of the dodo, and Owen bought a shipment of dodo bones originally meant for Newton, which led to rivalry between the two. Owen described the bones in Memoir on the Dodo in October 1866, but erroneously based his reconstruction on the Edwards's Dodo painting by Savery, making it too squat and obese. In 1869 he received more bones and corrected its stance, making it more upright. Newton moved his focus to the RC)union solitaire instead. The remaining bones not sold to Owen or Newton were auctioned off or donated to museums. In 1889, ThC)odor Sauzier was commissioned to explore the "historical souvenirs" of Mauritius and find more dodo remains in the Mare aux Songes. He was successful, and also found remains of other extinct species. Skeleton assembled from subfossils found in 2006, Naturalis In 2005, after a hundred years of neglect, a part of the Mare aux Songes swamp was excavated by an international team of researchers (International Dodo Research Project). To prevent malaria, the British had covered the swamp with hard core during their rule over Mauritius, which had to be removed. Many remains were found, including bones of at least 17 dodos in various stages of maturity (though no juveniles), and several bones obviously from the skeleton of one individual bird, which have been preserved in their natural position. These findings were made public in December 2005 in the Naturalis museum in Leiden. 63% of the fossils found in the swamp belonged to turtles of the extinct genus Cylindraspis, and 7.1% belonged to dodos, which had been deposited within several centuries, 4,000 years ago. Subsequent excavations suggested that dodos and other animals became mired in the Mare aux Songes while trying to reach water during a long period of severe drought about 4,200 years ago. Furthermore, cyanobacteria thrived in the conditions created by the excrements of animals gathered around the swamp, which died of intoxication, dehydration, trampling, and miring. Though many small skeletal elements were found during the recent excavations of the swamp, few were found during the 19th century, probably owing to the employment of less refined methods when collecting. Subfossil bones rediscovered in the Grant Museum in 2011 Louis Etienne Thirioux, an amateur naturalist at Port Louis, also found many dodo remains around 1900 from several locations. They included the first articulated specimen, which is the first subfossil dodo skeleton found outside the Mare aux Songes, and the only remains of a juvenile specimen, a now lost tarsometatarsus. The former specimen was found in 1904 in a cave near Le Pouce mountain, and is the only known complete skeleton of an individual dodo. Thirioux donated the specimen to the Museum Desjardins (now Natural History Museum at Mauritius Institute). Thrioux's heirs sold a second mounted composite skeleton (composed of at least two skeletons, with a mainly reconstructed skull) to the Durban Museum of Natural Science in South Africa in 1918. Together, these two skeletons represent the most completely known dodo remains, including bone elements previously unrecorded (such as knee-caps and various wing bones). Though some contemporary writers noted the importance of Thrioux's specimens, they were not scientifically studied, and were largely forgotten until 2011, when sought out by a group of researchers. The mounted skeletons were laser scanned, from which 3-D models were reconstructed, which became the basis of a 2016 monograph about the osteology of the dodo. In 2006, explorers discovered a complete skeleton of a dodo in a lava cave in Mauritius. This was only the second associated skeleton of an individual specimen ever found, and the only one in recent times ------------------------------ Date: Sat, 29 Aug 2020 08:53:30 -0400 From: "Archives of Neurology" Subject: Best Fruit Before Bed Best Fruit Before Bed http://perperon.today/70MOOdMRwEhO2j-BFmFEZJzPBhM5oar9rx6P3Lj2wvQhykzS http://perperon.today/ZQt1HQOOqUaDgdowHzG7Eqrx7ewIaqukO6Kzai1bIvtlER7g These classifications overlap with the geological definitions of "upland" and "lowland". In geology an "upland" is generally considered to be land that is at a higher elevation than the alluvial plain or stream terrace, which are considered to be "lowlands". The term "bottomland" refers to low-lying alluvial land near a river. Many freshwater fish and invertebrate communities around the world show a pattern of specialisation into upland or lowland river habitats. Classifying rivers and streams as upland or lowland is important in freshwater ecology as the two types of river habitat are very different, and usually support very different populations of fish and invertebrate species. Upland In freshwater ecology, upland rivers and streams are the fast-flowing rivers and streams that drain elevated or mountainous country, often onto broad alluvial plains (where they become lowland rivers). However, altitude is not the sole determinant of whether a river is upland or lowland. Arguably the most important determinants are those of stream power and stream gradient. Rivers with a course that drops rapidly in altitude will have faster water flow and higher stream power or "force of water". This in turn produces the other characteristics of an upland riverban incised course, a river bed dominated by bedrock and coarse sediments, a riffle and pool structure and cooler water temperatures. Rivers with a course that drops in altitude very slowly will have slower water flow and lower force. This in turn produces the other characteristics of a lowland riverba meandering course lacking rapids, a river bed dominated by fine sediments and higher water temperatures. Lowland rivers tend to carry more suspended sediment and organic matter as well, but some lowland rivers have periods of high water clarity in seasonal low-flow periods. The generally clear, cool, fast-flowing waters and bedrock and coarse sediment beds of upland rivers encourage fish species with limited temperature tolerances, high oxygen needs, strong swimming ability and specialised reproductive strategies to prevent eggs or larvae being swept away. These characteristics also encourage invertebrate species with limited temperature tolerances, high oxygen needs and ecologies revolving around coarse sediments and interstices or "gaps" between those coarse sediments, Lowland Amazon River near Manaus, Brazil, an example of a lowland river habitat. The generally more turbid, warm, slow-flowing waters and fine sediment beds of lowland rivers encourage fish species with broad temperature tolerances and greater tolerances to low oxygen levels, and life history and breeding strategies adapted to these and other traits of lowland rivers. These characteristics also encourage invertebrate species with broad temperature tolerances and greater tolerances to low oxygen levels and ecologies revolving around fine sediments or alternative habitats ------------------------------ Date: Sat, 29 Aug 2020 06:37:32 -0400 From: "**Keto Bread**" Subject: #1 Greatest Danger in the American Diet #1 Greatest Danger in the American Diet http://routiine.today/X1mbpGx5uSnQcL8V6VUWA-noMknTMBB4Tzfc2P1xmwBpueHn http://routiine.today/XjVkSIgu3x7XvQGJAun-0xx24VsroR_959e_Ayh2VkkG5HDf Soil depletion occurs when the components which contribute to fertility are removed and not replaced, and the conditions which support soil's fertility are not maintained. This leads to poor crop yields. In agriculture, depletion can be due to excessively intense cultivation and inadequate soil management. Soil fertility can be severely challenged when land-use changes rapidly. For example, in Colonial New England, colonists made a number of decisions that depleted the soils, including: allowing herd animals to wander freely, not replenishing soils with manure, and a sequence of events that led to erosion. William Cronon wrote that "...the long-term effect was to put those soils in jeopardy. The removal of the forest, the increase in destructive floods, the soil compaction and close-cropping wrought by grazing animals, ploughing--all served to increase erosion." One of the most widespread occurrences of soil depletion as of 2008 is in tropical zones where nutrient content of soils is low. The combined effects of growing population densities, large-scale industrial logging, slash-and-burn agriculture and ranching, and other factors, have in some places depleted soils through rapid and almost total nutrient removal. The depletion of soil has affected the state of plant life and crops in agriculture in many countries. In the middle east for example, many countries find it difficult to grow produce because of droughts, lack of soil, and lack of irrigation. The Middle East has three countries that indicate a decline in crop production, the highest rates of productivity decline are found in hilly and dryland areas. Many countries in Africa also undergo a depletion of fertile soil. In regions of dry climate like Sudan and the countries that make up the Sahara Desert, droughts and soil degradation is common. Cash crops such as teas, maize, and beans require a variety of nutrients in order to grow healthy. Soil fertility has declined in the farming regions of Africa and the use of artificial and natural fertilizers has been used to regain the nutrients of ground soil. Topsoil depletion occurs when the nutrient-rich organic topsoil, which takes hundreds to thousands of years to build up under natural conditions, is eroded or depleted of its original organic material. Historically, many past civilizations' collapses can be attributed to the depletion of the topsoil. Since the beginning of agricultural production in the Great Plains of North America in the 1880s, about one-half of its topsoil has disappeared. Depletion may occur through a variety of other effects, including overtillage (which damages soil structure), underuse of nutrient inputs which leads to mining of the soil nutrient bank, and salinization of soil. Irrigation water effects The quality of irrigation water is very important to maintain soil fertility and tilth, and for using more soil depth by the plants. When soil is irrigated with high alkaline water, unwanted sodium salts build up in the soil which would make soil draining capacity very poor. So plant roots can not penetrate deep into the soil for optimum growth in Alkali soils. When soil is irrigated with low pH / acidic water, the useful salts ( Ca, Mg, K, P, S, etc.) are removed by draining water from the acidic soil and in addition unwanted aluminium and manganese salts to the plants are dissolved from the soil impeding plant growth. When soil is irrigated with high salinity water or sufficient water is not draining out from the irrigated soil, the soil would convert into saline soil or lose its fertility. Saline water enhance the turgor pressure or osmotic pressure requirement which impedes the off take of water and nutrients by the plant roots. Top soil loss takes place in alkali soils due to erosion by rain water surface flows or drainage as they form colloids (fine mud) in contact with water. Plants absorb water-soluble inorganic salts only from the soil for their growth. Soil as such does not lose fertility just by growing crops but it lose its fertility due to accumulation of unwanted and depletion of wanted inorganic salts from the soil by improper irrigation and acid rain water (quantity and quality of water). The fertility of many soils which are not suitable for plant growth can be enhanced many times gradually by providing adequate irrigation water of suitable quality and good drainage from the soil. ------------------------------ Date: Sat, 29 Aug 2020 10:54:08 -0400 From: "hdl cholesterol low" Subject: Foods to avoid with high cholesterol and triglycerides Foods to avoid with high cholesterol and triglycerides http://perperon.today/gG4qHU_9izSJVlGzoE7fzPbxUTnshq6-SXsK1_XzlVfUnMWN http://perperon.today/AHOlFPwvTQ7gsesQUxPVN_V35K57mOdVgLTTZ02HoeTjquwd The types of depositional plains include: Abyssal plains, flat or very gently sloping areas of the deep ocean basin. Planitia, the Latin word for plain, is used in the naming of plains on extraterrestrial objects (planets and moons), such as Hellas Planitia on Mars or Sedna Planitia on Venus. Alluvial plains, which are formed by rivers and which may be one of these overlapping types: Alluvial plains, formed over a long period of time by a river depositing sediment on their flood plains or beds, which become alluvial soil. The difference between a flood plain and an alluvial plain is: a flood plain represents areas experiencing flooding fairly regularly in the present or recently, whereas an alluvial plain includes areas where a flood plain is now and used to be, or areas which only experience flooding a few times a century. Flood plain, adjacent to a lake, river, stream, or wetland that experiences occasional or periodic flooding. Scroll plain, a plain through which a river meanders with a very low gradient. Glacial plains, formed by the movement of glaciers under the force of gravity: Outwash plain (also known as sandur; plural sandar), a glacial out-wash plain formed of sediments deposited by melt-water at the terminus of a glacier. Sandar consist mainly of stratified (layered and sorted) gravel and sand. Till plains, plain of glacial till that form when a sheet of ice becomes detached from the main body of a glacier and melts in place depositing the sediments it carries. Till plains are composed of unsorted material (till) of all sizes. Lacustrine plains, plains that originally formed in a lacustrine environment, that is, as the bed of a lake. Lava plains, formed by sheets of flowing lava. Erosional plains Erosional plains have been leveled by various agents of denudation such as running water, rivers, wind and glacier which wear out the rugged surface and smoothens them. Plain resulting from the action of these agents of denudation are called peneplains (almost plain) while plains formed from wind action are called pediplains. Structural plains Structural plains are relatively undisturbed horizontal surfaces of the Earth. They are structurally depressed areas of the world that make up some of the most extensive natural lowlands on the Earth's ------------------------------ End of alt.music.moxy-fruvous digest V14 #4864 **********************************************